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This device has been applied to measuring the sodium solubility and sodium-metal oxide activity at 1350 °C in the anorthite diopside eutectic melt composition of the CaO MgO Al2O3 SiO2 system.
The near-solidus melt composition of a primitive peridotite at 1 GPa has been determined by Falloon et al. (2008) with the sandwich method (Takahashi and Kushiro 1983) using a fertile peridotite composition (MM3).
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This suggests that TEXAS-VI is able to analyze the effect of prototypic melt compositions on the steam explosion phenomena.
The Dη/T product was found to be almost independent of melt composition.
E1/2 and peak potentials measured in neutral and basic melts were practically independent of melt composition; however a small but significant shift to less negative potentials was observed in the absence of chloride ions (ie in pure ImAlCl4).
Although bulk rock compositions generally do not represent melt compositions towing to selective phenocryst accumulation, trial calculations utilizing groundmass composition as the melt composition resulted in aberrant H2O estimation of the melt and, therefore, selected the bulk rock composition to calculate the equilibrium H2O contents of relatively primitive arc basalt magmas using Equation 1.
Despite the large range of tested melt compositions (0 < CaO and MgO < 40; 40 < SiO2 < 100; in wt%), we found that Na2O solubility is conveniently modeled as a linear function of the optical basicity calculated on a Na-free basis melt composition.
The influence of the melt composition on the redox ratio of copper in binary sodium silicates at 1000 °C was determined by means of in situ electrochemical methods.
Major element versus MgO variation diagram of melt compositions obtained through hydrous melting experiments by Hamada and Fujii (2008).
Therefore, it is considered a reasonable approach to calculate the density of these near-solidus melts using the density data of these reference melt compositions by interpolation.
After pressure compensation, values of densities at the target pressure were obtained at different temperatures for three of the five melt compositions.
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