Relations Between Degrees of Loess Structure and Matric Suction or Compressive Yield Deformation
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摘要: 黄土是一种具有特殊结构性的非饱和土。为探讨非饱和黄土基质吸力与构度、压缩屈服变形间的定量关系,对不同场地的黄土试样分别做原状、重塑及原状饱和状态下的单轴抗压强度试验,分析不同含水率黄土的构度变化规律,并测试对应黄土试样的土-水特征曲线,测得不同含水率下的原状黄土的基质吸力指标;在综合物理量与构度定量关系的基础上,建立了基质吸力与构度的关系,并论证了其适用性。通过等向压缩试验,测试确定了等向压缩屈服应力与构度的关系,建立了Q2、Q3黄土的压缩屈服应力与构度的关系。通过黄土的构度与压缩屈服应力及等向压缩屈服变形的关系,建立了Q2、Q3黄土的构度-压缩屈服-压缩变形的关系式。Abstract: Loess is a kind of unsaturated soil with special structure. To explore the quantitative relations between structural degrees of unsaturated loess and matric suction or compressive yield deformation, uniaxial compressive strength tests were conducted on loess specimens from different sites in intact, remolded and saturated intact conditions, and the variation laws of structural degrees of loess with different contents of water were analyzed. The soil-water characteristic curves of corresponding loess specimens were tested, and the matric suction indexes of intact loess with different contents of water were measured. Based on the quantitative relations between the physical quantity and the structural degree, the relation between matric suction and the structural degree was established, and its applicability was demonstrated. Through isotropic compression tests, the relation between the yield stress and the structural degree was determined, and the relations between the yield stress and the structured degree of Q2 loess or Q3 loess were established. Through the relations between the structural degree of loess and the compressive yield stress or isotropic compressive yield deformation, the relations among the structural degree of Q2 loess or Q3 loess, compressive yield and compressive deformation were established.
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Key words:
- loess structure degree /
- matric suction /
- compression yielding /
- compression deformation
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