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土壤中离子扩散的动力学研究
引用本文:李航,薛家骅.土壤中离子扩散的动力学研究[J].土壤学报,1996,33(4):327-336.
作者姓名:李航  薛家骅
作者单位:[1]西南农业大学资源环境学院 [2]南京农业大学基础部
摘    要:本文首先从理论上分析了土壤中离子扩散的动力学问题,提出了土壤中离子扩散的三种动力学类型,即扩散的一级动力学、零级动力学和负一极动力学,并且还指出,一级动力学是土壤中离子扩散的普遍形式,负一级动力学只出现在过程的初期阶段,而扩散的零级动力学则存在于有快速表面反应的情况下。在此基础上进行了Mg^2+在土壤和石英砂中的扩散动力学实验研究,结果发现不论在298K还是在308K的温度下,两个体系中Mg^2+

关 键 词:土壤  离子扩散  动力学
收稿时间:1995/10/15 0:00:00

STUDY ON ION DIFFUSION KINETICS IN SOIL SYSTEMS
Li Hang and Xue Jiahua.STUDY ON ION DIFFUSION KINETICS IN SOIL SYSTEMS[J].Acta Pedologica Sinica,1996,33(4):327-336.
Authors:Li Hang and Xue Jiahua
Institution:College of Resources and Environment, Southwest Agricultural University, Chongqing 630716;Basic Course Department, Nanjing Agricultural University, Nanjing
Abstract:First, this paper discusses ion diffusion kinetics in soil systems theoritically. Ion diffusion kinetics in soils can be classified into three types: negative first-order, zero-order and first-order kinetics. Based on this, an experiment on Mg2+ diffusion kinetics was done in soil and quartz sand systems. The results showed that Mg2+ diffusion kinetics in the two systems were a first-order kinetic process. But at the temperature of 298K and in the initial stage of diffusion, first-order and negative first-order kinetic processes coexisted in Mg2+ diffusion in the soil system. Through the study of Mg2+ diffusion in quartz sand systems, we also found that an exchange reaction might take place between Mg2+ and hydrogen at the hydration SiO2 surface, and the Mg2+ which took part in exchange reaction was at diffused in the quartz sand within the initial ten minutes.
Keywords:Soil  Ion diffusion  Kinetics
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