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Viscosity of hydrous kimberlite and basaltic melts at high pressures. / Persikov, E. S.; Bukhtiyarov, P. G.; Sokol, A. G.

In: Russian Geology and Geophysics, Vol. 58, No. 9, 01.09.2017, p. 1093-1100.

Research output: Contribution to journal › Article › peer-review

Harvard

Persikov, ES, Bukhtiyarov, PG & Sokol, AG 2017, 'Viscosity of hydrous kimberlite and basaltic melts at high pressures', Russian Geology and Geophysics, vol. 58, no. 9, pp. 1093-1100. https://doi.org/10.1016/j.rgg.2017.08.005

APA

Persikov, E. S., Bukhtiyarov, P. G., & Sokol, A. G. (2017). Viscosity of hydrous kimberlite and basaltic melts at high pressures. Russian Geology and Geophysics, 58(9), 1093-1100. https://doi.org/10.1016/j.rgg.2017.08.005

Vancouver

Persikov ES, Bukhtiyarov PG, Sokol AG. Viscosity of hydrous kimberlite and basaltic melts at high pressures. Russian Geology and Geophysics. 2017 Sept 1;58(9):1093-1100. doi: 10.1016/j.rgg.2017.08.005

Author

Persikov, E. S. ; Bukhtiyarov, P. G. ; Sokol, A. G. / Viscosity of hydrous kimberlite and basaltic melts at high pressures. In: Russian Geology and Geophysics. 2017 ; Vol. 58, No. 9. pp. 1093-1100.

BibTeX

@article{eaf1896cc68d4b98813509d3113db208,
title = "Viscosity of hydrous kimberlite and basaltic melts at high pressures",
abstract = "New experimental data on the temperature and pressure dependences of the viscosity of synthetic hydrous kimberlite melts (82 wt.% silicate + 18 wt.% carbonate; degree of depolymerization: 100NBO/T = 313 for anhydrous melts and 100NBO/T = 247 for melts with 3 wt.% H2O) were obtained at a water pressure of 100 MPa and at lithostatic pressures of 5.5 and 7.5 GPa in the temperature range 1300-1950 °C. The temperature dependence of the viscosity of these melts follows the exponential Arrhenius-Frenkel-Eyring equation in the investigated range of temperatures and pressures. The activation energies of viscous flow for hydrous kimberlite melts were first shown to increase linearly with increasing pressure. Under isothermal conditions (T = 1800 °C), the viscosity of hydrous kimberlite melts increases exponentially by about an order of magnitude as the pressure increases from 100 MPa to 7.5 GPa. The new experimental data on the viscosity of hydrous kimberlite melts (error ± 30 rel.%) are compared with forecast viscosity data for anhydrous kimberlite and basaltic melts (100NBO/T = 51.5) and for hydrous basaltic melts (100NBO/T = 80). It is shown that at comparable temperatures, the viscosity of hydrous kimberlite melts at a moderate pressure (100 MPa) is about an order of magnitude lower than the viscosity of hydrous basaltic melts, whereas at a high pressure (7.5 GPa) it is more than twice higher. It is first established that water dissolution in kimberlite melts does not affect seriously their viscosity (within the measurement error) at both moderate (100 MPa) and high (7.5 GPa) pressures, whereas the viscosity of basaltic melts considerably decreases with water dissolution at moderate pressures (100 MPa) and remains unchanged at high pressures (P > 3.5 GPa).",
keywords = "basalt, Earth's crust, kimberlite, mantle, melt, model, pressure, temperature, viscosity, water, SYSTEM, LIQUID, MAGMATIC MELTS, EARTHS CRUST, PARAMETERS, SILICATE MELTS, ORIGIN, GPA, CONSTRAINTS, WATER",
author = "Persikov, {E. S.} and Bukhtiyarov, {P. G.} and Sokol, {A. G.}",
note = "Publisher Copyright: {\textcopyright} 2017",
year = "2017",
month = sep,
day = "1",
doi = "10.1016/j.rgg.2017.08.005",
language = "English",
volume = "58",
pages = "1093--1100",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "9",

}

RIS

TY - JOUR

T1 - Viscosity of hydrous kimberlite and basaltic melts at high pressures

AU - Persikov, E. S.

AU - Bukhtiyarov, P. G.

AU - Sokol, A. G.

