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微膨胀泥岩地基原位水分入渗响应特征试验研究

余云燕 丁小刚 马丽娜 崔文豪 杜乾中

岩土力学2024,Vol.45Issue(3):647-658,12.
岩土力学2024,Vol.45Issue(3):647-658,12.DOI:10.16285/j.rsm.2023.1110

微膨胀泥岩地基原位水分入渗响应特征试验研究

Experimental study on in-situ water infiltration response characteristics of slightly-expansive mudstone foundation

余云燕 1丁小刚 1马丽娜 1崔文豪 1杜乾中1

作者信息

  • 1. 兰州交通大学土木工程学院,甘肃兰州 730070
  • 折叠

摘要

Abstract

The red bedded mudstone,known for its expansive and water-sensitive nature,poses a long-term potential threat to the construction and post-construction deformation control of regional highways and high-speed railroads.In this study,an in-situ water infiltration response characteristics test was conducted on slightly-expansive mudstone foundations using a red mudstone road cut in Lanzhou,Gansu Province.The test aimed to analyze the spatial and temporal evolution of swelling deformation volume,swelling force,and volumetric water content of the mudstone foundations,as well as to compare the differences between laboratory tests and in-situ tests.The results reveal that the water infiltration forms in the red mudstone foundation include fissure flow and pore flow.The distribution of water in the rock mass exhibits significant spatial and temporal heterogeneity,with rock mass fissures promoting seepage and expansion.During the infiltration process,the water absorption and expansion of the mudstone exhibit significant time dependence.The expansion amount and expansion force of the in-situ foundation experience stages of rapid increase,slow growth,and eventually fail to converge.After reaching the infiltration peak,the surface of the mudstone gradually softens or even turns into mud,leading to a decrease in the bearing capacity of foundation.Additionally,through the analysis of macroscopic expansion time history variation characteristics and microscopic pore structure distribution laws of indoor and in-situ mudstone,it is found that laboratory tests provide limited characterization of the water infiltration response characteristics of in-situ soil.

关键词

岩石力学/红层泥岩/微膨胀/原位试验/水分入渗

Key words

rock mecharucs/red mudstone/slightly-expansive/in-situ test/water infiltration

分类

建筑与水利

引用本文复制引用

余云燕,丁小刚,马丽娜,崔文豪,杜乾中..微膨胀泥岩地基原位水分入渗响应特征试验研究[J].岩土力学,2024,45(3):647-658,12.

基金项目

甘肃省教育厅产业支撑计划项目(No.2021CYZC-28) (No.2021CYZC-28)

甘肃省科技计划资助(No.21YF5GA050) (No.21YF5GA050)

甘肃省自然科学基金(No.23JRRA854).This work was supported by the Education Department of Gansu Province:Industrial Support Plan Project(2021CYZC-28),the Science and Technology Project of Gansu Province(21YF5GA050)and the Gansu Provincial Natural Science Foundation(23JRRA854). (No.23JRRA854)

岩土力学

OA北大核心CSTPCD

1000-7598

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