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• W2007112380 endingPage "1317" @default.
• W2007112380 startingPage "1314" @default.
• W2007112380 abstract "Density measurements on several hydrous (≤19 mole percent of H 2 O) silicate melts demonstrate that dissolved water has a partial molar volume ( V̄ H 2 O ) that is independent of the silicate melt composition, the total water concentration, and the speciation of water. The derived value for V̄ H 2 O is 22.9 ± 0.6 cubic centimeters per mole at 1000°C and 1 bar of pressure, whereas the partial molar thermal expansivity (∂ V̄ H 2 O /∂ T ) and compressibility (∂ V̄ H 2 O /∂ P ) are 9.5 ± 0.8 × 10 −3 cubic centimeters per mole per kelvin and −3.2 ± 0.6 × 10 −4 cubic centimeters per mole per bar, respectively. The effect of 1 weight percent dissolved H 2 O on the density of a basaltic melt is equivalent to increasing the temperature of the melt by ∼400°C or decreasing the pressure of the melt by ∼500 megapascals. These measurements are used to illustrate the viability of plagioclase sinking in iron-rich basaltic liquids and the dominance of compositional convection in hydrous magma chambers." @default.
• W2007112380 created "2016-06-24" @default.
• W2007112380 creator A5073014308 @default.
• W2007112380 creator A5088998476 @default.
• W2007112380 date "1999-02-26" @default.
• W2007112380 modified "2023-10-14" @default.
• W2007112380 title "The Density of Hydrous Magmatic Liquids" @default.
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• W2007112380 doi "https://doi.org/10.1126/science.283.5406.1314" @default.
• W2007112380 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/10037599" @default.
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