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Quantification of the pore structures of Malan loess and the effects on loess permeability and environmental significance, Shaanxi Province, China: an experimental study

机译:中国陕西省马兰黄土孔隙结构的定量及其对黄土渗透性的影响及环境意义

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The pore microstructures of loess control the porosity and permeability of the loess, affecting the patterns of groundwater flow and the transport of contaminants. In the present study, the pore microstructure of Malan loess was investigated quantitatively in samples from five different loess layers. Specimens were examined via SEM, and pore microstructure parameters were determined using the digital image analysis method. Pore structures (including pore area ratio (PAR), pore size distribution, pore shape and pore morphology), the effects of the pore structure on loess permeability and the environmental significance of these factors are discussed in this paper. The results indicate that the samples of five loess layers in this study are considered to be porous soil, according to both the PAR and porosity values. The number of micropores, small pores, mesopores and macropores decreased significantly. The differences in number were mainly due to the significant reduction in the number of round pores, indicating that round pores tend to be small. In terms of area, micropores, small pores, mesopores and macropores were dominated by elongated and irregular pores. The macro-and mesopore structural characteristics of loess determined the transfer characteristics of groundwater and pollutants in the loess. Additionally, the 62% area reduction in the area of elongated or irregular macro-and mesopores and the decreasing connectivity from top to bottom layers caused by the deformation and destruction of the pores due to the overlying soil reduced the permeability and the water/pollutant migration rate with depth.
机译:黄土的孔隙微结构控制着黄土的孔隙度和渗透率,影响地下水的流动方式和污染物的输送。在本研究中,对来自五个不同黄土层的样品中马兰黄土的孔微结构进行了定量研究。通过SEM检查样品,并使用数字图像分析方法确定孔微结构参数。本文讨论了孔隙结构(包括孔隙面积比(PAR),孔隙大小分布,孔隙形状和孔隙形态),孔隙结构对黄土渗透性的影响以及这些因素的环境意义。结果表明,根据PAR和孔隙率值,本次研究中的五个黄土层样品被认为是多孔土壤。微孔,小孔,中孔和大孔的数量明显减少。数量上的差异主要是由于圆孔数量的显着减少,表明圆孔趋于变小。就面积而言,微孔,小孔,中孔和大孔以细长和不规则的孔为主。黄土的宏观和中孔结构特征决定了黄土中地下水和污染物的迁移特征。此外,上覆或不规则的大孔和中孔的面积减少了62%,并且由于上覆土壤导致的孔隙变形和破坏导致顶层与底层的连通性降低,从而降低了渗透性和水/污染物迁移随深度变化。

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