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Page 1: Organic arsenic removal from drinking water

Organic arsenic removal from drinking water

O.S. Thirunavukkarasu a, T. Viraraghavan a,*, K.S. Subramanian b, S. Tanjore c

a Environmental Systems Engineering, Faculty of Engineering, University of Regina, Regina, Sask., Canada S4S 0A2b Product Safety Bureau, Health Canada, Ottawa, Ont., Canada K1A 0K9

c Waterworks Technologies, Calgary, Alta., Canada T2N 1J7

Received 11 May 2001; received in revised form 6 March 2002; accepted 30 April 2002

Abstract

Arsenic occurs in both inorganic and organic forms in water. Although various methods have been adopted to remove inorganic

species of arsenic from drinking water, not much emphasis has been given to the removal of organic species of arsenic. In the present

study column studies were conducted using manganese greensand (MGS), iron oxide-coated sand (IOCS-1 and IOCS-2) and ion

exchange resin in Fe3þ form, to examine the removal of organic arsenic (dimethylarsinate) spiked to required concentrations in tap

water. Batch studies were conducted with IOCS-2, and the results showed that the organic arsenic adsorption capacity was 8 lg/gIOCS-2. Higher bed volumes (585 BV) and high arsenic removal capacity (5.7 lg/cm3) were achieved by the ion exchange resinamong all the media studied. Poor performance was observed with MGS and IOCS-1.

� 2002 Elsevier Science Ltd. All rights reserved.

Keywords: Adsorption; Batch studies; Column studies; Filtration; Ion exchange resin; Iron oxide-coated sand; Manganese greensand; Organic

arsenic species; Water Treatment

1. Introduction

Extensive arsenic contamination of surface and

groundwater has been reported in many parts of the

world. The possible long term effects and the risks

associated with the ingestion of arsenic contaminated

water have compelled the regulatory agencies to pro-

mulgate a lower standard for arsenic in drinking water.

The World Health Organization (WHO) standard for

arsenic is 10 lg/l. The maximum acceptable concentra-tion for arsenic is 25 lg/l in Canada; recently the UnitedStates Environmental Protection Agency (USEPA)

adopted a new arsenic standard for drinking water at 10

lg/l (USEPA, 2001). The existing arsenic standard fordrinking water in Australia is 7 lg/l, whereas EuropeanUnion has stipulated an arsenic standard of 10 lg/l(Yamamura, 2001).

Arsenic, a common toxic element, is present in bothinorganic and organic forms in water. Arsenic contam-

ination of surface water is mainly due to weathering of

rocks, geochemical reactions, contact of arsenic bearing

sediments with aquifer, industrial waste discharges,

volcanic emissions, fertilizers, and mining and smeltingoperations. Though arsenic contamination of ground-

water in Taiwan was reported about three decades ago

(Tseng et al., 1968), the general awareness and attention

of the public has been focussed recently because of

similar reports of contamination of surface and sub

surface waters by As from many other regions in the

world, such as Bangladesh, Mexico, China, Chile, USA,

Canada and India (Burkel & Stoll, 1999; Cebrian,Albores, Aguilar, & Blakely, 1983; Dhar, Biswas, &

Samanta, 1997; Karim, 2000; Koch et al., 1999;

Meranger & Subramanian, 1984).

Arsenic occurs in several different species depending

upon the pH and oxidation potential of the water. The

four arsenic species commonly reported are arsenite

[As(III)], arsenate [As(V)], monomethylarsonate (MMA)

and dimethylarsinate (DMA). Despite the fact that in-organic species are predominant in natural waters, the

presence of MMA and DMA has also been reported

(Anderson & Bruland, 1991; Andreae, 1977; Banerjee,

Helwick, & Gupta, 1999; Braman & Foreback, 1973;

Del Razo, Arellano, & Cebrian, 1990; Chen, Yeh, Yang,

& Lin, 1995).

In the studies conducted by Del Razo et al. (1990), one

of the water samples collected from the wells in the

*Corresponding author. Tel.: +1-306-585-4094; Fax:+1-306-585-

4855.

