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1 MOBILITY OF HEAVY METALS FROM THE UNIVERSITY OF NIGERIA SEWAGE- SLUDGE DISPOSAL SITE TO THE SURROUNDING SOILS AND PLANTS BY EZEUDO VICTOR C. REG NO: PG/M.Sc/10/52369 B. AGRIC. TECH. (FUTO) A DISSERTATION SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE AWARD OF THE DEGREE OF MASTER OF SCIENCE (M.Sc) IN SOIL SCIENCE (SOIL CHEMISTRY AND MINERALOGY) DEPARTMENT OF SOIL SCIENCE UNIVERSITY OF NIGERIA, NSUKKA FEBRUARY, 2014

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Page 1: MOBILITY OF HEAVY METALS FROM THE UNIVERSITY … · Our Lady of Perpetual Help College Orba whose assistance has made this work success. Finally,

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MOBILITY OF HEAVY METALS FROM THE UNIVERSITY OF NIGERIA SEWAGE-

SLUDGE DISPOSAL SITE TO THE SURROUNDING SOILS AND PLANTS

BY

EZEUDO VICTOR C.

REG NO: PG/M.Sc/10/52369

B. AGRIC. TECH. (FUTO)

A DISSERTATION SUBMITTED IN PARTIAL FULFILMENT OF THE

REQUIREMENTS FOR THE AWARD OF THE DEGREE OF MASTER OF SCIENCE

(M.Sc) IN SOIL SCIENCE (SOIL CHEMISTRY AND MINERALOGY)

DEPARTMENT OF SOIL SCIENCE

UNIVERSITY OF NIGERIA, NSUKKA

FEBRUARY, 2014

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CERTIFICATION

EZEUDO, VICTOR C. a postgraduate student of the department of soil science, with the

registration number PG/M.Sc/10/52369, has satisfactorily completed the research work for the

Award of the Master of Science Degree in Soil Science. The work embodied in this dissertation is

original and has not been submitted in part or full for any other diploma or degree of this or any

other institution.

---------------------------------- -------------------------------

PROF. C.L.A. ASADU Dr. P.I EZEAKU

Supervisor Head of Department

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DEDICATION

This work is dedicated to Our Lady of Perpetual Help

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ACKNOWLEDGEMENT

I am highly grateful to God Almighty and to Our Lady of Perpetual Help whose out of

their assistance and protection has made this work a success. I appreciate the support, assistance,

encouragement and the guidance of my supervisor, Prof. C.L.A. Asadu.

I will ever remain grateful and indebted to all the lecturers as well as the administrative

and the laboratory staff of the Department of Soil Science, University of Nigeria, Nsukka. I

acknowledge the assistance of Dr Obalum, Rev Fr. Dr. David Omego and the entire community of

Our Lady of Perpetual Help College Orba whose assistance has made this work success.

Finally, I hereby express my profound gratitude to every member of my extended family

more especially, Mr & Mrs Chris Ezido (KSM), Oluchi, Chinwendu, Ozioma, Ogochukwu,

Ugwumsinachi and my friend Oluchi who had suffered much to ensure that this work comes to a

successful end. May the good Lord reward you abundantly.

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TABLE OF CONTENTS

Content Page

Title page- - - - - - - - - - - i

Certification- - - - - - - - - - - ii

Dedication- - - - - - - - - - - iii

Acknowledgement- - - - - - - - - - iv

Table of Contents- - - - - - - - - - v

List of Tables- - - - - - - - - - viii

List of Plates - - - - - - - - - - ix

Abstract- - - - - - - - - - - x

CHAPTER ONE

INTRODUCTION- - - - - - - - - - 1

CHAPTER TWO

LITERATURE REVIEW- - - - - - - - - 5

2.1 Sewage Sludge - - - - - - - - - 5

2.2 Heavy Metal Toxicity and its Mobility - - - - - - 7

2.3 Effect of pH and Organic Matter in Heavy Metal Mobility - - - 9

2.4 Effect of Sewage Sludge Application in Soil - - - - - 10

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2.5 Sludge-Soil Interaction - - - - - - - - 20

2.6 Implications of Trace Metal in Soil and Plant - - - - - 23

2.7 Plant Factors Influencing Metal Uptake - - - - - - 25

CHAPTER THREE

MATERIALS AND METHODS - - - - - - - 30

3.1 Site description - - - - - - - - - 30

3.2 The Sewage System - - - - - - - - 30

3.3 Field Sampling - - - - - - - - - 35

3.4. Routine Analysis - - - - - - - - - 35

3.5 Determination of the soil content of heavy metals (Pb, Cu, Cd and Hg) - - 36

3.5 Sample Preparations and Digestion of crop plant for Heavy Metal Determination 36

3.6 Data analysis - - - - - - - - - - 37

CHAPTER FOUR

RESULTS- - - - - - - - - - - 38

4.1 Sewage sludge - - - - - - - - - - 38

4.2 Physicochemical properties at various distances away from sewage site - 40

4.3 Physicochemical Properties at Various Soil Depths - - - - 42

4.4 The Simple matrix Distance and Depth on Soil Physicochemical Properties- - 44

4.4.1 Soil pH as influenced by sewage disposal - - - - - 44

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4.4.2 The Organic Matter Concentration and Nitrogen Content of the Soil - - 44

4.4.3 Soil Exchangeable Bases - - - - - - - 44

4.4.4 Total Exchangeable Acidity (TEA) - - - - - - 45

4.4.5 Available phosphorus - - - - - - - - 45

4.5 Heavy Metals in Soil - - - - - - - - - 49

4.5.1 Effect of distance on heavy metal contents of the soil- - - - 49

4.5.2 The Main Effects of Depth on Selected Heavy Metal Content of the Soil - 51

4.5.3 The Simple matrix of Distance and Depth on the Concentration of the Selected

Heavy Metal in Soils - - - - - - - - - 53

4.6 Heavy Metal concentration in Plant - - - - - - 55

4.6.1 Cadmium - - - - - - - - - - 55

4.6.2 Copper - - - - - - - - - - 55

4.6.3 Mercury- - - - - - - - - - 56

4.6.4 Lead- - - - - - - - - - - 56

4.7 The Bioconcentration Factor (BCF) of Cassava - - - - - - 58

4. 8 The Bioconcentration Factor (BCF) of Maize - - - - - 60

4.9 The Bioconcentration Factor (BCF) of Pannicum maximum` - - - 62

CHAPTER FIVE

DISCUSSION- - - - - - - - - - 65

5.1 Physicochemical Properties of the Soil - - - - - `65

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5.2 Heavy metals in soil - - - - - - - - 70

5.3 Heavy Metal in Plant - - - - - - - - 73

5.4 The bioconcentration factor (BCF) - - - - - - 75

CHAPTER SIX

SUMMARY AND CONCLUSION - - - - - - - 76

REFERENCES- - - - - - - - - - 79

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LIST OF TABLES

Tables Pages

1. Mean Values of Some Chemical Properties and Heavy Metal Contents of the Sewage

Sludge - - - - - - - - - - 39

2. Effects of Distances from the Sewage Site on Soil Physicochemical Properties. 41

3. Effects of Depth from the Sewage Site on Soil Physicochemical Properties. 43

4a. The Mean Simple Matrix of Distance and Depth on the Soil Physicochemical Properties 47

4b. The Mean Simple Matrix of Distance and Depth on the Soil Physicochemical Propertie

(contd) - - - - - - 48

5. Effects of Distance on Soil Heavy Metals Distributions - - - 50

6. Effects of Depth on Soil Heavy Metals Distribution - - - 52

7. The Mean Simple Matrix Of Distance And Depth On The Soil Heavy Metal Content 55

8. The Main Effects of Distance, Plant and Plant parts on heavy metal accumulation- 57

9. Bioconcentration Factor (BCF) in root and leaf of cassava - - - 59

10. Bioconcentration Factor (BCF) in root and leaf of Maize - - - 61

11. Bioconcentration factor (BCF) in root and leaf of Pannicum Maximum - 63

12. Guideline for safe limits of heavy metals in soil and plant - - - 64

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LIST OF PLATES

Plates Pages

1. The sewage system - - - - - - - - 31

2. The settling chamber - - - - - - - - 32

3. The oxidation pond - - - - - - - - 33

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ABSTRACT

This study was carried out at the University of Nigeria, Nsukka sewage disposable site. The study

was to quantify the mineral contents of sewage sludge and assess their mobility in the soil and

plants around UNN disposal site. The experimental layout was a 4x3 factorial in RCBD in which

distance from the sewage disposal site and soil depth were the two factors under consideration.

The distances from sewage pond were 0 (edge), 100, 300 and 2000 m away from the sewage pond

with 2000 m serving as control while soil depths were 0 – 40, 40 – 80, and 80 – 20cm. Soil and

plant sampling was carried out from three distances in both sewage site and at the control site.

Physico-chemical properties of the soil were determined. Four heavy metals (Cd, Cu, Hg and Pb)

were determined from the soil, plant samples as well as the sewage sludge. Results showed that

the effects of distance and soil depth were significant (P < 0.05) on pH, exchangeable bases,

cation exchange capacity, organic matter, total nitrogen, exchangeable acidity and available

phosphorous. At the control site there were no differences among soil properties except organic

matter that decreased significantly (P < 0.05) with increase in depth. All the chemical properties

determined decreased with increase in depth, except exchangeable acidity which increased with

increase in depth. Cadmium, Cu, Hg, and Pb, significantly (P < 0.05) decreased as both distance

and depth increased. There was an obvious high heavy metal content in the soil of disposal site

when compared with the control soil. In the tissues of the three plants (Manihot spp, Zea mays,

Pannicum maximum) studied, Cd, Cu, Hg, Pb concentrations were significantly different (P <

0.05) at 0, 100, 300 and 2000 m distances. Heavy metal content observed in plant tissues at the

disposal site was relatively high when compared to that of the control site. Therefore, it follows

that the studies at the University of Nigeria Nsukka sewage disposal site results in an increased

concentration of soil property, such as organic matter, macro and micro nutrients. The mobility of

heavy metals (Cd, Cu, Hg, and Pb) from soil to leaves suggest that all these metals were mobile

from soil to plant components. Heavy metal concentrations varied among the tested crop plant,

which reflects their differences in their uptake capabilities and their further translocation to the

shoot portion of the plant. The bioconcentration factor at both root and leaf tissues of crop plant

did not show any abnormal accumulation of heavy metals at sewage site. From the study the

heavy metal contents of the sludge, soil and plant species were below toxicity levels when

compared to WHO/FAO standards.

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CHAPTER ONE

1.0 INTRODUCTION

Sewage sludge is a solid, semisolid, or liquid muddy looking residue that results after human and

other waste from households, industries and run-off from road is treated at a sewage plant.

Quantitative and qualitative composition of the sewage sludge is very complicated. It is rich in

organic matter, nitrogen, phosphorus, calcium, magnesium, sulphur and other microelements

necessary for the survival of plants and soil fauna. Of the microelement commonly found in

sewage sludge heavy metals such as, cadmium, lead, mercury and arsenic are toxic to humans

whereas zinc, copper, and nickel are harmful to plants (Jane-Hope, 1986). There release to soil

liquid phase may cause leaching through the soil profile to the ground water table, and also

facilitate plant uptake of heavy metals thus posing a risk to environment.

Heavy metals have a density greater than 5.0 g cm-3

(Seaward and Richardson, 1990) and metal

transfer from sewage sludge to soil and subsequently to groundwater and plants represents

potential health and environmental risks (McBride et al., 1997; Bhogal et al., 2003). The greater

the mobility the higher the toxicity risk of these metals. Heavy metal mobility mainly depends on

soil properties (Rowell, 1994).

One important process affecting heavy metal mobility in soil is sorption. The importance of pH in

metal solubility is well-known as it influences heavy metal adsorption, retention and movement

(Sauve et al., 1997).Organic matter is another important soil component that influences metal

mobility. It has a nutritional function by serving as a source of N, P and S, and has a high binding

capacity for cations and organic contaminants (Oste et al., 2002). It has been shown that heavy

metals are accumulated in surface organic layers in agricultural and urban soils. It therefore

appears that soil properties such as sorptivity, organic matter and soil pH may have a major effect

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on metal mobility. The addition of organic matter may also affect metal mobility, by increasing

soluble organic matter and Cu mobility may be enhanced, especially in sandy soils of high pH

(Udom et al., 2000, McBride et al., 1999).

There are several indices of heavy metal mobility in soils, the retardation factor, Rd, being a

straight forward, unitless one (Kookana et al., 1994). The meaning of Rd is that it is the ratio of

the rate of movement of the heavy metal to the rate of movement of water in which the metal is

dissolved.

The fate of heavy metals in sewage sludge is mainly related to their mobility in soil. A

traditionally held view on the mobility of heavy metals in sewage sludge-amended soils is that the

metals’ migration is insignificant and that the metals tend to remain in the site of input, i.e. in the

topsoil (Chang et al., 1984; Schirado et al., 1986). Heavy metals are dangerous because they are

non-biodegradable, bioavailable and toxic to different crops (Mahler, 2003; Garcia and

Dorronsoro, 2005).

Distribution of heavy metals in plant body depends upon availability and concentration of the

heavy metal as well as upon the particular plant species and its population ( Punz and Seighardt,

1973). Plants have a natural ability to extract elements from the soil and to distribute them

between roots and shoot depending on the biological processes in which the element is involved

(Ximénez-Embun et al., 2002). In addition to the uptake of nutrients, toxic compounds such as

heavy metal can also be taken up by the plants. The plants store high levels of toxic heavy metals

within their roots, shoots, and leaves. The growth and metabolism of many plant species were

reported to be affected adversely by excess supply of heavy metals (Foy et al, 1978, Wong and

Lau 1985).

