Peat Decomposition

Peat Decomposition is a microbial decomposition process characterized by the anaerobic breakdown of organic matter in water-saturated peatland environments, distinguished from other decomposition pathways by its exceptionally slow rate due to persistent saturation, low temperatures, and acidic conditions that inhibit complete microbial mineralization.

1.1K

Publications

63.5K

Citations

3K

Authors

962

Institutions

Publications per year

2017–2026

265

Authors

3K

  1. TR
    Tim R. Moore

    McGill University, Canada

    25 publications · 2.1K citations

    22

    h-index

  2. CF
    Chris Freeman

    Bangor University, United Kingdom

    18 publications · 1.7K citations

    16

    h-index

  3. RL
    Raija Laiho

    University of Helsinki, Finland

    17 publications · 1.9K citations

    15

    h-index

  4. JP
    Jeffrey P. Chanton

    Florida State University, United States

    17 publications · 1.8K citations

    15

    h-index

  5. KK
    Klaus‐Holger Knorr

    University of Münster, Germany

    15 publications · 1K citations

    14

    h-index

1–5 of 3K

Venues

  1. Soil Biology and Biochemistry

    54 publications · 4.2K citations

    34

    h-index

  2. Biogeosciences

    26 publications · 3.1K citations

    25

    h-index

  3. The Science of The Total Environment

    32 publications · 1.3K citations

    23

    h-index

  4. Global Change Biology

    26 publications · 2.2K citations

    21

    h-index

  5. Canadian Journal of Soil Science

    CJSS · 24 publications · 1.2K citations

    19

    h-index

1–5