1989
DOI: 10.1080/00015128909438528
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Chlorsulfuron Adsorption by Selected Soil Samples

Abstract: Ten selected soil samples from Denmark and Tanzania were extracted with ammonium acetate, EDTA, and dithionite-EDTA (DE) to fractionate aluminium and iron oxides. During these treatments various amounts of organic matter u.ere also removed. Chlorsulfuron adsorption by the pretreated soil samples was investigated under concentration and pH conditions similar to those in most natural soils, using 0.01 hl CaCI, as background electrolyte and a soil : solution ratio I : 5. Chlorsulfuron adsorption \\as highly corre… Show more

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Cited by 15 publications
(7 citation statements)
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“…Linear and Freundlich models were fit to the prosulfuron isotherms measured on model sorbents and variable‐charge soils (Tables 2 and 3) The goodness of fit ( r 2 ) values for linear and Freundlich fits were greater than 0.95 in most cases with the exception of prosulfuron sorption by highly weathered subsurface Oxisols (A1) in 5 m M Ca(H 2 PO 4 ) 2 ( r 2 = 0.82), where prosulfuron sorption was low ( K d = 0.11 L kg −1 ). The Freundlich K f and linear sorption coefficient K d values are within the 95% confidence intervals in most cases, suggesting that a linear estimation is adequate within the range of equilibrium aqueous concentrations obtained in this study (0.4–7.3 μ M ), in agreement with several sulfonylurea sorption studies (Borggaard and Streibig, 1989; Ukrainczyk and Ajwa, 1996; Werkheiser and Anderson, 1996).…”
Section: Resultssupporting
confidence: 90%
See 1 more Smart Citation
“…Linear and Freundlich models were fit to the prosulfuron isotherms measured on model sorbents and variable‐charge soils (Tables 2 and 3) The goodness of fit ( r 2 ) values for linear and Freundlich fits were greater than 0.95 in most cases with the exception of prosulfuron sorption by highly weathered subsurface Oxisols (A1) in 5 m M Ca(H 2 PO 4 ) 2 ( r 2 = 0.82), where prosulfuron sorption was low ( K d = 0.11 L kg −1 ). The Freundlich K f and linear sorption coefficient K d values are within the 95% confidence intervals in most cases, suggesting that a linear estimation is adequate within the range of equilibrium aqueous concentrations obtained in this study (0.4–7.3 μ M ), in agreement with several sulfonylurea sorption studies (Borggaard and Streibig, 1989; Ukrainczyk and Ajwa, 1996; Werkheiser and Anderson, 1996).…”
Section: Resultssupporting
confidence: 90%
“…However, anion exchange, hydrogen bonding, and charge transfer mechanisms have been shown to be significant for sorption by aluminum and iron oxides, clay minerals, humic acid, and anion exchange resins (Shea, 1986; Borggaard and Streibig, 1988). For variable‐charge minerals, Borggaard and Streibig (1989) observed chlorsulfuron sorption to be positively correlated with extractable Al and Fe oxide content as well as soil OC content in the range of 0.1 to 1.58%. For primisulfuron sorption, sorption was correlated with extractable Fe for lower OC soils (<1%), but not in high OC soils (>15%).…”
mentioning
confidence: 90%
“…The phenomenum of negative adsorption has been reported earlier in studies concerning the sorption of acidic chemicals (Weber et al, 1965). Borggaard and Streibig (1989) reported negligible adsorption of CHL at pH >7-8, and similar results were found by Shea (1986) and . Additionally, experiments performed using soil thin-layer chromatography showed that CHL mobility was positively correlated with pH (Mersie and Foy, 1986).…”
Section: Sorptionsupporting
confidence: 87%
“…This indicates that organic matter may be the primary binding factor reducing bioavailability in a soil system. Soil organic matter content has been positively correlated to sulfonylurea sorption (4,13). Sugarbeet response was not correlated with pH in the range of these growth chamber experiments (pH 6.4 to 8.1) (Table 4).…”
Section: Resultsmentioning
confidence: 86%