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The partial molar volume of carbon dioxide in peridotite partial melt at high pressure

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Please use this identifier to cite or link to this item: http://hdl.handle.net/1928/11109

The partial molar volume of carbon dioxide in peridotite partial melt at high pressure

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Title: The partial molar volume of carbon dioxide in peridotite partial melt at high pressure
Author: Duncan, Megan
Advisor(s): Agee, Carl
Committee Member(s): Jones, Rhian
King, Penelope
Department: University of New Mexico. Dept. of Earth and Planetary Sciences
Subject: partial molar volume of CO2
high pressure experiments
komatiite
kimberlite
LC Subject(s): Komatiite.
Forsterite.
Kimberlite.
Alkalic igneous rocks.
Carbon dioxide.
Degree Level: Masters
Abstract: The partial molar volume of CO2 (VCO2) in silicate melt was determined for a komatiite composition using high pressure sink/float experiments in a multi-anvil press. The density of the experimental melt at pressure was determined by observing sinking and floating of pure forsterite (Fo100) and 90% forsterite (Fo90) buoyancy markers. Values for VCO2 were bracketed at 4.3 GPa (23.71 cm3/mol) and at 5.5 GPa (22.06 cm3/mol), normalized to 1850°C. Combining the current data with previous work we now more accurately constrain the compression curve of VCO2 over the pressure range of 1 bar to 20 GPa. These data allow the calculation of density at pressure of carbonated silicate melts, such as kimberlite and silica undersaturated alkali basalts, and the determination of their buoyancy and eruptibility.
Graduation Date: July 2010
URI: http://hdl.handle.net/1928/11109


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