Crack Initiation and Damage Evolution of Micritized Framework Reef Limestone in the South China Sea

Triaxial compression tests are conducted for the micritized framework reef limestone, which is sampled from a reef island in the South China Sea. The lateral strain response method (LSR) is applied to figure out the crack initiation stress of the reef limestone sample under different confining press...

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Veröffentlicht in:Rock mechanics and rock engineering 2021-11, Vol.54 (11), p.5591-5601
Hauptverfasser: Liu, Haifeng, Zhu, Changqi, Zheng, Kun, Ma, Chenghao, Yi, Mingxing
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container_issue 11
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container_title Rock mechanics and rock engineering
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creator Liu, Haifeng
Zhu, Changqi
Zheng, Kun
Ma, Chenghao
Yi, Mingxing
description Triaxial compression tests are conducted for the micritized framework reef limestone, which is sampled from a reef island in the South China Sea. The lateral strain response method (LSR) is applied to figure out the crack initiation stress of the reef limestone sample under different confining pressures. With a low porosity and a high dry density, the micritized framework reef limestone has higher compressive strength compared to the rudstone and bioclastic limestone from shallow reef associated strata. Under a confining pressure of 0–8 MPa, the crack initiation stress of the specimen is estimated to be 52%–69% of the peak compressive strength. The crack initiation stress increases when the confining pressure increases. Under different confining pressures, the lateral strain of the specimen when it fails is smaller than terrigenous rocks all the time. Further analysis shows that the lateral strains of the specimen when crack initiation occurs under different confining pressures are similar (with a value of 
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The lateral strain response method (LSR) is applied to figure out the crack initiation stress of the reef limestone sample under different confining pressures. With a low porosity and a high dry density, the micritized framework reef limestone has higher compressive strength compared to the rudstone and bioclastic limestone from shallow reef associated strata. Under a confining pressure of 0–8 MPa, the crack initiation stress of the specimen is estimated to be 52%–69% of the peak compressive strength. The crack initiation stress increases when the confining pressure increases. Under different confining pressures, the lateral strain of the specimen when it fails is smaller than terrigenous rocks all the time. Further analysis shows that the lateral strains of the specimen when crack initiation occurs under different confining pressures are similar (with a value of &lt; 0.0004). Between the point of crack initiation and the point of rock dilation, the lateral strain increases in a logarithmic manner under all the confining pressures. After reaching the point of rock dilation, the lateral damage variable is estimated to be 0.56–0.74, larger than the axial damage variable. 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subjects Civil Engineering
Compression
Compressive strength
Confining
Crack initiation
Damage
Dilation
Dry density
Earth and Environmental Science
Earth Sciences
Empirical analysis
Evolution
Frameworks
Geophysics/Geodesy
Limestone
Original Paper
Porosity
Reefs
Rocks
Strain
Triaxial compression tests
title Crack Initiation and Damage Evolution of Micritized Framework Reef Limestone in the South China Sea
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