Japan Geoscience Union Meeting 2014

Presentation information

Poster

Symbol S (Solid Earth Sciences) » S-MP Mineralogy & Petrology

[S-MP47_1PO1] Physics and Chemistry of Minerals

Thu. May 1, 2014 6:15 PM - 7:30 PM Poster (3F)

Convener:*Okudera Hiroki(School of Natural System, College of Science and Engineering), Atsushi Kyono(Graduate School of Life and Environmental Sciences, University of Tsukuba)

6:15 PM - 7:30 PM

[SMP47-P02] Thermal expansion of Ca(OD)2 at high pressure

*Takaya NAGAI1, Asami SANO2, Riko IIZUKA3, Hiroyuki KAGI3, Takanori HATTORI4 (1.Faculty of Science, Hokkaido Universuty, 2.Japan Atomic Energy Agency, 3.Graduate School of Science, The University of Tokyo, 4.Materials and Life Science Division, J-PARC Center)

Keywords:portlandite, thermal expansion, high pressure, synchrotron X-ray diffraction, TOF neutron diffraction

Ca(OH)2 is one of the important hydrous minerals to understand structural behavior at high pressure and high temperature, because this type of structure is a building unit in more complex hydrous phases such as chondrodite. It is surprising that only a few previous researches can be found on crystallography of Ca(OH)2 in the conditions of simultaneously high pressure and high temperature. We gave an oral presentation about some preliminary results in this conference last year. We have continued to analyze the data carefully and will add some new information.Deuterated samples were prepared via hydrothermal treatment with CaO fine powders and excess D2O water in a Teflon lined stainless steel autoclave at 493 K for 4 days. After the hydrothermal treatment was completed, precipitates were filtered out, washed with D2O water, and then dried at 383 K under vacuum for 3 hours. The products were confirmed to have the CdI2-type structure by conventional powder X-ray diffraction measurements and were checked to be deuterated by IR absorption spectra. Synchrotron X-ray diffraction experiments were performed at the beamline AR-NE5C, KEK, Japan in order to obtain cell parameters of Ca(OD)2 at various P-T conditions from 2-4 GPa and 300-800 K. TOF neutron powder diffraction measurements of Ca(OD)2 were carried out from 300 to 773 K at high pressure at the PLANET beamline in J-PARC, Japan. Pressure was estimated by comparing unit cell parameters with those obtained by synchrotron experiments.All our TOF data obtained include only Ca(OD)2 peaks and no peaks from sample surrounding materials such as ZrO2 pressure medium, graphite furnace and WC anvils could be detected owing to radial collimators equipped with the 6-ram pressure apparatus (Atsuhime). The detailed structure parameters such as lattice parameters and atomic coordinates could be reasonably refined by the Rietveld method by using a program GSAS. It is an interesting result that thermal expansion along the c-axis seems to be suppressed at high pressure comparing to that at ambient pressure. Mechanism of the thermal expansion of Ca(OD)2 at high pressure will be discussed.