Wetting-induced collapse of loess: Tracing microstructural evolution

Loess is a silt-dominated, clastic yellow-to-yellowish brown aeolian sediment with high porosity and low density. The metastable microstructure of loess makes it highly susceptible to collapse, which plays a major role in landform evolution, geohazard development and engineering damages, particularl...

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Bibliographic Details
Published in:	Engineering geology Vol. 340; p. 107673
Main Authors:	Wang, Yuanyuan, Li, Yanrong
Format:	Journal Article
Language:	English
Published:	Elsevier B.V 01.10.2024
Subjects:	calcium clay deformation Force chain Hydroconsolidation model landforms loess macropores Material alteration Metastable microstructure microstructure porosity Structural evolution Structural evolution Metastable microstructure Material alteration Hydroconsolidation model Force chain
ISSN:	0013-7952
Online Access:	Get full text
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