Periglacial Soil Development
Periglacial Soil Development is a geomorphological process denoting the formation and transformation of soils in sub-freezing, seasonally thawed environments where freeze-thaw cycles, cryoturbation, and periglacial weathering processes dominantly shape soil stratigraphy, structure, and mineral assemblages distinct from those in non-periglacial climates.
140
Publications
7.7K
Citations
435
Authors
227
Institutions
Publications per year
2017–2026
16
140
1–5 of 140
435
11
h-index
5
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4
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3
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1–5 of 435
227
University of Wisconsin–Madison
Madison, United States
12 h-index
17 publications
542 citations

University of Waikato
Hamilton, New Zealand
6 h-index
8 publications
209 citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
16 publications
1.4K citations
University of Zurich
Zurich, Switzerland
6 h-index
22 publications
1.9K citations
Natural Resources Conservation Service
Washington, United States
4 h-index
5 publications
179 citations

Chinese Academy of Sciences
Beijing, China
4 h-index
15 publications
487 citations
United States Geological Survey
Reston, United States
4 h-index
10 publications
381 citations

University of Alaska Fairbanks
Fairbanks, United States
4 h-index
10 publications
365 citations
1–8 of 227
QR · 10 publications · 405 citations
10
h-index
9 publications · 444 citations
9
h-index
8 publications · 589 citations
8
h-index
7 publications · 300 citations
7
h-index
SSSAJ · 6 publications · 171 citations
6
h-index
1–5