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黄土-红层滑带土界面剪切强度特性与微观机制研究

张舒晴 王新刚 陆梅 臧国军 薛晨 田发国 刘凯 闫渊

中国地质灾害与防治学报2026,Vol.37Issue(3):112-121,10.
中国地质灾害与防治学报2026,Vol.37Issue(3):112-121,10.DOI:10.16031/j.cghc.202511018

黄土-红层滑带土界面剪切强度特性与微观机制研究

Shear strength characteristics and microscopic mechanisms of the loess-red bed slip zone soil interface

张舒晴 1王新刚 1陆梅 2臧国军 3薛晨 4田发国 2刘凯 1闫渊1

作者信息

  • 1. 西北大学地质学系,陕西 西安 710069||数字孪生与重大设施灾害防控陕西省高等学校重点实验室,陕西 西安 710069
  • 2. 中国石油长庆油田分公司油气工艺研究院,陕西 西安 710018
  • 3. 中国石油长庆油田分公司油田开发事业部,陕西 西安 710018
  • 4. 西安石油大学地球科学与工程学院,陕西 西安 710065
  • 折叠

摘要

Abstract

Loess-red bed interface landslides occur frequently in Northwest China,and the critical conditions for their initiation are closely related to the dynamic evolution of the shear strength at the contact interface.To investigate the initiation mechanisms of such landslides,this study takes the slip zone soils of typical loess-red bed interface landslides as research objects.Through ring shear tests and scanning electron microscopy(SEM)analyses conducted on three types of samples(pure loess,pure red bed,and loess-red bed composites)the study systematically evaluates the evolution of shear strength and microscopic structures under varying normal stresses,water contents,and shear rates.The results show that:(1)The peak and residual shear strengths of all three soil types increase markedly with increasing normal stress.The peak shear strength exhibits a unimodal variation with water content and shows a slight increasing trend with increasing shear rate.(2)The loess-red bed composite samples are most sensitive to water content changes,with the most significant strength attenuation.Their brittleness index reaches 15.6%,significantly higher than that of the single-component soils,indicating a stronger tendency toward strain-softening failure.(3)Microscopic observations reveal that increasing water content weakens cementation of clay particles,and the enhanced lubricating of flaky minerals promotes the formation of smooth shear surfaces,leading to a significant reduction in interfacial shear strength.Integrating field investigations with laboratory tests,the initiation mechanism of loess-red bed interface landslides is clarified.The hydraulic weakening effect of the loess-red bed interface is identified as the core mechanism controlling slope instability.

关键词

黄土-红层接触面滑坡/界面剪切/剪切强度/微观结构/边坡失稳

Key words

loess-red bed interface landslide/interfacial shear/shear strength/microstructure/slope instability

分类

天文与地球科学

引用本文复制引用

张舒晴,王新刚,陆梅,臧国军,薛晨,田发国,刘凯,闫渊..黄土-红层滑带土界面剪切强度特性与微观机制研究[J].中国地质灾害与防治学报,2026,37(3):112-121,10.

基金项目

国家重点研发计划项目(2023YFC3008401) (2023YFC3008401)

陕西省自然科学基础研究计划重点项目(2024JC-ZDXM-19) (2024JC-ZDXM-19)

中国地质灾害与防治学报

1003-8035

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