Physical Weathering
Physical Weathering is a geological process whereby rocks and minerals are broken down into smaller fragments without altering their chemical composition, distinguished from chemical and biological weathering by the absence of chemical transformation and the predominance of mechanical forces such as freeze-thaw cycles, thermal expansion, and abrasion.
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529
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278
Institutions
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2017–2026
40
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Fine Particulate Emissions Due to Wind Erosion
Dale A. Gillette · Transactions of the ASAE · 1977 · 244 citations
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Chinese Academy of Sciences
Beijing, China
11 h-index
50 publications
1.3K citations
University of Chinese Academy of Sciences
Beijing, China
6 h-index
16 publications
369 citations
University of Wyoming
Laramie, United States
4 h-index
12 publications
936 citations
University of Oxford
Oxford, United Kingdom
4 h-index
8 publications
592 citations

University of Calabria
Rende, Italy
4 h-index
17 publications
687 citations

University of Bristol
Bristol, United Kingdom
3 h-index
7 publications
195 citations

Pennsylvania State University
State College, United States
3 h-index
5 publications
450 citations

University of Göttingen
Göttingen, Germany
3 h-index
5 publications
666 citations
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8 publications · 408 citations
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5 publications · 247 citations
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JG · 5 publications · 384 citations
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NZJG · 4 publications · 219 citations
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