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American Mineralogist; February 2000; v. 85; no. 2; p. 279-282
© 2000 Mineralogical Society of America
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Differential laser-interferometer for thermal expansion measurements

Koji Masuda1,*, Dave Erskine2 and Orson L. Anderson3

1 Geological Survey of Japan, Tsukuba 305-8567, Japan
2 Lawrence Livermore National Laboratory, Livermore, California 94551, U.S.A.
3 University of California, Los Angeles, Los Angeles, California 90095, U.S.A.

Correspondence: * E-mail: masuda{at}gsj.go.jp

The differential laser interferometry method and its application for measuring the thermal expansion of samples is described. The thermal expansion of single-crystal Al2O3 (corundum) was measured up to 1000 K with the differential laser-interferometer. The changes in the distance between two faces of a stepped shape sample are measured. The main feature of the apparatus is simultaneously monitoring two fringe signals that are 90° out of phase. This improvement of the basic laser-interferometer allows us to remotely measure the thermal expansion of minerals with high precision. The overall sensitivity with which we can detect changes in length is about 1/100 of the wavelength of the He-Ne laser (1/100 of 0.6328 x 10–6 m). After adjusting for errors caused by heat, the thermal expansion data measured with the differential laser-interferometer are in good agreement with previous reports. Use of this apparatus allows the investigation of the high-temperature thermodynamic properties of important rock-forming minerals.




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