Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Compression wave studies in Blair dolomite

Technical Report ·
DOI:https://doi.org/10.2172/7178929· OSTI ID:7178929

Dynamic compression wave studies have been conducted on Blair dolomite in the stress range of 0-7.0 GPa. Impact techniques were used to generate stress impulse input functions, and diffuse surface laser interferometry provided the dynamic instrumentation. Experimental particle velocity profiles obtained by this method were coupled with the conservation laws of mass and momentum to determine the stress-strain and stress-modulus constitutive properties of the material. Comparison between dynamic and quasistatic uniaxial stress-strain curves uncovered significant differences. Energy dissipated in a complete load and unload cycle differed by almost an order of magnitude and the longitudinal moduli differed by as much as a factor of two. Blair dolomite was observed to yield under dynamic loading at 2.5 GPa. Below 2.5 GPa the loading waves had a finite risetime and exhibited steady propagation. A finite linear viscoelastic constitutive model satisfactorily predicted the observed wave propagation. We speculate that dynamic properties of preexisting cracks provides a physical mechanism for both the rate dependent steady wave behavior and the difference between dynamic and quasistatic response.

Research Organization:
Sandia Labs., Albuquerque, N.Mex. (USA); New Mexico Univ., Albuquerque (USA)
DOE Contract Number:
AT(29-1)-789
OSTI ID:
7178929
Report Number(s):
SAND-76-0005
Country of Publication:
United States
Language:
English