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Solubility of Siderite (FeCO3) in NaCl Solutions
Authors:Carlos A. R. Silva  Xuewu Liu  F. J. Millero
Affiliation:(1) Departamento de Oceanografia e Limnologia, Centro de Biociências, Universidade Federal do Rio Grande do Norte, CP 1202, 59075-970, Brasil;(2) Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Causeway, Miami, Florida, 33149-1098
Abstract:The solubility of siderite (FeCO3) at 25°C under constant CO2 partial pressure [p(CO2)] was determined in NaCl solutions as a function of ionic strength. The dissolution of FeCO3(s) for the reaction

$$begin{gathered}{FeCO}_{3} ({s}) + 2{text{H}}^+ = {Fe}^{2 + } + {CO}_{2} ({g}) + {H}_{2}{O} hfill  K{so}^{*} = [{Fe}^{2 + } ];p{CO}_{2} /[{H}^{ + } ]^2 hfill  end{gathered} $$
has been determined as a function of pH = – log[H+]. From these values we have determined the equilibrium constant for the stoichiometric solubility to FeCO3(s) in NaCl

$$K_{so}^{*} = [{Fe}^{2 + }];left[{CO}_{3}^{2} - right]$$
These values have been fitted to the equation

$$log [K_{sp}^{*}] = - 10.9 + 2.518;I^{0.5} - 0.657;I$$
with a standard error of s = 0.15. The extrapolated value of log(Kosp) – 10.9 in water is in good agreement with data in the literature (– 10.8 to – 11.2) determined in solutions of different composition and ionic strength.The measured values of the activity coefficient, gammaT(Fe2+) gammaT(CO32–), have been used to estimate the stability constant for the formation of the FeCO3 ion pair, K*(FeCO3). The values of K*(FeCO3) have been fitted to the equation (s = 0.09)

$$log [K^* ({FeCO}_{3})] = 6.3 - 2.3135;I^{0.5} + 0.7091;I$$
The value of log[Ko(FeCO3)] in water found in this study (6.3 ± 0.2) is slightly higher than the value found from extrapolations in 1.0 m NaClO4 solutions (5.9 ± 0.2). These differences are related to the model used to determine the activity coefficients of the Fe(II) and carbonate species in the two solutions.
Keywords:Siderite  solubility  activity coefficients  sodium chloride  Pitzer equations
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