Alternatives to a power-law creep model for rock salt at temperatures below 160/sup 0/C
Five sets of steady state creep estimates for rock salt were analyzed to compare the results of power-law fits for dislocation climb with the fits by models for cross-slip, glide, and a combination of cross-slip and climb. It was determined that a cross-slip model yields the mechanistically most credible fit with activation energies and activation areas matching those published for NaCl single crystals. High power-law stress exponents also ruled out the possibility that pressure solution and recrystallization played a major role to the lowest recorded strain rates on the order of 10/sup -10/ s/sup -1/. The conclusion concerning cross-slip as the rate controlling step during creep of rock salt below 160/sup 0/C is consistent with many glide related microstructural features in samples deformed in the laboratory at or below 110/sup 0/C. It is emphasized, however, that the role of cross-slip does not imply the absence of other mechanisms including dislocation climb and subgrain formation but merely suggests that they are not dominant. 58 refs., 6 figs., 4 tabs.
- Research Organization:
- Sandia National Labs., Albuquerque, NM (USA)
- DOE Contract Number:
- AC04-76DP00789
- OSTI ID:
- 6338024
- Report Number(s):
- SAND-85-2453C; CONF-8409302-1; ON: DE86003917
- Resource Relation:
- Conference: 2. conference on mechanical behavior of salt, Hannover, F.R. Germany, 24 Sep 1984
- Country of Publication:
- United States
- Language:
- English
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