Solubility Phase Equilibrium of the Quaternary Reciprocal System Ca2+, Mn2+//F–, SO42– + H2O at 298.15 K
Author:
Affiliation:
1. College of Chemistry and Chemical Engineering, Central South University, 410083 Changsha, P.R.China
2. Guangdong Guanghua Sci-tech Co., Ltd., Daxue Road 295, 515061 Shantou, P.R. China
Funder
National Natural Science Foundation of China
Publisher
American Chemical Society (ACS)
Subject
General Chemical Engineering,General Chemistry
Link
https://pubs.acs.org/doi/pdf/10.1021/acs.jced.9b00051
Reference13 articles.
1. Experimental Measurement of the Solid–Liquid Equilibrium of the Systems MF2 + H2O (M = Mg, Ca, Zn) from 298.15 to 353.15 K
2. Solubility and Ionic Interaction of the CaF2–CaSO4–H2O System at 298.1 K
3. Solubility of Gypsum in MSO4 Solutions (M = Mg, Mn, Co, Ni, Cu, Zn) at 298.15 K and 313.15 K
4. Experimental Determination and Modeling of the Solubility Phase Diagram of the Quaternary System MgCl2+LiCl+NH4Cl+H2O at 298.15 K and Its Applications in Industry
5. Prediction and Measurement of Gypsum Solubility in the Systems CaSO4 + HMSO4 + H2SO4 + H2O (HM = Cu, Zn, Ni, Mn) at 298.15 K
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1. Solubility Experiments and Thermodynamic Modeling for the Quaternary System MgF2–MnF2–MnSO4–H2O and Its Subsystems at 298.15 K;Industrial & Engineering Chemistry Research;2023-12-19
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5. Computational and solubility equilibrium experimental insight into Ca2+–fluoride complexation and their dissociation behaviors in aqueous solutions: implication for the association constant measured using fluoride ion selective electrodes;Physical Chemistry Chemical Physics;2021
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