Abstract:This study evaluated the potential of water‐dispersible soil colloids with diverse physicochemical and mineralogical characteristics to adsorb and mediate the transport of atrazine through macropores of intact soil columns. The soil columns were taken from the upper solum of an Alfisol (Maury) and a Mollisol (Loradale) in the Bluegrass region of Kentucky. Six different colloid suspensions mixed with atrazine [2‐chloro‐4‐(ethylamino)‐6‐(isopropylamino)‐s‐triazine] were introduced at a constant flux into the und… Show more
“…The atrazine isotherm resulted in high Freundlich constants (Table 4). As K f ind ica tes the str eng th or deg ree of the adsorption and 1/n indicates the curve slope (Sonon and Scwab, 1995), results show that atrazine has high adsorption to the 0 horizon. This behavior was expected sinc e atrazin e shows high adsorption to soil particles and low solubility.…”
Section: Resultsmentioning
confidence: 98%
“…The adsorption pattern of atraz ine and picloram was fit to the Freundlich isotherm, whi ch is in agr eement wit h other studie s (Gover, 1971;Sonon and Scwab, 1995). The Freundlich isotherm has been commonly used in studies of adsorption, and it is well suited to the adsorptive behavior of herbicide (Ebato et al, 2001).…”
Section: Resultsmentioning
confidence: 99%
“…This behavior was expected sinc e atrazin e shows high adsorption to soil particles and low solubility. The high adsorption to the 0 horizon can be noted when comparing the atrazi ne K f value (67 .54 ) to the fou nd for atr azi ne adsorption to whole soil particles (1.0 to 4.0) (Barriuso et al, 1992;Nakagawa et al, 1995;Seta and Karathanasis, 1997;Gomes et al, 2002). On the oth er han d, the amount of atrazine adsor bed by the amount of litt er, represented by the normalized mass (Table 3) was lower in the 0 horizon (1.01 µg g -1 ) when compared to 6.35 µg g -1 obtained by (Huang et al, 1984) for clay particles.…”
Section: Resultsmentioning
confidence: 99%
“…Ma ny st udie s ha ve be en re port ed on the adsorption of herbicides on different soils and soil constituents (Barriuso et al, 1992;Gover, 1971;Huang et al, 1984;Seta and Karathanasis, 1997;Wauchope and Myers, 1985) but few studies have reported herbicide ads orp tion to for est soi l org ani c hor izo ns (Sundaram, 1995). Adsorption of herbicides within organic horizons of forested SMZs may play an important role in limiting herbicide movement from recently treated sites under conditions where high precipitation generates surface runoff.…”
-Adsorption of two herbicides, atrazine and picloram, displaying different sorption characteristics, were evaluated for O (organic) horizon samples collected from SMZs (streamside management zones) in Piedmont (Ultisol) of Georgia, USA. Samples were randomly collected from within 5 SMZs selected for a study of surface flow in field trials. The five SMZs represented five different slope classes, 2, 5, 10, 15 and 20%. Results indicate that 0 horizons have the potential for sorbing atrazine from surface water moving through forested SMZs. Atrazine adsorption was nearly linear over a 24-hour period. Equilibrium adsorption, determined through 24-hour laboratory tests, resulted in a Freundlich coefficient of 67.5 for atrazine. For picloram, negative adsorption was observed in laboratory experiments. This seemed to be due to interference with ELISA analyses; however, this was not confirmed. The adsorption coefficient (Kd) obtained for atrazine in 0 horizons was greater than it would have been expected for mineral soil (from 1 to 4). Picloram was not sorbed in 0 horizons at any significant degree. Although there is a significant potential for the direct adsorption of soluble forms of herbicides in SMZs, the actual value of this adsorption for protecting water is likely to be limited even for relatively strongly sorbed chemicals, such as atrazine, due to relatively slow uptake kinetics.