E-mail address: [email protected] (T. Viraraghavan).

1462-0758/02/$ - see front matter � 2002 Elsevier Science Ltd. All rights reserved.PII: S1462-0758 (02 )00029-8

Urban Water 4 (2002) 415–421

www.elsevier.com/locate/urbwat

Page 2: Organic arsenic removal from drinking water

Lagunera Region, Northern Mexico had a high DMA

concentration of 20 lg/l. The results of studies by Chenet al. (1995) showed that most of the water samples from

the wells in northeast and northwest Taiwan (endemic

area for blackfoot disease) had a high DMA concen-

tration of 7 lg/l. Anderson and Bruland (1991) reportedthat the methylated species (dominant species was

DMA) comprised on average of 24% of the total dis-solved As in surface waters of the various lakes examined

in California, USA, with the exception of Mono and

Pyramid lakes. In recent studies by Banerjee et al. (1999),

the concentration of organic arsenic species was 10% of

the total arsenic concentration in the groundwater sam-

ples from a superfund site in the northeastern United

States, where the total As concentration was 30 mg/l.

Upon ingestion of inorganic arsenicals, it is methy-lated in the human body and the metabolites of ingested

arsenic eliminated by the kidney and excreted in urine

within 1–3 days (Crecelius, 1977; Vahter, 1994). DMA is

the predominant metabolite excreted in urine and faeces

of animals and humans exposed to inorganic arsenic

(Styblo, Delnomdedieu, Hughes, & Thomas, 1995).

DMA appears to be a potent clastogenic agent causing

gene amplification (Endo, Kuroda, Okamoto, & Horig-uchi, 1992). Yamamoto et al. (1995) showed that chronic

exposure to DMA enhanced tumor development in the

kidney, liver and urinary bladder of F 344 rats. The

toxicity of different arsenic species varies in the order:

arsenite > arsenate� monomethylarsonate ðMMAÞ >dimethylarsinate ðDMAÞ. Inorganic arsenic species areabout 10 to 60 times more toxic than organic arsenic

compounds (MMA and DMA). Methylation of inor-ganic arsenic in the body is a detoxification process,

which reduces the affinity of the compounds for tissues

(Jain & Ali, 2000; Lewis & Tatken, 1978; Penrose, 1974).

The LD50 values for various arsenic species are shown in

Table 1.

Recent research (Kenyon & Hughes, 2001; Petrick,

Jagadish, Mash, & Aposhian, 2001) pointed out, how-

ever, that organic arsenic species are more toxic than

initially thought. Therefore more research is needed for

an estimation of the global arsenic toxicity based onspeciation. It is anticipated that the USEPA may ap-

proach the wide range in arsenic species toxicity as it is

done with mercury, whereby the more toxic species are

the most closely regulated. It is unlikely that organoar-

senic species will be as tightly regulated unless they are

in a high concentration (Miller, Norman, & Frisch,

2000; USEPA (1999, 2000)). Only a few studies have

been conducted to remove organic arsenic from drink-ing water. Ghosh and Yuan (1987) reported that

the adsorption behaviour of both monomethylarsonate

(MMA) and dimethylarsinate (DMA) onto activated

alumina were similar to that of arsenate. Vogels and

Johnson (1998), in their studies with ferrous and ferrate

ions reported that better removal of MMA than DMA

was obtained. In the present study, column studies were

conducted using manganese greensand (MGS) to ex-amine the removal of organic arsenic (DMA) spiked in

tap water. Further, studies with iron oxide-coated sand

(IOCS) prepared by two different methods (IOCS-1 and

IOCS-2) and ion exchange (Amberlite IR-120 resin ac-

tivated with ferric ions) resin were also conducted to

remove organic arsenic (DMA) spiked in tap water, and

the results were compared with the data from the MGS

studies.

