Periglacial Soils
Periglacial Soils is a pedological construct denoting a soil type distinguished by development under periglacial conditions characterized by freeze-thaw cycles, permafrost influence, and cryoturbation in high-latitude or high-altitude environments.
108
Publications
4.9K
Citations
320
Authors
191
Institutions
Publications per year
2017–2026
20
Parents
108
Recognition of cryoturbation for classifying permafrost-affected soils
James G. Bockheim, C. Tarnocai · Geoderma · 1998 · 197 citations
1–5 of 108
320
6
h-index
4
h-index
4
h-index
3
h-index
3
h-index
1–5 of 320
191
University of Wisconsin–Madison
Madison, United States
7 h-index
7 publications
573 citations

University of Alaska Fairbanks
Fairbanks, United States
6 h-index
12 publications
898 citations

Stockholm University
Stockholm, Sweden
5 h-index
8 publications
506 citations

Imperial College London
London, United Kingdom
4 h-index
5 publications
267 citations
Universität Hamburg
Hamburg, Germany
4 h-index
10 publications
720 citations
National Park Service
Washington, United States
3 h-index
3 publications
561 citations
United States Geological Survey
Reston, United States
3 h-index
4 publications
985 citations

Universidade Federal de Viçosa
Viçosa, Brazil
3 h-index
7 publications
416 citations
1–8 of 191
8 publications · 262 citations
8
h-index
QR · 5 publications · 249 citations
5
h-index
4 publications · 259 citations
4
h-index
4 publications · 163 citations
4
h-index
4 publications · 174 citations
4
h-index
1–5