Mud Cracking
Mud Cracking is a geological phenomenon characterized by the formation of polygonal desiccation cracks on the surface of fine-grained sediments due to the evaporation of water, distinguishing it from other types of soil cracking by its occurrence in saturated, cohesive mud deposits under drying conditions.
70
Publications
3.7K
Citations
228
Authors
106
Institutions
Publications per year
2017–2026
25
Parents
70
Evolution of mud-crack patterns during repeated drying cycles
Lucas Goehring, Rebecca Conroy, Asad Akhter et al. · Soft Matter · 2010 · 147 citations
1–5 of 70
228
Vignan's Foundation for Science, Technology & Research, India
3 publications · 185 citations
3
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Vignan's Foundation for Science, Technology & Research, India
3 publications · 185 citations
3
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Max Planck Institute for Dynamics and Self-Organization, Germany
2 publications · 204 citations
2
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2
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2
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1–5 of 228
106

Centre National de la Recherche Scientifique
Paris, France
3 h-index
8 publications
370 citations

University of Glasgow
Glasgow, United Kingdom
2 h-index
4 publications
106 citations
China University of Geosciences
Wuhan, China
2 h-index
2 publications
80 citations

Vignan's Foundation for Science, Technology & Research
Guntur, India
2 h-index
6 publications
320 citations
University of Cambridge
Cambridge, United Kingdom
2 h-index
6 publications
812 citations
Institute of Rock and Soil Mechanics
Wuhan, China
2 h-index
9 publications
342 citations
University of Chinese Academy of Sciences
Beijing, China
2 h-index
3 publications
114 citations
University of Oxford
Oxford, United Kingdom
2 h-index
5 publications
237 citations
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JSR · 8 publications · 278 citations
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4 publications · 75 citations
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3 publications · 397 citations
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3 publications · 186 citations
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2 publications · 56 citations
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