水溶性阳离子在工程黄土中的扩散特性
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陕西省自然科学研究计划项目


Diffussion Characteristics of Water Soluable Cations in Engineering Loess
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    摘要:

    该文采用水平扩散池观测了水溶性盐阳离子在工程黄土中的扩散过程。结果表明:水溶性盐阳离子在土壤中的扩散特性因离子种类而异,Ca2+的扩散系数最高,Mg2+,Na+,K+依次降低,其由两个模型测定的平均值分别为2.6928×10-6,2.3127×10-6,1.6730×10-6,0.4504×10-6cm2/s.在距源溶液较近时,土壤胶体交换性K+,Na+,Mg2+均明显升高,特别是交换性K+升高幅度最大;而交换性Ca2+却明显减少,说明K+,Na+,Mg2+被土壤胶体吸附,而Ca2+不但没有吸附,反而被解吸。

    Abstract:

    Horizontal diffussion cells were used to observe and measure the diffussion processes of the water soluable salt cations in engineering loess.The results obtained showed that the diffussion characteristics of every cation changed with its variety.The diffussion coefficient of Ca2+was the highest,and that of Mg2+, Na+ and K+ dropped in turn.The mean values of them determined in the two models were 2.692 8×10-6,2.312 7×10-6,1.6370×10-6 and 0.4504×10-6cm2/s respectively.The significant increase of the exchangeable K+, Na+ and Mg2+,and the decrease of the exchangeable Ca2+in soil near the source solution indicated that the formers were absorpted and the later was desorpted by the soil collision.

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王朝辉,岳宝蓉.水溶性阳离子在工程黄土中的扩散特性[J].水土保持通报,1998,(2):9-13

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  • 收稿日期:1997-12-24
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  • 在线发布日期: 2014-11-28
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