Trace Element Diffusion

Trace Element Diffusion is a geochemical process that refers to the mass transfer of trace elements within solid or fluid phases through atomic-scale migration driven by concentration gradients, temperature, pressure, and crystal lattice defects, distinguishing it from bulk compositional changes or advective transport mechanisms.

79

Publications

5.9K

Citations

275

Authors

126

Institutions

Publications per year

2017–2026

15

Authors

275

  1. HO
    Hugh O’Neill

    Australian National University, Australia

    4 publications · 383 citations

    4

    h-index

  2. LR
    Luc R. Van Loon

    Paul Scherrer Institute, Switzerland

    3 publications · 266 citations

    3

    h-index

  3. JH
    Jörg Hermann

    Australian National University, Australia

    3 publications · 134 citations

    3

    h-index

  4. EB
    E. Bruce Watson

    Rensselaer Polytechnic Institute, United States

    3 publications · 129 citations

    3

    h-index

  5. MH
    Matthias Hahn

    Technische Universität Dresden, Germany

    2 publications · 72 citations

    2

    h-index

1–5 of 275

Venues

  1. Geochimica et Cosmochimica Acta

    8 publications · 696 citations

    8

    h-index

  2. Contributions to Mineralogy and Petrology

    8 publications · 1.1K citations

    8

    h-index

  3. Analytical Chemistry

    4 publications · 1.5K citations

    4

    h-index

  4. Earth and Planetary Science Letters

    3 publications · 111 citations

    3

    h-index

  5. Atmospheric Environment (1967)

    3 publications · 148 citations

    3

    h-index

1–5