Spodic Horizons

Spodic Horizon is a subsurface soil horizon characterized by the accumulation of illuviated organic matter, aluminum, and often iron, which distinguishes it from other diagnostic horizons by its specific geochemical signature and role in podzolization processes.

102

Publications

5.1K

Citations

243

Authors

124

Institutions

Publications per year

2017–2026

3

Variants

Spodic Horizon

Authors

243

  1. SS
    Sadao Shoji

    Tohoku University, Japan

    8 publications · 192 citations

    8

    h-index

  2. DL
    D. L. Mokma

    Michigan State University, United States

    5 publications · 194 citations

    5

    h-index

  3. NB
    N. B. Comerford

    University of Florida, United States

    5 publications · 326 citations

    5

    h-index

  4. JA
    J. A. McKeague

    Agriculture and Agri-Food Canada, Canada

    5 publications · 865 citations

    5

    h-index

  5. JP
    Jon Petter Gustafsson

    KTH Royal Institute of Technology, Sweden

    4 publications · 196 citations

    4

    h-index

1–5 of 243

Venues

  1. Soil Science Society of America Journal

    SSSAJ · 37 publications · 2.1K citations

    23

    h-index

  2. Soil Science

    15 publications · 448 citations

    13

    h-index

  3. Canadian Journal of Soil Science

    CJSS · 4 publications · 133 citations

    4

    h-index

  4. Geoderma

    4 publications · 414 citations

    4

    h-index

  5. European Journal of Soil Science

    3 publications · 132 citations

    3

    h-index

1–5