EQUATION OF STATE FOR AQUEOUS SILICA SPECIES AT PRESSURES FROM 1 BAR TO 20 KBAR AND TEMPERATURES FROM 25O TO 900°C BASED ON SIMULATED VALUES OF THE DIELECTRIC CONSTANT

dc.contributor.authorWasserman E.
dc.contributor.authorWood B.
dc.contributor.authorDavies A.
dc.date.accessioned2020-11-24T02:06:17Z
dc.date.available2020-11-24T02:06:17Z
dc.date.issued1995
dc.description.abstractWe have used modified Born theory to extend the Shock-Helgeson-Sverjensky equation of state of aqueous silica to 20 kbar and 900°C. An important requirement of this equation of state is the dielectric constant of the solvent (ε), which has been experimentally measured only to 5 kbar and 550°C. Our extension of the Shock-Helgeson-Sverjensky equation relies, therefore, on molecular dynamics simulations which we have previously shown to reproduce the experimental data at densities between 0.25 and 1.0 g cm-3 and temperatures up to 1000°C (pressure ranging from 0.5 to 20 kbar). A combination of recent solubility measurements and of simulated values of ε provide the basis for a quantitative description of the thermodynamic properties of aqueous silica over most of the range of geologic interest from 1 bar to 20 kbar and 25-900°C.
dc.identifierhttps://elibrary.ru/item.asp?id=656408
dc.identifier.citationChemical Geology, 1995, , 1, 3-9
dc.identifier.issn0009-2541
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/19458
dc.titleEQUATION OF STATE FOR AQUEOUS SILICA SPECIES AT PRESSURES FROM 1 BAR TO 20 KBAR AND TEMPERATURES FROM 25O TO 900°C BASED ON SIMULATED VALUES OF THE DIELECTRIC CONSTANT
dc.typeСтатья

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