Qi Yongqiang, Donahoe Rona J
Beijing Water International, East 411 Kequn Plaza, 30 Xueyuan Road, Beijing 100083, China.
Environ Toxicol Chem. 2009 Jun;28(6):1338-45. doi: 10.1897/08-487.1.
The application of arsenical herbicides has created legacy environmental problems by contaminating soil in some agricultural areas and at various industrial sites. Numerous previous studies have suggested that the adsorption of arsenic by common soil components is largely controlled by kinetic factors. Four arsenic-contaminated soil samples collected from industrial sites were characterized and subjected to sequential leaching using a synthetic acid rain solution in order to study the release of arsenic. A dual-site numerical sorption-desorption model was constructed that describes arsenic desorption from these soils in terms of two different release mechanisms: Release from type I (equilibrium) and type II (kinetic) sorption sites. Arsenic held on both type I and II sorption sites is accessible through extensive acid rain leaching. Arsenic desorption from these sites follows a linear Kd model; the manner of approaching the Kd model, however, differs. Arsenic desorption from type I sites reached equilibrium with the aqueous phase under the physical environment provided by the experiment (shaking for 24 h at 25 degrees C), while desorption from type II sites followed a first-order kinetic pattern when approaching equilibrium. During synthetic acid rain sequential leaching of the soils, type I sites released their sorbed arsenic rapidly and subsequent desorption was dominated by the kinetic release of arsenic from type II sites. This shift in desorption mechanism dominance generated data corresponding to two intersecting straight lines in the n-logC dimension for all four soils. The dual-site desorption model was solved analytically and proven to be successful in simulating sorption processes where two different mechanisms are simultaneously controlling the aqueous concentration of a trace element.
砷类除草剂的应用在一些农业地区和各类工业场地造成了土壤污染,遗留了环境问题。此前众多研究表明,常见土壤成分对砷的吸附很大程度上受动力学因素控制。采集了四个来自工业场地的受砷污染土壤样本进行表征,并使用模拟酸雨溶液进行连续淋洗,以研究砷的释放情况。构建了一个双位点数值吸附 - 解吸模型,该模型根据两种不同的释放机制描述这些土壤中砷的解吸:从I型(平衡)和II型(动力学)吸附位点释放。I型和II型吸附位点上吸附的砷均可通过大量酸雨淋洗而释放出来。这些位点上砷的解吸遵循线性Kd模型;然而,接近Kd模型的方式有所不同。在实验提供的物理环境(25℃下振荡24小时)中,I型位点上的砷解吸与水相达到平衡,而II型位点在接近平衡时的解吸遵循一级动力学模式。在土壤的模拟酸雨连续淋洗过程中,I型位点迅速释放其所吸附的砷,随后的解吸主要由II型位点上砷的动力学释放主导。这种解吸机制优势的转变使得所有四种土壤在n - logC维度上产生了对应两条相交直线的数据。对双位点解吸模型进行了解析求解,并证明其成功模拟了两种不同机制同时控制微量元素水相浓度的吸附过程。