The effect of pH, grain size, and organic ligands on biotite weathering rates-Reference-Cited by-同舟云学术

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The effect of pH, grain size, and organic ligands on biotite weathering rates

Published:2015-09 Issue: Volume:164 Page:127-145
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Bray Andrew W.,Oelkers Eric H.,Bonneville Steeve,Wolff-Boenisch Domenik,Potts Nicola J.,Fones Gary,Benning Liane G.

Funder

UK Natural Environment Research Council Weathering Science Consortium

The Geological Society of London

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference78 articles.

1. The influence of pH on biotite dissolution and alteration kinetics at low temperature;Acker;Geochim. Cosmochim. Acta,1992

2. Fungal degradation of calcium-, lead- and silicon-bearing minerals;Adeyemi;Biometals,2005

3. Basal plane reactivity of phyllosilicates studied in situ by hydrothermal atomic force microscopy (HAFM);Aldushin;Geochim. Cosmochim. Acta,2006

4. Mineral dissolution kinetics as a function of distance from equilibrium – new experimental results;Arvidson;Chem. Geol.,2010

5. Dissolution rates of phyllosilicates as a function of bacterial metabolic diversity;Balland;Geochim. Cosmochim. Acta,2010

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