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Lessons learned from Wireline Formation Testing with Single and Multiple Probes

机译:从单根或多根探针进行电缆形成测试中获得的经验教训

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Previously there were few RFT data available for the Wararnformation of the Greater Burgan field. Therefore, duringrnrecent drilling, pressure measurements were made torninvestigate if vertical pressure equilibrium exists in thernformation after a production history of more than fifty years.rnThe erratic nature of measured pressure profiles indicates thatrnvertical communication is poor in the reservoir.rnIn each of the pressure measurements, a single probe wasrninserted into the mud filtrate zone, and then about 20 cc ofrnliquid was collected. In addition to obtaining the pressurernvalue, we also derived the permeability value by diagnosingrnthe pressure derivative signatures. Multiple probes were alsornused to evaluate vertical permeability over an interval of 2.3rnfeet. This paper describes how we analyze the data andrnovercome the problems encountered. We demonstrate thatrn3D-reservoir simulation of the formation test can improve thernquality of data interpretation. A summary of the analyticalrnmethod development is also given.rnDue to the high precision, 0.01 psi, of the quartz gauge, thernsingle-probe pressure derivative data quality was satisfactoryrnfor low permeability sands and the analytical method couldrnderive both the horizontal and vertical permeability valuesrnsuccessfully. However, for high permeability sands, therernoften existed a pressure hump immediately after shut-in and itrnresulted in unrecognizable signatures.rnA non-linear regression method was used to interpretrnmultiple-probe test data. However, sometimes a simultaneousrnpressure match for all the probes was difficult to achieve byrnthe analytical model. 3D finite-difference simulation wasrnrequired to fit the data and characterize the geologicalrnheterogeneity. Single-probe pre-test results were used tornprovide a good initial permeability guess for the numericalrnmodel. Gamma ray and formation image loggings were provenrnvaluable to determine the layering of the numerical model.rnFinally, core measurement and buildip test results wererncompared with formation test results.
机译:以前,大布尔根地区Wararnformation的RFT数据很少。因此,在最近的钻探过程中,对压力测量进行了研究,以调查生产超过50年后在地层中是否存在垂直压力平衡.rn测量的压力曲线的不稳定特性表明储层中的垂直连通性很差.rn在每个压力测量中,将一个探针插入泥浆滤液区,然后收集约20 cc的液体。除了获得压力值外,我们还通过诊断压力导数签名来导出渗透率值。还使用了多个探针来评估2.3英尺间隔内的垂直渗透率。本文介绍了我们如何分析数据并克服遇到的问题。我们证明了地层测试的3D储层模拟可以提高数据解释的质量。归纳了分析方法的发展。由于石英表的精度高(0.01 psi),对于低渗透率砂岩,单探针压力导数数据质量令人满意,该分析方法可以成功地推导出水平和垂直渗透率值。但是,对于高渗透性砂土,关井后立即出现压力驼峰,并导致无法识别的特征。非线性回归方法用于解释多探针测试数据。但是,有时很难通过分析模型实现所有探头的同时压力匹配。需要进行3D有限差分模拟以拟合数据并表征地质非均质性。单探针预测试结果用于为数值模型提供良好的初始渗透率猜测。伽马射线和地层图像测井被证明对确定数值模型的分层具有重要的价值。最后,岩心测量和内部测试结果与地层测试结果进行了比较。

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