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Variation of Matric Suction in Unsaturated Loess Soils

机译:不饱和黄土污垢中的测力变异

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It is well-known that natural loess soil occurs in unsaturated state.Hence,its shear strength is largely controlled by the matric suction presented in the unsaturated soils.To explore variation characteristics of matric suction within loess soils and its influencing factors apart from moisture content,an experimental study was performed using the loess soils collected from Lanzhou city,China.The results showed that structure,mineral compositions and soluble salts were the most important three factors controlling the variation of the matric suction in the loess soils.It seems that variation of the matric suction,particularly the residual moisture content,had inverse correlations with density of the soils,the abundance of interlayered smectite and illite (I/S) within the soils,while they had somewhat linear relations with abundance of soluble salts present in the soils.
机译:众所周知,众所周知,在不饱和状态下发生自然黄土。因此,其剪切强度主要由在不饱和土壤中呈现的原始抽吸来控制。探讨黄土土壤中的原味吸力的变化特性及其影响因素与水分含量分开,使用从中国兰州市收集的黄土污染进行了实验研究。结果表明,结构,矿物组合物和可溶性盐是控制黄土污染中的测量型在黄土污垢中的变化的最重要的三个因素。似乎变化在原始的吸入物中,特别是残留的水分含量,与土壤密度,土壤内的叠层和伊利钠(I / S)的密度有反向相关性,而它们具有稍微线性的关系,其具有丰富的可溶性盐土壤。

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