2. Materials and methods

Tap water from the City of Regina, Saskatchewan,

Canada was used as the water source for all the exper-

iments. The pH of the tap water was 7.6, and not ad-justed for any of the experiments. In the studies, tap

water was supplemented with the required concentra-

tions of DMA. DMA stock solution (1000 lg/l) was

Nomenclature

C equilibrium concentration (lg/l)Ce effluent adsorbate concentration (lg/l)C0 influent adsorbate concentration (lg/l)k Thomas rate constant (ml/min lg)x mass of solute adsorbed (lg)m mass of adsorbent (g)

K the Freundlich constant indicative of the ad-

sorption capacity of the adsorbent (l/lg)

n experimental constant indicative of the ad-

sorption intensity of the adsorbent

Q volumetric flow rate (ml/min)

q0 maximum solid phase concentration (lg/g)V throughput volume (ml) andr regression coefficient

Table 1

The LD50 values for arsenic species

Arsenic species LD50 (mg/kg) Reference

DMA 1200 Penrose, 1974; Lewis and Tat-

ken, 1978; Jain and Ali, 2000.

As(V) 14

As(III) 4.5

416 O.S. Thirunavukkarasu et al. / Urban Water 4 (2002) 415–421

Page 3: Organic arsenic removal from drinking water

prepared by dissolving 1.1678 g of cacodylic acid(C2H6AsO2Na, Sigma Chemical, Ontario) in 1 l distilled

water and preserved with 0.5% nitric acid (trace metal

grade). The required working standards were prepared

daily from the stock solution.

MGS manufactured by Inversand company, New

Jersey, USA, was purchased from Watergroup Canada

Ltd., Regina, and used in the column studies. MGS was

conditioned prior to the column studies and the detailsare available elsewhere (Viraraghavan, Subramanian,

& Aruldoss, 1999). Amberlite IR-120 cation exchange

resin manufactured by Rohm and Haas Company,

Pennsylvania, USA, was purchased from Watergroup

Canada Ltd., Regina. The resin was activated with Fe3þ

ions and used in the studies. The activation of the resin

was carried out by mixing 300 g of resin in 0.1M

FeCl3 � 7H2O solution using a paddle mixer for 4 h.The red flint sand used in the preparation of IOCS

was purchased from Watergroup Canada Ltd., Regina.

IOCS-1 was prepared by adding 40 ml of 1M FeCl3 �H2O solution per 500 g of sand and the mixture was

allowed to remain in the column for 12 h. The column

was backwashed for a short duration before starting

the run. In the second method IOCS-2 was prepared as

per Benjamin, Sletten, Bailey, and Bennet (1996) withmodifications. The sand was sieved to a geometric mean

size of 0.6–0.8 mm, acid washed (pH 1; 24 h), rinsed with

distilled water three times and dried at 110 �C for 20 hbefore use. IOCS-2 was prepared in two steps. In step 1,

the solution containing a mixture of 80 ml of 2M

Fe(NO3)3 � 9H2O and 1 ml of 10 M NaOH was pouredover 200 g dried sand placed in a heat resistant dish, and

the mixture was heated at an elevated temperature. Thenthe sand was cooled and washed with distilled water.

In step 2, the solution containing the same mixture of

Fe(NO3)3 � 9H2O and NaOH was poured over 100 g ofthe coated sand from step 1, and heated for a desired

duration. Further the coated sand from the second step

was subjected to five more drying cycles, which consisted

of drying at 110 �C for 4 h followed by 20 h at roomtemperature. The coated sand was stored in cappedbottles.

Batch studies were conducted only with IOCS-2 at

the room temperature of 22� 1 �C using a portablebenchtop C2 classic platform shaker with digital display

on the control panel. In the experiments, the respective

mass of IOCS-2 was transferred to 250 ml conical flasks

containing 100 ml of tap water spiked with DMA. The

flasks were sealed with parafilm and the samples wereshaken at 175 rpm. After completion of the contact

time, the samples from each flask were decanted and

analyzed for residual DMA.

