Primary Mineral Dissolution

Primary Mineral Dissolution is the chemical weathering process in which primary minerals, originally formed during igneous or metamorphic rock crystallization, break down through hydrolysis, oxidation, or dissolution reactions that release constituent ions into soil solutions, thereby contributing to soil formation and nutrient cycling.

98

Publications

6.1K

Citations

327

Authors

173

Institutions

Publications per year

2017–2026

27

Authors

327

  1. SR
    Sigurður R. Gíslason

    University of Iceland, Iceland

    3 publications · 527 citations

    3

    h-index

  2. MA
    Mark A. Torres

    Rice University, United States

    3 publications · 66 citations

    3

    h-index

  3. TY
    Tao Yang

    North China Institute of Science and Technology, China

    2 publications · 182 citations

    2

    h-index

  4. JD
    J. D. Fambrough

    Indiana University, United States

    2 publications · 48 citations

    2

    h-index

  5. CM
    Carl Montgomery

    ConocoPhillips (United States), United States

    2 publications · 48 citations

    2

    h-index

1–5 of 327

Venues

  1. Geochimica et Cosmochimica Acta

    9 publications · 541 citations

    8

    h-index

  2. Chemical Geology

    8 publications · 915 citations

    8

    h-index

  3. Contributions to Mineralogy and Petrology

    4 publications · 144 citations

    4

    h-index

  4. American Mineralogist

    3 publications · 221 citations

    3

    h-index

  5. Applied Geochemistry

    3 publications · 94 citations

    3

    h-index

1–5