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Studies on Materials Under Ultrahigh P-T at the Advanced Photon Source

Published online by Cambridge University Press:  10 February 2011

G. Shen ,
T. Duffy ,
Y. Wang ,
M. Rivers  and
S. Sutton
G. Shen
Affiliation:
Consortium for Advanced Radiation Sources, The Univ. of Chicago, Chicago, IL 60637
T. Duffy
Affiliation:
Consortium for Advanced Radiation Sources, The Univ. of Chicago, Chicago, IL 60637
Y. Wang
Affiliation:
Consortium for Advanced Radiation Sources, The Univ. of Chicago, Chicago, IL 60637
M. Rivers
Affiliation:
Consortium for Advanced Radiation Sources, The Univ. of Chicago, Chicago, IL 60637
S. Sutton
Affiliation:
Consortium for Advanced Radiation Sources, The Univ. of Chicago, Chicago, IL 60637
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Abstract

The Advanced Photon Source (APS) is a third-generation synchrotron now in operation at Ar-gonne National Laboratory. A national user facility for research in the Earth sciences is being constructed by the GeoSoilEnviro group of the Consortium for Advanced Radiation Sources (GSECARS). One component of this effort is the program for diamond anvil cell (DAC) research, to study materials at ultrahigh pressure and temperature conditions using a variety of techniques.

In this paper, we describe the DAC facility that is being developed at the GSECARS. Recent progress in developing a laser heating system is presented.

Type
Research Article
Information
MRS Online Proceedings Library (OPL) , Volume 499: Symposium DD – High Pressure Materials Research , 1997 , 283
Copyright
Copyright © Materials Research Society 1998

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References

REFERENCES

[1] Eng, P., Rivers, M., Yang, B., and Schildkamp, W., Proc. SPIE, 2516, 41–51, (1995).Google Scholar
[2] Rivers, M., Duffy, T., Wang, Y., Eng, P., Sutton, S., and Shen, G., High Pressure Temperature Research: Properties of Earth and Planetary Materials, in press, (1997).Google Scholar
[3] Mao, H.K., Wu, Y., Chen, L.C., Shu, J.F., Jephcoat, A., J. Geophys. Res., 95, 21737, (1990).Google Scholar
[4] Loubeyre, P., Toullec, R., Hausermann, D., Hanflank, M., Finger, L., Hemley, R., and Mao, H.K., Nature, 383, 702, (1996).Google Scholar
[5] Jephcoat, A., Finger, L., and Cox, D., High Pressure Res., 8, 667, (1992).Google Scholar
[6] Fuji, Y., Hose, K., Ohishi, Y., Fujihisa, H., Hamaya, N., Tekemura, K., Shimomura, O., Kikegawa, T., Amemiya, Y., and Matsushita, T, Phys. Rev. Lett., 63, 536, (1989).Google Scholar
[7] Hausermann, D., and Itie, J., Rev. Sci. Instrum., 63, 1080, (1992).Google Scholar
[8] Shen, G., Mao, H.K., Hemley, R., Advanced Material'96 - New trends in high pressure research, 149, (1996).Google Scholar