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Potentially toxic metal concentrations are not the same in all portions of the plant. A survey of a

number of food crops revealed that the tuber, seed, or fruit tissue had a lower amount of Cd than

plant leaf tissue. Comparisons between crop species show wide variations in their ability to absorb

potentially toxic trace elements from the sludge-soil system. Cereals and legumes accumulated

less Cd in shoots than leafy vegetables, like curly cress (LepidiumsativamL.), lettuce (Lactuca

sativa L.), and spinach (Spinaciaoleracea L.) (Bingham et al., 1975). An earlier study in the site

of present study showed that the build-up of heavy metals to critical level could be phyto-toxic

and might result in reduced plant growth (Udom, 2000, and Asadu et al, 2008). There is a concern

that heavy metals in the composted product may transfer from soil and accumulate in edible

plants. Some of these heavy metals can be detrimental to human, plant or animal life if they are

present above certain limits.

At the University of Nigeria Nsukka (UNN) the sewage sludge discharged from the administrative

blocks, hostels and surrounding staff quarters are continuously disposed at the sewage sludge site.

Heavy metal content of the sewage sludge is likely to be high due to the usage of cosmetics,

detergents, fats, oils, chemicals and cigarette ends flushed down the toilets. There are vegetation

and farmlands with different kinds of crops surrounding the sewage disposal site. Heavy metals in

sewage sludge and the toxicological implications are of concern in agricultural production due to

the adverse effects on food quality (safety and marketability) and crop growth (phytotoxicity).

Metals such as lead, mercury, cadmium and copper are cumulative poisons. These metals cause

environmental hazards and are exceptionally toxic. Crops and vegetations around take up metals

by absorbing them from contaminated soils, animal graze upon this vegetation and this heavy

metal enter into the food chain. This exposes the consumers of these crops and animals to

bioaccumulation of heavy metals with time. It has been reported that nearly half of the mean

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ingestion of lead, cadmium and mercury through food is due to plant origin (Mohsen and Mohsen

2008).

Therefore, the major objective of this work was to assess the mobility of some heavy metals from

sewage sludge in soils and plants around UNN disposal site. The specific objectives were to:

1 determine the chemical composition of sewage sludge;

2 determine the chemical compositions of the soils around the pond;

3 quantify the accumulation of the heavy metals laterally away from the pond to the soil

around; and

4 determine the accumulation of heavy minerals in the roots, and leafs systems of selected

crops/plants so as to compare with safety standards.

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CHAPTER 2

LITERATURE REVIEW

2.1 Sewage Sludge

Sewage sludge is a solid, semisolid, or liquid muddy looking residue that results after human and

other waste from households, industries and run-off from road is treated at a sewage plant.

The composition of sewage sludge varies from one treatment to another, depending on the extent of

treatment and on the differences in the original sewage make-up. Domestic and municipal waste

water and sewage are treated so that the final products of sludge and effluents may be disposed of

with minimum adverse effect on the soil and environment.

Sewage sludge contains an abundance of trace elements necessary for plant growth (boron, copper,

iron, manganese, molybdenum, and zinc) as well as others considered to be nonessential (e.g.,

cadmium, chromium, mercury, lead). The trace elements in sludge are sometimes called the heavy

metals, because most of them (boron being the major exception) have a density greater than 5.0

(Page, 1974). Industrialized sludges, of course, can contain high concentrations of trace elements.

Source control with limits on discharges of toxic trace elements is practiced by cities that use their

sludge for agricultural purposes. But even the tightest source control is unlikely to reduce the trace-

element content much below the median value (Dean and Smith, 1973). This is because household

products contain trace elements. The trace elements likely to cause toxicities to plants in soils

treated with large amounts (for example, 400 t ha–1

) of domestic sludge for a number of years (15

yr) are cadmium, copper, zinc, boron, and possibly nickel (Page, 1974). In industrialized sludges, in

addition to the elements listed, concentrations of arsenic, barium, cobalt, chromium, manganese,

lead, and vanadium may be sufficiently high to reduce crop yields when applied in large amounts.

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Plants can grow normally and yet contain concentrations of selenium, cadmium, molybdenum, and

possibly lead that are toxic to man and animals.

Cadmium is the element of most concern in sludge, because it poses the greatest threat to human

health (Sommers and Barbarick, 1986). Food obtained from plants grown on sludge treated soil

might contain concentrations of cadmium toxic to man and animals. Cadmium is used in

electroplating, pigments, chemicals, batteries, alloys, photographic supplies, fungicides, as well as

other products. Even though industrial sources of cadmium in sludge can be controlled, domestic

sources cannot. For example, cigarette ends flushed down toilets raises the cadmium concentration

in sludge, because tobacco has a high concentration of cadmium (Juste and Mench, 1992). Long-

term studies suggest that cadmium is a problem in sludge-treated soils (Juste and Mench, 1992).

Nine years after a one-time sludge addition to a fine sandy loam, Bell et al. (1991) found that the

cadmium was more extractable (up to 60%) than zinc, manganese, and iron (less than 4%), which

indicated a greater potential mobility for cadmium than for the other metals.

Dowdy et al., (1991) reported that after 14 years of large additions of sludge (765 t ha–1

total

added), sludge-born cadmium moved out of the tillage zone into the subsoil. At the 83–100 cm

depth, the concentration of extractable cadmium in the soil was 2.5 times higher in the sludge

treated plots than in control plots. Kirkham (1975) showed that, at the 30–61 cm depth, a silt-loam

soil spread with moderate amounts of sludge (28 t ha–1

yr–1

) for 35 years had 46 times more total

cadmium than a control soil, and leaves of corn plants growing on that soil had concentrations of

cadmium higher than normal.

In addition, synergistic and antagonistic interactions occur between elements in sludge and soil that

affect the absorption of elements by plant roots. For example, high phosphorus levels in soil often

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inhibit uptake of trace elements. Therefore, it is possible to decrease uptake of one element by

supplying another element to the soil. After application to soil, trace elements tend to remain in the

plow layer with the sludge residue, although cadmium appears to be an exception. Trace elements

are often associated with the organic-rich sludge fractions Oxides of iron and manganese absorb

trace elements and limit their movement (Bell et al., 1991).

Citric acid, present in sewage sludge (e.g., from washing fluids), forms complexes with metals,

which may play a part in migration of metals away from disposal sites (Francis et al., 1992).

Chelating agents such as organic acids produced in the rhizosphere by root exudation or by

microbial activity also affect the mobility of heavy metals in soils and their transfer to plants. In

addition, microbes can absorb heavy metals and prevent their transfer to plants (Munier-Lamy et al.,

1991). However, microbes are short-lived, and when they die the metals will again be available for

uptake by plants.

2.2 Heavy Metal Toxicity and its Mobility

The sludge contains heavy metals which have potential ecological, biological and health impact.

The heavy metal contents of sludge from various countries has been reported Berrow and Webber,

1972; Fergusson, 1990). Heavy metals like As, Cd, Co, Cu, Ni, Zn, and Cr is phytotoxic either at

all concentrations or above certain threshold levels. Toxic metals are biologically magnified through

the food chain. They infect the environment by affecting soil properties, its fertility, biomass and

crop yields and ultimately human health.

Depending on the origin and composition, however, sludge may contain substantial amounts of

toxic metals as well as beneficial nutrients (Wong et al., 2007). However, the mentioned application

can pose a threat to environment and the major concern arises from the fact that sewage sludge,

especially those from the heavily urbanized and industrialized areas, contains a relatively high

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concentration of heavy metals (Selivanovskaya and Latypova, 2003; Singh et al., 2004). However,

sludge’s often contain appreciable amounts of metals, e.g. Zn, Cu, Ni, Cd and Pb (Chander and

Brookest, 1991). Metal transfer from sewage sludges to soil and subsequently to groundwater and

plants represents potential health and environmental risks (McBride et al., 1997; Bhogal et al., 2003

Heavy metal ions may have toxic effects on plants, animals or humans, and their toxicity is linked

to their mobility in soil. The greater the mobility the higher the toxicity risk of these metals. Heavy

metal mobility mainly depends on soil properties (Rowell 1994). One important process affecting

heavy metal mobility in soil is sorption. Sorption is the phenomenon in which metal ions, which

typically bear a positive charge, are attracted to solid particles in the soil such as clay and organic

matter, which mostly bear a net negative charge.

This binding is often reversible, and metals bound onto the solids are in equilibrium with metals in

the soil water. This means that strongly retained metal ions are removed from the soil water and

become less mobile than weakly retained ions. It has long been thought that heavy soils, that is, high

clay content soils, tend to bind and immobilize heavy metals, so that many industries feel safe when

disposing of their wastes in clayey soils (Sharma and Lewis 1994). Yet, this simplification is not

always true, since the transport of contaminants even in clayey soils can be significant and needs to

be addressed and quantified.

There are several indices of heavy metal mobility in soils, the retardation factor, (Rd) being a

straightforward, unitless one (Kookana et al. 1994). The natural meaning of Rd is that it is the ratio

of the rate of movement of the heavy metal to the rate of movement of water in which the metal is

dissolved. To give a rather simplistic example, if Ni is dissolved in water, and the water moves 100

m in the soil, but Ni moves 5 m, then Ni Rd is 20 (20=100/5). It is easy to see that the greater the

metal Rd, the higher the metal retention by the soil, and, thus, the lower the metal mobility.

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The distribution and bioavailability of heavy metals vary, depending on the soil fraction. Iyengar et

al., (1981) reported that water soluble, exchangeable, and absorbed fractions are readily available to

plants; while primary and secondary soil minerals are relatively unavailable to plants. The metal

species present and their relative bioavailability within the soil are of greater importance than the

total metal concentration in the environment that determines the overall physiological and toxic

effects on biological systems (Bernhard et al., 1986; Hughes et al., 1989; Morrison et al., 1989).

Heavy metal contamination due to sludge application has received much attention due to concerns

regarding uptake by plants and contamination of groundwater or surface waters (Cunningham et al.,

1975).

2.3 The Effect of pH and Organic Matter in Heavy Metal Mobility

The importance of pH in metal solubility is well-known as it influences heavy metal adsorption,

retention and movement (Sauve et al., 1997). Organic matter is another important soil component

that influences metal availability. It has a nutritional function by serving as a source of N, P and S,

and has a high binding capacity for cations and organic contaminants (Oste et al., 2002). It has been

shown that heavy metals are accumulated in surface organic layers in agricultural and urban soils.

However, the extent to which topsoil heavy metals can be mobilized to labile forms remains

uncertain (Mico et al., 2006). Some of the heavy metals emitted by this sludge are known to be

toxic to human and plants, even at low concentrations (Pendias and Mukherjee, 2007).

The fate of heavy metals in sewage sludge is mainly related to their mobility in soil. A traditionally

held view on the mobility of heavy metals in sewage sludge-amended soils is that the metals’

migration is insignificant and the metals tend to remain in the site of input, i.e. in the topsoil (Parker

et al., 1978, Chang et al., 1984; Schiradoe et al., 1986; Dowdy et al., 1991). However, in several

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field-base experiments the apparent migration of heavy metals down the soil depth has been

observed (Bell et al., 1991; McBride et al., 1997).

Furthermore, in column leaching (Ashworth and Alloway, 2004) and batch experiments, (Burton et

al., 2003). It has been shown that heavy metal ions may leach more easily in the presence of sewage

sludge than in its absence. They ascribed such elevated mobility to the high contents of dissolved

organic matter (DOM) in sewage sludge (Liu et al., 2007). Due to its net negative charge at typical

soil pH, DOM generally moves very easily through soil system (Dunnivant et al., 1992). In

addition, metal sorption on soils is strongly related to soil properties. Researches have shown that

metal sorption by soils increased with increasing the pH (Naidu et al., 1994), organic matter

(Gerriste and Driel, 1984; Udom et al., 2004), cation exchange capacity (Buchter et al., 1989), and

the contents of iron and manganese oxides. However, there is a lack of information concerning the

adsorption of sludge-borne heavy metals on different soils (Sigua, 2005).

In case DOM in sewage sludge decreases metal sorption, and thereby increases their mobility in

soil, there might be a greater potential for adverse impacts on the surrounding environment. The

most direct and obvious impact is the threat to ground water quality. Therefore, when we calculate

the sludge application rate to agriculture land, it is necessary to consider the effects of DOM derived

from sewage sludge on heavy metal sorption and also of the soil physicochemical properties (Liu et

al., 2007).

In a study, pH of the sewage sludge was 7.19. The total concentrations of Cu, Ni and Pb were

189.86, 27.24 and 8.90 mg/kg, respectively. The sludge sample contained 53.4% organic matter,

24.9 g/kg DOC and 1.3 cmolc/kg CEC (Centi mole charge per kilogram CEC). Speciation of Ni, Cu

and Pb in the sludge filtrate obtained, showed that they were present mainly as dissolved organic

metallic complexes with 98.93% for Ni, 99.96% for Cu, and 99.98% for Pb, respectively. The

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sewage sludge filtrate has a relatively high content of dissolved organic carbon (1245.6 mg/L), of

which 53% was within the hydrophilic DOC fraction. The large proportion of hydrophilic DOC

could contribute to the composting processes (Liu et al., 2007).