In the column studies with MGS, IOCS-1 and resin, a

column of 10 cm in diameter and 180 cm high was used.

Tap water spiked with the required concentration of

DMA was pumped into the column using a submersible

pump. In the case of studies with MGS and IOCS-1, thepacked volume of the media in the column was 4681 ml

and the empty bed contact time (EBCT) was 5.64 min.

The flow rate to the column was kept at 0.83 l/min (117

m3 m2 d�1). In the studies with ion exchange resins in

Fe3þ form, the flow rate, packed volume, and the EBCT

were 1.23 l/min (176 m3 m2/d), 4182 ml, and 3.4 min

respectively. The column study with IOCS-2 was con-

ducted in a column of size 16 mm diameter and 400 mmlong with suitable stoppers. A mesh was placed inside

the stopper to prevent the escape of adsorbent during

filtration. The flow rate, packed volume, and EBCT

were 17.5 ml/min (96 m3 m2/d), 23 ml, and 2.64 min

respectively. Samples were collected at regular intervals

and analyzed for residual DMA concentration.

The instrument used in this study for the measurement

of arsenic was Varian type SpectrAA––600 ZeemanGFAAS equipped with GTA 100––graphite tube atom-

izer and PSD––100 programmable sample dispenser.

Pyrolytically coated notched partition graphite tubes

(Varian Canada Inc., Toronto) were used in the experi-

ments, and argon gas of ultrahigh purity (99.995%;

Praxair Products Inc., Ontario) was used to sheath the

atomizer and to purge internally. Arsenic hollow cath-

ode lamp (Varian Canada Inc., Toronto) was usedat a wavelength of 193.7 nm with a slit width of 0.5

nm. Nickel nitrate solution at 50 mg/l or palladium-

ð1500 lg=lÞ þmagnesium nitrate (1000 lg/l) solutionwas used as matrix modifiers for calibration.

3. Results and discussion

3.1. Batch studies

Batch kinetic and isotherm studies were conducted

with IOCS-2, in which the initial DMA concentration inthe tap water was 100 lg/l. The results of the kineticstudies showed that the minimum concentration of

DMA achieved was 30.82 lg/l (a removal of 69.18%) ata contact time of 7 h. Ho’s pseudo second order model

(Ho, Wase, & Forster, 1996), shown below was used to

analyze the adsorption data obtained in the kinetic

studies:

tq¼ 1

2kq2eþ tqe

ð1Þ

where k is the rate constant for adsorption (g/lgmin);qe, the amount of adsorbate at equilibrium (lg/g); q, theamount of adsorbate at any time t (lg/g). The aboveequation is rearranged to

q ¼ 2kq2e t1þ 2kqet

ð2Þ

The experimental results from the kinetic studies were

subjected to non-linear analysis using Ho’s model, with

O.S. Thirunavukkarasu et al. / Urban Water 4 (2002) 415–421 417

Page 4: Organic arsenic removal from drinking water

‘Statistica for Windows’ (release 5.1, ’97 edition) soft-ware using a Quasi-Newton method. The estimated

modelled values obtained with time are shown in Fig. 1.

The amount of adsorbate at equilibrium qe was esti-mated at 14.61 lg/g. The correlation coefficient (r) forthe plot was 0.99 representing a good correlation to the

observed data, and the model was found to provide a

realistic description of adsorption kinetics of arsenic

(DMA). Isotherm studies were conducted by varying themass of IOCS-2 from 0.1 to 0.9 g, and the equilibrium

time of 7 h from the kinetic studies was kept as the

contact time. A maximum DMA removal of 73.6% (23.4

lg/l) was achieved with 0.9 g of sand. The removal ofDMA (73.6%) obtained in this study was higher than

