Microcrack pattern propagations and Rock Quality Designation of Batu Caves Limestone
Microcrack pattern of limestone with various grade of natural weathering were studied to examine the microcrack initiation and propagations in relation to Rock Quality Designation (RQD) and shear strength parameters such as shear stress and normal stress. The degree of natural weathering were determ...
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my.uniten.dspace-305072023-12-29T15:48:38Z Microcrack pattern propagations and Rock Quality Designation of Batu Caves Limestone Pauzi N.I.M. Omar H. Huat B.K. Misran H. Yusoff Z.M. 26536518100 7006098814 35361794900 6506899840 36873775700 Grade of weathering Microcrack propagations of limestone Rock quality designation Scanning electron microscope Electron microscopes Limestone Rocks Scanning Scanning electron microscopy Shear strength Shear stress Soil mechanics Confidence levels Grade of weathering Microcrack initiation Natural weathering Normal stress Rock quality designation Scanning electron microscope Scanning electron microscopes Schmidt hammer tests Shear strength parameters Weathering grades crack propagation limestone microcrack rock property scanning electron microscopy shear strength shear stress weathering Weathering Microcrack pattern of limestone with various grade of natural weathering were studied to examine the microcrack initiation and propagations in relation to Rock Quality Designation (RQD) and shear strength parameters such as shear stress and normal stress. The degree of natural weathering were determined using Schmidt hammer test and it was found that as the weathering grade increased from grade I to grade IV, the microcrack length changed from ca. 500 ?m to a longer length of ca. 800 ?m. The increased in microcrack length were coupled with the increased in width of the cracks as observed using Scanning Electron Microscope (SEM). Furthermore, it was suggested that the microcrack length of limestone is inversely proportional to RQD value with confidence level of 60%. However, the microcrack length of limestone was observed to be directly proportional with shear stress and normal stress with confidence level of 95% and 99% respectively. � 2011 ejge. Final 2023-12-29T07:48:38Z 2023-12-29T07:48:38Z 2011 Article 2-s2.0-79954620605 https://www.scopus.com/inward/record.uri?eid=2-s2.0-79954620605&partnerID=40&md5=949edcd06ae7a08ae32316ad1c0edee7 https://irepository.uniten.edu.my/handle/123456789/30507 16 F 591 604 Scopus |
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Grade of weathering Microcrack propagations of limestone Rock quality designation Scanning electron microscope Electron microscopes Limestone Rocks Scanning Scanning electron microscopy Shear strength Shear stress Soil mechanics Confidence levels Grade of weathering Microcrack initiation Natural weathering Normal stress Rock quality designation Scanning electron microscope Scanning electron microscopes Schmidt hammer tests Shear strength parameters Weathering grades crack propagation limestone microcrack rock property scanning electron microscopy shear strength shear stress weathering Weathering |
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Grade of weathering Microcrack propagations of limestone Rock quality designation Scanning electron microscope Electron microscopes Limestone Rocks Scanning Scanning electron microscopy Shear strength Shear stress Soil mechanics Confidence levels Grade of weathering Microcrack initiation Natural weathering Normal stress Rock quality designation Scanning electron microscope Scanning electron microscopes Schmidt hammer tests Shear strength parameters Weathering grades crack propagation limestone microcrack rock property scanning electron microscopy shear strength shear stress weathering Weathering Pauzi N.I.M. Omar H. Huat B.K. Misran H. Yusoff Z.M. Microcrack pattern propagations and Rock Quality Designation of Batu Caves Limestone |
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Microcrack pattern of limestone with various grade of natural weathering were studied to examine the microcrack initiation and propagations in relation to Rock Quality Designation (RQD) and shear strength parameters such as shear stress and normal stress. The degree of natural weathering were determined using Schmidt hammer test and it was found that as the weathering grade increased from grade I to grade IV, the microcrack length changed from ca. 500 ?m to a longer length of ca. 800 ?m. The increased in microcrack length were coupled with the increased in width of the cracks as observed using Scanning Electron Microscope (SEM). Furthermore, it was suggested that the microcrack length of limestone is inversely proportional to RQD value with confidence level of 60%. However, the microcrack length of limestone was observed to be directly proportional with shear stress and normal stress with confidence level of 95% and 99% respectively. � 2011 ejge. |
author2 |
26536518100 |
author_facet |
26536518100 Pauzi N.I.M. Omar H. Huat B.K. Misran H. Yusoff Z.M. |
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Article |
author |
Pauzi N.I.M. Omar H. Huat B.K. Misran H. Yusoff Z.M. |
author_sort |
Pauzi N.I.M. |
title |
Microcrack pattern propagations and Rock Quality Designation of Batu Caves Limestone |
title_short |
Microcrack pattern propagations and Rock Quality Designation of Batu Caves Limestone |
title_full |
Microcrack pattern propagations and Rock Quality Designation of Batu Caves Limestone |
title_fullStr |
Microcrack pattern propagations and Rock Quality Designation of Batu Caves Limestone |
title_full_unstemmed |
Microcrack pattern propagations and Rock Quality Designation of Batu Caves Limestone |
title_sort |
microcrack pattern propagations and rock quality designation of batu caves limestone |
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2023 |
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1806426117885657088 |
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13.214268 |