Soil organic matter can not only provide sorption sites for metals directly, but also combine with

soil minerals and increase the sorption sites (Kaiser and Guggenberger, 2003). Regarding to

environmental risks, it is worthwhile mentioning that the real sludge application risk has been

certainly determined by many other factors except for the sludge matrix and soil properties, such as

land usage, microbial activity and plant root-soil interactions (Qureshi et al., 2003; Qureshi et al.,

2004; Seguin et al., 2002; Vervaeke et al., 2004).

In soils which had received metal-contaminated sewage sludge (high-metal soils), the amounts of

biomass were decreased by up to 50%. Also, there was no relationship between biomass C and total

soil organic C in the high-metal soils. Downward migration of heavy metals was observed 7 years

after sludge application, where soluble Cu, Zn and Cd were higher at 40 to 60 cm depth in the

sludge treated soils (Campbell and Beckett, 1988). The decrease in soil pH following sludge

application was a major reason for the higher mobility of heavy metals in sludge-treated soils

(Robertson et al., 1982). However, leaching of Cd, Cu and Pb in sludge-treated soils was also

observed in soils with higher pH values in some other field experiments (Darmody et al., 1983).

The incorporation of C-rich sludge to soils has been shown to increase the amount of dissolved

organic matter (DOM), which can facilitate metal transport in soil and groundwater by acting as a

“carrier” through formation of soluble metal–organic complexes (McCarthy and Zachara, 1989).

The leaching of metals was facilitated by higher amounts of dissolved organic matter in the soil/soil

solution. Furthermore, metal mobility might have been substantially higher shortly after sludge

application than many years later because laboratory-determined distribution coefficients Kd

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(Distribution Coefficient), for the metals in newly prepared sludge/soil mixtures were lower than Kd

values of the aged sludge-treated field soil (McBride et al., 1999). It is suggested that under the field

condition soluble organic matter from organic wastes decomposition and preferential flow paths

were the two dominant factors enhancing increasing metal movement in soil (Wong et al., 2007).

However, some researchers revealed that Zn and Cd have a weak ability to bind to DOM compared

with Cu or Pb. The increased concentrations of soluble Zn and Cd in soil with long term sludge

application is not only determined by the total input of metals, but also strongly related to soil pH.

The lower metal solubility in soil of high pH was more obvious for metals like Zn and Cd that tend

not to complex strongly with soluble organics (McBride et al., 1997).

The concentrations of Cr, Hg, Cu, and As in soil percolates were positively correlated with DOM.

In contrast, Cd and Zn mobilization depend on soil pH and soluble elemental content, but not on

DOM. Moreover, DOM is of minor importance in the mobilization of heavy metals in soils with a

low soil pH (Zhou and Wong, 2001). It has also been shown that the addition of sludge DOM, to a

certain extent, reduced the sorption of both Cd and Zn by acidic sandy loam, calcareous clay loam

and calcareous sandy loam. (Wong et al., 2007).

The environmental risk caused by metal leaching and phytotoxicity due to the heavy application of

sewage sludge in agricultural soils should be taken into consideration especially in near-neutral and

alkaline soils, and anaerobically digested sludge with relatively high pH, because DOM derived

from sludge could significantly reduce metal sorption and increase its mobility through the

formation of soluble DOM–metal complexes in these soils (Wong et al., 2007). Thus, in basic soils

metal persistency is expected to be generally very high.

A number of studies on acid soils have examined the leaching of heavy metals in sewage sludge

amended-soil columns. While some studies have shown that the migration of heavy metals is

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negligible (Schiradoe et al., 1986; Dowdy et al., 1991; Camobreco et al., 1996), other studies have

demonstrated that significant amounts of Zn, Cr, Cu and Cd (among others) were readily leached

(Frenkel et al., 1997; Karathanasi et al., 2005). It therefore appears that soil properties such as

organic matter and soil pH may have a major effect on metal mobility. The addition of organic

matter may also affect metal mobility, for instance, by increasing soluble organic matter, Cu

mobility may be enhanced, especially in sandy soils of high pH (McBride et al., 1999).

Basic soils showed a marked pH-decrease after the application of sewage sludges, the acid loam soil

showed a pH-increase that was even larger than the decrease in basic soils.

The low mobility of metals in the basic soils may be related to high CaCO3 and organic matter

content. Furthermore increased mobilization of these elements in the acid loam may be related to

the lower organic matter, clay, and CaCO3 content of this soil (Toribio and Romanya, 2006).

When considering different kinds of contaminants, heavy metals are especially dangerous because

of their persistence and toxicity (Adriano, 2001). Agricultural used of sewage sludge and inorganic

phosphate fertilizers can cause substantial accumulation of cadmium in soils (Nicholson et al.,

1994; Wiseman, 1994). In most soils, adsorption of Cd increases strongly with increasing organic

matter and pH (Boekhold and Zee; 1992; Hinz and Selim, 1994).

The allowable amount of applied sludge that has been calculated without the interference of

dissolved organic matters is higher than that of interference. This issue indicated that the effect of

dissolved organic matter is a factor of great importance for estimating the allowable amount of

application of sewage sludge. Nevertheless, the real allowable amount of applied sludge depends on

not only dissolved organic matter content and physicho-chemical soil properties, but also to other

factors including land use and microbial activities as well as the interaction between the soil and

plants roots (Liu et al., 2007; Toribio and Romanya, 2006).

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In all types of several applications, heavy metals accumulation existed in plants that their ultimate

destinations were human beings and living creatures as well as the environmental risks posed to

both soil and water (Nicholson et al., 2003; Pendias and Mukherjee, 2007; Adriano, 2001). With an

increase in concentration of dissolved organic matter, movement and translocation of heavy metals

in soil increases while, with an increase in soil organic matter (Bounded with soil particles) and pH

as well, their mobility decrease (Liu et al., 2007; McBride et al., 1999). With an increase in soil pH

as well as the amount of clay in the soil, the mobility of heavy metals present in applied sewage

sludge decrease (Wong et al., 2007;)

2.4 Effect of Sewage Sludge Application in Soil

Application of sewage sludge to agricultural soil is a common practice because of low costs and

recycling of nutrients achieved (Sigua et al., 2005). Disposal of municipal sewage sludge and

effluents has recently received much publicity because of the in- circling amounts of these wastes

produced by urban and industrial activities. Due to growing concern over disposal of sewage sludge

in the oceans and the high cost of its incineration, land application and land tilling are becoming

more common. Disposal of sewage sludge to land can be beneficial because it contains plant

nutrients (especially N and P) and organic matter, which can be of agronomic benefit (Chander and

Brookest, 1991). Agricultural application has become a common waste treatment alternative for

sewage sludge because of practical and economic reasons (Cunningham et al., 1975). Sewage

sludge contains organic matter and nutrients that have the potential to enhance forest productivity

and several soil characteristics (Henry and Cole, 1997; Losada et al., 2001).

High CEC organic soils have been observed as good application sites for sewage sludge and

effluents. Current guidelines (Keeney et al; 1975) set heavy metal limits based on soil pH and

cation exchange capacity (CEC). Studies have shown that heavy metal availability was related to

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the soil CEC and organic matter content (Robertson et al., 1982), while another work has shown

CEC to be a poor prediction of heavy mental availability (Dowdy and Volk, 1984) stressing that

although heavy metal availability was reduced by high organic matter content , extensive leaching

of mineral occurred where disposal rates of sewage sludge were excessive and the soil were coarse-

textured with low concentrations of hydrous oxides.

With respect to the improvement of soil fertility, many studies have shown that soil fertility increase

after land application of sewage sludge and effluence (Keeley and Quin, 1979; Hart and Speir,

1992). For example , study on the effects of over 80 years of application of sewage effluents to

limore silt in Canterbury , New Zealand (Hart and Spier, 1992) shown considerable increase in soil

N, P, K, S, Ca, Mg, organic carbon , pH , and base saturation. Short-term studies (Bernial et al.,

1992) also showed significant increase in soil N, P, K, and micro nutrient concentrations, 8 months

after application of sludge to a calcareous soil in Spain. Augers and N’Dayegamiye (1991) observed

that organic carbon content of a sandy loamy soil increase from 1.5% to 2.2% after 7 years of

applying sewage sludge at the rate of 5 t ha-1

year-1

.

An increase in soil organic matter content resulting from the application of sludge and effluent can

produce a concomitant increase in soil cation exchange capacity. Bernal et al. (1992) observed that

the application of sewage waste-water at rates from 200 to 1000 m3

ha-1

year-1

resulted in significant

increase in soil organic carbon and cation exchange capacity. Similarly, Stadelmmann and Furrer

(1985) observed that 7 years of application of sewage sludge at 5 t ha-1

year-1

to a sandy loam soil

increased the CEC from 172 Cmol kg-1

in the control plots to 23.7 and 22.2 Cmol kg-1

in the treated

plots, respectively. Significant increase in base saturation was also observed following application

of sewage sludge that contained significant quantities of the exchangeable cations, Ca2+

, Mg2+,

Na+,

and K+. However, Guisquiani et al., (1995) observed that though CEC increased significantly in

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sewage treatment soils it was lower than expected. This was most likely due to the fact that the

transition metals added to the soil could have been complexed , thus causing a decrease in the

negative surface charge of the organic matter.

Significant increase in soil nitrogen has also been observed as a result of land application of sewage

sludge and effluents. Studies by Kelling et al., (1977) on the changes with time in the concentration

of soil organic N, inorganic N and available P in the soil profile of two sites treated with liquid,

digested sewage sludge shown that application of large amount of inorganic N, organic N, and

available P in a sandy loam and a silty loam soil in south-central Wisconsin. However, substantial

losses of sludge –applied N were observed to occur by leaching, denitrification, volatilization or a

combination of these.

Mbagwu and Piccolo (1990) observed that the application of sewage sludge at the rate of 200 t ha-1

increase the total N and available P content of soil by 57% and 642%, respectively, whilst

application of other types of organic waste such as pig slurry (40 t ha-1

) and cattle slurry (8 t ha-1

)

increased the soil N content by 18 and 13% and available P content by 430 and 372%, respectively.

Ross et al. (1982) also observed that application of untreated meat processing effluents over a

period of over 80 years (1899-1982) increasing soil organic carbon from 5.6 to 6.8% as well as

mineralized N, and available P.

High N content in most sewage sludge and effluents can cause a decline in soil and plant

concentration of K over a period of time. For example, palazzo and Jenkins (1979) observed a dec

line in plant and soil concentration of K over a 4-year period of land application of sewage waste

–water at the site of treatment , and related it to the K:N ratio of the sewage waste-water applied

because the sewage waste-water contain more than twice as much N as K.

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With respect to the movement of P with soil depth, Bond et al., (1995) observed no increase in P

concentration of the soil water at a depth of 1.2 m in a cropped clay soil receiving 5 cm of effluents

per week for 8 years. The P concentration of the effluent ranged from 4.1 to 9.9 ppm while the P

concentration of the soil water at the 1.2 m depth was less than 0.10 ppm.

In addition to the beneficial effects of land disposal of sewage sludge on the soil chemical properties

a number of detrimental effects and risks associated with the agronomic utilization of sewage sludge

and effluents have been highlighted by Summer and Mclaughian (1996) and Cameron et al., (1996).

Such detrimental effects and /or risks include increased concentration of dissolved p in runoff,

build-up of heavy metals, nitrate leaching to ground water, salt concentration and elevated or

extremely low pH.

Studies of Sabey et al., (1977) on the influence of sewage sludge and wood waste mixtures

application on land indicated that a good combination and proper management of the mixture was a

valuable resource that governed nitrate supply, controlled nitrate leaching and enhanced physical

and chemical properties of the soil. But Agbim et al. (1977) observed that application of sewage

sludge alone to the soil resulted in inefficient utilization of soil nitrogen by plants and/or toxicity

due to high salt content on micro-organism. However, metal toxicity according to Lieffering and

Mclay (1996) was alleviated by liming the soil; moreover, continued crop production required a

near-neutral soil pH, even year after sludge application was discontinued, in order to reduce

mobility of heavy metals that were added to the soil.

Significant increase in soil pH and elevated salt concentration has been observed in soil when

secondary –treated sewage effluent with a high sodium adsorption ratio (SAR) was applied

(Summer and Mclaughlan, 1996). John and Mcconchie (1994) observed that the application of

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secondary treated dilute sewage effluents to soil growing bananas at Woolgoola more than double

the soil sodium concentration from 0.11 to 0.31 cmol kg-1

. Despite the low electrical conductivity of

the effluents (0.44 d sm-1) the soil exchangeable sodium percentage (ESP) value reached 4% during

the trail.

Similarly, land disposal of treated sewage effluents to a waimakakiriri sandy loam in Canterbury,

New Zealand significantly increased soil increase salinity. The electrical conductivity of the soil

increased from 0.4 mm cm-1

to 5.5 mm cm-1

; reduce growth and yields of many crops were

observed (Balks et al; 1996). A high concentration of Na in soil is of concern because it can cause a

decrease in infiltration rate and an increase in the risk of runoff.

High concentration of boron, sodium, chloride, carbonates, and total dissolve solids in sewage water

could damage plant because the advantage use of effluents on land depends on the quality of waste

water, soil type, crop, and climate. Crops vary in their tolerance to salts. For example, Balk et al.

(1996) observed that the beans, red clover, groundnut and citrus were more sensitive to salts and

organic compounds associated with sewage waste-water than grasses, barley, and cotton.

