The chemical composition and charge of the biotite near-surface, in contact with NaCl
bearing aqueous solutions at 25° C from pH 1 to 12, have been derived via zeta potential …

The close spatial association of detrital biotite with diagenetic carbonate, prehnite, or
laumontite is attributed to attraction of H+ to the mica surface, resulting in an increase in pore …

Biotite dissolution rates were determined at 25° C, at pH 2–6, and as a function of mineral
composition, grain size, and aqueous organic ligand concentration. Rates were measured …

Microbially assisted dissolution of biotite was studied using four environmentally important
species (Bacillus subtilis, Shewanella putrefaciens, Streptomyces acisdiscabies, and …

Large single crystals of biotite and near endmember phlogopite were reacted with acidic Cr
(VI)-and Cr (III)-bearing solutions, at 24–27° C and 1 atm. After reaction of the micas with Cr …

The rate and stoichiometry of biotite dissolution were studied in the pH range 2–10 using
thin-film continuous flow reactors. The release of interlayer K is relatively fast and becomes …

We have used a direct imaging technique, in situ atomic force microscopy (AFM), to observe
the dissolution of the basal biotite surface by oxalic acid over a range of temperatures close …

Large single crystals of biotite and near-endmember phlogopite were reacted with aqueous
solutions bearing 20 μM Cr (VI) and different concentrations of NaCl, LiCl, RbCl, CsCl …

The aim of this study was to investigate the dissolution and transformation characteristics of
phyllosilicate under low molecular weight organic acids in the farmland environment (pH 4.0 …

We have used a direct imaging technique, in situ atomic force microscopy (AFM) to observe
the earliest stages of the dissolution of a biotite surface byoxalic acid at temperatures close …