首页 | 本学科首页   官方微博 | 高级检索  
     

Microearthquake analysis for hydraulic frac-turing proces
引用本文:李应平. Microearthquake analysis for hydraulic frac-turing proces[J]. 地震学报(英文版), 1996, 9(3): 377-387. DOI: 10.1007/BF02650973
作者姓名:李应平
作者单位:李应平
摘    要:Microearthquakeanalysisforhydraulicfrac┐turingprocesYING-PINGLI(李应平)DepartmentofEarth,AtmosphericandPlanetarySciences,Masach...

关 键 词:hydraulic fracture zone   waveform correlation   earthquake location   fracture dimension and growth rate   empirical Greens function   source parameters.
收稿时间:1995-08-15
修稿时间:1996-01-23

Microearthquake analysis for hydraulic fracturing process
YING PING LI. Microearthquake analysis for hydraulic fracturing process[J]. Acta Seismologica Sinica(English Edition), 1996, 9(3): 377-387. DOI: 10.1007/BF02650973
Authors:YING PING LI
Affiliation:(1) Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, 02142 Cambridge, MA, USA
Abstract:The hydraulic fracture technique is widely applied in the enhancement of petroleum and natural gas productions and in the development of geothermal energy. This technique is also used to create an underground fracture zone system for disposal of solid and liquid wastes. This is the most recent development in the application of industrial techniques to environmental protection scientific problems. Knowledge of mechanical properties and geometrical parameters of a hydraulic fracture zone is important for both energy resource development and safe disposal of waste. Hydraulic fracturing often induces many microearthquakes. Analysis of the spatial-temporal distribution of the induced seismicity yields the geometry of a hydraulic fracture zone, and kinetic and dynamic parameters associated with the fracture growth process. Applying a waveform correlation analysis and a space-time grid search method, we precisely determined hypocentral locations for 157 microearthquakes induced by hydraulic fracturing. Spatial distribution of the induced seismicity clearly shows the dimension and orientation of a hydraulic fracture zone. Variation of the seismicity distribution in time and space was used to infer the growth rate and direction of the fracture zone. An empirical Green’s function (EGF) method was applied to earthquake doublets to retrieve relative source time functions (RSTF’s) and to estimate source parameters, such as seismic moment, source radius, and stress drop, for larger microearthquakes. Azimuthal variation of the RSTF of a master event indicates that the source ruptured to the northwest, which aggrees with the fracture zone growth direction. Large variation of stress drops for these induced earthquakes reflects the significant heterogeneity of mechanical properties in the hydraulic fracture zone.
Keywords:hydraulic fracture zone  waveform correlation  earthquake location  fracture dimension and growth rate  empirical Green’  s function  source parameters
本文献已被 CNKI SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号