西南石油大学学报(自然科学版) ›› 2025, Vol. 47 ›› Issue (5): 151-165.DOI: 10.11885/j.issn.1674-5086.2023.06.13.02

• 石油与天然气工程 • 上一篇    下一篇

碎屑堆积体基岩-覆土接触面剪切实验研究

邱恩喜1,2,3, 赵剑杰1, 万旭升1, 王知深1, 刘君1   

  1. 1. 西南石油大学土木建筑与测绘学院, 四川 成都 610500;
    2. 地质灾害防治与地质环境保护国家重点实验室, 四川 成都 610059;
    3. 中国科学院武汉岩土力学研究所岩土力学与工程国家重点实验室, 湖北 武汉 430071
  • 收稿日期:2023-06-13 发布日期:2025-11-04
  • 通讯作者: 王知深,E-mail:ashenlittle@hotmail.com
  • 作者简介:邱恩喜,1981年生,男,汉族,四川成都人,副教授,博士,主要从事岩土工程方面的研究。E-mail:enxiqiu@163.com
    赵剑杰,1995年生,男,汉族,四川泸州人,硕士,主要从事岩土工程方面的研究。E-mail:1245186559@qq.com
    万旭升,1971年生,男,汉族,四川成都人,教授,博士后,主要从事盐胀机理及寒区工程的研究。E-mail: wanxs@swpu.edu.cn
    王知深,1987年生,男,汉族,四川成都人,讲师,博士,主要从事岩土工程的数值模拟与室内实验的研究。E-mail: ashenlittle@hotmail.com
    刘君,1988年生,男,汉族,四川成都人,讲师,博士,主要从事桥梁工程、岩土工程的研究。E-mail:liujun_sichuan@126.com
  • 基金资助:
    四川省科技计划(2025ZNSFSC0331);地质灾害防治与地质环境保护国家重点实验室开放基金(SKLGP2021K017);四川高速公路建设开发集团有限公司科技项目(2022 cg 1y 3);西藏自治区科技计划重点研发(XZ202402ZY0010)

An Experimental Study of Shear at the Bedrock-cover Contact Surface of a Clastic Accumulation

QIU Enxi1,2,3, ZHAO Jianjie1, WAN Xusheng1, WANG Zhishen1, LIU Jun1   

  1. 1. School of Civil Engineering and Geomatics, Southwest Petroleum University, Chengdu, Sichuan 610500, China;
    2. State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu, Sichuan 610059, China;
    3. State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China
  • Received:2023-06-13 Published:2025-11-04

摘要: 藏东南地区地层岩性复杂,碎屑堆积体分布广泛,基覆界面多为此类堆积体边坡的潜在滑移面,其剪切力学特性是控制边坡稳定性的关键因素。为探究堆积体基覆界面的力学特性,开展了4因素[含石率、节理粗糙度系数(JRC)、含水量、基岩软硬程度]3水平的室内正交直剪实验。研究结果表明,土石混合体-基岩界面的剪应力-剪切位移曲线形态以塑性应变为主,但在高垂直压力下,JRC值为18.7的实验曲线存在应变软化现象,且应变软化阶段长短与含石率大小呈正相关;此外,剪应力-剪切位移曲线易出现“应力跳跃”现象,这主要与块石和基岩嵌固咬合、块石和基岩的破碎、块石在基岩面的位置调整有关;对于土石混合体-基岩界面抗剪强度,基岩软硬程度和含水量的影响程度最为显著,影响黏聚力和内摩擦角的关键因素是基岩软硬程度和含水量,而影响剪胀性的关键因素为JRC和基岩软硬程度,影响剪缩性的关键因素为含石率和含水量。

关键词: 藏东南, 碎屑堆积体, 基覆界面, 节理粗糙度系数, 剪切力学特性, 正交实验法

Abstract: In the southeast Tibetan region, the stratigraphic lithology is complex, the clastic accumulation is widely distributed, and the base cover interface is mostly the potential slip surface of the slope of such accumulation, whose shear mechanical properties are the key factor to control the stability of the slope. To investigate the mechanical properties of the base cover interface of the accumulation, a 3-level indoor orthogonal direct shear experiment with 4 factors (rock content, joint roughness coefficient (JRC), water content, and bedrock softness) was conducted. The results show that the shear stress-shear displacement curve pattern of the soil-stone mixture-bedrock interface is dominated by plastic strain, but there is strain softening in the test curve with a JRC value of 18.7 at high vertical pressure, and the length of the strain softening phase is positively correlated with the size of the rock content. In addition, the shear stress-shear displacement curve is prone to the phenomenon of“stress jump”, which is mainly related to the block and bedrock embedded occlusion, block and bedrock fragmentation, block in the bedrock surface position adjustment; for the shear strength of soil-stone mixture-bedrock interface, the degree of bedrock softness and water content have the most significant degree of influence. The key factors affecting cohesion and internal friction angle are the degree of bedrock softness and water content, while the key factors affecting shear expansion are JRC and bedrock softness and hardness, and the key factors affecting shear contraction are rock content and water content.

Key words: southeast Tibet, clastic accumulation, bedrock-cover interface, JRC, shear mechanical properties, orthogonal experimental method

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