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Prediction of Formation Pore Pressures for Tophole Well Integrity

机译:井下完整性的地层孔隙压力预测

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Knowledge about formation pore pressures is important for planning and control of offshore well drilling operations.rnParticularly, a combination of unconsolidated clay/shale sediments and in-situ pore pressures exceeding hydrostatic values canrncreate a distinctly adverse setting for tophole well integrity. If unanticipated, well completion may fail.rnPore pressure prediction for the tophole section generally relies on use of multiple methods, as no single technology isrnavailable. Actual measurement of in-situ pore pressure is necessary. Pore Pressure Dissipation Testing PPDT with a push-inrnpiezoprobe or piezocone penetrometer is currently the most efficient and accurate method for actual measurement of formationrnpore pressure in unconsolidated sediments. The method can be used in a pre-well site survey, during pre-setting a tophole wellrnsection or combined with well installation itself.rnCapabilities and limitations are highlighted for predicting and accurately measuring formation pore pressures in shallowrnunconsolidated clay/shale sediments. Use is made of a unique database containing more than 160 PPDT piezoprobernmeasurements. The database probably covers a majority of piezoprobe measurements ever completed for offshore topholernsections. It includes (1) hydrostatic pressure profiles, (2) excess pore pressures due to natural phenomena and (3) excess porernpressures due to formation damage caused by earlier well drilling. Depth coverage is up to 400 m below seafloor.rnAchievable accuracy for measurement of pore pressure is typically estimated at about 50 kPa (= 5 m water column) or 5%rnof penetration pore pressure, whichever is the greater. Difficulties are noted for establishing formation pore pressures wherern(1) clay/shale sediments have been affected by formation damage caused by earlier drilling and (2) clay/shale sedimentsrninclude shallow gas zones. Opportunities for improvement are discussed.
机译:有关地层孔隙压力的知识对于规划和控制海上钻井作业非常重要。特别是,未固结的粘土/页岩沉积物与超过静水压力的原位孔隙压力相结合,可能对顶孔井完整性造成明显不利的影响。如果无法预料,则完井可能会失败。由于没有单一技术可用,因此对顶孔段的孔压预测通常依赖于多种方法。实际测量原位孔隙压力是必要的。孔隙压力耗散测试使用推入式压电探针或压电锥度渗透计进行PPDT是目前最有效,最准确的方法,用于实际测量未固结沉积物中的地层孔隙压力。该方法可用于井前现场勘测,顶井井段预设或与井架本身结合使用。突出了预测和准确测量浅层未固结黏土/页岩沉积物中地层孔隙压力的能力和局限性。使用了一个独特的数据库,其中包含160多个PPDT压电探针测量值。该数据库可能涵盖了迄今为海上顶板剖面完成的大多数压电探针测量。它包括(1)静水压力曲线,(2)由于自然现象而导致的超孔隙压力,以及(3)由于较早的钻井造成的地层破坏而导致的超孔隙压力。深度覆盖距离海床以下最多400m。rn估计的孔隙压力测量精度通常约为50 kPa(= 5 m水柱)或5%rnof渗透孔隙压力,以较大者为准。在建立地层孔隙压力方面存在困难,其中(1)早期钻探造成的地层破坏已经影响了粘土/页岩沉积物,(2)包括浅层气层的粘土/页岩沉积物。讨论了改进的机会。

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