WANG Ping, ZHU Yong-jian, YU Wei-jian, et al. Experimental analysis on fractional compaction mechanical
characteristics of soft and broken rock[J]. 2019, 40(7): 2703-2712.
DOI:
WANG Ping, ZHU Yong-jian, YU Wei-jian, et al. Experimental analysis on fractional compaction mechanical
characteristics of soft and broken rock[J]. 2019, 40(7): 2703-2712.DOI: 10.16285/j.rsm.2018.0460.
Experimental analysis on fractional compaction mechanical
characteristics of soft and broken rock
The mechanical properties of the regenerated rock mass are intrinsically changed due to the reorganisation of the structure and components in the coal mine. In this study
the fractured rock mass was repeatedly compressed during the compaction and diagenesis process of the regenerated rock mass. Then the fractional compaction test under confined conditions was carried out using the broken surrounding rock of the regenerated roof of the Zhoujing coal mine in Guangxi. The results show that the process of fractional compression can be divided into three stages: compaction crushing
compaction stress memory and compaction consolidation. At the first compression
the compacting characteristic curve changes linearly
and the subsequent compaction curve gradually changes to an exponential form
while the stage of compaction stress memory shows a polynomial change. Under the confined compression condition
the criterion of minimum potential energy is used to determine the crushing fracture of irregular rock samples. The compression characteristics of fractured rock samples are influenced by the number of compaction and the height of rock mass. When the times of compaction are larger
the cumulative compression strain is greater
and the stress increment in the subsequent compression is higher. As the loading height is higher
the cumulative total strain is greater at the same compressive stress. When the compaction stress reaches a certain degree
the grain-size distribution of the broken rock samples with different coarse-grained sizes tends to be consistent. Therefore
the correlation between the size distribution of broken rock samples and the compaction degree of the regenerated rock mass is established.