FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2045472687> ?p ?o ?g. }

• W2045472687 endingPage "165" @default.
• W2045472687 startingPage "155" @default.
• W2045472687 abstract "The molar volumes of 19 hydrous albitic liquids (1.9 to 6.1 wt% H2Ototal) were determined at one bar and 505–765 K. These volume data were derived from density measurements on hydrous glasses at 298 K, followed by measurements of the thermal expansion of each glass from 298 K to its respective glass transition temperature. The technique exploits the fact that the volume of a glass is equal to that of the corresponding liquid at the limiting fictive temperature (T f′), and that T f′ can be approximated as the temperature near the onset of the rapid increase in thermal expansion that occurs in the glass transition interval. The volume data of this study were combined with available volume data for anhydrous, Na2O-Al2O3-SiO2 liquids to derive the partial molar volume (±1) of the H2O component in an albitic melt at ∼565 K and one bar. To extend the determination of to higher temperatures and pressures, the molar volumes of the hydrous albitic liquids determined in this study were combined with those measured by previous authors at 1023–1223 K and 480–840 MPa, leading to the following fitted values (±1) at 1673 K and one bar: (±0.46)×10−3 cm−3/mol-K, and dV¯ H 2 O total /dP=−3.82 (±0.36)×10−4 cm3/mol-bar. The measured molar volumes of this study and those of previous authors can be recovered with a standard deviation of 0.5%, which is within the respective experimental errors. There is a significant difference between the values for derived in this study as a function of temperature and pressure and those obtained from an existing polynomial, primarily caused by the previous absence of accurate density measurements on anhydrous silicate liquids. The coefficients of thermal expansion (=4.72×10−4/K) and isothermal compressibility ( T =1.66×10−5/bar) for the H2O component at 1273 K and 100 MPa, indicate that H2Ototal is the single most expansive and compressible component in silicate liquids. For example, at 1473 K and 70 MPa (conditions of a mid-ocean ridge crustal magma chamber), the presence of just 0.4 wt% H2O will decrease the density of a basaltic liquid by more than one percent. An equivalent decrease in melt density could be achieved by increasing the temperature by 175 degrees or the decreasing pressure by 230 MPa. Therefore, even minor quantities of dissolved water will have a marked effect on the dynamic properties of silicate liquids in the crustal environment." @default.
• W2045472687 created "2016-06-24" @default.
• W2045472687 creator A5073014308 @default.
• W2045472687 creator A5089295061 @default.
• W2045472687 date "1997-10-28" @default.
• W2045472687 modified "2023-09-27" @default.
• W2045472687 title "The partial molar volume, thermal expansivity, and compressibility of H 2 O in NaAlSi 3 O 8 liquid: new measurements and an internally consistent model" @default.
• W2045472687 cites W1573051457 @default.
• W2045472687 cites W1972982204 @default.
• W2045472687 cites W2052743360 @default.
• W2045472687 cites W2093854966 @default.
• W2045472687 cites W2107197640 @default.
• W2045472687 cites W2111853879 @default.
• W2045472687 cites W2122544092 @default.
• W2045472687 cites W2152410369 @default.
• W2045472687 cites W2158093609 @default.
• W2045472687 cites W2163927442 @default.
• W2045472687 cites W2340141371 @default.
• W2045472687 cites W2343701239 @default.
• W2045472687 doi "https://doi.org/10.1007/s004100050329" @default.
• W2045472687 hasPublicationYear "1997" @default.
• W2045472687 type Work @default.
• W2045472687 sameAs 2045472687 @default.
• W2045472687 citedByCount "106" @default.
• W2045472687 countsByYear W20454726872012 @default.
• W2045472687 countsByYear W20454726872013 @default.
• W2045472687 countsByYear W20454726872014 @default.
• W2045472687 countsByYear W20454726872015 @default.
• W2045472687 countsByYear W20454726872016 @default.
• W2045472687 countsByYear W20454726872017 @default.
• W2045472687 countsByYear W20454726872018 @default.
• W2045472687 countsByYear W20454726872019 @default.
