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Mapping a fracture network formed by hydraulic fracturing in a shale gas reservoir

creativeworkseries.issn2299-8004
dc.contributor.authorWęglińska, Elżbieta
dc.contributor.authorLeśniak, Andrzej
dc.contributor.authorPasternacki, Andrzej
dc.contributor.authorWandycz, Paweł
dc.contributor.departmentWydział Geologii, Geofizyki i Ochrony Środowiska
dc.date.available2024-10-30T11:12:19Z
dc.date.issued2024
dc.description.abstractMicroseismic monitoring is an important technique that can be used to identify fractures in rock mass. The aim of this article is to identify, on the basis of the location of microseismic events, structures formed by hydraulic fracturing in the Wysin-2H/2Hbis horizontal well from the Baltic Basin in northern Poland, and to compare the patterns of these structures with the direction of regional stresses. The authors proposed a novel multi-step workflow for finding these structures. To be able to delineate the structures from microseismic events with greater accuracy, a collapsing algorithm was used. Then, based on the Hierarchical Density-Based Spatial Clustering of Applications with Noise (HDBSCAN) clustering algorithm and the elongation coefficient of each cluster, probable fissures were identified and compared against the maximum horizontal stress direction. In addition, based on the 3D seismic data from the Wysin and the calculated geomechanical parameters in the monitoring well, the probability classes of brittleness indices in the LMR (??-??) parameter domain were determined. A comparative analysis was performed between the two variants of microseismic event location (before and after the collapsing procedure) and the estimated probability of a given class of brittleness index. The comparison of the event location with the 3D seismic data was used to validate the results before and after collapsing due to the high resolution of the seismic method. It is shown that the collapsed events appeared in more rigid regions, where more energy release is expected.en
dc.description.placeOfPublicationKraków
dc.description.versionwersja wydawnicza
dc.identifier.doihttps://doi.org/10.7494/geol.2024.50.3.213
dc.identifier.eissn2353-0790
dc.identifier.issn2299-8004
dc.identifier.urihttps://repo.agh.edu.pl/handle/AGH/109750
dc.language.isoeng
dc.publisherWydawnictwa AGH
dc.relation.ispartofGeology, Geophysics & Environment
dc.rightsAttribution 4.0 International
dc.rights.accessotwarty dostęp
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/legalcode
dc.subjectfracture networken
dc.subjectshale gasen
dc.subjectmicroseismicityen
dc.subjectcollapsingen
dc.subjectHDBSCANen
dc.subjectBaltic Basinen
dc.titleMapping a fracture network formed by hydraulic fracturing in a shale gas reservoiren
dc.title.relatedGeology, Geophysics & Environmenten
dc.typeartykuł
dspace.entity.typePublication
publicationissue.issueNumberNo. 3
publicationissue.paginationpp. 213-230
publicationvolume.volumeNumberVol. 50
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relation.isJournalIssueOfPublication634d202e-2045-4933-9fe3-d701cb3f559e
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