High concentration of Na+ and C1

- was also observed in the top 15 cm of soils treated with beef

feedlot effluents (Tiarks et al., 1974). The major factor responsible for that development, according

to the study, was the high Na+

content of the feedlot effluents. The application to the soil of effluent

from a pulp and paper mill in New Zealand, increase the sodium adsorption ratio (SAR) from 2 to

16 and increase the sodium concentration in ground water (Johnson and Ryder, 1988). Brechin and

McDonald (1994) also detected increase sodium content in soil fertilized with pig slurry in South

Australia and suggested that this could become a problem in the long-term.

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Heavy metal contamination due to sludge application has received much attention due to concerns

regarding uptake by plants and contamination of groundwater or surface waters (Cunningham et al.,

1975). Thus application of sewage sludge to agricultural soil may result in elevated concentrations

of toxic metals, which may then threaten ground water quality and lead to food chain contamination

(Selivanovskaya and Latypova, 2003; Singh et al., 2004).

Heavy metals are often highly persistent in soil, with residence times as long as thousands of years

(Alloway, 1990). Metals applied with sewage sludge may be retained in the soil as a result of their

adsorption on hydrous oxides, clays, and organic matter; the formation of insoluble salts; or the

presence of residual sewage sludge particles (Alloway and Jackson, 1991). Moreover, soil CaCO3

has often been found to increase soil metal retention (Raikhy and Takkar, 1983). Heavy metal

accumulation in soils can result in a loss of soil functions leading to concerns about environmental

quality protection, maintenance of human health and productivity. Soil pollution can have

implications in phytotoxicity at high concentrations and result in the transfer of heavy metals to the

human diet from crop uptake or soil ingestion by grazing livestock (Pendias and Pendias, 2001;

Nicholson et al., 2003; Pendias and Mukherjee, 2007). Industrial waste incinerators also are being

sources of heavy metal and organic compound pollution (Hu et al., 2003).

Application of sewage sludge to cropland could result in soil contamination, phytotoxicity, and

accumulation of trace elements in the food supply. The magnitude of the problem depends on the

interrelationships of a number of factors, such as the composition of sludge, the rate and frequency

of applications, soil characteristics, and plant species. Sludge type and sludge-soil interactions

influence the chemical forms of a metal which determine its availability for plant uptake. However,

additional plant and soil factors further modify the uptake and the concentration of elements in

crops.

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2.5 Sludge-Soil Interaction

Limited information is available on the reactions of metals in municipal sewage sludge with soils,

so reactions between metals in sludges and soils are not completely understood. Many researchers

have reported that after municipal sewage sludge is incorporated into soil, portions of the metals

revert to non-extractable, less available chemical forms (Beckett et al., 1979; Wollan and Beckett,

1979; Lagerwerff et al., 1977;). The variability in the results of incubation studies suggested to

Beckett et al. (1979) that the initial stages of the sludge-soil interaction are microbial rapid

decomposition of metal compounds in sewage sludge with microbial immobilization of the released

ions. On the one hand, with time, these ions form inorganic compounds or stable organic complexes

which resemble the "native" soil forms of these metals [Beckett et al., 1979; Wollan and Beckett,

1979; Lagerwerff et al., 1977; Cunningham et al., 1975).

On the other hand, after addition to the soil, some metals change only slightly in chemical character.

Chromium, which is present as a colloidal precipitate in municipal sewage sludge, changed little in

its chemical form. It remained mostly insoluble after incorporation of sludge in soil (Grove and

Ellis, 1980).

The chemical and physical properties of soils that receive sludge influence metal conversions

(Stover et al., 1976). Soil properties, such as CEC, pH, organic matter content, sesquioxide content,

redox potential, texture, and presence of other elements affect plant uptake, solubility, and mobility

of these metals (Soon, 1981; Zwarich and Mills,1979; Street et al., 1977, 1978; CAST, 1976;

MacLean et al., 1969). Not all metals react similarly to changes in these soil properties. For

instance, soil pH levels which decrease the availability of metal cations to plants increase the

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availability of Mo (La Hann, 1976). Dowdy and Larson (1975) mixed municipal sewage sludge into

two topographically associated soils with different pH levels of 5.9 and 7.9 (with free carbonates).

After incubating the sludge-soil samples for one growing-degree year, the researchers grew barley

(Hordeum vulgare L.) to measure the quantities of plant-available potentiaily toxic metals.

Incubation, sludge application rate, and soil pH affected metal accumulation within the roots and

tops of barley seedlings. As sludge application rates increased, an increase in the removal of Cr, Ni,

Zn, and Pb occurred when barley was grown on the acid soil.

However, there was no change in the uptake of these metals when barley was grown on the high pH

soil. Thus, with different levels of soil pH, metals released by the decomposition of sewage sludge

either increased or decreased in availability for plant uptake. Lagerwerff et al., (1977) suggest that

the formation or the strengthening of metal complexes with higher soil pH levels and incubation

affects their availability. The presence and the concentrations of other metals can have a

pronounced effect on the uptake of the metal in question (Ham and Dowdy, 1978; Cunningham et

al., 1975). Cadmium concentration increased in plant tissue as soil Cu levels increased

(Cunningham, 1975); the levels of Cr, Ni, and Zn also affected the magnitude of the increase. These

interactions are extremely complex and are not well understood

Land application of sewage sludge can have many beneficial effects. Supplying nutrients (N, P,

secondary nutrients, and micronutrients) to the crops, improving soil physical properties, and

increasing soil organic matter content are several advantages of land application of municipal

sewage sludge. Although these are obvious benefits, there are also concerns that must be addressed

to insure a safe, economical, and environmentally sound approach to applying sewage sludge to the

soil. The most commonly voiced concerns include: 1) the potential for nitrate or phosphate

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33

contamination of waters; 2) the potential for damage to soils, plants, animals, and humans because

of possible toxic metal applications; and 3) the potential for pathogen transfer.

Municipal sewage sludge added to soil can improve soils biological, chemical, and physical

properties. Changes in the properties of sludge amended soils vary with the characteristics of the

sludge and soil (Mitchell et al., 1978; Gupta et al., 1977). The faunal and microfloral components of

soils were altered when sewage sludge was added (Mitchell et al., 1978). A rapid increase in

nematode (predominantly Rhabditidae spp.) populations and a slower increase in enchytraeid

populations occurred in sludge amended soil. Both of these organisms feed on soil microbial flora

(bacteria for nematodes, fungi for enchytraeids).

A change in soil pH can result from application of sewage sludge. Increased soil pH occurred when

municipal sewage sludge was added to soils (Silviera and Sommers, 1977; Gaynor and Halstead,

1976). Other researchers noted a decrease in soil pH in sludge-amended soils (Silviera and

Sommers, 1977; Epstein et al., 1976; LaHann, 1976). Silviera and Sommers (1977) related changes

in soil pH to the calcium carbonate content of sludges and the acid production during sludge

decomposition. Whether a sludge-soil mixture increases or decreases pH is an important

consideration in relation to potentially toxic metal uptake by crops, since these metals generally are

more available to plants at lower pH levels. The addition of relatively high rates of sludge increases

the cation exchange capacity (CEC) of soils (Soon, 1981; Mitchell et al., 1978). This increase in

CEC results in additional cation binding sites which retain essential plant nutrients within the

rooting zone. Possibly the CEC increase causes more complexing of heavy metals in an unavailable

form for plant uptake (Kladivko and Nelson, 1979).

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Organic matter, which constitutes approximately 50 percent of the solid fraction of most sludges,

improves the physical condition of soils (Khaleel et al., 1981; Kladivko and Nelson, 1979;). An

increase in organic matter content decreases bulk density (Kladivko and Nelson, 1979), increases

aggregate stability, increases water holding capacity and promotes greater water infiltration

(Kladivko and Nelson, 1979, 1979; Kelling et al., 1977).

Improving the physical properties of soil increases soil productivity (Kelling et al., 1977). In coarse-

textured soils, higher productivity occurs from the increase in the amount of water available to

crops. In fine textured soils, productivity increases because reduction in bulk density increases

infiltration, porosity, and aeration by aggregation of soil particles. The improvement of soil

productivity by treatment with sewage sludge is shown dramatically in experiments using

drastically disturbed lands (Garcia et al., 1981; Stucky et al., 1980; Stucky and Newman, 1977).

2.6 Implications of Trace Metal in Soil and Plant

Trace elements have been defined as the elements that occur in natural systems in small amounts

and when present in excessive concentrations, are toxic to living organisms (Kirkham, 1977). The

plants oil system has three protective mechanisms that can limit these potentially toxic trace

elements in the aerial portions of a plant, and so minimize health problems to animals or humans.

The ''Soil-Plant Barrier,'' as it is called by Chaney (1980), includes: Elements that are insoluble in

soil and do not accumulate in the plant (Pb, Hg, Cr, F, Ag, Au, Ti, Sn, Si, and Zr), elements that are

absorbed into the root but are insoluble in the root or have limited translocation to the shoot (Fe, Al,

and occasionally Hg and Pb); and elements which when applied in excess cause phytotoxicity, so

plants are not consumed by man or domestic animals (Zn, Cu, Ni, Co, Mn, As, and B). Not all trace

elements present in municipal sewage sludges fall into one of these three categories. Important

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35

exceptions are Cd, Se, and Mo which can cause toxicities in animals and humans. Molybdenum and

Se are present in sewage sludges in low concentrations, thus these elements normally do not limit

the rate of sludge application to soil. Cadmium, however, has caused adverse health effects in

humans who ingested plants grown on soils contaminated with high levels of Cd (Chaney, 1980).

Ingestion of soil or a sludge-soil mixture by grazing animals provides a direct pathway to adding

excessive trace elements (especially Pb) to the food chain (Chaney, 1980). The Council for

Agricultural Science and Technology (CAST, 1976) classified Cd, Cu, Mo, Ni, and Zn as potential

hazards in land application of municipal sewage sludges. These metals tend to accumulate in plants

and cause either reduced yields or health problems to animals or humans that ingest the plants. A

number of investigations have been conducted in the greenhouse and in the field to assess the

phytotoxicity and availability of potentially toxic elements to plants grown under three different soil

conditions: soils treated with sludge, soils treated with sludges supplemented with metal salts, or

soils treated with metal salts alone. The concentrations of Cd, Cu, Mn, Ni, Pb, and Zn in the edible

parts of lettuce tops (Lactuca sativa L.) and onion bulbs (Allium cepa) were generally much higher

when the plants were grown on sludge-amended soils in the greenhouse rather than when the plants

were grown in the field (DeVries and Tiller, 1978). Moreover, reduced yields and higher Cr, Cu,

and Zn concentrations were observed in plants grown in soils treated with additions of inorganic

salts than were observed in plants grown in soils treated with equivalent amounts of these metals

from sludge additions (Cunningham et al., 1975).

Therefore, plant data from studies in the greenhouse or from additions of inorganic metal salts

should not be used as the only indicator of the potential adverse effects of applying municipal

sewage sludge under field conditions. Practices that promote good soil aeration, such as drainage

and structure development, lead to decreasing solubility of trace elements. Also, soils with high

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cation exchange capacities are desirable for sludge disposal, because they have a great ability to

hold and immobilize trace elements. Because of the nitrification reaction and the microbial

production of carbon dioxide, sewage sludge usually lowers the pH of soils; thus, liming is

recommended at sludge-disposal sites, but only when the soil pH is acidic (i.e., < pH 6). Liming

also controls the uptake of trace elements of concern in sludge (cadmium, nickel, and zinc). Trace

elements can form inert and insoluble compounds with clays and organic compounds. Therefore,

they may be less available to plants than total concentrations of these elements in the soil indicate.

Trace elements tend to move little with percolating water and remain at the site of application,

unless they are transported away on eroded sediments.

2.7 Plant Factors Influencing Metal Uptake

The increased availability of heavy metals for plant uptake may lead to phytotoxicity, whereas less

phytotoxic elements may accumulate in higher amount in plants. This later process enhances their

transfer into the food chain, thus posing serious environmental hazard to the population. Once

present in agricultural fields, the availability and uptake of heavy metals by plants roots is

determined by what happens at or near the soil plant root, stem and leaves interface.

The myriad of parameters regulating the chemical fate of specific elements in soils determine their

solubility and availability for plant uptake. The plant uptake of chemical species in soil solution is

also dependent on a number of plant factors. These include: physical processes such as root

intrusion, water, and ion fluxes and their relationship to the kinetics of metal solubilization in soils;

biological parameters, including kinetics of membrane transport, ion interactions, and metabolic fate

of absorbed ions; and the ability of plants to adapt metabolically to changing metal stresses in the

environment.

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The accumulation of metal ions by root systems is a key function in terrestrial plants, which exhibit

extensive ramifications through soil. Distribution of heavy metals in plant body depends upon

availability and concentration of heavy metals as well as particular plant species and its population

(Punz and Seighardt, 1973). For instance, roots usually show higher heavy metal concentration than

shoots, because they are the origin, which comes into contact with the toxic metals present in the

soil (Breckle, 1991). In recent past, Bunzl et al. (2001) investigated soil to plant transfer of heavy

metals like, Cu, Pb and Zn by vegetables. Studies on heavy metal uptake revealed that vegetables

grown at environmentally contaminated sites in Addis Ababa, Tanzania, could take up and

accumulate metals at levels that are toxic to human health

Metal uptake differences by leafy vegetables are attributed to plant differences in tolerance to heavy

metals (Itanna, 2002). Cadmium, copper and nickel levels in vegetables from industrial and

residential areas of Lagos City, Nigeria was studied by Yusuf et al. (2002), which revealed that

levels of Cd, Cu and Ni in different edible vegetables along with its soils on which they were grown

were higher in industrial areas than those of the residential areas due to pollution. Trace element and

heavy metal concentrations in fruits and vegetables of the Gediz River region were intensively

studied by Delibacak et al. (2002). Also edible portions of five varieties of green vegetables viz.

