首页|期刊导航|工程地质学报|干湿循环作用下黏黄土微观结构响应及强度劣化机制研究

干湿循环作用下黏黄土微观结构响应及强度劣化机制研究OA

MICROSCOPIC RESPONSE OF CLAYEY LOESS TO WETTING-DRYING CYCLES AND STRENGTH DETERIORATION MECHANISM

中文摘要英文摘要

黏黄土对降雨、干旱等引起的土体含水率频变、骤变较为敏感,力学性能劣化显著.本文通过三轴剪切试验研究干湿循环作用下黏黄土的强度劣化规律;测量并记录不同受力状态(侧限、无侧限)的黄土试样宏观胀缩特性及裂隙发育过程;利用压汞法(MIP)、X射线衍射(XRD)等研究黄土孔隙结构、物质组成等微观结构响应,以此分析黏黄土强度劣化的微观机制.研究结果表明:干湿循环作用使黄土抗剪强度发生劣化,高围压下,劣化效应显著增强.强度的劣化主要体现为内摩擦角随干湿循环次数的增加呈降低趋势,黏聚力呈先减小后增大的趋势.干湿循环作用导致黄土内团聚体散化、黏粒含量增加,黏土矿物的亲水能力增强.无侧限条件下,孔隙比随干湿循环次数呈增加趋势,孔隙尺寸整体增大,结构更加疏松.侧限条件下,孔隙比没有明显的规律性变化,小孔隙(2~8 μm)占比明显降低.两种条件下孔隙结构的变化与宏观变形、裂隙发育基本一致.黄土强度的劣化受控于颗粒级配、颗粒间胶结作用、孔隙结构等因素的变化.干湿循环作用下,黏粒含量的增加一定程度强化了颗粒间的胶结作用;与此同时,团聚体散化以及疏松的孔隙结构弱化了颗粒、团聚体之间的咬合摩擦.后续研究黄土干湿作用下宏观水-力行为时应重点关注矿物组分及性质的变化,以及黄土体的实际受力状态.

Clayey loess is sensitive to frequent and sudden change in water content caused by precipitation and drought,the mechanical properties deterioration is therefore serious.This paper focuses on strength deterioration of the clay loess subjected to wetting-drying(WD)cycles based on triaxial shear tests.The macroscopic swell-shrink feature and crack development for both confined and unconfined samples were measured and recorded.The changes in pore structure and mineral composition were analyzed using mercury intrusion method(MIP)and X-ray diffraction(XRD)to explore the strength deterioration mechanism.The results indicate that WD cycles induced loess strength deterioration,particularly,the deterioration enhanced under high confining pressure.The internal friction angle decreased with the cycle number increasing,while the cohesion slightly decreased at first and then increased greatly.At the microscopic scale,WD cycles dispersed the clay aggregates in loess soils and increased the clay content as well as the hydrophilicity of clay minerals.For the unconfined loess samples,the void ratio increased with the cycle number increasing,the pore size totally increased and the pore structure became looser.While when the loess samples were confined by cutting ring,the void ratio changed slightly without regularity,the volume percentage of small pores(2~8 μm)decreased obviously.The above two types of change in pore structure were consistent with the macroscopic deformation and crack development of the loess samples with and without lateral restraint.The deterioration of loess strength is controlled by the grain-size distribution,cementation between particles,pore structure and some other factors.The increase of clay content caused by WD cycles enhanced the cementation between particles,while the discretization of clay aggregates and loess pore structure weakened the occluding friction among particles.In the future work,the change in clay mineral composition and property with WD cycles should be paid attention to when addressing macroscopic behaviours,in addition,the actual confined or unconfined condition should be considered because the pore structure showed different responses to WD cycles.

陈航航;魏亚妮;范文;史梓豪

长安大学,地质工程与测绘学院,西安 710054,中国长安大学,地质工程与测绘学院,西安 710054,中国长安大学,地质工程与测绘学院,西安 710054,中国||矿山地质灾害成灾机理与防控重点实验室,西安 710004,中国长安大学,地质工程与测绘学院,西安 710054,中国

天文与地球科学

黏黄土干湿循环强度劣化黏土矿物孔隙结构

Clayey loessWetting-drying cycleStrength deteriorationClay mineralPore structure

《工程地质学报》 2026 (2)

449-462,14

国家自然科学基金项目(资助号:42372314,42220104005),中央高校基本科研业务费专项资金(资助号:300102263204).This research is supported by the National Natural Science Foundation of China(Grant Nos.42372314,42220104005)and the Fundamental Re-search Funds for the Central Universities,CHD(Grant No.300102263204).

10.13544/j.cnki.jeg.2025-0034

评论