The Tunisian salt lakes are considered as an important materials resource useful for industry and agriculture. They are called sebkhat or chott, and they cover a large part of Tunisian land. Their brines correspond to the quinary system: Na + , K + , Mg 2+ / Cl, SO 4 2 H 2 O. In the first part of this paper, a short description and abstracted geochemical and economical data about some Tunisian salt lakes are given. In the second part, the fitting equations used for modeling the quinary system are established and applied to the subsystems NaClKClH 2 O, NaClMgCl 2 H 2 O, KClMgCl 2 H 2 O, and to NaClNa 2 SO 4 H 2 O, KClK 2 SO 4 H 2 O, Na 2 SO 4 K 2 SO 4 H 2 O. The coherence between the calculated and the experimental diagrams is discussed.
Contents
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Publicly AvailableTreatment of Tunisian salt lakes using solubility phase diagramsJanuary 1, 2009
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Publicly AvailablePhase diagrams at high temperature and high pressure. Determination and consequent developmentsJanuary 1, 2009
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Publicly AvailableThermodynamic modeling of crystal deposition in humansJanuary 1, 2009
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Publicly AvailableDissolution and formation of nuclear materials in molten mediaJanuary 1, 2009
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Publicly AvailableSolid-state solubility and its limits. The alkali halide caseJanuary 1, 2009
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Publicly AvailableReliable solubility data in the age of computerized chemistry. Why, how, and when?January 1, 2009
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Publicly AvailableSolubility equilibria in multicomponent oceanic salt systems from t = 0 to 200 °C. Model parameterization and databasesJanuary 1, 2009
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Publicly AvailableDefinitions of basic terms relating to low-molar-mass and polymer liquid crystals (IUPAC Recommendations 2001)January 1, 2009