that (a maximum of 28%) obtained by Vogels and

Johnson (1998) in their studies with ferrous and ferrate

ions.The Freundlich isotherm was used to describe ad-

sorption. The Freundlich isotherm describes equilibrium

on heterogeneous surfaces and is widely recommended

due to its accuracy. It gives more accurate results than

the Langmuir isotherm for a wide variety of heteroge-

neous adsorption systems (Al-Duri, 1996). The isotherm

equation is as follows

xm

¼ KC1=n ð3Þ

where x is the mass of the solute adsorbed at any time t

(lg); m, the mass of adsorbent (g); K, n the experimentalconstant indicative of the adsorption capacity and in-

tensity of the adsorbent, and C, the equilibrium con-

centration (lg/l).The experimental results of isotherm studies were

subjected to non-linear analysis, and the estimated

modelled values were plotted with the concentration of

DMA remaining in solution (Fig. 2). The Freundlich

constants ‘K’ and ‘n’ were estimated at 0.07, and 0.71respectively. The low K value ð0:07 < 1Þ and high 1=nvalue suggested that the arsenic adsorption capacity was

low. A correlation coefficient ‘r’ of 0.94 for the Fre-

undlich isotherm showed that the arsenic adsorption can

be best described by the Freundlich isotherm. The ad-

sorption capacity of IOCS-2 for arsenic (DMA) removalat a residual concentration of 23.4 lg/l was estimated as8 lg/g.

3.2. Column studies

The initial DMA concentration was kept at 100 lg/lfor all the adsorbents used in the column studies. Fixed

bed adsorption columns operated in the downflow modemay perform two functions, namely adsorption and fil-

tration. Breakthrough or exhaustion curves were devel-

oped from the column data by plotting the ratio of

Ce=C0 with the volume of water processed. Variousmathematical models have been developed to predict the

dynamic behavior of the column; the model developed

by Thomas (1948), which is used in the design of fixed

bed adsorption systems is as shown below (Reynolds &Richards, 1996):

CeC0

¼ 1

1þ exp kQ q0m� C0Vð Þ

h i ð4Þ

where Ce is the effluent adsorbate concentration (lg/l);C0, the influent adsorbate concentration (lg/l); k, theThomas rate constant (l/min lg); q0, the maximum solidphase concentration of the solute (lg/g); m, the mass ofthe adsorbent (g); V , the throughput volume (ml); andQ, the volumetric flow rate (ml/min).The results of the column tests were analyzed using

the Thomas model, and the estimated modelled values

of Ce=C0 were compared with the observed values. Theseare shown in Figs. 3 and 4. The results of column studies

are summarized in Table 2. The results showed that

studies with ion exchange resin was the only treatment

method effective in reducing DMA to a level below thebreakthrough concentration of 10 lg/l ðCe=C0 ¼ 0:1Þ.The column filled with the resin continued to remove

DMA below 10 lg/l for a period of six and a half hours.

Fig. 1. Arsenic (DMA) removal in the kinetic studies.Fig. 2. Isotherm plot for arsenic (DMA) removal using IOCS-2.

418 O.S. Thirunavukkarasu et al. / Urban Water 4 (2002) 415–421

Page 5: Organic arsenic removal from drinking water

In the case of DMA removal with the resin, 585 bed

volumes achieved <25 lg/l residual DMA, and the over-all removal capacity (5.7 lg/cm3) was highest among allother media used. However the maximum solid phase

arsenic concentration q0 (64.8 lg/g) estimated from theThomas model for IOCS-2 was high compared to the

other media used. Increase in the mass of the adsorbent(IOCS-2) or reduction of flow rate to the column might

have enhanced DMA removal in the case of IOCS-2.

The results of kinetic studies using IOCS-2 (Vira-

raghavan, Thirunavukkarasu, & Subramanian, 2000) to

remove inorganic arsenic species [As(III) and As(V)] of

arsenic showed that 85–90% arsenic was removed in theinitial phase (1 h) of contact, where the initial concen-

trations of arsenite and arsenate were 100 lg/l; morethan 95% removal was obtained for both As(III) and

As(V) at a pH of 7.6 after six hours of contact. Con-

tinuous column studies were conducted at the University

of Regina, Canada with IOCS-2 for the removal of

inorganic forms of arsenic from drinking water, and

the results were encouraging (Thirunavukkarasu, Vira-raghavan, & Subramanian, 2002). Since the concentra-

tions of organic arsenic present in natural waters are less

compared to inorganic forms (Anderson & Bruland,

1991), it is anticipated that IOCS-2 will be able to re-

move the DMA present in natural waters along with the

inorganic forms. Based on the results of the present

column studies, the performance of IOCS-2 was better

than that of IOCS-1 because in the preparation ofIOCS-2, an effective coating of iron oxide was achieved

on the sand through a high temperature coating process.

