environmental soil chemistry || soil solution-solid phase equilibria
Post on 15-Dec-2016
Embed Size (px)
4 Soil SolutionSolidPhase Equilibria
There are a number of complex chemical reactions that can occur insoils. These various reactions interact with each other through thesoil solution (Fig. 4.1). The soil solution is defined as the aqueousliquid phase of the soil and its solutes (Glossary of Soil Science Terms, 1997).The majority of solutes in the soil solution is ions, which occur either as freehydrated ions (e.g., Al3+ which is expressed as Al(H2O)6
3+) or as various complexeswith organic or inorganic ligands. When metal ions and ligands directly interactin solution (no water molecules are present between the metal ion and theligand) they form what are known as inner-sphere complexes. An outer-spherecomplex is formed when a water molecule is positioned between the metal ionand the ligand. Outer-sphere complexes are not as tightly bound as inner-sphere complexes. An uncharged outer-sphere complex is often referred to asan ion pair (e.g., Ca2+ plus SO4
2 ions are known to form ion pairs, CaSO40).
Soil solutions, therefore, are composed of a variety of ion species, eithercomplexed or noncomplexed. The speciation of the soil solution refers todetermining the distribution of ions in their various chemical forms.
The soil solution is the medium from which plants take up ions (1 inFig. 4.1) and in which plant exudates reside (2). Ions in the soil solution canbe sorbed on organic and inorganic components of the soil (3) and sorbedions can be desorbed (released) into the soil solution (4). If the soil solutionis supersaturated with any mineral in the soil, the mineral can precipitate (5)until equilibrium is reached. If the soil solution becomes undersaturated withany mineral in the soil, the mineral can dissolve (6) until equilibrium isreached. Ions in the soil solution can be transported through the soil (7) intogroundwater or removed through surface runoff processes. Throughevaporation and drying upward movement of ions can also occur (8).Microorganisms can remove ions from the soil solution (9) and when theorganisms die and organic matter is decomposed, ions are released to the soilsolution (10). Gases may be released to the soil atmosphere (11) or dissolvedin the soil solution (12).
Measurement of the Soil SolutionThe concentration of a particular ion in the soil solution (intensity factor)and the ability of solid components in soils to resupply an ion that is depletedfrom the soil solution (capacity factor) are both important properties of a
116 4 Soil SolutionSolid Phase Equilibria
Solute Transport,Evaporation & Runoff
Solid Phases& Minerals
Organic Matter& Microorganisms
FIGURE 4.1. Dynamic equilibria reactions in soils. From W. L. Lindsay, ChemicalEquilibria in Soils. Copyright 1979 John Wiley & Sons. Reprinted by permission of JohnWiley & Sons, Inc.
Measurement of the Soil Solution 117
given soil. The measurement of the intensity factor is critical in predictingand understanding reactions in the soil environment such as weathering andthe bioavailability, mobility, and geochemical cycling of nutrients andinorganic and organic chemicals in soils (Wolt, 1994). However, themeasurement of soil solution components in situ is very difficult, and,technically, not possible for most ion species. In addition, the actualconcentration of the ion species in the soil solution changes with changes insoil moisture content (Wolt, 1994).
A number of laboratory methods are used to obtain samples of the soil solution. These are described in detail by Adams (1971) and Wolt (1994) and will be discussed only briefly here. The methods can be classified as displacement techniques including column displacement(pressure or tension displacement, with or without a displacing solution),centrifugation (perhaps with an immiscible liquid), and saturation extracts(e.g., saturation pastes).
In the column displacement method, a field moist soil is packed into aglass column and a displacing solution is added to the soil. The displaced soilsolution is collected at the bottom of the column and analyzed for its ioncontent. The column displacement method is probably the most reliablemethod for obtaining a sample of the soil solution. However, the procedureis tedious, requiring an analyst who is experienced in packing the columnwith soil. Furthermore, the procedure is very time-consuming.
The centrifugation method uses an immiscible liquid, such as carbontetrachloride or ethyl benzoylacetate, to physically remove the soil solution(which is essentially water) from the solid matrix of the moist soil. During centrifugation (>1 MPa for from 30 min to 2 hr), the immiscibleliquid passes through the soil and soil solution is displaced upward. The displaced soil solution is then decanted and filtered through a phase-separating filter paper (to remove traces of the immiscible liquid) and then through a 0.2-m membrane filter to remove suspended clayparticles (Wolt, 1994). Centrifugation methods are the most widely usedbecause they are relatively simple and equipment to carry out the procedureis usually available.
