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Evidence for SiO2-NaCl complexing in H2O-NaCl solutions at high pressure and temperature

机译:在高压和高温下H2O-NaCl溶液中SiO2-NaCl络合的证据

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Experimental studies reveal complex dissolution behavior of quartz in aqueous NaCl solutions at high temperatureand pressure, involving variation from salting-in to salting-out that changes with temperature, pressure, and salt concentration. The behavior is not explainable by traditional electrostatic theory. An alternative hypothesis appeals to complexing of SiO2 with NaCl and can explain the observations. However, the hypothesis of complexing, as previously applied, is inadequate in several respects: it neglects polymerization of solute silica, regards the SiO2-NaCl hybrid complex(es) as anhydrous, which seems unlikely, and invokes an incorrect stoichiometry of the hydrated silica monomer, now known to be Si(OH)4•2H2O. These neglected features can be incorporated into the complexing model in a revised formulation based on a simple thermodynamic analysis using existing quartz solubility data. The analysis leads to a quasi-ideal solution model with silica monomers, dimers, and two distinct hydrous SiO2-NaCl hybrid complexes with overall NaCl:H2O=1:6, one Na-bearing and one Cl-bearing. Their (equal) molar concentrations (Xhc) are governed by a pressure- and temperature-dependent equilibrium constant, Khc=Xhc2/(aNaclaH2O6), where aNacl and aH2O are the respective activities of the solvent components. The stability of the hybrid complexes (i.e., their concentration) is very sensitive to H2O activity. The entire set of experimental quartz-solubility data at 700°C, 1–15kbar, is reproduced with high fidelity by the expression logKhc=−4.585+0.2691P−2.023×10−3P2 (P is pressure in kbar), including the transition from low-pressure salting-in to high pressure salting-out. The results indicate that hybrid SiO2-NaCl complexes are the main hosts for dissolved silica at NaCl concentrations greater than 6 wt%, which are likely common in crustal fluids. At higher temperatures, approaching the critical end point in the system SiO2-H2O, the model becomes progressively inaccurate, probably because polymers higher than the dimer become significant as SiO2 concentration increases.
机译:实验研究表明,在高温高压下,石英在NaCl水溶液中的溶解行为复杂,涉及到随温度,压力和盐浓度的变化而从盐化到盐化的变化。这种行为无法用传统的静电理论来解释。另一个假设吸引了SiO2与NaCl的络合,并可以解释这些现象。但是,以前应用的络合假说在几个方面是不充分的:它忽略了溶质二氧化硅的聚合,认为SiO2-NaCl杂化络合物是无水的,这似乎不太可能,并且引起了水合二氧化硅化学计量的错误。单体,现在已知为Si(OH)4•2H2O。这些被忽略的特征可以在使用现有石英溶解度数据进行简单热力学分析的基础上,以修订后的公式纳入复杂模型中。分析得出了具有二氧化硅单体,二聚体和两种截然不同的含水SiO2-NaCl杂化配合物(总NaCl:H2O = 1:6),一种含Na和一种含Cl的准理想溶液模型。它们的(相等)摩尔浓度(Xhc)由压力和温度相关的平衡常数Khc = Xhc2 /(aNaclaH2O6)决定,其中aNacl和aH2O是溶剂组分的各自活性。杂合复合物的稳定性(即它们的浓度)对H2O活性非常敏感。通过表达式logKhc = −4.585 + 0.2691P−2.023×10−3P2(P为压力,单位为kbar),以高保真度再现了700°C,1–15kbar时的整个实验石英溶解度数据集。从低压盐析到高压盐析。结果表明,杂化SiO2-NaCl络合物是NaCl浓度大于6 wt%时溶解二氧化硅的主要基质,这在地壳流体中很常见。在更高的温度下,接近系统SiO2-H2O的临界终点,模型逐渐变得不准确,这可能是因为随着SiO2浓度的增加,高于二聚体的聚合物变得很重要。

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