Amaranth, Chinese Cabbage, Cowpea leaves, Leafy Cabbage and Pumpkin leaves collected from

several areas in Dar Es Salaam, Africa were analyzed for Pb, Cd, Cr, Zn, Ni and Cu. There was a

direct positive correlation between Zn and Pb levels in soils with levels in vegetables. The relation

was absent for other heavy metals (Othman et al., 2002).

Plants growing on polluted soils may contain elevated levels of heavy metals (Gallego et al., 2002;

Zornoza et al., 2002). Heavy metal ions such as zinc, manganese and nickel are essential

micronutrients for plants but, when present in excess, these, and also non-essential heavy metals

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such as cadmium, can accumulate in plant parts used for human or animal nutrition to undesirably

high contents. At even higher levels, they can become toxic to the plant (Williams et al., 2000).

Comparisons between crop species show wide variations in their ability to absorb potentially toxic

trace elements from the sludge-soil system. Cereals and legumes accumulated less Cd in shoots than

leafy vegetables, like curlycress (Lepidium sativam L.), lettuce (Lactuca sativa L.), and spinach

(Spinacia oleracea L.) (Bingham et al., 1975). Tomato plants (Lycopersicon esculentum Mill.)

accumulated more Cd from municipal sewage sludge-amended soils than either barley or bean

plants (Phaseolus spp.) did (Bradford et al., 1975). Furr et al. (1980) grew bush bean (Phaseolus

vulgaris), cabbage (Brassica oleracea var. capitata), carrot (Daucus carota var. sativa), Japanese

millet (Echinochloa crusgalli var. frumentacea), onion (Allium cepa), potato (Solanum tuberosum)

and tomato plants on sludge-ash amended soils and analyzed plant tissue for B, Cd, Mo, Ni, Se, and

Zn. These plants exhibited differing affinities for the absorption of specific elements. Differences in

accumulation of these metals in plant tissues occured even within plant species, varieties [Boggess

et al., 1978], and hybrids (Hinesly et al., 1978).

This finding suggests that the capacity to accumulate metals may be under genetic control (Hinesly

et al., 1978). Sensitivity of plants to metal toxicity can be associated with the tendency to

accumulate the metal in shoots (Boggess et al., 1978; Bingham et al., 1975). Bingham et al. (1975)

observed that spinach, soybeans, lettuce, and curlycress were injured by soil Cd levels of 4 to 13,

ug/g soil. These plants tended to accumulate Cd in shoots; whereas, lower shoot accumulators like

tomato and cabbage could tolerate soil Cd levels of 170, ug/g without injury. Some plant species

can tolerate high levels of metals in tissue or can confine accumulated metals to the roots and

provide resistance to toxicity (Davis and Beckett, 1978). Potentially toxic metal concentrations are

not the same in all portions of the plant. A survey of a number of food crops revealed that the tuber,

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seed, or fruit tissue had a lower amount of Cd than plant leaf tissue had (Ritter and Eastburn, 1978;

Giordano and Mays, 1977; Bingham et al., 1975).

Hyperaccumulating plants must have the ability to accumulate heavy metals, have a high biomass

production, and disease and pest resistance in order to flourish within toxic heavy metal

contaminated soil. However, concentration of heavy metals in the roots of clover and wheat were

much higher than their shoots. These disproportional metal concentrations within the roots may be

due to the plants not reaching maturity. Comparisons between crop species show wide variations in

their ability to absorb potentially toxic trace elements from the sludge-soil system. This finding

suggests that the capacity to accumulate metals may be under genetic control (Hinesly et al., 1978).

Sensitivity of plants to metal toxicity can be associated with the tendency to accumulate the metal in

shoots (Boggess et al., 1978; Bingham et al., 1975).

The plants that are not deep rooted are highly affected by the heavy metals because the metals

remain in the top soils and do not leached deeper (Yin et al., 2009; Zupan i et al., 2009). Some plant

species can tolerate high levels of metals in tissue or can confine accumulated metals to the roots

and provide resistance to toxicity (Davis and Beckett, 1978).

In conclusion, it has become obvious from the literature that the majority of research into land

treatment or disposal of sewage and effluents has been carried out. Heavy metal contamination due

to sludge application has received much attention due to concerns regarding uptake by plants and

contamination of groundwater or surface waters. More studies are needed on sites that have

received sludge for many years to evaluate the mobility and bioavailability of minerals in soils and

crop plants. However, heavy minerals in sewage sludge and the toxicological implications are of

concern in agricultural production due to the adverse effects on food quality (safety and

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marketability) and crop growth (phyto-toxicity). There is need for this study in developing

countries, because it will represent one of the long term problems associated with disposal of

sewage sludge and effluents in Nigeria.

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CHAPTER THREE

MATERIALS AND METHOD

3.1 Site Description

The study was carried out at the University of Nigeria Nsukka (UNN) sewage disposable site.

Ecologically, Nsukka belongs to derived savannah zone of Nigeria and is located on latitude

06◦52ʹN and longitude 07

◦ 24ʹE. It is on an average elevation of 447 m above mean sea level

and is characterized by tropical wet climate usually from April to October and dry climate usually

from the month of November to March. The mean annual rainfall is about1600mm. The relative

humidity is rarely below 60% (Asadu et al., 2002). Nsukka has high temperature throughout the

year. The mean maximum and minimum temperature are about 35◦ and 22

◦C, respectively.

The soils of the area have been classified using key to soil taxonomy as arenic kandiustult based

on USDA Soil Taxanomy (Soil Survey Staff, 1984), derived from false bedded sandstone

(Akamigbo and Igwe, 1990). Its clay mineralogy is composed mainly of kaolinite and quartz

(Akamigbo and Igwe, 1990). The soil of the site has been subjected to heavy application of

partially treated sewage sludge and effluent for over 40 years and the farming community has

been taking advantage of the sewage sludge and effluent to grow various crops like vegetable,

cassava (manihot spps), maize (zea mays)etc.

3.2 The Sewage System

The sewage sludge and effluent are received through a network of underground pipes from the

residential and administrative area of the UNN. This is because the sewage site is at almost the

lowest elevation place within the university area. The effluent moves gravitationally through the

network of underground pipes to where it is received at the central collecting centre. The sewage

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sludge and effluent from any part of the university at lower elevation than the central collecting

centre were conveyed by the conveyor (tractor tank) and emptied at the central reservoir at the

sewage site.

The central sewage system is constructed so well that no seepage is allowed; it has concrete down

to the base (Plate 1). The walls are thickly sealed with concrete down the base. The sewage

sludge is made to pass through the primary treatment path way. Primary treatment pathway

involves sedimentation of the biosolid. Settling is hastened by gravity and chemical flocculation

with aluminum and hydrated lime treatment. The sewage does not pass through further

stabilization involved in the secondary and tertiary pathway before they are discharged as partly

treated sewage sludge and effluent through open gutter to oxidation pond. These sewage sludge

and effluent are allowed to seep freely into the soil profile and some of the farmers make use of

the water from the oxidation pond to irrigate their crops.

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Plate 1: The central sewage system (Photo courtesy of Ezeudo VC.)

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Plate 2: The settling chamber (Photo courtesy of Ezeudo VC.)

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Plate 3: The oxidation pond (Photo courtesy of Ezeudo VC.)

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3.3 Field Sampling

Sludge samples were collected in two different position at the central sewage system. Auger soil

samples (0 – 40, 40 – 80 and 80 – 120 cm depths) were collected along two transects around the

oxidation pond at disposal site (0(edge), 100 and 300 m) and approximately 2000 m (control)

away from the disposal site. A total of 24 soil samples were collected. The sludge and soil

samples were air-dried (the sludge sample were additionally ground) and passed through 2mm

sieve and stored in black polyethylene bags preparatory for analysis.

Three samples of most common plants (cassava, maize, and Pannicum maximum) were collected

at 0(edge), 100, 300 and approximately 2000 m away from the disposal site.

3.4. Routine Analysis

The particle size analysis of the soil was determined using the Bouycous hydrometer method as

described by Gee and Or (2002). Soil pH was determined potentiometrically using pH meter in a

soil-water/KCl ratio of 1:2.5. The exchangeable acidity was done using 1N KCl displacement

method. Organic carbon concentration in the sludge and soil samples were determined by the

dichromate wet oxidation method of Walkley and Black as described by Nelson and Sommer

(1982). This was converted to organic matter concentration by multiplying with a correction

factor of 1.724. The total nitrogen was determined using the Kjeldhal method as described by

Bremner (1996). Available phosphorus was extracted using Bray II extractant as described by

Bray and Kurtz (1945) and determined using photo-electric calorimeter. Exchangeable calcium,

magnesium, sodium and potassium were extracted with NH4OAc at pH of 7.0. Calcium and

magnesium were determined using Ethylene diamine tetra-acetic acid (EDTA) titration method

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while Potassium and sodium were determined by flame photometer (Rhoades, 1982). Cation

exchange capacity was determined titrimetrically using 0.01N NaOH. Exchangeable acidity (EA)

will be determined 1NKCl (Mclean, 1995)

3.5 Determination of the soil content of heavy metals (Pb, Cu, Cd and Hg)

The methods developed by the United States Environmental Protection Agency for total available

heavy metals in soil, sediments and sludge (USEPA SW-846, method 3050) (USEPA 1986), were

used in the preparation of the soil samples for the determination of their contents of total available

metals content in this study.

Cadmium was determined using xylenol orange indicator as described by Vogel (1965). Copper

was determined by ferro cyanide method as described by Alexegev (1969). Mercury was

determined ferrocyanide method as described by Alexegev (1969). Lead was determined by

sulphide method as described by Vogel (1965).

3.6 Sample Preparations and Digestion of crop plant for Heavy Metal Determination

All crops/plants were rinsed in distilled water gently; moisture and water droplets were removed

with the help of blotting paper. The plant samples were separated into roots, and leaves, and dried

before grinding to fine powder. The drying was done in an oven at 80◦C for 72 hours. The dry

samples were blended in a blending machine.

Metal concentration in plant tissues was determined by using the wet digestion method. The metal

accumulation of each plant species was determined by spectrophotometer method.

The levels of metal concentration in plants were compared with safety standard (WHO/FAO).

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3.7 Data analysis

The design was a 4x3 factorial in which distance from the sewage disposal site and soil depth

were the two factors under consideration, factor A - Distances from sewage pond (0 edge, 100, 300 and

2000 m (control) away from the sewage pond) and factor B – soil depths (0-40, 40-80, and 80-120 cm).

Data obtain were subjected to two-way analysis of variance. Significant treatment mean were separated

using fisher’s least significant difference (LSD) at 5% probability level.

Bioconcentration Factor (BCF) was calculated to understand the extent of risk and associated

hazard due to the mobility of the heavy metals in soil and metal accumulation in each plant part.

The BCF was calculated as the ratio of concentration of metal in plant part to the concentration of

metal in soil. BCF = ������������� � ����� �� ����

������������� � ����� �� ����

Descriptive statistics was also employed in some aspects of data analysis.

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CHAPTER FOUR

RESULTS

4.1 Sewage sludge

The results of the analysis of the sludge showed that the sludge was slightly acidic (pH of 6.5)

and was composed of high content of organic matter and total nitrogen, high level of available

phosphorous and potassium, and high concentrations of Cd, Cu, Hg, and Pb.

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Table 1: Mean values of some elemental characteristics of sewage sludge and the corresponding

FAO/WHO standards.

FAO/WHO standards

pH in water 6.5 -

Organic matter (%) 6.10 -

Nitrogen (% ) 3.50 -

Phosphorous ( ppm) 35.00 -

K (cmol/kg) 2.52 -

Cd (mg/kg) 4.33 3000 – 6000

Cu (mg/kg) 26.01 140000

Hg (mg/kg) 5.01 23000

Pb (mg/kg) 1.50 300000

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4.2 Physicochemical properties at various distances away from sewage site

The main effect of distance from sewage sludge on soil chemical properties shows that there were

significant differences (P < 0.05) in soil pH, organic matter concentration, nitrogen,

K+,Ca

2+,Mg

2+, total exchangeable base, cation exchange capacity and available phosphorous.

These soil parameters gradual decreased from the edge (0 m) of the disposal site through the 300

m distance to the control site (2000 m).Notably, the exchangeable sodium and total exchangeable

acidity though not significant (P < 0.05) showed negligible decrease as distance increased from

the edge to 2000 m from the soil(control) (Table 2).

