Principles of thermal expansion in the feldspar system

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Principles of thermal expansion in the feldspar system

Show simple item record Hovis, Guy L. Medford, A. Conlon, M. Tether, A. Romanoski, A. 2012-01-13T19:06:50Z 2012-01-13T19:06:50Z 2010
dc.identifier.citation Hovis, G. L., et al. (2010) "Principles of thermal expansion in the feldspar system." American Mineralogist 95 (7): 1060-1068 en_US
dc.description.abstract Following the recent thermal expansion work of Hovis et al. (2008) on AlSi(3) feldspars, we have investigated the thermal expansion of plagioclase, Ba-K, and Ca-K feldspar crystalline solutions. X-ray powder diffraction data were collected between room temperature and 925 degrees C on six natural plagioclase specimens ranging in composition from anorthite to oligoclase (and as well on their K-exchanged equivalents) and five synthetic Ba-K feldspars with compositions from 25 to 99 mol% BaAl(2)Si(2)O(8). The resulting thermal expansion coefficients for volume (alpha(V)) have been combined with earlier results for end-member Na- and K-feldspars. Unlike AlSi(3) feldspars, Al(2)Si(2) feldspars, including anorthite and celsian from the present study, and Sr- and Pb-feldspar from other workers, show essentially constant, and relatively limited, thermal expansion. In the context of structures where the Lowenstein rule requires Al and Si to alternate among tetrahedra, the proximity of bridging Al-O-Si O atoms to divalent neighbors (ranging from 0 to 2) results in Ca-O (or Ba-O) bonds that are especially short. It is suggested that short bonds such as these have a partly covalent character resulting from the requirement for local charge balance. This, in turn, stiffens the structure. For feldspar series with coupled substitution, the change away from a purely divalent M-site occupant gives the substituting (less strongly bonded) monovalent cations increasingly greater influence on thermal expansion. Overall, thermal expansion in the feldspar system is well represented on a plot of alpha(V) against room-temperature volume (V(RT)), where one sees a quadrilateral bounded by data for: (1) AlSi3 feldspars whose expansion behavior is governed largely by the size of the monovalent alkali-site occupant; (2) Al2Si2 feldspars whose expansion is uniformly limited by divalent cations having stronger, partially covalent, bonds to bridging Al-O-Si O atoms; and (3,4) plagioclase and Ba-K feldspars where expansion behavior across the series transitions from one control to the other. Overall, the coefficient of thermal expansion in any binary feldspar series is a linear function of V(RT) between the pertinent end-members. This makes it possible to predict the thermal expansion behavior of any feldspar simply from knowledge of its chemical system and room-temperature volume. en_US
dc.publisher American Mineralogist en_US
dc.subject thermal expansion en_US
dc.subject feldspar en_US
dc.subject plagioclase en_US
dc.subject celsian en_US
dc.title Principles of thermal expansion in the feldspar system en_US
dc.identifier.doi 10.2138/am.2010.3484

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