FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1977520137> ?p ?o ?g. }

• W1977520137 endingPage "82" @default.
• W1977520137 startingPage "70" @default.
• W1977520137 abstract "Dehydration experiments on basaltic, andesitic and dacitic glasses with 1.1, 0.7 and 1.0 wt.% total water, respectively, were performed at 400–675 °C and 0.1 MPa. The dehydration rates were measured by in situ infrared (IR) spectroscopy and modeled by assuming the diffusion of one component water (total water). The diffusivities of total water in basalt and dacite were found to be linearly dependent on total water contents, but that in andesite was weakly dependent on or independent of total water contents at water content and temperature ranges of this study. The total water diffusivities in basalt and dacite were determined by assuming the linear-dependent diffusivity on total water contents and that in andesite was obtained by assuming the constant diffusivity. The obtained diffusivities of total water D (μm2/s) can be expressed by the following equations:DBasalt=C/C0⁢exp⁡[(20.2±2.1)−(166,000±13,000)/R⁢T]DAndesite=exp⁡[(12.4±1.4)−(138,000±10,000)/R⁢T]DDacite=C/C0⁢exp⁡[(13.9±0.9)−(133,000±6000)/R⁢T],where C is the total water contents in weight percent; C0, reference total water contents of 1.1 and 1.0 wt.% for basalt and dacite, respectively; and T, temperature in Kelvin. These equations cover the temperature ranges of 400–575, 500–675 and 500–675 °C, and the water content ranges of < 1.1, 0.7 and 1.0 wt.% for basalt, andesite and dacite, respectively. The obtained diffusivities of total water in basalt, andesite and dacite and previous data for water diffusivity in rhyolite show that at 0.7 wt.% and 400–675 °C, the total water diffusivity decreases from rhyolite to andesite, but the total diffusivity in basalt is higher than that in dacite and lower than that in rhyolite. On the other hand, the results of this study predict that the diffusivities of total water in basalt to rhyolite increase with depolymerization of silicate structures at higher temperatures, which results from the crossovers of diffusivity–temperature trends." @default.
• W1977520137 created "2016-06-24" @default.
• W1977520137 creator A5034138909 @default.
• W1977520137 creator A5050764191 @default.
• W1977520137 date "2006-03-01" @default.
• W1977520137 modified "2023-09-26" @default.
• W1977520137 title "Water diffusion in basaltic to dacitic glasses" @default.
• W1977520137 cites W1614071512 @default.
• W1977520137 cites W1975629210 @default.
• W1977520137 cites W1985139759 @default.
• W1977520137 cites W1985681689 @default.
• W1977520137 cites W1989857282 @default.
• W1977520137 cites W2006217228 @default.
• W1977520137 cites W2007112380 @default.
• W1977520137 cites W2028316328 @default.
• W1977520137 cites W2035128903 @default.
• W1977520137 cites W2045172266 @default.
• W1977520137 cites W2050623549 @default.
• W1977520137 cites W2056327655 @default.
• W1977520137 cites W2062196436 @default.
• W1977520137 cites W2066242884 @default.
• W1977520137 cites W2086285344 @default.
• W1977520137 cites W2091515974 @default.
• W1977520137 cites W2096406716 @default.
• W1977520137 cites W2101045622 @default.
• W1977520137 cites W2104310391 @default.
• W1977520137 cites W2118722869 @default.
• W1977520137 cites W2128878590 @default.
• W1977520137 cites W2142843053 @default.
• W1977520137 cites W2161481750 @default.
• W1977520137 cites W2166606719 @default.
• W1977520137 cites W2169659075 @default.
• W1977520137 cites W2277305172 @default.
• W1977520137 cites W2464794336 @default.
• W1977520137 cites W4233124127 @default.
• W1977520137 doi "https://doi.org/10.1016/j.chemgeo.2005.09.009" @default.
• W1977520137 hasPublicationYear "2006" @default.
• W1977520137 type Work @default.
• W1977520137 sameAs 1977520137 @default.
• W1977520137 citedByCount "35" @default.
• W1977520137 countsByYear W19775201372012 @default.
• W1977520137 countsByYear W19775201372013 @default.
• W1977520137 countsByYear W19775201372014 @default.
• W1977520137 countsByYear W19775201372016 @default.
• W1977520137 countsByYear W19775201372017 @default.
• W1977520137 countsByYear W19775201372018 @default.
• W1977520137 countsByYear W19775201372019 @default.
• W1977520137 countsByYear W19775201372020 @default.
• W1977520137 countsByYear W19775201372021 @default.
• W1977520137 countsByYear W19775201372022 @default.
• W1977520137 countsByYear W19775201372023 @default.
• W1977520137 crossrefType "journal-article" @default.
• W1977520137 hasAuthorship W1977520137A5034138909 @default.
• W1977520137 hasAuthorship W1977520137A5050764191 @default.
• W1977520137 hasConcept C107504934 @default.
• W1977520137 hasConcept C107872376 @default.
• W1977520137 hasConcept C113196181 @default.
• W1977520137 hasConcept C120806208 @default.
• W1977520137 hasConcept C121332964 @default.
• W1977520137 hasConcept C127313418 @default.
• W1977520137 hasConcept C161509811 @default.
• W1977520137 hasConcept C17409809 @default.
• W1977520137 hasConcept C185592680 @default.
• W1977520137 hasConcept C187320778 @default.
• W1977520137 hasConcept C192241223 @default.
• W1977520137 hasConcept C199289684 @default.
• W1977520137 hasConcept C24939127 @default.
• W1977520137 hasConcept C2778769901 @default.
• W1977520137 hasConcept C2781323139 @default.
• W1977520137 hasConcept C36986328 @default.
• W1977520137 hasConcept C37668627 @default.
• W1977520137 hasConcept C55493867 @default.
• W1977520137 hasConcept C69357855 @default.
• W1977520137 hasConcept C97355855 @default.
• W1977520137 hasConceptScore W1977520137C107504934 @default.
• W1977520137 hasConceptScore W1977520137C107872376 @default.
• W1977520137 hasConceptScore W1977520137C113196181 @default.
• W1977520137 hasConceptScore W1977520137C120806208 @default.
• W1977520137 hasConceptScore W1977520137C121332964 @default.
• W1977520137 hasConceptScore W1977520137C127313418 @default.
• W1977520137 hasConceptScore W1977520137C161509811 @default.
• W1977520137 hasConceptScore W1977520137C17409809 @default.
• W1977520137 hasConceptScore W1977520137C185592680 @default.
• W1977520137 hasConceptScore W1977520137C187320778 @default.
• W1977520137 hasConceptScore W1977520137C192241223 @default.
• W1977520137 hasConceptScore W1977520137C199289684 @default.
• W1977520137 hasConceptScore W1977520137C24939127 @default.
• W1977520137 hasConceptScore W1977520137C2778769901 @default.
• W1977520137 hasConceptScore W1977520137C2781323139 @default.
• W1977520137 hasConceptScore W1977520137C36986328 @default.
• W1977520137 hasConceptScore W1977520137C37668627 @default.
• W1977520137 hasConceptScore W1977520137C55493867 @default.
• W1977520137 hasConceptScore W1977520137C69357855 @default.
• W1977520137 hasConceptScore W1977520137C97355855 @default.
• W1977520137 hasIssue "1-2" @default.
• W1977520137 hasLocation W19775201371 @default.
• W1977520137 hasOpenAccess W1977520137 @default.
• W1977520137 hasPrimaryLocation W19775201371 @default.

• next