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Table 2: Effect of distance from the sewage site on soil physicochemical properties

Soil property Distance (m)

LSD(0.05)

0 (edge) 100 300 ~2000 (control)

Clay (g/kg) 95 95 111 171 NS

Silt (g/kg) 129 116 94 186 NS

F. sand (g/kg) 256 251 238 232 NS

C. sand (g/kg) 561 556 561 387 NS

pH in H2O 4.3 4.5 4.5 4.7 0.3

OM (g/kg) 1.7 1.5 0.6 0.40 0.2

N (g/kg) 0.3 0.2 0.1 0.06 0.06

Na+

(cmol/kg) 0.17 0.16 0.16 0.07 NS

K +

(cmol/kg) 0.19 0.17 0.13 0.10 0.04

Mg2+

(cmol/kg) 2.6 2.3 1.9 0.9 0.6

Ca2+

(cmol/kg) 2.8 2.6 1.9 0.9 0.6

TEB (cmol/kg) 5.7 4.8 3.6 2.1 0.8

CEC (cmol/kg) 22.6 20.8 18.2 9.94 1.5

H +(cmol/kg) 1.5 1.4 1.3 1.3 NS

Al2+

(cmol/kg) 1.4 1.3 1.3 1.3 NS

TEA(cmol/kg) 2.7 2.6 2.5 2.5 NS

P(mg/kg) 29.4 25.6 22.3 8.1 5.6

F. sand – fine sand; C. sand – coarse sand

TEB – total exchangeable base; TEA – total exchangeable acidity; CEC – cation exchange capacity

NS – non significant

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4.3 Physicochemical Properties at Various Soil Depths

The main effect of depth on chemical property of the soil results in high accumulation of soil chemical

properties at 0 – 40 cm depth when compared to corresponding soil depths of 40 – 80 cm and 80 –120 cm.

Significance differences (P < 0.05) were observed among soil pH, organic matter content, total N,

exchangeable K, Mg and Ca, cation exchange capacity CEC and available phosphorous (Table 3).

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Table 3: Effects of depth from the sewage site on soil physicochemical properties

Depth (cm)

Soil property 0-40 40-80 80-120 LSD0.05

Clay( g/ kg) 99 111 143 NS

Silt(g/ kg) 132 131 130 NS

F. sand(g/ kg) 260 228 246 NS

C. sand(g/ kg) 534 513 501 NS

pHinH2O 4.4 4.6 4.5 0.3

OM (g/ kg) 1.54 1.20 0.68 0.3

N (g/ kg) 0.21 0.13 0.11 0.05

Na+

(cmol/kg) 0.27 0.2 0.2 0.10

K +

(cmol/kg) 0.21 0.13 0.11 0.03

Mg2+

(cmol/kg) 2.1 1.9 1.7 0.3

Ca2+

(cmol/kg) 2.4 2.1 1.7 0.5

TEB (cmol/kg) 4.4 4.6 4.5 0.7

CEC(cmol/kg) 19.0 17.7 15.8 1.3

H +( cmol/kg) 1.5 1.2 1.2 0.3

Al2+

( cmol/kg) 1.3 1.3 1.3 NS

TEA(cmol/kg) 2.8 2.6 2.6 NS

P(mg/kg) 25.4 24.3 14.4 4.9

F. sand – fine sand; C. sand – coarse sand

TEB – total exchangeable base; TEA – total exchangeable acidity; CEC – cation exchange capacity

NS – non significant

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4.4 Simple Matrix of Distance and Depth on Soil Physicochemical Properties

4.4.1 Soil pH as influenced by sewage disposal

At 0 m(edge) 100 m and 300 m of the disposal site soil pH gradually increased from 0 – 40 cm

depth to 80–120 cm depth. Notably the soil pH increased significantly (P ʹ 0.05) with depth at

the disposal site (0 m – 300 m) but decreased significantly with depth at the control site (2000 m)

Irrespective of the distance and depth the range of soil pH was 4.0 – 5.2 (Table 4a).

4.4.2 The Organic Matter Concentration and Nitrogen Content of the Soil

At all distances the organic matter concentration tends to decrease with increase in depth. The

organic matter content of the soil decreased with a definite pattern as distance increased from edge

to the control site. The result shows that organic matter content of the soil was significant (P ʹ

0.05) irrespective of the distance and depth. Total Nitrogen has a similar trend as that of organic

matter being much higher at the 0 m (edge) and decreased through 100 m and 300 m distance to

the control site (2000 m). Nitrogen content also decreased as soil depth increased from 0 – 40 to

80 – 120 cm interval (Table 4a).

4.4.3 Soil Exchangeable Bases

The results of simple matrix of distances and depths on the exchangeable bases show that

exchangeable sodium made no obvious difference. There were negligible decrease as distance and

soil depth increased from 0 to 2000 m and 0 to 120 cm respectively, then soil exchangeable

sodium ranges from 0.2 – 0.7 cmol/kg irrespective of distance and soil depth. Exchangeable

potassium consistently decreased from the 0 – 40 cm depth through 40 - 80 and 80 -120 cm soil

depth at each distance from the disposal site with exception of control (2000 m) where

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exchangeable potassium concentration increased with increase in the soil depth (Table 4b). There

was significant difference (P ʹ 0.05) along four distances. Exchangeable calcium and magnesium

showed similar trends where 0 – 40 cm soil depth of each distance at the sewage disposal site

showed highest values for exchangeable bases while 2000 m or the control shows reverse

trend(Table 4b).

4.4.4 Total Exchangeable Acidity (TEA)

The soil total exchangeable acidity increased with depth in a definite pattern at 2000 m(control

site) (Table 4b) but varied considerably at the sewage site. The effects of distance and depth on

TEA were significant (P ʹ 0.05). Low accumulation of total exchangeable acidity was observed

at different soil depths at each distance at the sewage site (0 m 100 m and 300 m) compared with

similar soil depths at 2000 m(control) from the site (Table 4b).

There were significant (P ʹ 0.05) effects of distance and depth on cation exchange capacity

(CEC) content of the soil. The CEC values of the soils ranged from 8.5 - 24.8 cmol/kg with the

highest value 24.8 recorded at 0 – 40 cm soil depth at 0 m distance. CEC consistently decreased

from 0 –120 cm soil depth at each distance. Notably the soil CEC concentration of the disposal

site was about two times higher than that observed from the control (Table 4b).

4.4.5 Available Phosphorous

Available phosphorous distribution in the soil ranged from 7.5 to 34.4 mg/kg, available

phosphorous showed a gradual decrease from edge (0 m) through the 300m distance to the

control (2000 m), though different soil depth at each distance varied considerably along the four

distances (Table 4b). However, there were significant (P ʹ 0.05) effects of distance and depth on

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available phosphorous. The available phosphorous concentration was significantly higher at

sewage site when compared to the control site (Table 4b).

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Table 4a: The Mean Simple matrix of Distance and Depth on the Soil Physicochemical Properties

Distance

(m)

Depth (cm) Clay Silt F.sand C.sand pH in H2O OM% N% Na

(cmol/kg)

K

(cmol/kg)

0-40 80 133 27.6 564 4.0 2.24 0.37 0.22 0.29

0(edge) 40-80 80 125 24.14 551 4.3 2.0 0.21 0.16 0.16

80-120 124 130 25.41 568 4.5 0.80 0.2 0.13 014

0-40 7.5 13.9 27.7 54.1 4.2 1.77 0.24 0.18 0.27

100 40-80 8.9 11.1 22.8 57.7 4.6 1.50 0.16 0.13 0.14

80-120 12.2 9.8 24.7 54.9 4.8 1.11 0.11 0.11 0.11

0-40 9.7 9.5 25.4 56.9 4.1 1.22 0.16 0.16 0.16

300 40-80 9.7 8.7 22.8 56.9 4.5 0.98 0.10 0.11 0.11

80-120 14.0 10.1 23.1 54.4 4.7 0.51 0.1 0.08 0.08

0-40 14.4 16.0 23.4 46.4 5.2 0.87 0.1 0.06 0.9

2000 40-80 17.7 20.0 21.4 35.5 4.8 0.64 0.07 0.07 0.12

80-120 18.8 19.3 24.9 34.3 4.0 0.40 0.04 0.08 0.12

FLSD0.05 NS NS NS NS 0.6 0.6 0.11 NS 0.06

F. sand – fine sand; C. sand – coarse sand

TEB – total exchangeable base; TEA – total exchangeable acidity; CEC – cation exchange capacity

NS – non significant

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Table 4b: The Mean Simple matrix of distance and depth on the soil physicochemical properties (contd.)

Distance

(m)

Depth

(cm)

Mg

(cmol/kg)

Ca

(cmol/kg)

TEB

(cmol/kg)

CEC

(cmol/kg)

H

(cmol/kg)

Al

(cmol/kg)

TEA

(cmol/kg)

P

(ppm)

0-40 3.12 3.01 6.57 24.8 1.4 1.11 2.59 34.4

0(edge) 40-80 2.65 3.05 5.78 22.2 1.07 1.41 2.41 34.4

80-120 2.05 2.5 4.74 20.7 1.41 1.38 2.76 19.31

0-40 2.81 3.2 6.55 21.4 1.52 1.08 2.60 29.2

100 40-80 2.23 2.6 5.64 20.1 1.41 1.33 2.74 30.6

80-120 1.90 2.02 4.05 18.5 1.36 1.41 2.76 17.08

0-40 1.94 2.50 4.25 19.6 1.7 1.07 2.76 28.6

300 40-80 1.84 2.01 4.09 19.3 1.23 1.31 2.54 27.9

80-120 1.07 1.30 2.33 13.6 1.47 1.45 2.72 13.7

0-40 0.55 0.80 1.58 10.3 1.95 1.30 3.01 9.2

2000 40-80 1.06 0.81 1.92 9.4 1.9 1.40 3.20 7.5

80-120 1.25 1.04 2.79 8.5 1.85 1.8 3.65 7.59

FLSD0.05 0.69 1.02 1.4 2.5 0.41 0.35 0.42 9.8

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4.5 Heavy Metals in Soil

4.5.1 Effect of distance on selected heavy metal contents of the soil

The main effects of distance on selected heavy metals contents of the soil are shown in Table 5. It

is evident from the table that the 0 m (edge) distance accumulated much of the heavy metals.

These heavy metals significantly (P ʹ 0.05) decreased consistently as distance increased from the

edge (0 m) to the control (2000 m). However, the result of the study reveals that the sewage site

distances (0, 100 and 300 m) had higher concentrations of the soil heavy metal when compared

with the 2000 m or control distance.

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Table 5: Effects of distance on soil heavy metals distributions

0 m 100 m 300m 2000 m FLSD0.005

Cd (mg/kg) 1.3 1.1 0.7 0.3 0.07

Cu (mg/kg) 28.6 26.9 21.4 12.6 1.0

Hg (mg/kg) 4.1 3.1 2.4 1.1 0.32

Pd (mg/kg) 1.3 1.3 1.0 0.3 0.12

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4.5.2 The Main Effects of Depth on Selected Heavy Metal Content of the Soil

The main effects of soil depth on selected heavy metal content shown in (Table 6) indicate that

irrespective of distance from the sewage site, there was significantly higher accumulation of

heavy metal at the top soil (0 – 40 cm). Heavy metal concentration significantly (P ʹ 0.05)

decreased in a definite pattern as soil depth interval increased from 0–40 cm to 80–120 cm. It was

observed that copper had the maximum concentration at each soil depth interval while cadmium

was the least at each interval.

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Table 6: Effects of depth on soil heavy metals distribution

Depth (cm) Cd ( mg/kg) Cu ( mg/kg) Hg ( mg/kg) Pb ( mg/kg)

0-40 1.1 26.4 3.2 1.3

40-80 1.0 25.9 1.5 1.1

80-120 0.5 14.8 0.3 0.5

FLSD 0.05 0.06 1.0 0.7 0.1

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4.5.3 The Simple Matrix of Distance and Depth on the Concentration of the Selected

Heavy Metal in Soils

The simple matrix of distance and depth on the concentration of the selected heavy metal in soil

are shown in Table 7. The result show that there was greater accumulation of heavy metals at

different soil depth of sewage disposal site distances (0, 100, and 300 m) when compared with the

value obtained from the control. There were significant interaction (P ʹ 0.05) effects of cadmium

concentration. The highest cadmium concentration of disposal site soil (1.84 kg/mg) was obtained

from 0 m (edge) distance at 0–40 cm soil depth while the lowest (0.14 kg/mg) was from 300 m

distance at 80 – 120 cm soil depth. The control (2000 m) varied inconsistently among the soil

depth. However, the other three heavy metals ( Cu, Hg and Pd) content of the disposal site gave

similar pattern as that of cadmium by decreasing significantly (P ʹ 0.05) in a definite pattern at 0

m distance with soil depth interval while the same heavy metals considerably varied at the soil

depth of the control. Similar trend was maintained at 100, 300 and 200 m. Irrespective of soil

depths and distance Cd, Cu, Hg, and Pd ranges from 0.11-1.84, 8.84-33.7, 0.9-4.7 and 0.29-1.7

mg/kg respectively. Copper had the highest concentration among the four heavy metals studied at

both the sewage soil and the control soil while lead was the lowest.

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Table 7: The mean simple matrix of distance and depth on the soil heavy metal content

Distance (m) Depth(cm) Cd ( mg/kg) Cu ( mg/kg) Hg ( mg/kg) Pb ( mg/kg)

0-40 1.84 33.7 4.7 1.70

0(edge) 40-80 1.41 30.5 4.6 1.40

80-120 0.75 20.6 2.9 0.9

0-40 1.59 30.9 3.5 1.8

100 40-80 1.06 26.6 4.4 1.6

80-120 0.67 19.9 1.3 1.7

0-40 0.59 27.8 3.2 1.40

300 40-80 0.25 24.6 3.0 1.30

80-120 0.24 9.9 0.9 0.30

0-40 0.2 14.6 1.5 0.23

2000 40-80 0.28 8.9 1.41 0.43

80-120 0.40 14.9 1.7 0.29

FLSD0.05 0.3 2.1 0.6 0.1

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4.6 Heavy Metal concentration in Plant

Table 8 show the main and interaction effects of the three factors considered (distance, plant and

plant parts) on heavy metal content of the soil. Generally the heavy metal concentration obtained

from the test plants decreased significantly (P ʹ 0.05)with increase in distance indicating high

accumulation of heavy metals in plants at the sewage areas compared to the control (2000 m).

