کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4700766 1637731 2008 12 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Solubility of corundum in the system Al2O3–SiO2–H2O–NaCl at 800 °C and 10 kbar
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات ژئوشیمی و پترولوژی
پیش نمایش صفحه اول مقاله
Solubility of corundum in the system Al2O3–SiO2–H2O–NaCl at 800 °C and 10 kbar
چکیده انگلیسی

The solubility of corundum was measured at 800 °C and 10 kbar in NaCl–H2O–SiO2 fluids over NaCl mole fractions (XNaCl) of 0 to 0.5 and SiO2 concentrations of zero to quartz or albite + melt saturation, depending on XNaCl. Experiments were performed in a piston-cylinder apparatus. Dissolved Al2O3 and SiO2 were determined by weight losses of corundum and quartz crystals, or by bulk compositions of bracketing experiments. Although kyanite and sillimanite are slightly more stable than corundum + quartz at these pressures (P) and temperatures (T), neither appeared in any of the experiments. Results indicate that the enhancement of corundum solubility by NaCl at this P and T is further promoted by the addition of SiO2. At quartz saturation, significant enhancement occurs in initially pure H2O and addition of NaCl yields yet higher Al2O3 concentrations. At 0.03 ≤ XNaCl ≤ 0.1, quartz saturation is replaced by albite + silicate melt. The anhydrous melt composition is nearly on the join NaAlSi3O8–SiO2. Al2O3 molality rises rapidly with NaCl concentration to 0.038 at XNaCl = 0.1 and then increases more slowly to 0.052 at halite saturation. There is, in addition, a measurable reciprocal enhancement of Si solubility by virtue of dissolved Al at a fixed XNaCl. Quench pH in NaCl-bearing fluids is strongly acidic and Na/Cl < 1 in quench solutes, suggesting low pH at high P and T. These observations, combined with previous work indicating Si–Al and Na–Al complexing, lead to the hypothesis that the reciprocal solubility enhancement of Al and Si is due to formation of Na-aluminosilicate complexes. Mass balance consideration suggests that the bulk Si/Al ratio of the group of complexes ranges from 1 to 2 in the NaCl-free system, to > 3 at high XNaCl. Our data show that Al2O3 is a moderately soluble component in quartz + aluminosilicate-saturated rocks in the presence of intergranular salt solutions at deep-crustal metamorphic P–T conditions and commonly realized salinities. Al2O3 should not be regarded as a fixed reference component, because it may exhibit substantial mobility.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Chemical Geology - Volume 249, Issues 3–4, 15 April 2008, Pages 250–261
نویسندگان
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