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首页> 外文期刊>Environmental Geology >Laboratory tests on effects of wetting-drying cycles and loess layer thickness on release and transport of loess colloidal particles in artificial loess columns
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Laboratory tests on effects of wetting-drying cycles and loess layer thickness on release and transport of loess colloidal particles in artificial loess columns

机译:湿法干燥周期和黄土层厚度对人工黄土柱中黄土胶体颗粒释放和迁移的影响的实验室测试

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摘要

Although it is known that wetting-drying (W-D) cycles can enhance the release and transport of soil colloidal particles (SCPs), the effects of cycle times and soil layer thickness on the enhancement are open questions. Artificial loess column laboratory tests were conducted for these questions. The results showed that the concentration of SCPs has one initial peak and several secondary peak concentrations in leachate, and all the peak concentrations decreased with increasing loess layer thickness. The concentrations of 30-, 20- or 10-cm-thick loess layer finally changes into stable levels at about 10, 16 and 23mgL(-1) within 48h, respectively. Via ten W-D cycles, the initial peak concentrations of 30-, 20- or 10-cm-thick loess layer increased by 37.02%, 40.21% and 53.76%, respectively. After the same number of W-D cycles, the initial peak concentration from 10-cm-thick loess layer was about double that from 30cm. In short, the release and transport of SCPs would increase with the increase of the times of W-D cycle and the decrease of loess layer thickness, which demonstrates a memory effect and a leapfrogging mode in time and space, respectively. The mobile SCPs have the potential to enhance the co-transport with contaminants in vadose zone, and even to groundwater. These findings can help to better understand the release and transport of SCPs and contaminants under seasonal rainfall climate conditions, and are helpful in evaluating the risk of soil and groundwater pollution.
机译:尽管已知干湿循环(W-D)可以增强土壤胶体颗粒(SCPs)的释放和运输,但循环时间和土壤层厚度对增强的影响尚待解决。针对这些问题进行了人工黄土柱实验室测试。结果表明,渗滤液中SCPs的浓度有一个初始峰和几个次要峰,且随着黄土层厚度的增加,所有峰浓度均降低。最后,在48小时内,分别将30、20或10厘米厚的黄土层的浓度变为稳定水平,分别为10、16和23mgL(-1)。经过十个W-D循环,黄土层30、20或10 cm的初始峰值浓度分别增加了37.02%,40.21%和53.76%。经过相同数量的W-D循环后,来自10厘米厚的黄土层的初始峰浓度约为30厘米处的初始峰浓度的两倍。简而言之,SCP的释放和运输将随着W-D循环次数的增加和黄土层厚度的减少而增加,这分别表现出记忆效应和时空跳跃模式。移动SCP具有增强与渗流带中污染物甚至与地下水的共运的潜力。这些发现有助于更好地了解季节性降雨气候条件下SCP和污染物的释放和运输,并有助于评估土壤和地下水污染的风险。

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