Experimental determination of the solubility product of dolomite at 50-253°C

被引:52
作者
Benezeth, Pascale [1 ]
Berninger, Ulf-Niklas [1 ,2 ]
Bovet, Nicolas [3 ]
Schott, Jacques [1 ]
Oelkers, Eric H. [1 ]
机构
[1] Univ Toulouse, CNRS, GET, IRD,OMP, 14 Ave Edouard Belin, F-31400 Toulouse, France
[2] Ludwig Maximilians Univ Munchen, Dept Geo & Umweltwissensch, Theresienstr 41, D-80333 Munich, Germany
[3] Univ Copenhagen, Nanosci Ctr, Dept Chem, Univ Pk 5, DK-2100 Copenhagen, Denmark
关键词
Dolomite solubility product; Thermodynamic properties; Stability; MOLAL THERMODYNAMIC PROPERTIES; DISSOLUTION KINETICS; HYDROTHERMAL DOLOMITE; AQUEOUS-SOLUTIONS; PHANEROZOIC TIME; HEAT-CAPACITIES; CARBON-DIOXIDE; NACL MEDIA; DEGREES-C; MAGNESITE;
D O I
10.1016/j.gca.2018.01.016
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The 'dolomite problem', the scarcity of present-day dolomite formation near the Earth's surface, has attracted much attention over the past century. Solving this problem requires having reliable data on the stability and kinetics of formation of this mineral. Toward this goal, the solubility of natural dolomite (CaMg(CO3)(2)) has been measured from 50 to 253 degrees C in 0.1 mol/kg NaCl solutions using a hydrogen electrode concentration cell (HECC). The obtained apparent solubility products (Kapp-sp-dol), for the reaction: CaMg(CO3)(2) = Ca2+ + Mg2+ + 2CO(3)(2-), were extrapolated to infinite dilution to generate the solubility product constants for this reaction (Ksp degrees-dol). The derived equilibrium constants were fit and can be accurately described by log(10) Ksp degrees-dol = a + b/T (K) + cT (K) where a = 17.502, b = -4220.119 and c = -0.0689. This equation and its first and second derivatives with respect to T were used together with corresponding aqueous species properties to calculate the revised standard state thermodynamic properties of dolomite at 25 degrees C and 1 bar, yielding a Gibbs energy of formation (Delta fG degrees(298.15)) equal to -2160.9 +/- 2 kJ/mol, (log(10) Ksp degrees-dol = -17.19 +/- 0.3); an enthalpy of formation (Delta H-f degrees(298.15)) of -2323.1 +/- 2 kJ/mol, an entropy (S degrees(298.15)) of 156.9 +/- 2 J/mol/K and heat capacity (C degrees(p298.15)) of 154.2 +/- 2 J/mol/K (uncertainties are 3 sigma). The dolomite solubility product derived in this study is nearly identical to that computed using SUPCRT92 (Johnson et al., 1992) at 200 degrees C, but about one order of magnitude higher at 50 and 25 degrees C, suggesting that dolomite may be somewhat less stable than previously assumed at ambient temperatures. (C) 2018 Elsevier Ltd. All rights reserved.
引用
收藏
页码:262 / 275
页数:14
相关论文
共 69 条
[1]  
[Anonymous], J SEDIMENT PETROL
[2]  
[Anonymous], [No title captured]
[3]  
Antao SM, 2004, AM MINERAL, V89, P1142
[4]  
ARCHER DG, 1992, J PHYS CHEM REF DATA, V21, P1, DOI 10.1063/1.555913
[5]   The dolomite problem: Control of precipitation kinetics by temperature and saturation state [J].
Arvidson, RS ;
Mackenzie, FT .
AMERICAN JOURNAL OF SCIENCE, 1999, 299 (04) :257-288
[6]   The role of magnesium in the growth of calcite: An AFM study [J].
Astilleros, J. M. ;
Fernandez-Diaz, L. ;
Putnis, A. .
CHEMICAL GEOLOGY, 2010, 271 (1-2) :52-58
[7]  
Barnes I., 1964, US GEOLOGICAL SURVEY, V160, P179
[8]   Solubility product of siderite (FeCO3) as a function of temperature (25-250 °C) [J].
Benezeth, P. ;
Dandurand, J. L. ;
Harrichoury, J. C. .
CHEMICAL GEOLOGY, 2009, 265 (1-2) :3-12
[9]   Dawsonite synthesis and reevaluation of its thermodynamic properties from solubility measurements:: Implications for mineral trapping of CO2 [J].
Benezeth, Pascale ;
Palmer, Donald A. ;
Anovitz, Lawrence M. ;
Horita, Juske .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2007, 71 (18) :4438-4455
[10]   Experimental determination of the solubility product of magnesite at 50 to 200 °C [J].
Benezeth, Pascale ;
Saldi, Giuseppe D. ;
Dandurand, Jean-Louis ;
Schott, Jacques .
CHEMICAL GEOLOGY, 2011, 286 (1-2) :21-31