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首页> 外文期刊>Plant, Soil and Environment >Laboratory study of retention and release of weak acid herbicide MCPA by soils and sediments and leaching potential of MCPA
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Laboratory study of retention and release of weak acid herbicide MCPA by soils and sediments and leaching potential of MCPA

机译:土壤和沉积物对弱酸性除草剂MCPA的保留和释放以及MCPA的浸出潜力的室内研究

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MCPA sorption and desorption in five surface soils (denoted as A1-5), three bottom sediments (S1-3), two river sediments (L1-2) and one subsurface soil (SS) at two initial concentrations in aqueous solution – C0 = 0.5 and 10 mg/l were studied. No significant effect of the initial concentration on MCPA equilibrium distribution between soil/sediment and aqueous solution was observed. The difference between distribution coefficient KD at C0 = 0.5 mg/l and KD at C0 = 10 mg/l was found only in the case of one bottom sediment (S2). A simple regression analysis between KD at C0 = 0.5 and 10 mg/l and soil/sediment properties indicated that the most important property which determined the variation in MCPA sorption is organic carbon (r = 0.886*** and r = 0.926***, respectively). Similarly, desorption of MCPA was inversely proportional to organic carbon content of the soils and sediments used (r = –0.862* and r = –0.842**). These observations showed that MCPA sorption and desorption in soils and sediments were primarily controlled by organic components of the geosorbents used. Overall, the percentage of MCPA sorption in soils and sediments was low (Psorp ≈ 3–53%; KD = 0.077–2.827 l/kg) and the percentage of MCPA desorbed was relatively high (Pdes ≈ 11–70%), especially in the soils and sediments with lower organic carbon content. The experimental results and calculated values of groundwater ubiquity score GUS and relative leaching potential index RLPI imply that MCPA is very mobile in all the surface soils and has a potential to contaminate groundwater.
机译:在水溶液中两种初始浓度下,MCPA在五种表层土壤(表示为A1-5),三种底泥(S1-3),两种河流沉积物(L1-2)和一种地下土壤(SS)中的吸附和解吸– C0 =研究了0.5和10 mg / l。没有观察到初始浓度对土壤/沉积物和水溶液之间MCPA平衡分布的显着影响。仅在一个底部沉积物(S2)的情况下才发现C0 = 0.5 mg / l时的分布系数KD和C0 = 10 mg / l时的KD之间的差异。在CD = 0.5和10 mg / l之间的KD与土壤/沉积物特性之间的简单回归分析表明,决定MCPA吸附变化的最重要特性是有机碳(r = 0.886 ***和r = 0.926 *** , 分别)。同样,MCPA的解吸与所用土壤和沉​​积物的有机碳含量成反比(r = –0.862 *和r = –0.842 **)。这些观察结果表明,MCPA在土壤和沉积物中的吸附和解吸主要受所用地质吸附剂的有机成分控制。总体而言,土壤和沉积物中MCPA的吸附百分比较低(Psorp≈3–53%; KD = 0.077–2.827 l / kg),而MCPA的解吸百分比相对较高(Pdes≈11–70%),特别是在有机碳含量较低的土壤和沉积物。实验结果和地下水普遍存在得分GUS的计算值以及相对浸出潜力指数RLPI暗示MCPA在所有表层土壤中的流动性很高,并且有可能污染地下水。

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