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Hydraulic fracturing and wellbore completion of coalbed methane wells in the Powder River Basin, Wyoming: Implications for water and gas production

机译:怀俄明州粉河盆地煤层气井的水力压裂和井筒完井:对水和天然气生产的影响

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摘要

Excessive water production (more than 7000 bbl/month per well) from many coalbed methane (CBM) wells in the Powder River Basin of Wyoming is also associated with significant delays in the time it takes for gas production to begin. Analysis of about 550 water-enhancement activities carried out during well completion demonstrates that such activities result in hydraulic fracturing of the coal. Water-enhancement activities, as the operators in the basin call this procedure, consists of pumping 60 bbl of water/min into the coal seam during approximately 15 min. This is done to clean the wellbore and to enhance CBM production. Hydraulic fracturing is of concern because vertical hydraulic fracture growth could extend into adjacent formations and potentially result in excess CBM water production and inefficient depressurization of coals. Analysis of the pressure-time records of the water-enhancement tests enabled us to determine the magnitude of the least principal stress (S3) in the coal seams of 372 wells. These data reveal that because S3 switches between the minimum horizontal stress and the overburden at different locations, both vertical and horizontal hydraulic fracture growth is inferred to occur in the basin, depending on the exact location and coal layer. Relatively low water production is observed for wells with inferred horizontal fractures, whereas all of the wells associated with excessive water production are characterized by inferred vertical hydraulic fractures. The reason wells with exceptionally high water production show delays in gas production appears to be inefficient depressurization of the coal caused by water production from the formations outside the coal. To minimize CBM water production, we recommend that in areas of known vertical fracture propagation, the injection rate during the water-enhancement tests should be reduced to prevent the propagation of induced fractures into adjacent water-bearing formations. In areas where S3 is unknown, a minifrac should be done to determine the magnitude of S3 (to know whether fracture propagation will be vertical or horizontal), so the water-enhancement activities at the time of well completion are done to minimize water production and optimize gas production.
机译:怀俄明州粉河盆地许多煤层甲烷(CBM)井的水产量过高(每口井超过7000桶/月) 也与怀俄明州的显着延迟有关。 开始生产天然气所需的时间。对在完井过程中进行的约550次增水活动的分析表明,这些活动导致了煤的水力压裂。盆地中的操作员 称此程序为增水活动,包括在大约15分钟的时间内向煤层中抽水60 bbl / min。 这样做是为了清洁井眼并提高煤层气产量。 水力压裂是令人关注的问题,因为垂直水力压裂可能会扩展到相邻的地层中并可能 > 导致过量的煤层气产水和煤炭效率低的 。通过对水增强测试的压力时间记录的分析,我们可以确定最小主应力(S 3 )的大小。 372口井的煤层。这些数据揭示了 ,因为S 3 在最小水平应力 和垂直和 盆地内水平水力压裂裂缝的发生取决于确切的位置和煤层。推断水平压裂裂缝的井的产水量相对较低,而所有与水分压裂生产过剩相关的井的特征均在于推断的垂直水力。 断裂。出水量特别高的井 显示出气体生产延迟的原因似乎是由于 外部地层的水生产所导致的煤的高效降压 。煤炭。为了最大程度地减少煤层气的产水量,我们建议在已知垂直裂缝扩展的区域中,在增水试验中将注入量降低到 。 >防止诱导的裂缝扩展到相邻的含水层中。在S 3 未知的区域,应进行小裂缝以确定S 3 的大小(以了解是否断裂 < / sup>传播是垂直或水平的),因此在完井时进行水增强 活动以最大程度地减少 产水量和优化天然气产量。 >

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  • 来源
    《AAPG Bulletin》 |2007年第1期|51-67|共17页
  • 作者单位

    Department of Geophysics, Stanford University, Stanford, California 94305 present address: Kalchbuehlstrasse 20, Zurich 8038, Switzerland lbcf@pangea.stanford.edu;

    Department of Geophysics, Stanford University, Stanford, California 94305;

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