EXPERIMENTAL STUDIES OF HALITE DISSOLUTION KINETICS - II - THE EFFECTOF THE PRESENCE OF AQUEOUS TRACE ANIONS AND K3FE(CN)(6)

Citation
M. Alkattan et al., EXPERIMENTAL STUDIES OF HALITE DISSOLUTION KINETICS - II - THE EFFECTOF THE PRESENCE OF AQUEOUS TRACE ANIONS AND K3FE(CN)(6), Chemical geology, 143(1-2), 1997, pp. 17-26
Citations number
25
Journal title
ISSN journal
00092541
Volume
143
Issue
1-2
Year of publication
1997
Pages
17 - 26
Database
ISI
SICI code
0009-2541(1997)143:1-2<17:ESOHDK>2.0.ZU;2-5
Abstract
The dissolution rates of compressed halite powders were measured using rotating disk techniques at constant halite saturation states and in the presence of trace concentrations of aqueous F-, Br-, and I-. All e xperiments were performed at 25 degrees C. The presence of each trace anion decreased the overall halite dissolution rate and the degree of inhibition increases with increasing anion concentration. The order of constant concentration effectiveness in inhibiting rates is I- > Br- > F-. Dissolution inhibition by these anions is interpreted to result from their adsorption on the halite surface. Application of a combined transition state theory/Langmuir adsorption model to these experiment al results allows both the description of measured rates and their ext rapolation to other solution compositions. In contrast, work on aqueou s K3Fe(CN)(6) indicates that trace quantities of this electrolyte has little effect on halite dissolution rates, except at relatively high e lectrolyte concentration or high halite saturation state where Na3Fe(C N)(6) precipitation occurs on the halite surface. (C) 1997 Elsevier Sc ience B.V.