2021
DOI: 10.3390/soilsystems5010013
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Sorption Mechanisms of Chemicals in Soils

Abstract: Sorption of chemicals onto soil particle surfaces is an important process controlling their availability for uptake by organisms and loss from soils to ground and surface waters. The mechanisms of chemical sorption are inner- and outer-sphere adsorption and precipitation onto mineral surfaces. Factors that determine the sorption behavior are properties of soil mineral and organic matter surfaces and properties of the sorbing chemicals (including valence, electron configuration, and hydrophobicity). Because soi… Show more

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Cited by 95 publications
(38 citation statements)
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“…Conclusions from several previous studies were derived from sorption behavior of the organic compounds in low concentration ranges (19,26,39). Although organic compounds in lower solution concentrations might exhibit linear sorption behavior, non-linear behavior is often observed in higher concentrations, which could alter the measured sorption capacity (33). Data from this study is consistent with studies showing a positive relationship between OC and ciprofloxacin sorption with pH-independent charges playing a critical role.…”
Section: Discussionsupporting
confidence: 83%
See 1 more Smart Citation
“…Conclusions from several previous studies were derived from sorption behavior of the organic compounds in low concentration ranges (19,26,39). Although organic compounds in lower solution concentrations might exhibit linear sorption behavior, non-linear behavior is often observed in higher concentrations, which could alter the measured sorption capacity (33). Data from this study is consistent with studies showing a positive relationship between OC and ciprofloxacin sorption with pH-independent charges playing a critical role.…”
Section: Discussionsupporting
confidence: 83%
“…Sorption of organic molecules to soil particles is driven by hydrophobic effect, coulombic attraction resulting in van der Waals forces, or cation bridging. Mechanisms include cation exchange, outer-& inner-sphere adsorption, and precipitation on mineral surfaces (33,34). Sorption in soil is affected by the chemical nature of the compound and the soil, including functional groups, charge and pH of the reaction mixture, soil CEC, and quantity and types of clay minerals, organic compounds, and metal ions in the soil.…”
Section: Discussionmentioning
confidence: 99%
“…Owing to their high surface area and ubiquitous presence throughout sediments, oils, aquifers and oil reservoirs, clay minerals exert a strong control on transport of dissolved ions and fluids in the sub-surface [1]. Although much research has highlighted the importance of layer charge and type of interlayer cation on the hydration and adsorption properties of clay minerals [2], less effort has focused on understanding how these properties might be affected under the anaerobic conditions typical for saturated soils and hydrocarbon reservoirs. In these reducing environments, structural Fe in clay minerals becomes reduced, increasing the clay mineral's layer charge, which is balanced by uptake of cations [3].…”
Section: Introductionmentioning
confidence: 99%
“…The concept of sorption covers two phenomena: absorption, which is the ability of a substance to be absorbed by the entire volume of another substance (the absorbent); and desorption, which results in compaction of the sorbed substance only on the surface of the adsorbent [ 22 , 23 ].…”
Section: Introductionmentioning
confidence: 99%