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首页> 外文期刊>Vadose Zone Journal >Modeling Dynamic Sorption of Cadmium in Cropland Soils
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Modeling Dynamic Sorption of Cadmium in Cropland Soils

机译:农田土壤中镉的动态吸附模拟

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摘要

In sorption experiments, Cd in the solution phase may be surface adsorbed or immobilized and precipitated into mineral phases. The reaction kinetics can be described by a two-site model combining a linear instantaneous model for the surface adsorption and a first-order reaction kinetic model with forward and backward reaction constants for the immobilization and precipitation of the mineral phase. A simplified sequential procedure was developed to study the contribution of these two processes. Results of batch Cd adsorption experiments with two California soils were used to illustrate the model validity. When the Cd sorption was obtained by varying the initial Cd solution concentration and maintaining constant equilibration time, the amounts of Cd in the solid phase as well as the adsorbed and mineral phases increase linearly with the initial Cd solution concentrations. As much as 90% of the sorbed Cd may be in the mineral phase. When the Cd sorption was examined at varying equilibration time and a constant Cd initial solution concentration, the sorbed Cd in the mineral phase increased exponentially to approach a maximum with time. The forward and backward reaction constants were obtained by fitting the sorption data to the model equations. It showed that the forward reaction was five times faster than the backward reaction for both soils and the reaction rates were two times faster in the heavier textured Holtville clay loam soil than the Arlington sandy loam soil.
机译:在吸附实验中,溶液相中的Cd可能被表面 吸附或固定化并沉淀成矿物相。 反应动力学可以通过结合两个位置的模型来描述。 > 表面吸附的线性瞬时模型和 具有向前和向后 反应常数的一阶反应动力学模型,用于固定和沉淀 < / sup>矿物相。开发了一种简化的顺序程序来研究这两个过程的作用。 使用两种加利福尼亚州的土壤进行批量Cd吸附实验的结果用于说明模型的有效性。通过改变初始Cd溶液浓度 并保持恒定的平衡时间获得Cd 吸附时,固相中 Cd的量也是如此因为吸附相和矿物相 随初始Cd溶液浓度线性增加。 吸附的Cd中有90%可能在矿物相中。 在变化的平衡时间 和恒定的Cd初始溶液浓度下检测Cd吸附时,矿物相中吸附的 Cd呈指数增加,接近 最大的时间。通过将吸附数据与模型方程拟合得到正向和反向反应常数 表明正向反应速率比 快五倍。质地较重的Holtville粘土 壤土中两种土壤的向后反应和反应速率 快于阿灵顿沙质壤土。

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  • 来源
    《Vadose Zone Journal》 |2006年第4期|1216-1221|共6页
  • 作者单位

    Department of Environmental Sciences, Univ. of California, Riverside, CA 92521;

    Department of Environmental Sciences, Univ. of California, Riverside, CA 92521;

    Department of Environmental Sciences, Univ. of California, Riverside, CA 92521;

    Department of Environmental Sciences, Univ. of California, Riverside, CA 92521;

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