Expansivity and compressibility of wadeite-type K2Si4O9 determined by in situ high T/P experiments, and their implication

Physics and Chemistry of Minerals - Tập 40 - Trang 29-40 - 2012
Linlin Chang1,2, Zhiqiang Chen3, Xi Liu1,2, Hejing Wang1,2
1Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education of China (MOE), Peking University, Beijing, People’s Republic of China
2School of Earth and Space Sciences, Peking University, Beijing, People’s Republic of China
3National Synchrotron Light Source, Brookhaven National Laboratory, Upton, USA

Tóm tắt

Wadeite-type K2Si4O9 was synthesized with a cubic press at 5.4 GPa and 900 °C for 3 h. Its unit-cell parameters were measured by in situ high-T powder X-ray diffraction up to 600 °C at ambient P. The T–V data were fitted with a polynomial expression for the volumetric thermal expansion coefficient (αT = a 0 + a 1 T), yielding a 0 = 2.47(21) × 10−5 K−1 and a 1 = 1.45(36) × 10−8 K−2. Compression experiments at ambient T were conducted up to 10.40 GPa with a diamond-anvil cell combined with synchrotron X-ray radiation. A second-order Birch–Murnaghan equation of state was used to fit the P–V data, yielding K T = 97(3) GPa and V 0 = 360.55(9) Å3. These newly determined thermal expansion data and compression data were used to thermodynamically calculate the P–T curves of the following reactions: 2 sanidine (KAlSi3O8) = wadeite (K2Si4O9) + kyanite (Al2SiO5) + coesite (SiO2) and wadeite (K2Si4O9) + kyanite (Al2SiO5) + coesite/stishovite (SiO2) = 2 hollandite (KAlSi3O8). The calculated phase boundaries are generally consistent with previous experimental determinations.

Tài liệu tham khảo

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