Poor performance was observed with MGS and IOCS-1.

4. Practical applicability of treatment systems

A treatment system such as an ion exchange system

was considered by the USEPA (1999, 2000) as one of the

best available technologies for arsenic removal, which

may be applicable to urban water facilities in USA, UK,and Canada. On the other hand, IOCS filtration, an

emerging technology (USEPA, 1999, 2000) may be

suitable for small water facilities, especially in develop-

ing countries such as Bangladesh, Chile, India, and

Mexico because of its simplicity, and ease of operation.

Removal of organic species has limited practical appli-

cability, as they are usually associated with inorganic

species in natural systems. The inorganic species presentin higher concentrations are obviously influencing and

interfering in the ion exchange process. More accessi-

ble and cost effective ion exchangers and/or adsor-

bents should be also studied such as, natural zeolites

and carbonaceous adsorbents as opposed to expensive

synthetic organic ion exchangers (Elizalde-Gonzalez,

Mattusch, Einicke, & Wennrich, 2001). Present studies

Fig. 3. DMA removal in the column studies using MGS, IOCS-1, and

resin.

Fig. 4. DMA removal in the column studies using IOCS-2.

Table 2

Summary of the results from the column studies

Adsorbent MGS IOCS- 1 Resin IOCS- 2

DMA concentration (lg/l) 100 100 100 100

Flow rate (ml/min) 830 830 1230 17.5

Volume of the media (ml) 4681 4681 4182 23

EBCT (min) 5.6 5.6 3.4 2.6

Total throughput volume (l) 572 547 1107 35.7

‘k’ value from Thomas model (ml/minlg) 0.27 0.12 1.23 0.28

Maximum solid phase concentration q0 (lg/g) from Thomas model 0.5 0.5 25 64.8

Bed volumes achieved upto 25 lg/l of As – – 585 480

Overall removal capacity of the media (lg/cm3) 0.7 0.4 5.7 2.6

O.S. Thirunavukkarasu et al. / Urban Water 4 (2002) 415–421 419

Page 6: Organic arsenic removal from drinking water

clearly showed that both ion exchange resin and IOCSare capable of removing organic species of arsenic from

drinking water. The removal of organic species along

with the inorganic species of arsenic from drinking water

by iron oxide-coated sand clearly showed that IOCS

would be the best choice amongst the treatment systems

for arsenic removal, applicable to small water facilities,

especially in developing countries.

5. Conclusions

1. Batch study results with IOCS-2 showed that the ar-

senic (DMA) adsorption can be best described by the

Freundlich isotherm based on the correlation co-

efficient.

2. The constants estimated from the Freundlich iso-

therm indicated that the arsenic (DMA) adsorption

capacity of IOCS-2 was low.

3. The arsenic (DMA) removal capacities of the mediaused in the column studies decreased in the following

order:

Ion exchange resin > IOCS-2 >MGS > IOCS-1

4. High bed volumes and high bed capacity were

achieved with ion exchange resin in the column stud-ies; these results suggested that ion exchange resin can

be effectively used to remove organic arsenic (DMA)

in drinking water. Poor performance of DMA re-

moval was observed with MGS and IOCS-1.

Acknowledgements

The authors acknowledge major support from Health

Canada for this study.

References

Al-Duri, B. (1996). Adsorption modeling and mass transfer. In G.

McKay (Ed.), Use of adsorbents for the removal of pollutants from

wastewaters (pp. 133–173). New York: CRC press.

