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American Mineralogist; March 1999; v. 84; no. 3; p. 341-344
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High-pressure X-ray diffraction study on the structure of NaCl melt using synchrotron radiation

Satoru Urakawa, Naoki Igawa, Osamu Shimomura, and Hideo Ohno

Okayama University, Department of Earth Sciences, Okayama, Japan

Molten NaCl was analyzed by high-pressure X-ray diffraction experiments using synchrotron radiation up to 5 GPa and 1600 degrees C along the melting curve. The interference function Qi(Q) and the correlation function g(r) were derived from the diffraction data. The first-neighbor distance r 1 is about 2.7 Aa and the second-neighbor distance appears around 1.4r 1 -1.5r 1 . The coordination number, CN, of the nearest neighbor ions increases with pressure from 3.5 at 0.1 MPa to 4.5 at 5 GPa. This is the evidence that the NaCl melt has a B1-like structure with large vacancies over this pressure range and becomes densified by an increase in CN as a result of second neighbor compaction.

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