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Loess structure: Evolution and a scale-based classification

delete2024-02-01
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OA
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李彦荣 封面图
李彦荣 (Yanrong Li) *
Y
Yuanyuan Wang
A
Adnan Aydın
DOI:10.1016/j.earscirev.2023.104665delete
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摘要

摘要

En 中文
Loess structure plays a vital role in the evolution of loess landforms, which mainly involves water erosion and slope collapse processes. The existing literature on loess structure lacks a comprehensive and systematic overview covering structural characteristics and features at all relevant spatial scales and explaining how they underlie these processes. This paper presents a detailed discussion of loess structure from this perspective and proposes a structural classification over three contiguous ranges of spatial scales (micro-, meso- and macro-) in terms of nature of particles and pore patterns. Then it details how the initial loess structure is modified by various environmental processes, and outlines cross-scale relations of inheritance among the solid structural elements (microscopic particle assemblies, mesoscopic fragments and macroscopic blocks) and weak segments (pores, channels, pipes, biological pores, abiogenic joints and cracks) making up the present-day loess structure. The ascending impact of ubiquitous micro-scale structure is evidenced by similarity in shapes and spatial arrangement patterns of all features across the scale ranges. Vertically aligned strong units (particle assemblies) coupled with vertically aligned weak segments (pores) defining micro-scale loess structure set the stage for the formation of the structural elements at larger scales. This structure, named as vertiloess, extends to field-scale landforms (>10 m) bounded and shaped with vertical features throughout the loess plateau.
Keyword:
Loessification
Structure classification
Structure inheritance
Vertiloess

期刊

E
Earth-Science Reviews
IF:
10
论文数:
3.8K
被引数:
4.2W

机构

T
Taiyuan University of Technology
学者数:
2.2W
论文数: 1.4W
被引数: 1.8W
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