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Simulation of adsorption equilibrium of heavy metal cations on soils in circumneutral aqueous solution: influences of solution pH and dissolved humus substances

机译:循环水溶液中土壤中重金属阳离子吸附平衡的仿真:溶液pH与溶质腐殖质物质的影响

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Adsorption isotherms are often required for understanding mobility, fate and bioavailability of contaminants in soils. Those about Pb (II) and Cd (II) on Andosols and Kanto loam were investigated in this work. Results show that adsorption increased with cation equilibrium concentration (10~(-4) - 1 meq L~(-1)) and solution pH (5 - 7), and also that most adsorption isotherms can be simulated precisely with the ion-exchange-based Urano model. The applicability of model in predicting adsoiption equilibriums of cations on soils in circumneutral aqueous solution (pH 5 - 7) were experimentally confirmed. There is an exception as to the Pb (II) adsorption on Andosols with the solid-to-liquid phase ratio higher than 1:1 00, there adsorption isotherms at pH 5 and pH 7 crossed, and the measurement precision decreased. The Urano model equation becomes inapplicable. Further experiment where humus substances (HS) were added indicated that the abnormal phenomenon can be attributed to dissolved HS and their complexation with Pb (II). The dissolution of HS with solution pH has enhanced Pb (II) concentration in solution but hardly reduced the total amount of adsorption on soil.
机译:吸附等温线通常需要了解土壤中污染物的流动性,命运和生物利用度。关于PB(II)和CD(II)的那些在这项工作中调查了PB(II)和CD(II)。结果表明,吸附随阳离平衡浓度(10〜(-4) - 1meq L〜(-1))和溶液pH(5-7),以及大多数吸附等温线可以用离子交换精确模拟基于urano模型。实验证实了模型在预测围绕水溶液(pH5-7)中阳离子阳离子均衡均衡的适用性。对于具有高于1:1 00的固体相比的Pb(II)对糖醇的吸附有一个例外,在pH5和越过pH7的吸附等温线,测量精度降低。乌拉诺模型方程变得不适当。加入腐殖质物质(HS)的进一步实验表明异常现象可归因于溶解的HS及其与Pb(II)的络合。 HS用溶液pH的溶解具有增强的Pb(II)浓度在溶液中,但几乎不降低土壤上吸附的总量。

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