Crack Flow
Crack Flow is a hydrological process in tile drainage systems whereby subsurface water preferentially moves through naturally occurring fissures or fractures in soil or bedrock, distinguished from matrix flow by its pathway through discontinuities rather than the porous medium itself.
83
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3.3K
Citations
261
Authors
118
Institutions
Publications per year
2017–2026
20
Parents
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Yan-Hua Huang, Sheng‐Qi Yang, P.G. Ranjith et al. · Computers and Geotechnics · 2017 · 225 citations
Engineering, Geological Engineering, Materials Engineering +16
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University of Sheffield
Sheffield, United Kingdom
3 h-index
8 publications
157 citations

Xi'an Jiaotong University
Xi'an, China
3 h-index
16 publications
472 citations
China University of Mining and Technology
Xuzhou, China
3 h-index
14 publications
1.5K citations

Lehigh University
Bethlehem, United States
2 h-index
3 publications
50 citations
Cardiff University
Cardiff, United Kingdom
2 h-index
5 publications
191 citations

Polytechnique Montréal
Montreal, Canada
2 h-index
3 publications
69 citations
Xi'an University of Technology
Xi'an, China
2 h-index
4 publications
92 citations

University of Birmingham
Birmingham, United Kingdom
2 h-index
5 publications
95 citations
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JSV · 2 publications · 83 citations
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2 publications · 79 citations
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2 publications · 216 citations
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2 publications · 20 citations
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2 publications · 69 citations
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