Keywords
“…The atrazine isotherm resulted in high Freundlich constants (Table 4). As K f ind ica tes the str eng th or deg ree of the adsorption and 1/n indicates the curve slope (Sonon and Scwab, 1995), results show that atrazine has high adsorption to the 0 horizon. This behavior was expected sinc e atrazin e shows high adsorption to soil particles and low solubility.…”
Section: Resultsmentioning
confidence: 98%
“…The adsorption pattern of atraz ine and picloram was fit to the Freundlich isotherm, whi ch is in agr eement wit h other studie s (Gover, 1971;Sonon and Scwab, 1995). The Freundlich isotherm has been commonly used in studies of adsorption, and it is well suited to the adsorptive behavior of herbicide (Ebato et al, 2001).…”
Section: Resultsmentioning
confidence: 99%
“…This behavior was expected sinc e atrazin e shows high adsorption to soil particles and low solubility. The high adsorption to the 0 horizon can be noted when comparing the atrazi ne K f value (67 .54 ) to the fou nd for atr azi ne adsorption to whole soil particles (1.0 to 4.0) (Barriuso et al, 1992;Nakagawa et al, 1995;Seta and Karathanasis, 1997;Gomes et al, 2002). On the oth er han d, the amount of atrazine adsor bed by the amount of litt er, represented by the normalized mass (Table 3) was lower in the 0 horizon (1.01 µg g -1 ) when compared to 6.35 µg g -1 obtained by (Huang et al, 1984) for clay particles.…”
Section: Resultsmentioning
confidence: 99%
“…Ma ny st udie s ha ve be en re port ed on the adsorption of herbicides on different soils and soil constituents (Barriuso et al, 1992;Gover, 1971;Huang et al, 1984;Seta and Karathanasis, 1997;Wauchope and Myers, 1985) but few studies have reported herbicide ads orp tion to for est soi l org ani c hor izo ns (Sundaram, 1995). Adsorption of herbicides within organic horizons of forested SMZs may play an important role in limiting herbicide movement from recently treated sites under conditions where high precipitation generates surface runoff.…”
-Adsorption of two herbicides, atrazine and picloram, displaying different sorption characteristics, were evaluated for O (organic) horizon samples collected from SMZs (streamside management zones) in Piedmont (Ultisol) of Georgia, USA. Samples were randomly collected from within 5 SMZs selected for a study of surface flow in field trials. The five SMZs represented five different slope classes, 2, 5, 10, 15 and 20%. Results indicate that 0 horizons have the potential for sorbing atrazine from surface water moving through forested SMZs. Atrazine adsorption was nearly linear over a 24-hour period. Equilibrium adsorption, determined through 24-hour laboratory tests, resulted in a Freundlich coefficient of 67.5 for atrazine. For picloram, negative adsorption was observed in laboratory experiments. This seemed to be due to interference with ELISA analyses; however, this was not confirmed. The adsorption coefficient (Kd) obtained for atrazine in 0 horizons was greater than it would have been expected for mineral soil (from 1 to 4). Picloram was not sorbed in 0 horizons at any significant degree. Although there is a significant potential for the direct adsorption of soluble forms of herbicides in SMZs, the actual value of this adsorption for protecting water is likely to be limited even for relatively strongly sorbed chemicals, such as atrazine, due to relatively slow uptake kinetics.
Keywords
“…Numerous studies have been undertaken that show pesticide can sorb to colloids and potentially enhance their transport (e.g. Vinten et al, 1983;Worrall et al, 1999;Seta and Karathanasis, 1997;Kulikova and Perminova, 2002).…”
Agrochemical contamination in groundwater poses a significant long term threat to water quality and is of concern for legislators, water utilities and consumers alike. In the dual porosity, dual permeability aquifers such as the Chalk aquifer, movement of pesticides and their metabolites through the unsaturated zone to groundwater is generally considered to be through one of two pathways; a rapid by-pass flow and a slower 'piston-flow' route via the rock matrix. However, the dissolved form or 'colloidal species' in which pesticides move within the water body is poorly understood. Following heavy rainfall, very high peaks in pesticide concentration have been observed in shallow Chalk aquifers. These concentrations might be well explained by colloidal transport of pesticides. We have sampled a Chalk groundwater beneath a deep (30 m) unsaturated zone known to be contaminated with the pesticide diuron. Using a tangential flow filtration technique we have produced colloidal fractions from 0.45µm to 1kDa. In addition, we have applied agricultural grade diuron to a typical chalk soil and created a soil water suspension which was also subsequently fractionated using the same filtration system. The deep groundwater sample showed no evidence of association between colloidal material and pesticide concentration. In comparison, despite some evidence of particle trapping or sorption to the filters, the soil water clearly showed an association between the <0.45µm and <0.1µm colloidal fractions which displayed significantly higher pesticide concentrations than the unfiltered sample.Degradation products were also observed and found to behave in a similar manner to the parent compound. Although relatively large colloids can be generated in the Chalk soil zone, 2 it appears transport to depth in a colloidal-bound form does not occur. Comparison with other field and monitoring studies suggests that rapid by-pass flow is unlikely to occur beneath 4-5 m. Therefore, shallow groundwaters are most at risk from rapid transport of high concentrations of pesticide-colloidal complexes. The presence of a deep unsaturated zone will mean that most of the colloidal-complexes will be filtered by the narrow chalk pores and the majority of pesticide transport will occur in a 'dissolved' form through the more gradual 'piston-flow' route.
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