In the saturation extract method a saturated soil paste is prepared byadding distilled water to a soil sample in a beaker, stirring with a spatula, andtapping the beaker occasionally to consolidate the soilwater mixture. Atsaturation, the soil paste should glisten. Prior to extraction the saturated soilpaste should be allowed to stand for 416 hr. Then, the soil paste istransferred to a funnel containing filter paper. The funnel is connected to aflask, vacuum is applied, and the filtrate is collected.
Table 4.1 shows the average ion composition of soil solutions for soilsfrom around the world. One will note that Ca is the most prevalent metalcation in the soil solution, which is typical for most soils. Nitrate, chloride,and sulfate are the common anions (ligands) in more acidic soils whilecarbonate can be important in some basic soils.
TABLE 4.1. Total Ion Composition of Soil Solutions from World Soilsa
Total ion composition of soil solution (mmol liter1)
Location pH Ca Mg K Na NH4 Al Si HCO3 SO4 Cl NO3of soils
Californiab 7.43 12.86 2.48 2.29 3.84 0.86 3.26 5.01 3.07 21.36
Georgiac 6.15 0.89 0.29 0.07 0.16 0.0004 0.13 1.18 0.21 0.10
UnitedKingdomd 7.09 1.46 0.12 0.49 0.31 0.01 0.34 0.32 0.75 0.69
Australiae 5.75 0.27 0.40 0.38 0.41 2.60 0.85 0.87 1.67 0.32
a Adapted from J. Wolt, Soil Solution Chemistry. Copyright 1994 John Wiley & Sons. Adapted by permission of John Wiley & Sons, Inc.b From Eaton et al. (1960); soil solution obtained by pressure plate extraction at 10 kPa moisture. The pH and total composition for each ion
represent the mean for seven soils.c From Gillman and Sumner (1987); soil solution obtained by centrifugal displacement at 7.5 kPa moisture. The pH and total composition for
each ion represent the mean for four Ap (surface) horizons.d From Kinniburgh and Miles (1983); soil solution obtained by centrifugal displacement at field moisture contents. The pH and total
composition for each ion represent the mean for 10 surface soils.e From Gillman and Bell (1978); soil solution obtained by centrifugal displacement at 10 kPa moisture. The pH and total composition for each
ion represent the mean value for six soils.
118 4 Soil SolutionSolid Phase Equilibria
Speciation of the Soil SolutionWhile total ion concentration (sum of free and complexed ions) of the soilsolution, as measured by analytical techniques such as spectrometry,chromatography, and colorimetry, provides important information on thequantities of ions available for plant uptake and movement through the soilprofile, it is important that the speciation or chemical forms of the free andcomplexed ions be known. Ions in the soil solution can form a number ofspecies due to hydrolysis, complexation, and redox (see Chapter 8) reactions.Hydrolysis reactions involve the splitting of a H+ ion from a water moleculewhich forms an inner-sphere complex with a metal ion (Baes and Mesmer,1976). The general hydrolysis reaction for a hydrated metal ([M(H2O)x]
n+)in solution is
[M(H2O)x]n+ [M(OH)y (H2O)xy]
(ny)+ + H+, (4.1)
where n+ refers to the charge on the metal ion, x the coordination number,and y the number of H+ ions released to solution. The degree of hydrolysisfor a solvated metal ion [extent of the reaction in Eq. (4.1)] is a function of pH. A general complexation reaction between a hydrated metal[(M(H2O)x]
n+ and a ligand, L1, to form an outer-sphere complex is
a[M(H2O)x]n+ + bL1 [M(H2O)x]a Lb, (4.2)
where a and b are stoichiometric coefficients.Analytically, it is not possible to determine all the individual ion
species that can occur in soil solutions. To speciate the soil solution, one must apply ion association or speciation models using the total concentration data for each metal and ligand in the soil solution. A mass
Speciation of the Soil Solution 119
balance equation for the total concentration of a metal, MTn+ in the solution
phase can be written as
MTn+ = Mn+ + MML, (4.3)
where Mn+ represents the concentration of free hydrated-metal ion species,and MML is the concentration of metal ion associated with the remainingmetalligand complexes. The ligands in the metalligand complexes could beinorganic anions or humic substances such as humic and fulvic acids. Similarmass balance equations can be written for the total concentration of eachmetal and ligand in the soil solu