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

Authors

435

  1. JG
    James G. Bockheim

    University of Wisconsin–Madison, United States

    11 publications · 395 citations

    11

    h-index

  2. ME
    Markus Egli

    University of Zurich, Switzerland

    5 publications · 421 citations

    5

    h-index

  3. FC
    F. C. Ugolini

    University of Florence, Italy

    4 publications · 161 citations

    4

    h-index

  4. DH
    Daniel H. Mann

    University of Alaska Fairbanks, United States

    4 publications · 123 citations

    4

    h-index

  5. JG
    Jean‐Claude Gloaguen

    Université de Rennes, France

    3 publications · 187 citations

    3

    h-index

1–5 of 435

Venues

  1. Quaternary Research

    QR · 10 publications · 405 citations

    10

    h-index

  2. Arctic Antarctic and Alpine Research

    9 publications · 444 citations

    9

    h-index

  3. Geoderma

    8 publications · 589 citations

    8

    h-index

  4. CATENA

    7 publications · 300 citations

    7

    h-index

  5. Soil Science Society of America Journal

    SSSAJ · 6 publications · 171 citations

    6

    h-index

1–5