首页> 外文期刊>Journal of Solution Chemistry >Thermodynamic Modeling of Aqueous Aluminum Chemistry and Solid-Liquid Equilibria to High Solution Concentration and Temperature. I. The Acidic H-Al-Na-K-Cl-H2O System from 0 to 100 °C
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Thermodynamic Modeling of Aqueous Aluminum Chemistry and Solid-Liquid Equilibria to High Solution Concentration and Temperature. I. The Acidic H-Al-Na-K-Cl-H2O System from 0 to 100 °C

机译:铝水化学和固液平衡对高溶液浓度和温度的热力学建模。 I.酸性H-Al-Na-K-Cl-H2 O系统的温度范围为0至100°C

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In this paper, we describe the development of a thermodynamic model that calculates solute/solvent activities and solid-liquid equilibria in the acidic aluminum system, H-Al3+-Na-K-Cl-H2O, to high molality from 0 ° to ≈100 °C. The model incorporates the concentration-dependent, specific interaction equations for aqueous solutions of Pitzer (Activity Coefficients in Electrolyte Solutions, 2nd edn., pp. 75–153, CRC Press, Boca Raton, 1991). Parameterization of this model adds Al3+ specific interactions in the binary Al-Cl-H2O and ternary Al-H-Cl-H2O, Al-Na-Cl-H2O and Al-K-Cl-H2O systems as well as the standard chemical potentials of AlCl3?6H2O(s) and Al(OH)3(s) (gibbsite) in the 0 ° to 100 °C range to our variable temperature (0–250 °C) model of acid-base reactions in the H-Na-K-OH-Cl-HSO4-SO4-H2O system (Christov and Moller in Geochim. Cosmochim. Acta 68:1309, 2004). In constructing our aluminum model, we used Emf, osmotic, equilibrium constant and solubility data. New Emf measurements using the cell Pt|H2(g, 101.325 kPa)|HCl(m 1), AlCl3(m 2)|AgCl(s)|Ag|Pt at temperatures ranging from 0 to 45 °C and at total ionic strength ranging from 0.1 to 3 mol?kg?1 are presented. Gibbsite and boehmite, AlOOH(s), solubility data are used in testing the model. Limitations of the model due to data insufficiencies are discussed.
机译:在本文中,我们描述了一种热力学模型的开发,该模型可计算酸性铝体系H-Al3 + -Na-K-Cl-H2 O中的溶质/溶剂活性和固液平衡,从0°到≈100°C的高摩尔浓度。该模型结合了Pitzer水溶液的浓度依赖性的特定相互作用方程式(电解质溶液中的活度系数,第二版,第75–153页,CRC出版社,Boca Raton,1991)。该模型的参数化在二元Al-Cl-H2 O和三元Al-H-Cl-H2 O,Al-Na-Cl-H2 中添加了Al3 +特异性相互作用> O和Al-K-Cl-H2 O系统以及AlCl3 ?6H2 O(s)和Al(OH)3 ()的标准化学势s)(三水铝石)在0°至100°C范围内变化为我们在H-Na-K-OH-Cl-HSO4 -SO4中酸碱反应的可变温度模型(0-250°C) -H2 O系统(Christopov和Moller in Geochim。Cosmochim。Acta 68:1309,2004)。在构建铝模型时,我们使用了电动势,渗透压,平衡常数和溶解度数据。使用单元格Pt | H2 (g,101.325 kPa)| HCl(m 1 ),AlCl3 (m 2 )| AgCl(s)| Ag进行新的电动势测量给出了在0至45°C的温度下和总离子强度在0.1至3 mol?kg?1 范围内的| Pt。锡矿和勃姆石AlOOH的溶解度数据用于测试模型。讨论了由于数据不足而导致模型的局限性。

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