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Showing 1 to 1 of 1 for “"mineral dissolution kinetics"”.

  1. Forsterite Dissolution Kinetics: Applications and Implications for Chemical Weathering

    Silicate minerals are the most common mineral group in the earth's crust so it is not surprising that their weathering reactions dominate the chemistry of many earth surface processes. This project used forsterite as a model system to identify the important factors that affect silicate mineral

    vt Repository record for Forsterite Dissolution Kinetics: Applications and Implications for Chemical Weathering (opens in a new tab)