FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4313460009> ?p ?o ?g. }

• W4313460009 endingPage "105307" @default.
• W4313460009 startingPage "105307" @default.
• W4313460009 abstract "Crack initiation and propagation are key scientific questions influencing rock failure. To study crack initiation and propagation during rock failure, CT scanning tests were performed on the sandstone samples. The initiation and propagation stages of sandstone cracks were analysed based on a reconstructed three-dimensional crack structure model. The types of crack initiation and propagation in minerals and the effects of mineral composition heterogeneity on crack initiation and propagation were studied using microscopic analytical techniques. The effect of mineral granularity on crack initiation and propagation was analysed using statistical methods. The results show that crack initiation and propagation can be divided into four stages: microcrack inoculation, mesocrack initiation, mesocrack evolution to macrocrack, and macrocrack penetration. Four cracks are formed at different locations, extending along the mineral edge, deflecting at the mineral edge, bifurcating at the mineral edge, and penetrating through the mineral. The poikilitic texture formed by quartz debris and cement makes it easy for cracks to extend along the mineral edges. In quartz debris with high crystallinity, the crack tends to deflect and bifurcate at the edge of quartz debris. The symbiotic structure of altered quartz and clay minerals easily causes cracks to propagate through the minerals. Furthermore, the distribution of mineral granularity affects crack initiation and propagation. The inhomogeneity of mineral granularity can easily cause the initiation and propagation of cracks. The size of the mineral granularity affects the width of the secondary crack. These research results can provide a basis and reference for predicting and evaluating the stability of rock masses." @default.
• W4313460009 created "2023-01-06" @default.
• W4313460009 creator A5006219225 @default.
• W4313460009 creator A5015536166 @default.
• W4313460009 creator A5021651601 @default.
• W4313460009 creator A5039981505 @default.
• W4313460009 creator A5064918194 @default.
• W4313460009 creator A5073474341 @default.
• W4313460009 date "2023-02-01" @default.
• W4313460009 modified "2023-10-14" @default.
• W4313460009 title "Effects of sandstone mineral composition heterogeneity on crack initiation and propagation through a microscopic analysis technique" @default.
• W4313460009 cites W1671611250 @default.
• W4313460009 cites W2047688185 @default.
• W4313460009 cites W2088174398 @default.
• W4313460009 cites W2151123531 @default.
• W4313460009 cites W2265146214 @default.
• W4313460009 cites W2549824359 @default.
• W4313460009 cites W2767630070 @default.
• W4313460009 cites W2768091608 @default.
• W4313460009 cites W2797941205 @default.
• W4313460009 cites W2806520808 @default.
• W4313460009 cites W2891614694 @default.
• W4313460009 cites W2892830078 @default.
• W4313460009 cites W2919640189 @default.
• W4313460009 cites W2920361211 @default.
• W4313460009 cites W2946879120 @default.
• W4313460009 cites W2967515774 @default.
• W4313460009 cites W2973110709 @default.
• W4313460009 cites W2974443957 @default.
• W4313460009 cites W3103039256 @default.
• W4313460009 cites W3120112885 @default.
• W4313460009 cites W4223979275 @default.
• W4313460009 cites W4289110551 @default.
• W4313460009 cites W4291570630 @default.
• W4313460009 cites W3028889242 @default.
• W4313460009 doi "https://doi.org/10.1016/j.ijrmms.2022.105307" @default.
• W4313460009 hasPublicationYear "2023" @default.
• W4313460009 type Work @default.
• W4313460009 citedByCount "1" @default.
• W4313460009 countsByYear W43134600092023 @default.
• W4313460009 crossrefType "journal-article" @default.
• W4313460009 hasAuthorship W4313460009A5006219225 @default.
• W4313460009 hasAuthorship W4313460009A5015536166 @default.
• W4313460009 hasAuthorship W4313460009A5021651601 @default.
• W4313460009 hasAuthorship W4313460009A5039981505 @default.
• W4313460009 hasAuthorship W4313460009A5064918194 @default.
• W4313460009 hasAuthorship W4313460009A5073474341 @default.
• W4313460009 hasConcept C111919701 @default.
• W4313460009 hasConcept C115961682 @default.
• W4313460009 hasConcept C127313418 @default.
• W4313460009 hasConcept C151730666 @default.
• W4313460009 hasConcept C154945302 @default.
• W4313460009 hasConcept C159985019 @default.
• W4313460009 hasConcept C177774035 @default.
• W4313460009 hasConcept C191897082 @default.
• W4313460009 hasConcept C192562407 @default.
• W4313460009 hasConcept C199289684 @default.
• W4313460009 hasConcept C2776432453 @default.
• W4313460009 hasConcept C2779870107 @default.
• W4313460009 hasConcept C2781195486 @default.
• W4313460009 hasConcept C41008148 @default.
• W4313460009 hasConcept C59085676 @default.
• W4313460009 hasConceptScore W4313460009C111919701 @default.
• W4313460009 hasConceptScore W4313460009C115961682 @default.
• W4313460009 hasConceptScore W4313460009C127313418 @default.
• W4313460009 hasConceptScore W4313460009C151730666 @default.
• W4313460009 hasConceptScore W4313460009C154945302 @default.
• W4313460009 hasConceptScore W4313460009C159985019 @default.
• W4313460009 hasConceptScore W4313460009C177774035 @default.
• W4313460009 hasConceptScore W4313460009C191897082 @default.
• W4313460009 hasConceptScore W4313460009C192562407 @default.
• W4313460009 hasConceptScore W4313460009C199289684 @default.
• W4313460009 hasConceptScore W4313460009C2776432453 @default.
• W4313460009 hasConceptScore W4313460009C2779870107 @default.
• W4313460009 hasConceptScore W4313460009C2781195486 @default.
• W4313460009 hasConceptScore W4313460009C41008148 @default.
• W4313460009 hasConceptScore W4313460009C59085676 @default.
• W4313460009 hasFunder F4320321001 @default.
• W4313460009 hasFunder F4320327832 @default.
• W4313460009 hasLocation W43134600091 @default.
• W4313460009 hasOpenAccess W4313460009 @default.
• W4313460009 hasPrimaryLocation W43134600091 @default.
• W4313460009 hasRelatedWork W10618697 @default.
• W4313460009 hasRelatedWork W1997150267 @default.
• W4313460009 hasRelatedWork W2048273426 @default.
• W4313460009 hasRelatedWork W2315771207 @default.
• W4313460009 hasRelatedWork W2317482477 @default.
• W4313460009 hasRelatedWork W2390689444 @default.
• W4313460009 hasRelatedWork W4205514933 @default.
• W4313460009 hasRelatedWork W4239460191 @default.
• W4313460009 hasRelatedWork W4386031966 @default.
• W4313460009 hasRelatedWork W2521419878 @default.
• W4313460009 hasVolume "162" @default.
• W4313460009 isParatext "false" @default.
• W4313460009 isRetracted "false" @default.
• W4313460009 workType "article" @default.