V23D-4819:
Thermal Expansion of Fluorapatite-Chlorapatite Solid Solutions
Tuesday, 16 December 2014
Guy L Hovis1, Tony Abraham2, William Hudacek3, Sarah Wildermuth4, Brian Scott1, Caitlin Altomare5, Aaron Medford6, Maricate Conlon7, Matthew Morris1, Amanda Leaman1, Christine Almer1, Gary Tomaino8 and Daniel Eric Harlov9, (1)Lafayette College, Geology and Environmental Geosciences, Easton, PA, United States, (2)University of Cambridge, Earth Sciences, Cambridge, United Kingdom, (3)American Museum of Natural History, MAT Program, New York, NY, United States, (4)University of Kansas, Geology, Lawrence, KS, United States, (5)Rice University, Earth Science, Houston, TX, United States, (6)University of Maine, Orono, ME, United States, (7)ENVIRON International Corporation Princeton, Princeton, NJ, United States, (8)Specialty Minerals, Inc., 640 13th. St., Easton, PA, United States, (9)Deutsches GeoForschungsZentrum GFZ, Potsdam, Germany
Abstract:
X-ray powder diffraction experiments have been performed on fifteen fluorapatite-chlorapatite solid solutions synthesized and chemically characterized at the GeoForschungsZentrum - Potsdam (Hovis and Harlov, 2010; Schettler, Gottschalk, and Harlov, 2011), as well as two natural near-end-member samples, from room temperature to ~900 °C at 50 to 75 °C intervals. NIST 640a Si was employed as an internal standard; data from Parrish (1953) were used to determine Si peak positions at elevated temperatures. Unit-cell parameters calculated using the software of Holland and Redfern (1997) result in volume-temperature (V-T) plots that are linear or slightly concave up (V plotted as the vertical axis) over the T range investigated. Relations for the "a" and "c" unit-cell dimensions with T for these hexagonal minerals are nearly linear but, as with V, commonly improved by quadratic fits to the data. Coefficients of thermal expansion for volume (αV), calculated as (1/V0°C) x (ΔV/ΔT) based on linear V-T relationships, mostly fall within the range 42 ± 2 x 10-6 deg-1 and show no obvious dependence on composition. Thermal expansion coefficients for individual unit-cell axes, however, do show clear relationships to composition, αa increasing from ~9.5 to ~13.5 x 10-6 deg-1 and αc decreasing from ~19.5 to ~13 x 10-6 deg-1 from the Cl to the F end member. Clearly, a compensating structural relationship accounts for the observed relationships. Such compositional dependence was not seen in the thermal expansion data for F-OH apatite solid solutions (Hovis, Scott, Altomare, Leaman, Morris, and Tomaino, American Mineralogist, in press). This difference can be explained by the similar sizes of F- and (OH)‑ versus the much greater size contrast between F‑ and Cl‑. Sincere thanks to the National Science Foundation for support of this work, which has provided numerous research experiences for Lafayette College undergraduates. Thanks also to the Earth Sciences Department, University of Cambridge, for providing X-ray facilities for a portion of these measurements. Finally, thanks to Jeff Post, National Museum of Natural History, and George Harlow, American Museum of Natural History, for providing the natural fluorapatite (NMNH 144954-3, Durango, Mexico) and chlorapatite (AMNH 23101, Kragero, Norway) samples, respectively.
