基于离散元法的粘土颗粒软化致黄土坍塌机理研究

IF 2.7 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Jinduo Yang, Xi-An Li, Li Wang, Biao Qin, Lincui Li
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引用次数: 0

摘要

黄土塌陷机理是研究黄土地区灾害的重要依据。本文采用采用元法(DEM)将崩塌的内部机理与其宏观表现联系起来。我们首次提出粘土颗粒与水接触后的软化是导致黄土坍塌的直接原因。在此基础上,提出了一种增强虚拟粘土法(Enhanced Virtual Clay Method, EVCM),该方法将有限元法(FEM)与DEM相结合,建立了基于微观粘土颗粒行为的黄土宏观崩塌数值模型。结果表明,数值模型的崩塌沉降值与理论值高度吻合。黄土的崩塌沉降主要来源于颗粒位移产生的孔隙空间,其次是黏土软化导致的黄土颗粒有效体积的减小。本文提出的黄土崩塌数值模型将微观黏土颗粒行为与宏观崩塌行为联系起来,为研究黄土宏微观性质之间的关系开辟了新的途径。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on the mechanism of loess collapse induced by clay particle softening based on discrete element method

The mechanism by which loess collapses serves as a critical basis for researching disasters in loess regions. This paper employed the employs element method (DEM) to link the internal mechanisms of collapse with its macroscopic manifestations. We first proposed that the softening of clay particles upon water contact is the direct cause of loess collapse. Additionally, an Enhanced Virtual Clay Method (EVCM) was developed, which integrates the finite element method (FEM) and DEM to construct a numerical model for characterizing macroscopic collapse of loess based on microscopic clay particle behaviours. The results revealed that the collapse settlement of the numerical model was highly consistent with theoretical values. Primarily, the collapse settlement of loess originated from the pore space generated by particle displacement, with secondary contributions from the reduction in the effective volume of loess particles caused by clay softening. The numerical model of loess collapse proposed in this study associates microscopic clay particle behaviours with macroscopic collapse behaviours, opening a new pathway for researching the relationship between the macro–micro-properties of loess.

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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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