• W2045472687 countsByYear W20454726872020 @default.
• W2045472687 countsByYear W20454726872021 @default.
• W2045472687 countsByYear W20454726872022 @default.
• W2045472687 countsByYear W20454726872023 @default.
• W2045472687 crossrefType "journal-article" @default.
• W2045472687 hasAuthorship W2045472687A5073014308 @default.
• W2045472687 hasAuthorship W2045472687A5089295061 @default.
• W2045472687 hasBestOaLocation W20454726872 @default.
• W2045472687 hasConcept C111368507 @default.
• W2045472687 hasConcept C113196181 @default.
• W2045472687 hasConcept C121332964 @default.
• W2045472687 hasConcept C127313418 @default.
• W2045472687 hasConcept C151730666 @default.
• W2045472687 hasConcept C178790620 @default.
• W2045472687 hasConcept C182899088 @default.
• W2045472687 hasConcept C185592680 @default.
• W2045472687 hasConcept C187714232 @default.
• W2045472687 hasConcept C188721877 @default.
• W2045472687 hasConcept C192562407 @default.
• W2045472687 hasConcept C199289684 @default.
• W2045472687 hasConcept C202271784 @default.
• W2045472687 hasConcept C20556612 @default.
• W2045472687 hasConcept C35249275 @default.
• W2045472687 hasConcept C43617362 @default.
• W2045472687 hasConcept C47463417 @default.
• W2045472687 hasConcept C84655787 @default.
• W2045472687 hasConcept C88371329 @default.
• W2045472687 hasConcept C97355855 @default.
• W2045472687 hasConceptScore W2045472687C111368507 @default.
• W2045472687 hasConceptScore W2045472687C113196181 @default.
• W2045472687 hasConceptScore W2045472687C121332964 @default.
• W2045472687 hasConceptScore W2045472687C127313418 @default.
• W2045472687 hasConceptScore W2045472687C151730666 @default.
• W2045472687 hasConceptScore W2045472687C178790620 @default.
• W2045472687 hasConceptScore W2045472687C182899088 @default.
• W2045472687 hasConceptScore W2045472687C185592680 @default.
• W2045472687 hasConceptScore W2045472687C187714232 @default.
• W2045472687 hasConceptScore W2045472687C188721877 @default.
• W2045472687 hasConceptScore W2045472687C192562407 @default.
• W2045472687 hasConceptScore W2045472687C199289684 @default.
• W2045472687 hasConceptScore W2045472687C202271784 @default.
• W2045472687 hasConceptScore W2045472687C20556612 @default.
• W2045472687 hasConceptScore W2045472687C35249275 @default.
• W2045472687 hasConceptScore W2045472687C43617362 @default.
• W2045472687 hasConceptScore W2045472687C47463417 @default.
• W2045472687 hasConceptScore W2045472687C84655787 @default.
• W2045472687 hasConceptScore W2045472687C88371329 @default.
• W2045472687 hasConceptScore W2045472687C97355855 @default.
• W2045472687 hasIssue "2-3" @default.
• W2045472687 hasLocation W20454726871 @default.
• W2045472687 hasLocation W20454726872 @default.
• W2045472687 hasOpenAccess W2045472687 @default.
• W2045472687 hasPrimaryLocation W20454726871 @default.
• W2045472687 hasRelatedWork W1974557597 @default.
• W2045472687 hasRelatedWork W2014778573 @default.
• W2045472687 hasRelatedWork W2044683374 @default.
• W2045472687 hasRelatedWork W2087411239 @default.
• W2045472687 hasRelatedWork W2281904468 @default.
• W2045472687 hasRelatedWork W2300307128 @default.
• W2045472687 hasRelatedWork W2583067947 @default.
• W2045472687 hasRelatedWork W2620660358 @default.
• W2045472687 hasRelatedWork W2771685727 @default.
• W2045472687 hasRelatedWork W4367843321 @default.
• W2045472687 hasVolume "129" @default.
• W2045472687 isParatext "false" @default.
• W2045472687 isRetracted "false" @default.

• next