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Kinetics of soil cadmium desorption under simulated acid rain

机译:模拟酸雨条件下土壤镉解吸动力学

摘要

Soil acidification can result in the release of heavy metals stabilized by soil components into soil solution, and therefore it causes ecological risk. The kinetics of Cd desorption from two Chinese soils (ultisol and oxisol) distributed in the acid rain sensitive areas of southern China, were studied using a flow-stirred method under simulated acid rain conditions. Cd desorption was well described by the first-order kinetic equation. Percentages of Cd desorbed were 80-99% in ultisol and 25-28% in oxisol, respectively. Cd desorption, regarded as a heterogeneous diffusion in soils, could be also fitted by the Elovich equation. The desorption process could be divided into a fast reaction and a slow reaction, which were corresponded to the exchangeable and the specific sorbed Cd, respectively. The obtained results are essential to understand the process of heavy metal release under acid deposition conditions and to evaluate the ecological risk of acid deposition in those acid rain sensitive areas of China. (C) 2009 Elsevier B.V. All rights reserved.
机译:土壤酸化会导致由土壤成分稳定的重金属释放到土壤溶液中,因此会带来生态风险。在模拟的酸雨条件下,采用流动搅拌法研究了分布在中国南部酸雨敏感地区的两种中国土壤(ultisol和oxisol)中Cd的解吸动力学。一阶动力学方程很好地描述了镉的解吸。在Ultisol中解吸的Cd的百分比分别为80-99%和在Oxisol中为25-28%。镉的解吸(被认为是土壤中的一种非均质扩散)也可以通过Elovich方程拟合。解吸过程可分为快反应和慢反应,分别对应于可交换的镉和特定的吸附镉。获得的结果对于了解酸性沉积条件下重金属的释放过程以及评估中国那些酸雨敏感地区酸性沉积的生态风险至关重要。 (C)2009 Elsevier B.V.保留所有权利。

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