4.6.1 Cadmium

There were significant (P ʹ 0.05) effect of distances on the cadmium concentration in plants at

both sewage site (0,100, and 300 m) and control (2000 m) The highest cadmium concentration

(1.34mg/kg) was obtained from the edge of the disposal site (Table 8) while the lowest was found

to be at the control distance (0.1mg/kg). Data presented in Table 8 also show that the differences

between cadmium content of plant (cassava, maize and pannicum) were significant (P ʹ 0.05).

Pannicum gave the maximum accumulation of cadmium (0.8mg/kg), while cassava recorded the

lowest concentration of Cd (0.6 mg/kg). Significant (P ʹ 0.05) differences were obtained among

plant part (leaf and root), with the root showing highest accumulation of cadmium.

4.6.2 Copper

Significant (P ʹ 0.05) differences were obtained among distances with respect to the

concentration of copper in plants. Table 8 shows that the highest concentration of copper (23.8

mg/kg) in plant was obtained at 0 m distance and the value consistently decreased through 300 m

distance to the control site (2000 m). As shown in Table 8, the copper content differed

significantly among cassava, maize and pannicum. Pannicum had the highest concentration of

copper while the lowest concentration was obtained from Cassava. The effects of plant part on the

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copper content were significant (P ʹ 0.05). The leave had higher (16.3mg/kg) accumulation of

copper than the root (15.9mg/kg).

4.6.3 Mercury

Analysis of variance (ANOVA) for the concentration of mercury reveals a significant (P ʹ 0.05)

effect on the plant due to distance. Maximum concentration of mercury was obtained at 0 m

distance (3.2 mg/kg) and the value decreased progressively through 300m distance, (1.7 mg/kg) of

the sewage site to the 2000 m distance (control) (0.8 mg/kg). However, the mercury contents in

plants (cassava maize and pannicum maximum) were significant (P ʹ 0.05). Pannicum maximum

had the maximum accumulation of the mercury content (2.3 mg/kg) while the lowest

concentration (1.8 mg/kg) was observed in cassava (Table 8). Table 8 reveals that mercury

concentration in plant parts (root and leaf) were also significant (P ʹ 0.05).

4.6.4 Lead

The results of effect of distance on the concentration of lead in plants were significant (P ʹ 0.05).

The concentration of lead in plant at 0 m (edge) was highest and decreased gradually through

100m (1.2 mg/kg), 300 m (1.0 mg/kg) and then to the control (0.4 mg/kg). The control (2000 m)

was about 3times lower than values obtained at each distance at the sewage disposal site (Table 8).

Cassava, maize and pannicum plant were significant (P ʹ 0.05). Pannicum had the highest

concentration of lead while maize plant was the least on lead concentration (Table 6). The leaf and

root was significant (P < 0.05) and the root recorded the highest concentration.

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Table 8: Mean effects of distance, plant and plant parts on heavy metal

accumulation

Cd ( mg/kg) Cu ( mg/kg) Hg ( mg/kg) Pb ( mg/kg)

Distance (m)

0 1.34 23.8 3.2 1.2

100 0.98 18.1 2.4 1.0

300 0.43 15.3 1.7 1.3

2000 0.1 7.3 0.8 0.4

FLSD 0.05 0.03 0.5 0.1 0.1

Plant

Cassava 0.6 14.3 1.8 0.9

Maize 0.7 15.1 2.0 0.8

Pannicum 0.8 18.9 2.3 1.1

FLSD 0.05 0.03 0.43 0.1 0.1

Plant part

Leaf of all plants 0.7 16.3 1.9 0.8

Root of all plants 0.8 15-9 2.2 1.1

FLSD0.05 0.1 0.4 0.1 0.1

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4.7 The Bioconcentration Factor (BCF) of Cassava

There were significant (P ʹ 0.05) effects of distance on the four heavy metals (Cd, Cu, Hg, and Pb). The

highest BCF value of the heavy metals was obtained at 0 m (edge) distance (Table 8) while the lowest was

found to be at the 2000 m (control). Data presented in Table 9 also show that the BCF of the leaf portion

were significant (P ʹ 0.05) among the four heavy metals, with 0 m (edge) recording the highest BCF

value while the control was the lowest. With exception of lead, the BCF value of the other three

heavy metals at the 2000 m (control site) appears to be less compared to the other distance at

sewage site (Table 9). Data on the table shows that Cu had the maximum accumulation in the leaf

rather than in the root of cassava plant. However, the result on table 9 reveals no hyper

accumulation of heavy metals in both root and leaf of cassava.

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Table 9: Bioconcentration factor (BCF) in root and leaf of cassava

Cd ( mg/kg) Cu ( mg/kg) Hg ( mg/kg) Pb ( mg/kg)

Root

0 m(Edge) 0.83 0.77 0.85 0.80

100 m 0.71 0.62 0.83 0.71

300 m 0.82 0.63 0.67 0.65

2 km(control) 0.36 0.57 0.66 0.80

FLSD 0.05 0.03 0.03 0.03 0.02

Leaf

0 m(Edge) 0.76 0.88 0.67 0.72

100 m 0.66 0.71 0.81 0.65

300 m 0.66 0.73 0.62 0.60

2 km(control) 0.28 0.52 0.60 0.55

FLSD 0.05 0.03 0.03 0.03 0.02

BioconcentrationFactor(BCF) = ������������� � ����� �� ����

������������� � ����� �� ����

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4.8 The Bioconcentration Factor (BCF) of Maize

The results of the effect of distance on the heavy metals were significant (P ʹ 0.05) (Table 10).

The BCF value of Cd, Cu, Hg and Pb had their maximum accumulation at both root and leaf of

maize at 0 m distance (edge) while the lowest accumulation of heavy metals in maize was at 2000

m (control) distance respectively (Table 9). The level of accumulation of heavy metals in maize

consistently decreased from 0 m (edge) through 300 m to the control (2000 m). The BCF value of

maize was higher in the root than in the leaf tissue of maize. Notably, there was no hyper

accumulation of heavy metal at both root and leaf of maize (Table13).

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Table 10: Bioconcentration factor in root and leaf of maize

Cd ( mg/kg) Cu ( mg/kg) Hg ( mg/kg) Pb ( mg/kg)

Root

0 m(Edge) 0.69 0.65 0.78 0.71

100 m 0.66 0.53 0.63 0.88

300 m 0.60 0.50 0.69 0.82

2 km(control) 0.32 0.46 0.53 0.84

FLSD 0.05 0.03 0.03 0.03 0.02

Leaf

0 m(Edge) 0.59 0.71 0.74 0.40

100 m 0.60 0.56 0.36 0.50

300 m 0.43 0.57 0.61 0.67

2 km(control) 0.20 0.50 0.39 0.60

FLSD 0.05 0.03 0.03 0.03 0.02

Bioconcentration Factor (BCF) = ������������� � ����� �� ����

������������� � ����� �� ����

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4.9 The Bioconcentration Factor (BCF) of Pannicum maximum

Significant (P ʹ 0.05) differences were obtained among heavy metals accumulation with respect

to distances at both roots and leaves of plant respectively. The result showed maximum

accumulation of cadmium, mercury and lead in the root than the leaf system of panncium

maximum plants at the sewage site (Table 11). The BCF value of Cd, Hg and Pb had their

maximum accumulation at both root and leaf of panncium maximum at 0 m distance, while the

lowest accumulation of heavy metals in pannicum maximum was at their respective 2000 m

(control) distance. Cadmium *had the BCF value of 1.00, but only in the root tissue of pannicum

maximum at 0 m distance.

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Table 11: Bioconcentration factor in root and leaf of pannicum maximum

Cd ( mg/kg) Cu ( mg/kg) Hg ( mg/kg) Pb ( mg/kg)

Root

0 m(Edge) 1.00 0.58 0.71 0.87

100 m 0.67 0.52 0.54 0.58

300 m 0.83 0.55 0.62 0.64

2 km(control) 0.14 0.44 0.67 0.60

FLSD 0.05 0.03 0.03 0.03 0.03

Leaf

0 m(Edge) 0.94 0.61 0.67 0.68

100 m 0.60 0.58 0.28 0.41

300 m 0.94 0.57 0.50 0.24

2 km(control) 0.40 0.46 0.61 0.54

FLSD 0.05 0.03 0.03 0.03 0.02

Bioconcentration Factor (BCF) = ������������� � ����� �� ����

������������� � ����� �� ����

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Table 12: Guideline for safe limits of heavy metals in soil and plant

Samples Standards Cd Cu Hg Pb

Soil (mg kg-1

) WHO/ FAO

commission

3000 – 6000 140000 23000 300000

Plant(mg kg-1

) WHO/ FAO

commission

200 40000 20000 – 30000 50000

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CHAPTER FIVE

DISCUSSION

5.1 Physicochemical Properties of the Soil

Most of the changes in soil chemical properties observed in this study are largely explained by

differences in distances away from the sewage pond and their corresponding soil depths. Close

distances to the sewage pond had an increased, exchangeable bases, soil organic matter, total

nitrogen, available phosphorous at the disposal site. These properties decreased as distance and

soil depth increased from 0 m to 2000 meters away from the pond.

The soil pH differed significantly among the three distances (0 m, 100 m 300 m) and three soil

depths. These values are expected as most of the observed increase in pH with increase in distance

and depth could be attributed to accumulation of organic acid generated during the process of

organic matter decomposition (Veerseh et al., 2003). Under condition of reduced oxygen,

decomposition would result in accumulation of more organic acid due to incomplete breakdown

of organic matter. The values obtained at the sewage site were however, lower on average when

compared to the value on the control. This may be attributed to the buffering effect of soil organic

matter against pH change in addition to the release of basic cation during the organic matter

decomposition (Oyedele et al., 2008).

The textural composition of the soil did not differ significantly with distance and among the three

depths. This is expected as soil texture is mainly inherited from soil forming parent materials. The

soil percentage of sand and silt generally decreased with increase in depth while the clay content

increased down the profile (Kadeba, 1978).

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Higher soil OM level was typically observed in the soils closer to the sewage site. This higher soil

OM content at the edge (0 meter distance) was associated with sewage pond seepage into the soil,

leading to more organic matter accumulation at 0m distance relative to other two distances. This

confirms an earlier indication by (Asadu et al., 2008, Udom et al., 2000) that sewage sludge

effluents are utilized for irrigation purposes and also increases soil fertility as well. The soil

organic matter content of the control (2000 m) was lower compared to the study site. Higher

organic matter content of the sewage site might be due to sewage waste application (Bhati and

Singh 2005). In general the suitability of soil for receiving waste water without deterioration

varies widely, depending on their infiltration capacity, permeability, CEC, phosphorous

adsorption capacity, texture, structure and type of clay minerals(Ivan and Ear)1972. The organic

matter contents of the sub soil plays important role in the absorption reaction in the soil thereby

preventing pollutants from reaching ground water (Alloway and Aryes 1997).

Like the organic matter content total nitrogen content showed significant differences among the

four distances and three soil depths. Increased soil nitrogen content was expected to result from

the sewage sludge site. This increase was evident on crops but appeared to decline slightly as

distance and depth increases. This decline in soil nitrogen content apparently resulted from

reduction of sewage sludge as we move away from the disposal site,this were in agreement with

the findings of (Gelsomins et al., 2006) Matovi et al., 2005 and Weber et al., 2007. The high

nitrogen content in the soils of sewage sludge could sometimes be detrimental to crop production,

particularly leguminous crops in view of interference in plants absorption of nutrients (Asadu et

al., 2008).

Exchangeable bases (Sodium, Potassium, Calcium and Magnesium) decreased as distance and

depth increased in the study site. These high concentrations of basic cations at 0 m and top soil

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was apparently because the cations were concentrated in the organic matter rich surface soil that is

mixed with waste materials at different stages of decomposition which continuously released the

cation (Oyedele et al., 2008).

The significantly higher concentration of K at the edge (0 m distance) and top soil (0–40 cm) at

the sewage site may be explained by the release of K from the sewage sludge.

The top soil (0 – 40 cm) at the sewage sludge site had significantly higher concentration of Ca at

all distances this might be due to high contents of sewage sludge and surface application of

sewage sludge at the study site.

The significant concentration of Mg at all distance and depth at the study site was consistent with

the idea that the main source of Mg is the exchangeable Mg found in the clay humus complex

(Brady and Weil, 2004) which was believed to be influenced by sewage sludge.

As expected the exchangeable Ca was higher than exchangeable Mg apparently as a result of high

level Ca in sewage sludge. Sewage sludge inputs are not only important for agricultural

productivity, but also for the supply of some internal nutrient elements.

Generally, the results show higher content of exchangeable base at sewage site relative to the

control site. Exchangeable bases also decreased consistently with distance and depth. These

results agree with some of the earlier work comparing sewage sludge soil and unamended soil

(Mbagwu et al., 1991, Anikwe and Nwobodo 2002, Asadu et al., 2008).

The concentration of cation exchange capacity in the soil differed significantly among three

different distances and three different depths at sewage site. The effect of the CEC was more

pronounced at 0 – meter distance and 0 - 40cm depth in sewage site. The decrease in CEC as both

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distance and depth increased might have resulted from differences in soil texture and organic

matter. High soil organic matter accounts for great percentage of the total cation in exchange site

at the sewage site. The higher CEC at the sewage site confirms the findings of Soon 1981, Asadu

and Nweke 1999, and Asadu et al.,(2008), that sewage sludge increases the CEC and organic

matter of soil. This also confirms the earlier indication by Udom et al., (2000) that the sewage soil

was more fertile than the control soil.

