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首页> 外文期刊>Arabian journal of geosciences >Soil-water characteristic curves and hydraulic conductivity of nanomaterial-soil-bentonite mixtures
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Soil-water characteristic curves and hydraulic conductivity of nanomaterial-soil-bentonite mixtures

机译:纳米材料-土壤-膨润土混合物的土壤水特征曲线和水力传导率

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摘要

This study evaluates the influence of nanomaterials (nano-copper and nano-alumina) on the suction and hydraulic conductivity of compacted soil-bentonite mixture with different plasticity indexes. The soil suction and hydraulic conductivity of the compacted soil-bentonite mixtures were measured before and after the addition of nanomaterials. Soil-water characteristic curves were then developed for compacted soil samples (with and without nanomaterial) using a pressure membrane apparatus. It was found that saturated water content was lower in the soil samples mixed with nanomaterials. The soil hydraulic conductivity also decreased with increasing nanomaterial content, except for S3 soil sample with nanocopper content. The decrease of hydraulic conductivity was possibly caused by the reduction of the effective porosity due to pore clogging. The results from testing samples after one to four drying times show that the largest rise in soil hydraulic conductivity occurred at first or second drying. Adding nanomaterials can reduce the soil hydraulic conductivity by as much as seven times for soil samples with high clay (bentonite) content.
机译:本研究评估了纳米材料(纳米铜和纳米氧化铝)对不同塑性指标的压实土-膨润土混合物的吸力和水力传导率的影响。在添加纳米材料之前和之后,测量压实的土壤-膨润土混合物的土壤吸力和水力传导率。然后使用压力膜设备绘制压实土壤样品(有和没有纳米材料)的土壤水特征曲线。结果发现,与纳米材料混合的土壤样品中的饱和水含量较低。土壤水导率也随着纳米材料含量的增加而降低,但S3土壤样品中的纳米铜含量除外。水力传导率的降低可能是由于孔堵塞引起的有效孔隙率降低所致。一到四次干燥后测试样品的结果表明,土壤水力传导率的最大增加出现在第一次或第二次干燥时。对于高粘土(膨润土)含量的土壤样品,添加纳米材料可使土壤的水力传导率降低多达7倍。

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