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Detailed Reference Information |
Meade, C. and Jeanloz, R. (1988). Yield strength of the B1 and B2 phases of NaCl. Journal of Geophysical Research 93. doi: 10.1029/88JB01313. issn: 0148-0227. |
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We have measured the quasi-static yield strength of NaCl to 41 GPa at room temperature. Between 0 and 28 GPa, the strength of the B1 phase increases eightfold, from 0.08 to 0.65 GPa. Across the B1-B2 transition, the strength of NaCl decreases about 50%. We show that this result is consistent with the measurements of Bridgman <1937> on the shear strength of the B1 and B2 potassium halides to 5 GPa. We propose that the simultaneous increases in coordination and nearest-neighbor distance have opposite effects on the change in shear strength across B1-B2 transitions. Increasing the atomic coordination makes the B2 structure stronger than the B1 while increasing the nearest-neighbor distance decreases the strength of the high pressure phase. In NaCl the large increase in nearest-neighbor distance more than offsets the effect of increased coordination, and thus the B2 phase is weaker than the B1 phase. ¿ American Geophysical Union 1988 |
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Abstract |
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Keywords
Physical Properties of Rocks, Fracture and flow, Tectonophysics, Rheology—general, Mineral Physics, Equations of state |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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