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The effect of Al and water on the compressibility of diopside

Polina Gavrilenko, Tiziana Boffa Ballaran and Hans Keppler
The effect of Al and water on the compressibility of diopside
American Mineralogist (April 2010) 95 (4): 608-616

Abstract

The equation of state of four clinopyroxenes was measured at room temperature by single-crystal X-ray diffraction in a diamond anvil cell up to 10 GPa. The bulk modulus of pure diopside is K (sub 0) =106(1) GPa, K'=6.1(5). The bulk modulus of a pure diopside containing 600 ppm by weight of water is K (sub 0) =108(1) GPa, K'=6.3(4). The effect of water on the elastic properties of pure diopside is therefore small. In addition, we studied two hydrous samples containing 9.6 wt% Al (sub 2) O (sub 3) that were synthesized on the join between diopside and Ca-Tschermak component (CaAlAlSiO (sub 6) ). The sample containing 976 ppm of water yielded K (sub 0) =120(1) GPa and K'=4.4(4), while the sample containing 2510 ppm of water yielded K (sub 0) =114(1) GPa and K'=5.8(5). Aluminum therefore clearly makes the clinopyroxene stiffer. A direct comparison of the two aluminous samples, however, is difficult, since the sample containing the lower amount of water appears also to contain some M2 vacancies, indicating some solid solution with Ca-Eskola component. This is consistent with a different substitution mechanism for water in the two samples, as indicated by differences in the infrared spectra. Our results suggest that detecting upper mantle water contents from variations in P wave velocities is probably impossible. Increasing water fugacity will increase the Al content in pyroxenes and hence their stiffness. The resulting increase in bulk modulus is opposite to the effect of water on olivine. The different response of olivine and pyroxenes to water is due to a different dissolution mechanism. Under conditions of low silica activity, water in clinopyroxenes is mostly dissolved by the coupled substitution of Al (super 3+) +H (super +) for Si (super 4+) , which does not create any vacancies. This dissolution mechanism is consistent with polarized infrared data (one single band at 3650 cm (super -1) ), with an excess of tetrahedral Al in the microprobe analyses of hydrous samples and with the results of structure refinements. Infrared bands at 3450 and 3500 cm (super -1) , which are seen in the Al-rich diopside with lower water content of this study, probably indicate Al on M1 charge compensated by a M2 vacancy and a proton.


ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 95
Serial Issue: 4
Title: The effect of Al and water on the compressibility of diopside
Affiliation: Universitaet Bayreuth, Bayerisches Geoinstitut, Bayreuth, Federal Republic of Germany
Pages: 608-616
Published: 201004
Text Language: English
Publisher: Mineralogical Society of America, Washington, DC, United States
References: 51
Accession Number: 2010-039439
Categories: Mineralogy of silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 8 tables
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, copyright, Mineralogical Society of America. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 201022
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