{"title":"The algorithm for elimination of data redundancy in hydraulic fracturing monitoring systems","authors":"Eugeniiy V. Rabinovich, P. I. Vaynmaster","doi":"10.1109/SIBIRCON.2017.8109866","DOIUrl":null,"url":null,"abstract":"The important stage in the monitoring of hydraulic fracturing is construction of a graphical model of a fractured area. However, real data recorded in the process of hydraulic fracturing are characterized by a high intensity of seismic activity in the monitoring area, which makes it difficult to correctly construct such a model. The original algorithm is described, which allows one to eliminate the redundancy of miscroseismic sources and to highlight the local hypocenters of microearthquakes. The results obtained were used to construct a three-dimensional graphical model of a fracture.","PeriodicalId":135870,"journal":{"name":"2017 International Multi-Conference on Engineering, Computer and Information Sciences (SIBIRCON)","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2017-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2017 International Multi-Conference on Engineering, Computer and Information Sciences (SIBIRCON)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/SIBIRCON.2017.8109866","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The important stage in the monitoring of hydraulic fracturing is construction of a graphical model of a fractured area. However, real data recorded in the process of hydraulic fracturing are characterized by a high intensity of seismic activity in the monitoring area, which makes it difficult to correctly construct such a model. The original algorithm is described, which allows one to eliminate the redundancy of miscroseismic sources and to highlight the local hypocenters of microearthquakes. The results obtained were used to construct a three-dimensional graphical model of a fracture.
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