2008
DOI: 10.4141/cjss07076
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Measurement and modeling of surface charge and cation binding in agricultural soil

Abstract: Taillon, K. M. and Hendershot, W. H. 2008. Measurement and modeling of surface charge and cation binding in agricultural soil. Can. J. Soil Sci. 88: 749Á759. Models of metal adsorption have typically been developed and tested for soil components rather than whole soils and at cation concentrations higher than usual environmental conditions. This study investigates whether the non-ideal consistent competitive adsorption (NICA) model can be applied to ion binding in whole soils at low total metal concentrations.… Show more

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Cited by 3 publications
(3 citation statements)
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“…Fluxes of Zn and Cd from the ionic exchange membranes were decreased by lime addition, whereas fluxes of Mo were increased. Thus, for these metals, their solubility was directly affected by soil pH [r00.71 to 0.76, P B0.01 (Kabata-Pendias 2001)], and the free ion forms were more prevalent, as opposed to Cu where almost all of the Cu added to soil is bound by the soil solid phase and the remaining in-soil solution is bound to dissolved organic C or other ligands (Taillon and Hendershot 2008). The same trends were observed with water extraction, but only for Zn and Mo.…”
Section: Soil Metals Availabilitymentioning
confidence: 99%
“…Fluxes of Zn and Cd from the ionic exchange membranes were decreased by lime addition, whereas fluxes of Mo were increased. Thus, for these metals, their solubility was directly affected by soil pH [r00.71 to 0.76, P B0.01 (Kabata-Pendias 2001)], and the free ion forms were more prevalent, as opposed to Cu where almost all of the Cu added to soil is bound by the soil solid phase and the remaining in-soil solution is bound to dissolved organic C or other ligands (Taillon and Hendershot 2008). The same trends were observed with water extraction, but only for Zn and Mo.…”
Section: Soil Metals Availabilitymentioning
confidence: 99%
“…The variable charge Si‐OH produced by the original saline‐alkali soil mainly comes from the variable charge produced by 2:1 type minerals (Phillips & Sheehan, 2005). After the addition of AHA, a large amount of Ca 2+ is introduced, and Ca 2+ will exchange exchangeable cations on the mineral surface, so the surface charge and variable negative charge of clay particles increase (Taillon & Hendershot, 2008).…”
Section: Discussionmentioning
confidence: 99%
“…Sheehan, 2005). After the addition of AHA, a large amount of Ca 2+ is introduced, and Ca 2+ will exchange exchangeable cations on the mineral surface, so the surface charge and variable negative charge of clay particles increase (Taillon & Hendershot, 2008).…”
Section: Effect Of 3% Aha Addition On Soil Colloid Surface Charge In ...mentioning
confidence: 99%