Anderson, L. C. D., & Bruland, K. D. (1991). Biochemistry of arsenic

in natural waters: the importance of methylated species. Environ-

mental Science and Technology, 25(3), 420–429.

Andreae, M. O. (1977). Determination of arsenic species in natural

waters. Analytical Chemistry, 49(6), 820–823.

Banerjee, K., Helwick, R. P., & Gupta, S. (1999). A treatment process

for removal of mixed inorganic and organic arsenic species from

groundwater. Environmental Progress, 18(4), 280–284.

Benjamin, M. M., Sletten, R. S., Bailey, R. P., & Bennet, T. (1996).

Sorption and filtration of metals using iron oxide coated sand.

Water Research, 30(11), 2609–2620.

Braman, R. S., & Foreback, C. C. (1973). Methylated forms of arsenic

in the environment. Science, 182, 1247–1249.

Burkel, R. S., & Stoll, R. C. (1999). Naturally occuring arsenic in

sandstone aquifer water supply wells of North eastern Wisconsin.

Groundwater Monitoring and Remediation, 19(2), 114–121.

Cebrian, M. E., Albores, A., Aguilar, M., & Blakely, E. (1983).

Chronic arsenic poisoning in the North of Mexico. Human

Toxicology, 2, 121–133.

Chen, S. L., Yeh, S. J., Yang, M. H., & Lin, T. H. (1995). Trace

element concentration and arsenic speciation in the well water of

a Taiwan area with endemic blackfoot disease. Biological Trace

Element Research, 48, 263–274.

Crecelius, E. A. (1977). Changes in the chemical speciation of arsenic

following ingestion by man. Environmental Health Perspectives, 19,

147–150.

Del Razo, L. M., Arellano, M. A., & Cebrian, M. E. (1990). The

oxidation states of arsenic in well water from a chronic arsenicism

area of Northern Mexico. Environmental Pollution, 64, 143–

153.

Dhar, R. K., Biswas, B. K., & Samanta, G., et al. (1997). Ground-

water arsenic calamity in Bangladesh. Current Science, 73(1), 48–

59.

Elizalde-Gonzalez, M. P., Mattusch, J., Einicke, W. D., & Wennrich,

R. (2001). Sorption on natural solids for arsenic removal. Chemical

Engineering Journal, 81, 187–195.

Endo, G., Kuroda, K., Okamoto, A., & Horiguchi, S. (1992).

Dimethylarsinic acid induces tetraploids in Chinese hamster cells.

Bulletin of Environmental Contamination and Toxicology, 48, 131–

137.

Ghosh, M. M., & Yuan, J. R. (1987). Adsorption of inorganic arsenic

and organoarsenicals on hydrous oxides. Environmental Progress,

6(3), 150–157.

Ho, Y. S., Wase, D. A. J., & Forster, C. F. (1996). Kinetic studies of

competitive heavy metal adsorption by sphagnum moss peat.

Environmental Technology, 17, 71–77.

Jain, C. K., & Ali, I. (2000). Arsenic: occurrence, toxicity and

speciation techniques. Water Research, 34(17), 4304–4312.

Karim, M. M. (2000). Arsenic in groundwater and health problems in

Bangladesh. Water Research, 34(1), 304–310.

Kenyon, E. M., & Hughes, M. F. (2001). A concise review of the

toxicity and carcinogenicity of dimethylarsenic acid (DMA).

Toxicology, 160(1–3), 227–236.

Koch, I., Feldman, J., Wang, L., Andrewes, P., Reimer, K. J., &

Cullen, W. R. (1999). Arsenic in the Meager Creek hot springs

environment, British Columbia, Canada. The Science of the Total

Environment, 236, 101–117.

Lewis, R. J., & Tatken, R. L. (1978). Registry of toxic effects of

chemical substances. US Department of Health, Education and

Welfare, Cincinnati, OH, USA.

Meranger, J. C., & Subramanian, K. S. (1984). Arsenic in Nova

Scotian groundwater. The Science of the Total Environment, 39, 49–

55.

