http://rdf.ncbi.nlm.nih.gov/pubchem/patent/CN-114169182-B
Outgoing Links
Predicate | Object |
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classificationCPCAdditional | http://rdf.ncbi.nlm.nih.gov/pubchem/patentcpc/G06F2119-14 http://rdf.ncbi.nlm.nih.gov/pubchem/patentcpc/G06F2111-04 |
classificationCPCInventive | http://rdf.ncbi.nlm.nih.gov/pubchem/patentcpc/G06F30-20 http://rdf.ncbi.nlm.nih.gov/pubchem/patentcpc/G16C10-00 |
classificationIPCAdditional | http://rdf.ncbi.nlm.nih.gov/pubchem/patentipc/G06F111-04 http://rdf.ncbi.nlm.nih.gov/pubchem/patentipc/G06F119-14 |
classificationIPCInventive | http://rdf.ncbi.nlm.nih.gov/pubchem/patentipc/G16C10-00 http://rdf.ncbi.nlm.nih.gov/pubchem/patentipc/G06F30-20 |
filingDate | 2022-02-14-04:00^^<http://www.w3.org/2001/XMLSchema#date> |
grantDate | 2022-05-31-04:00^^<http://www.w3.org/2001/XMLSchema#date> |
publicationDate | 2022-05-31-04:00^^<http://www.w3.org/2001/XMLSchema#date> |
publicationNumber | CN-114169182-B |
titleOfInvention | An ellipsoid model reconstruction method and equipment for rock face fractures |
abstract | The invention proposes a method and equipment for reconstructing an ellipsoid model of a rock face fracture. The method adopts an ellipsoid model to visually express the distribution characteristics of the fractures and pores. The invention adopts ellipsoid to reconstruct the rock mass surface crack field, and simplifies the surface crack field inside the rock mass into ellipsoid cracks, which is convenient for description in mathematical geometry, and establishes simplified crack field and rock mass physical and mechanical properties and deformation. The theoretical relationship between failures is of great significance to the development of fractured rock mechanics theory. |
priorityDate | 2022-02-14-04:00^^<http://www.w3.org/2001/XMLSchema#date> |
type | http://data.epo.org/linked-data/def/patent/Publication |
Incoming Links
Predicate | Subject |
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isDiscussedBy | http://rdf.ncbi.nlm.nih.gov/pubchem/substance/SID419559581 http://rdf.ncbi.nlm.nih.gov/pubchem/compound/CID297 |
Total number of triples: 18.