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有荷干湿循环下滑带土细观结构演变机制及宏观力学多尺度研究

黎细军 邓黎旭 张国栋 易庆林 邓茂林 尚敏 李俊 张亚鑫 杨剑飞

水利水电技术(中英文)2024,Vol.55Issue(12):180-192,13.
水利水电技术(中英文)2024,Vol.55Issue(12):180-192,13.DOI:10.13928/j.cnki.wrahe.2024.12.015

有荷干湿循环下滑带土细观结构演变机制及宏观力学多尺度研究

A multi-scale study on the evolution mechanism of micro-structure and macro-mechanics of soil in sliding zone under drying-wetting cycles with loads

黎细军 1邓黎旭 1张国栋 1易庆林 1邓茂林 1尚敏 1李俊 1张亚鑫 1杨剑飞1

作者信息

  • 1. 防灾减灾湖北省重点实验室,湖北宜昌 443002||湖北长江三峡滑坡国家野外观测研究站,湖北宜昌 443002||三峡库区地质灾害教育部重点实验室,湖北宜昌 443002
  • 折叠

摘要

Abstract

[Objective]The slip zone of landslides can be affected by changes in water levels in the reservoir,leading to cycles of wetting and drying with loads that can impact the stability of landslides.However,this complex issue involves the evolution of mi-crostructure and macroscopic mechanical properties at multiple scales.[Methods]The study focuses on the sliding zone soil of the Shuping landslide in the Three Gorges Reservoir area.Under loaded conditions,direct shear tests,scanning electron microscopy(SEM),and nuclear magnetic resonance(NMR)tests were conducted on reshaped sliding zone soil that underwent different wet dry cycles.The strength and microstructure evolution of reshaped sliding zone soil under loaded wet dry cycles were analyzed.[Results]With the increase in wetting and drying cycles under loading,the cohesion of the soil gradually increases(with a degra-dation degree of approximately-30%),while the internal friction angle of the soil shows a decreasing trend(with a degradation de-gree of approximately 22%);Microscopically,the small pores gradually connect to form large pores,but macroscopically,the po-rosity decreases exponentially(with a decrease of approximately 7%).Additionally,the micro-characteristics indicate a gradual disintegration of clump-like aggregates with each cycle,and a transformation in the way clay particles associate,from edge-to-face and edge-edge flocculation to face-to-face aggregation.These changes ultimately result in the friction angle deterioration.Mean-while,there is a significant positive correlation between moisture content and cohesion of dry soil,indicating that increased cohesion is closely related to the presence of water in clay minerals.[Conclusion]This study reveals the mechanism of soil microstructure's multiscale evolution,which is significant for studying geological hazards because of soil structure deterioration.

关键词

滑带土/有荷干湿循环/细观结构/多尺度演变/黏土矿物/滑坡/模型试验

Key words

soil in sliding zone/drying-wetting cycles with loads/microstructure/muti-scale structure evolution/clay minerals/landslides/model testing

分类

天文与地球科学

引用本文复制引用

黎细军,邓黎旭,张国栋,易庆林,邓茂林,尚敏,李俊,张亚鑫,杨剑飞..有荷干湿循环下滑带土细观结构演变机制及宏观力学多尺度研究[J].水利水电技术(中英文),2024,55(12):180-192,13.

基金项目

国家自然科学基金青年科学基金项目(4190323) (4190323)

国家野外科学观测研究站开放基金(2018KTL07) (2018KTL07)

水利水电技术(中英文)

OA北大核心CSTPCD

1000-0860

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