Solubility and dissolution kinetics of dolomite in Ca-Mg-HCO3/CO3 solutions at 25 degrees C and 0.1 MPa carbon dioxide

Dolomite solubility in water has been measured by a number of different methods during the past several decades, yielding inconsistent and unreliable results that vary more than three orders of magnitude. The most commonly used best value for dolomite solubility in water is based on HCI solution cal...

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Veröffentlicht in:Soil Science Society of America journal 2000-11, Vol.64 (6), p.1959-1968
Hauptverfasser: Sherman, Leslie A, Barak, Phillip
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container_end_page 1968
container_issue 6
container_start_page 1959
container_title Soil Science Society of America journal
container_volume 64
creator Sherman, Leslie A
Barak, Phillip
description Dolomite solubility in water has been measured by a number of different methods during the past several decades, yielding inconsistent and unreliable results that vary more than three orders of magnitude. The most commonly used best value for dolomite solubility in water is based on HCI solution calorimetry at 300.15K, which is not confirmed by earlier determinations based on heat capacity of dolomite nor by more recent acid solution and metal oxide melt calorimetric measurements.
doi_str_mv 10.2136/sssaj2000.6461959x
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source Wiley Online Library - AutoHoldings Journals
subjects Calorimetry
Carbon dioxide
Dolomite
Kinetics
Minerals
Solubility
Water
title Solubility and dissolution kinetics of dolomite in Ca-Mg-HCO3/CO3 solutions at 25 degrees C and 0.1 MPa carbon dioxide
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