N1 - Publisher Copyright: © 2017

PY - 2017/9/1

Y1 - 2017/9/1

N2 - New experimental data on the temperature and pressure dependences of the viscosity of synthetic hydrous kimberlite melts (82 wt.% silicate + 18 wt.% carbonate; degree of depolymerization: 100NBO/T = 313 for anhydrous melts and 100NBO/T = 247 for melts with 3 wt.% H2O) were obtained at a water pressure of 100 MPa and at lithostatic pressures of 5.5 and 7.5 GPa in the temperature range 1300-1950 °C. The temperature dependence of the viscosity of these melts follows the exponential Arrhenius-Frenkel-Eyring equation in the investigated range of temperatures and pressures. The activation energies of viscous flow for hydrous kimberlite melts were first shown to increase linearly with increasing pressure. Under isothermal conditions (T = 1800 °C), the viscosity of hydrous kimberlite melts increases exponentially by about an order of magnitude as the pressure increases from 100 MPa to 7.5 GPa. The new experimental data on the viscosity of hydrous kimberlite melts (error ± 30 rel.%) are compared with forecast viscosity data for anhydrous kimberlite and basaltic melts (100NBO/T = 51.5) and for hydrous basaltic melts (100NBO/T = 80). It is shown that at comparable temperatures, the viscosity of hydrous kimberlite melts at a moderate pressure (100 MPa) is about an order of magnitude lower than the viscosity of hydrous basaltic melts, whereas at a high pressure (7.5 GPa) it is more than twice higher. It is first established that water dissolution in kimberlite melts does not affect seriously their viscosity (within the measurement error) at both moderate (100 MPa) and high (7.5 GPa) pressures, whereas the viscosity of basaltic melts considerably decreases with water dissolution at moderate pressures (100 MPa) and remains unchanged at high pressures (P > 3.5 GPa).

AB - New experimental data on the temperature and pressure dependences of the viscosity of synthetic hydrous kimberlite melts (82 wt.% silicate + 18 wt.% carbonate; degree of depolymerization: 100NBO/T = 313 for anhydrous melts and 100NBO/T = 247 for melts with 3 wt.% H2O) were obtained at a water pressure of 100 MPa and at lithostatic pressures of 5.5 and 7.5 GPa in the temperature range 1300-1950 °C. The temperature dependence of the viscosity of these melts follows the exponential Arrhenius-Frenkel-Eyring equation in the investigated range of temperatures and pressures. The activation energies of viscous flow for hydrous kimberlite melts were first shown to increase linearly with increasing pressure. Under isothermal conditions (T = 1800 °C), the viscosity of hydrous kimberlite melts increases exponentially by about an order of magnitude as the pressure increases from 100 MPa to 7.5 GPa. The new experimental data on the viscosity of hydrous kimberlite melts (error ± 30 rel.%) are compared with forecast viscosity data for anhydrous kimberlite and basaltic melts (100NBO/T = 51.5) and for hydrous basaltic melts (100NBO/T = 80). It is shown that at comparable temperatures, the viscosity of hydrous kimberlite melts at a moderate pressure (100 MPa) is about an order of magnitude lower than the viscosity of hydrous basaltic melts, whereas at a high pressure (7.5 GPa) it is more than twice higher. It is first established that water dissolution in kimberlite melts does not affect seriously their viscosity (within the measurement error) at both moderate (100 MPa) and high (7.5 GPa) pressures, whereas the viscosity of basaltic melts considerably decreases with water dissolution at moderate pressures (100 MPa) and remains unchanged at high pressures (P > 3.5 GPa).

KW - basalt

KW - Earth's crust

KW - kimberlite

KW - mantle

KW - melt

KW - model

KW - pressure

KW - temperature

KW - viscosity

KW - water

KW - SYSTEM

KW - LIQUID

KW - MAGMATIC MELTS

KW - EARTHS CRUST

KW - PARAMETERS

KW - SILICATE MELTS

KW - ORIGIN

KW - GPA

KW - CONSTRAINTS

KW - WATER

UR - http://www.scopus.com/inward/record.url?scp=85031756439&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2017.08.005

DO - 10.1016/j.rgg.2017.08.005

M3 - Article

AN - SCOPUS:85031756439

VL - 58

SP - 1093

EP - 1100

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 9

ER -

ID: 9890469