Phosphorous shows a significantly higher concentration at the three distances and three depths in

the soils sewage site, with P concentration decreasing as distance and depth increases. The

difference in the mineralogical composition of soil may influence the changes in concentration of

available phosphorous. With the edge (0m distance) having more of sewage sludge its ability to

fix P may be more than soil of other corresponding distances. This may explain the higher P

content observed in sewage site distances (0 m, 100 m and 300 m) compared to 2000m of the

control site. The study by Gelsomino, et al., (2006) also found P increased in soil with high

organic amendment.

The high concentration of P at 40-80 cm depth at the sewage site is in agreement with earlier

finding by Asadu et al., 2008 that there was greater P mobility in the sewage soil indicating

possible leaching into the soil where it became more fixed. Phosphorous though beneficial to

crop, an excessive content of mobile P is eventually unfavourable because it might represent a risk

factor in water eutrophication (Karboulewsley 2002, Penn and Slino, 2002).The study also found

that there was threefold increase in P concentration in soils of the sewage site relative to the soils

of the control. This may be due to higher Fe content associated with the control soil may result in

the formation of insoluble phosphate further reducing P available Maguire et al., (2000).

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Exchangeable acidity of 0 meter distance have the lowest acidity measurement at the disposal site,

there was a significant increase in soil acidity as both distance and depth increase. The 0-meter

distance producing the lowest measurement of acidity may be explained by the larger

concentration of base cations and organic matter that are present in the sewage sludge such as

calcium, resulting in a nutrient upliftment which increased basic cations in the soil and decreased

acid cations, thereby decreasing the soil acidity of disposal site.

Furthermore, a low acidic environment will decrease the leaching of Ca because solubility of

aluminium and iron decreases, thus competing with acid cations for the binding sites. At the

control site the acidity decrease with increase in depth. This may be due to intense decomposition

taking place in the control site may possibly increase the release of H+ and Al

3+ ion from the

decomposing plant matter. These ions tend to kick base cations off the binding site, thus

increasing the acid cations on the binding sites causing the soil acidity to increase at the control

site.

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5.2 Heavy metals in soil

Soil is a dynamic and complex system where any changes in its physiochemical properties would

severely alter the fate of heavy metals within its body. Sewage sludge due to its heavy metal

content might be a threat to. the soil and the environment, if it is used for a long time (Epstein,

2003, Gasco et al., 2005). In general, the suitability of the soils for receiving waste without

deterioration varies widely depending on their infiltration capacity, permeability, Cation exchange

capacities, phosphorus adsorption capacity, texture, structure and type of clay minerals.

Using approximately 2000 m distance as a baseline for comparison, over 40 year disposal of

sewage sludge on to the soil of the sewage site resulted in an increment of the soil concentration

heavy metal in the different soil depth intervals, compared with soil depth intervals at the control

(2000 m).

The sequence of heavy metals in soil sample from sewage sludge site was in order Cu > Hg ʹ Cd

ʹ Pb. The concentration of heavy metal show progressive variations which might be ascribe to

the variation in heavy metals sources and the quantity of heavy metals in sewage sludge. In the

present study, concentration of heavy metal decreased significantly with the increase in distances

and soil depth at sewage sludge site. These results are in agreement with the findings obtained by

(Yada et al., 2002, Mascoid Tabari 2008). Since the surface is rich in heavy metal than the

underlying layer greater accumulation in the top soil is probably due to soil texture, low mobility

of heavy metal in soil (Afonia et al., 1998) and surface application of sewage sludge, (Asadu et

al, 2008).

The inconsistent pattern in the variation of heavy metal content with soil depths at the control

(2000 m) was in contrast with the consistent trend in the sewage site( 0 m 100 m 300

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m),suggesting the presence of discontinuities within sewage site due to low mobility of heavy

metal in soil.

The comparison of concentration of Cu, Cd, Hg and Pb in soil with WHO/FAO standard (Table

12) shows that they are below safe limits of heavy metals in soils. Continuous cultivation and

regular absorption by plants possibly keep the concentration of heavy metals in the soil within

safe limit at sewage site. Hence, the proximity of the sewage site to the cultivated land does not at

the present pose any threat to the soil.

Furthermore, since soil macro organisms and their activities are crucial to the maintenance of soil

fertility, there is considerable concern that these heavy metals could have permanent adverse

effect on soil quality and crop production. The solubility of the metals in soil and ground water is

predominantly controlled by pH, organic matter and CEC. From this present study heavy metal

mobility decreases with increase in soil pH. This was in agreement with the; Smith and Giller

(1992). The result shows that the soils of the study site are slightly acidic which favours the

precipitation and mobilization (Battachry et al., 2002).

The seepage of these heavy metals through the soil of sewage site can infiltrate directly through

unsaturated zones to cause severe pollution problems. Their presence in ground water can cause a

long term health risk to humans through food chain (Earth et al., 2000 Ogbonna et al., 2006).

Although metals are essential to plant, at high concentration they become toxic and present

different problems to soil micro organism because they cause oxidative stress by formation of free

radicals. They can also replace essential metals in pigment or enzymes, thus disrupting their

function (Henry 2000) and may render the land unsuitable for plant growth and destroy the

biodiversity.

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However, it was suggested that soil contamination may be considered high when concentrations

of an element in soil were two to three times greater than the average background level. There is

an indication that this metal are higher in sewage site, which was also reflected in the low level of

these metals obtained from the control. The degree of heavy metal contamination may be

considered to be high at the sewage site.

Therefore, the soil of sewage soil may be considered contaminated based on the fact that heavy

metal content in all control soil in this study was low. Although the mean concentration of the

heavy metal obtain from the sewage site fall within the acceptable safe limits proposed

WHO/FAO standard. Thus, sewage sludge seepage and anthropogenic input of these heavy metals

seemed to be less pronounced in the area of investigation.

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5.3 Heavy Metal in Plant

There was a progressive decrease in heavy metal content of selected plants at the disposal site as

the distance increased from edge (0 m) to control (2000 m). The low levels of heavy metals in the

test plants at the control (2000 m) might be due to low mobility of heavy metals. The high

concentration of Cu in leaves of the selected plants as compared with the roots is not consistent

with literature (Romana et al., 2005). The high concentration of Cu in the leaves of plant in this

study might be partly due to surface irrigation with the sewage water and partly to the fact that

copper was the most abundant metal in the soil at the three different distances in the sewage site.

With exception of Cu the roots have higher concentration of heavy metals than the leaves.

Ademoroti (1966) reported that plants accumulated considerable amount of heavy metals

especially Pb, Cu, and Zn in the root than the leaves. The concentration of heavy metals in all

plant sample analyze were lower than FAO/WHO guide lines values (Table 12). Liu, et al. 2005

and Sharma et al., 2007 demonstrates that plant grown on waste water irrigated soil are

contaminated with heavy metal and pose health concerns.

This study has shown little accumulation of Cd and Pb. This may be due to the reason that Cd and

Pb poses some toxic effect on plant (Anderson et al., 2004). Another possible explanation would

be unavailability of Cd and Pb due to high affinity of these metals to organic matter (Merrit and

Erich 2003, Migam et al., 2001, Strawn and Sparks 2000). The overall low concentration of the

Pb and Cd was observed in the both root and leaf of test plants.

The absorbance and accumulation of heavy metals in the plant tissue depends on metal

concentration and chemical forms in soil (Shen et al. 2000). Very little amount of lead was

extracted from the soil. These factor involved in the phyto-availability of this metal are organic

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matter, soil pH, plant root, and other soil condition (Zimdahl and Hassett, 1997). The limited

potentials of Phyto availability were due to low soil mobility and little tendency for the uptake Pb

into the root (Lasat, 2002) (low bio availability in the root).

The unconventional behaviour of Pb uptake is well renowned (Reeves and Brooks, 1983). It may

be due to this reason that plant respond differently to soil Pb as compared to other metal, (Huang

et al, 1997). Some other reason might be the high susceptibility of lead to change into sorption

form in soil matrix. Moreover root membrane barrier cannot be overlooked because mechanism of

Pb transport from soil to root tissue is not clear Blaylock et al. (1997).

The concentration of the heavy metal in the root and leaves of selected plant differed significantly

at different distance among different test plant and plant parts. Marked different in heavy metal

content may be due increased seepage and irrigation with water from the oxidation pond. This

result was in agreement with Singh and Bhati (2005) and Aghabarati et al. (2003) where

substantial greater concentration of these heavy metals were observed in the plants at the disposal

site and plants irrigated with sewage sludge compared to the plant at control site. However, the

presence sewage sludge and irrigation with sewage waste water did not result in toxicity of the

test plants.

Further more, in the present study many soil factors such as pH, organic matter interacted to

impact in the uptake of heavy metal by plant. The acidic range of soil is known to increase the

mobilization of heavy metals, thus increasing their uptake. The field data also support that soil pH

was acidic. The presence of organic matter has been reported to increase the uptake of Cu, Pb Cd

and Zn in the wheat Plant (Rupa et al., 2003). Earlier study on the site have it that the build up of

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86

these metals to critical level can be phyto toxic and may result in reduced plant growth and or

increase within the food chain (Asadu et al ., 2008)

5.4 The bioconcentration factor (BCF)

The bio concentration factor (BCF) which is the relationship between total metal content in plant

and soil shown in table 9, 10 and 11 had a significant effect among distances and among plants

parts. The BCF recorded in this study is an indication of the potential of heavy metal in the

sewage site to be transferred into the food chain through the consumption of edible plant on the

site by either animal or man. Variation in bioconcentration factor among different root and leafs

of plant may be attributed to differences in the concentration of heavy metal in the soil and

differences in element uptake by different plant (Cui et al., 2004, Zheng et al., 2007).

Notably, high accumulation of metal in the root than in the leaf was consistent with other work

(Bidar et al., 2007; Margiues et al., 2009). Metal in plant did not show any hyper accumulation

with those of soil. The BCF show that there is a higher accumulation of Cd and Pb in root of

Panincum maximum plant than in the leaves. The high concentration of heavy metal in the root of

Pannicum maximum was in agreement with findings of Yin et al. 2009 and Zupan et al. 2009 that

the plants that are not deep rooted are highly affected by the heavy metals because these metals

remain in the top soils and do not leached deeper in to soil.

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CHAPTER SIX

6.0 SUMMARY AND CONCLUSION

The study at the University of Nigeria Nsukka disposal site found that cation exchange capacity

pH, organic matter content, total N, P, K, Ca and Mg were increased in soil around the sewage

sludge site. The extents of improvement were highly significant with distance and depth. The

concentration of the soil properties was pronounced at the edge (0 m distance) and decreased with

distance through 100 m to 300m.There was higher concentration of these properties at 0 - 40 cm

depth and decreased gradually with depth, with the exceptions of soil pH that increased with soil

depth. The mobility of these soil properties was pronounced at the sewage site than the control

(2000 m).

The level of soil accumulation of heavy metal was high at the sewage site due to sewage water

free seepage in to the soil and probably due to irrigation with water from the oxidation pond

within this area. The level of heavy metal increased significantly (P ʹ 0.05)with distance and

depth. However, level of heavy metal in the soil was lower than those recommended by

WHO/FAO joint safe limit. Hence has not reached hazardous concentration even though their

concentration in the soil of the sewage site has increased about twice compared with the control.

Plants grown around the sewage site have increased heavy metal content. Heavy metal

accumulation in plant decreased with distance. The presence of heavy metals in plant has been

shown to be influenced by sewage pond around the sewage site. Among the root and leave tissues

of plant studied, the root has highest concentration of heavy metals compared with the leaves. The

concentrations of heavy metal in both root and leaves of plant are below WHO/FAO guide line

values.

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Therefore it follows that, free seepage and anthropogenic sources of heavy metal increase the

heavy metal content of the sewage sludge. Toxic heavy metals accumulate faster in the soil and

plant around sewage sludge due to their proximities to sewage pond. However, with an increase in

concentration of soil organic matter, soil exchangeable bases, movement and translocation of

heavy metals in soil decreased while, with a decrease in soil organic matter (Bounded with soil

particles) and pH as well, their mobility increase. The low mobility of metals in the sewage soils

may be related to high Ca and organic matter content. Furthermore increased mobilization of these

elements in the sewage may be related to the lower organic matter, clay, and Ca content of the

soil.

Conclusions drawn from this study are that;

� The University of Nigeria Nsukka sewage disposal site resulted in an increased

concentrations cation exchange capacity, pH, organic matter content, total N, P, K, Ca and

Mg in soil around the sewage sludge site.

� The study has also revealed presence of Cd, Cu, Hg, and Pb in the soils around sewage

sludge site but they were below the maximum allowable limit.

� The mobility of heavy metals (Cd, Cu, Hg, and Pb) from soil to leaves suggesting that all

these metals were mobile from soil to plant components

� Heavy metal concentrations varied among the tested crop/plant, which reflect the

differences in their uptake capabilities and their further translocation to the shoot portion

of the plant.

� The level of heavy metal in both crop/plant will not place the consumer of this crop/plant

grown within the vicinity of the sewage site at health risk with time.

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� The bioconcentration factor at both root and leaf tissues of crop plant did not show any

abnormal accumulation of the heavy metal at the sewage site.

It is therefore suggested that the regular monitoring of heavy metal in soil and plant grown around

sewage sites is essential since heavy metal is considered a serious agricultural concern.

.

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