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Sorption-Desorption of Aminocyclopyrachlor in Selected Brazilian Soils

机译:在某些巴西土壤中氨基环吡氯的吸附-解吸

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Aminocyclopyrachlor sorption/desorption was investigated in 14 soils from Brazil, representing a range of pH, and organic carbon (OC) and clay contents. The Freundlich equation adequately described behavior of aminocyclopyrachlor in soil. Freundlich sorption coefficient (K_f) values ranged from 0.06 to 1.64 and 1 values for ranged from 0.9 to 1.0. Sorption was correlated to OC (K_(foc) ranged from 11 to 64) and clay contents. The lowest sorption was found for soils with very low OC contents (0.50-0.65%) and loamy-sand to sand textures. The X values for desorption were lower than those observed for sorption, suggesting that aminocyclopyrachlor sorption by soil was not reversible; hysteresis coefficients ranged from 0.13 to 0.74. The results suggest that although aminocyclopyrachlor would be very mobile based on its sorption coefficients, its potential depth of leaching may be overestimated due to the hysteretic desorption.
机译:在来自巴西的14种土壤中研究了氨基环吡氯的吸附/解吸,这些土壤的pH范围,有机碳(OC)和黏土含量。 Freundlich方程充分描述了氨基环吡氯在土壤中的行为。 Freundlich吸附系数(K_f)值介于0.06至1.64之间,1 / n值介于0.9至1.0之间。吸附与OC(K_(foc)范围从11到64)和粘土含量相关。 OC含量极低(0.50-0.65%)且壤土-沙质地的土壤吸附力最低。解吸的X / n值低于观察到的解吸值,表明土壤对氨基环吡氯的吸附是不可逆的。磁滞系数范围从0.13到0.74。结果表明,尽管氨基环吡氯根据其吸附系数具有很高的流动性,但由于滞后解吸作用,其潜在的浸出深度可能被高估了。

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