Miller, G. P., Norman, D. I., & Frisch, P. L. (2000). A comment on

arsenic species separation using ion exchange. Water Research,

34(4), 1397–1400.

Penrose, W. R. (1974). Arsenic in the marine and aquatic environ-

ments. Analysis, occurrence and significance. CRC Critical Reviews

in Environmental Control, 4, 465–482.

Petrick, J. S., Jagadish, B., Mash, E. A., & Aposhian, H. V. (2001).

Monomethylarsonous acid (MMA) and arsenite: LD50 in hamsters

and in vitro inhibition of pyruvate dehydrogenase. Chemical

Research Toxicology, 14(6), 651–656.

Reynolds, T. M., & Richards, P. A. (1996). Unit operations and

processes in environmental engineering. Boston: PWS publishing

company.

Styblo, M., Delnomdedieu, M., Hughes, M. F., & Thomas, D. J.

(1995). Identification of methylated metabolites of inorganic

arsenic by thin-layer chromatography. Journal of Chromatography

B, 668, 21–29.

420 O.S. Thirunavukkarasu et al. / Urban Water 4 (2002) 415–421

Page 7: Organic arsenic removal from drinking water

Tseng, W. P., Chu, H. M., How, S. W., Fong, J. M., Lin, C. S., & Yeh,

S. (1968). Prevalence of skin cancer in an endemic area of chronic

arsenicism in Taiwan. Journal of the National Cancer Institute,

40(3), 453–463.

Thirunavukkarasu, O. S., Viraraghavan, T., & Subramanian, K. S.

(2002). Arsenic removal from drinking water using iron oxide-

coated sand. Water, Air and Soil Pollution, in press.

Thomas, H. G. (1948). Chromatography: a problem in kinetics. Annals

New York Academy of Sciences, 49, 161–182.

USEPA. (1999). Technologies and costs for removal of arsenic from

drinking water. Draft report, EPA-815-R-00-012, Washington,

DC.

USEPA. (2000). Proposed revision to arsenic drinking water standard.

http://www.epa.gov/safewater/arsenic.html (22 June 2000).

USEPA. (2001). Drinking water standard for arsenic. http://www.

epa.gov/safewater/arsenic.html (31 October 2001).

Vahter, M. (1994). Species differences in the metabolism of arsenic. In

W. R. Chappell, C. O. Abernathy, & C. R. Cothern (Eds.), Arsenic

exposure and health (pp. 171–180). Northwood: Science and

Technology Letters.

Viraraghavan, T., Subramanian, K. S., & Aruldoss, J. A. (1999).

Arsenic in drinking water––problems and solutions.Water Science

and Technology, 40(2), 69–76.

Viraraghavan, T., Thirunavukkarasu, O. S., & Subramanian, K. S.

(2000). Iron oxide-coated sand––an excellent adsorbent for arsenic

removal in drinking water. In M. M. Sozanski (Ed.), Proceedings of

the fourth international conference on water supply and water quality

(pp. 1013–1024). Poland: Krakow.

Vogels, C. M., & Johnson, M. D. (1998). Arsenic remediation in

drinking waters using ferrate and ferrous ions. Technical completion

report, New Mexico State University. Las Cruces, NM, USA.

Yamamoto, S., Konsishi, Y., Matsuda, T., Murai, T., Shibata, M. K.,

Yuasa, I. M., Otani, S., Kuroda, K., Endo, G., & Fukushima, S.

(1995). Cancer induction by an organic arsenic compound,

dimethylarsinic acid (cacodylic acid), in F344/DuCrj rats after

pretreatment with five carcinogens. Cancer Research, 55, 1271–

1276.

Yamamura, S. (2001). Drinking water guidelines and standards. In

United Nations Synthesis Report on Arsenic in Drinking Water

(draft report), WHO, Geneva.

O.S. Thirunavukkarasu et al. / Urban Water 4 (2002) 415–421 421