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thesis, University of Hawaii, Honolulu
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P. M. Nasch, thesis, University of Hawaii, Honolulu (1996).
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Nasch, P.M.1
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19
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1842277454
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-
note
-
The Fe-5%Ni-10%S sample was prepared by J.-F. Jeanneret and W.-D. Schneider of the University of Lausanne (Switzerland). The starting powder components for the Fe-5%Ni-10%S were 99.5%, 45-μm (325 mesh) iron (Pierce Inorganic, number P00170); 99.8%, 45-μm (325 mesh) nickel (Ventron, number 224); and 99.5%, 150-μm (100 mesh) sulfur (Cerac, number S2016). About 100 g of powder components were thoroughly mixed in the proper ratio measured in weight percent. The mixture was cold-compacted into 25-mm-diameter pellets. The pellets were then sintered at 1073 K for 1 to 2 hours.
-
-
-
-
20
-
-
1842312924
-
-
note
-
3) to identify misalignment of the buffer rods (asymmetry in the resonance peaks), poor transducer bonding or electronic tuning (low overall transmitted amplitude), and lack of parallelism or flatness of the rod faces (ripples in the decay pattern).
-
-
-
-
21
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0003689862
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T. B. Massalski, Ed. American Society for Metals, Metals Park, OH
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Estimated from the Fe-S phase diagram of O. Kubaschewski, in Binary Alloy Phase Diagrams, T. B. Massalski, Ed. (American Society for Metals, Metals Park, OH, 1986), vol. 1.
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0028333383
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s (102 GPa) [P. M. Nasch, M. H. Manghnani, R. A. Seco, J. Geophys. Res. 99, 4285 (1994)] has been corrected for thermal expansion to yield 110 ± 2 GPa [P. M. Nasch and M. H. Manghnani, in High Pressure-Temperature Research: Properties of Earth and Planetary Materials (American Geophysical Union, Washington, DC, in press)]. This result is in agreement with the 109.7 ± 0.7 GPa reported by W. W. Anderson and T. J. Ahrens [J. Geophys. Res. 99, 4273 (1994)].
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23
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0028315677
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s (102 GPa) [P. M. Nasch, M. H. Manghnani, R. A. Seco, J. Geophys. Res. 99, 4285 (1994)] has been corrected for thermal expansion to yield 110 ± 2 GPa [P. M. Nasch and M. H. Manghnani, in High Pressure-Temperature Research: Properties of Earth and Planetary Materials (American Geophysical Union, Washington, DC, in press)]. This result is in agreement with the 109.7 ± 0.7 GPa reported by W. W. Anderson and T. J. Ahrens [J. Geophys. Res. 99, 4273 (1994)].
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p of greater than 4000 [T. G. Masters and P. M. Shearer, J. Geophys. Res. 95, 21691 (1990); G. G. R. Buchbinder, Bull. Seismol. Soc. Am. 61, 429 (1971); I. S. Sacks, Carnegie Inst. Washington Yearb. 69, 414 (1971); A. Qamar and A. Eisenberg, J. Geophys. Res. 79, 758 (1974); V. F. Cormier and P. G. Richards, ibid. 81, 3066 (1976); D. L. Anderson and R. S. Hart, ibid. 83, 5869 (1978)]. Nasch (9) showed that a low Ni content (less than 15 weight %) introduces no or negligible contribution to the attenuation in liquid Fe.
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p of greater than 4000 [T. G. Masters and P. M. Shearer, J. Geophys. Res. 95, 21691 (1990); G. G. R. Buchbinder, Bull. Seismol. Soc. Am. 61, 429 (1971); I. S. Sacks, Carnegie Inst. Washington Yearb. 69, 414 (1971); A. Qamar and A. Eisenberg, J. Geophys. Res. 79, 758 (1974); V. F. Cormier and P. G. Richards, ibid. 81, 3066 (1976); D. L. Anderson and R. S. Hart, ibid. 83, 5869 (1978)]. Nasch (9) showed that a low Ni content (less than 15 weight %) introduces no or negligible contribution to the attenuation in liquid Fe.
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p of greater than 4000 [T. G. Masters and P. M. Shearer, J. Geophys. Res. 95, 21691 (1990); G. G. R. Buchbinder, Bull. Seismol. Soc. Am. 61, 429 (1971); I. S. Sacks, Carnegie Inst. Washington Yearb. 69, 414 (1971); A. Qamar and A. Eisenberg, J. Geophys. Res. 79, 758 (1974); V. F. Cormier and P. G. Richards, ibid. 81, 3066 (1976); D. L. Anderson and R. S. Hart, ibid. 83, 5869 (1978)]. Nasch (9) showed that a low Ni content (less than 15 weight %) introduces no or negligible contribution to the attenuation in liquid Fe.
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p of greater than 4000 [T. G. Masters and P. M. Shearer, J. Geophys. Res. 95, 21691 (1990); G. G. R. Buchbinder, Bull. Seismol. Soc. Am. 61, 429 (1971); I. S. Sacks, Carnegie Inst. Washington Yearb. 69, 414 (1971); A. Qamar and A. Eisenberg, J. Geophys. Res. 79, 758 (1974); V. F. Cormier and P. G. Richards, ibid. 81, 3066 (1976); D. L. Anderson and R. S. Hart, ibid. 83, 5869 (1978)]. Nasch (9) showed that a low Ni content (less than 15 weight %) introduces no or negligible contribution to the attenuation in liquid Fe.
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note
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Supported by grants from NSF (EAR-89-17531 and EAR-90-06790), the W. M. Keck Foundation, and the School of Ocean and Earth Science and Technology, University of Hawaii. P.M.N. further acknowledges financial support for graduate study from the following sponsors in Switzerland: Foundation L. and H. Mouttet (LEMO S.A.), Foundation Fern-Moffat (Société Académique Vaudoise), and Foundation Sunburst (Council of the Swiss Institutes of Technology). We acknowledge the valuable comments and suggestions made on the manuscript by D. Loper, Florida State University, and by the two anonymous reviewers. School of Ocean and Earth Science and Technology contribution number 4500.
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