PING Qi, SU Hai-peng, MA Dong-dong, et al. Experimental study on physical and dynamic mechanical properties of limestone after different high temperature treatments[J]. 2021, 42(4): 932-942.
PING Qi, SU Hai-peng, MA Dong-dong, et al. Experimental study on physical and dynamic mechanical properties of limestone after different high temperature treatments[J]. 2021, 42(4): 932-942.DOI: 10.16285/j.rsm.2020.1170.
To investigate the effect of high temperature on physical and dynamic mechanical properties of limestone
basic physical tests were conducted on limestone specimens at room temperature and high temperature treatment from 100 ℃ to 800 ℃. Moreover
dynamic impact compression tests under the same loading conditions were also conducted using SHPB test device. Test results indicate that the main mineral composition of limestone is calcite and dolomite. At room temperature
the limestone has a compact structure. With the increase of treating temperature
the dolomite gradually decomposes into micro-sized particles
and the surface color of test specimens gradually changes from off-white to white. Moreover
the volume of test specimens increases
while its mass
density and P-wave velocity decrease. These variation rates are closely related to the temperature. Dynamic compression stress-strain curves of limestone specimens under different high temperatures are basically consistent. A small increase followed by a significant decrease can be observed for both the dynamic compressive strength and dynamic elastic modulus with the increase of the temperature. An obvious negative quadratic function relationship is also found between these dynamic parameters and the treating temperature
and the maximum value is observed at 200 ℃. However
parameters including the dynamic strain and strain rate of test specimens
and the treating temperature are in a positive quadratic function relationship. The failure modes of specimens transit from brittle to ductile brittle
and damage degree is the lowest at 200 ℃. The damage degree increases with the increase of temperature
and the size of limestone fragments gradually decreases