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      An experimental study of basaltic glass–H2O–CO2 interaction at 22 and 50°C: Implications for subsurface storage of CO2

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      Geochimica et Cosmochimica Acta
      Elsevier BV

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          The effect of time on the weathering of silicate minerals: why do weathering rates differ in the laboratory and field?

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            Chemical weathering of basalt in Southwest Iceland; effects of runoff, age of rocks and vegetative/glacial cover

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              Mechanism, rates, and consequences of basaltic glass dissolution: II. An experimental study of the dissolution rates of basaltic glass as a function of pH and temperature

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                Contributors
                (View ORCID Profile)
                Journal
                Geochimica et Cosmochimica Acta
                Geochimica et Cosmochimica Acta
                Elsevier BV
                00167037
                February 2014
                February 2014
                : 126
                : 123-145
                Article
                10.1016/j.gca.2013.10.044
                e5bdb3fd-f472-4427-b436-75e3f4ecc113
                © 2014

                https://www.elsevier.com/tdm/userlicense/1.0/

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