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TIME-LAPSE SIMULTANEOUS AVO INVERSION OF THE WIDURI FIELD, OFFSHORE SOUTHEAST SUMATRA

机译:延时田野的延时同时举行的延长苏拉斯·苏门答腊

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Reservoir characterization of the Widuri field, offshore SE Sumatra, is complicated by complex lithology and difficulties in predicting changes in fluid distribution during production. In 2000 a monitor 3D seismic data set of the Widuri field was acquired and processed to take advantage of seismic AVO effects. The base line 1991 seismic data set was reprocessed in parallel. The primary reason for the monitor data set was to observe the reservoir pressure depletion state around a water-flooding project. Furthermore there was a need to improve the characterization of the reservoir sands and to develop a better understanding of the fluid movement over time. To support AVO based reservoir characterization the base line and monitor seismic data were processed to 3 partial angle stacks. These were subsequently inverted to acoustic and shear impedance using a global, Simultaneous AVO Inversion algorithm. Resultant multi-parameter impedance based reservoir characterization from well log data and the impedance inversion results show that sands and coals in the reservoir interval can now be discriminated. Previously, reliable interpretation of these lithologies away from well control from poststack seismic data was infeasible as the acoustic impedance of these lithologies overlap. To investigate and characterize fluid movement, a novel workflow involving joint Simultaneous AVO Inversion of baseline and monitor seismic data was applied. The results from the time-lapse AVO inversion confirm the hypothesis based on production history analysis that aquifer support comes from the SouthEast. The same technique is successfully used to map more specific features related to depletion. As a result of production, increased water cut was observed at most of the wells. In addition to this, pressure dropped below bubble point with gas coming out of solution, which accumulated at structural highs. Both factors influence production and are potential drilling risks for newly planned wells.
机译:普通卫生间的储层表征,海上SE苏门答腊,复杂的岩性和困难在预测生产过程中的流体分布变化方面是复杂的。在2000年,获取和处理Widuri领域的监视器3D地震数据集以利用地震避免效应。基线1991地震数据集并行重新处理。监视数据集的主要原因是观察水洪水项目周围的储层压力耗尽状态。此外,需要改善水库砂的表征,并在随着时间的推移更好地了解流体运动。为了支持基于AVO的储库表征,基线和监视器地震数据处理到3个部分角度堆叠。随后使用全局同时的AVO反转算法倒转到声学和剪切阻抗。由此产生的多参数阻抗基于井日志数据的储层表征,阻抗反演结果表明,现在可以区分储层间隔中的砂和煤。以前,这些岩性远离从后攻击地震数据的良好控制的可靠解释是不可行的,因为这些岩性重叠的声阻抗。为了研究和表征流体运动,应用了涉及基线和监测地震数据联合同时避平的新型工作流程。时间流逝AVO反演的结果证实了基于生产历史分析的假设,即含水层支持来自东南部。相同的技术被成功地用于映射与耗尽相关的更具体的特征。由于生产,在大多数井中观察到较高的水切口。除此之外,压力下降低于泡点与溶液出来的气体,其在结构高处累积。这两个因素都会影响生产,并对新规划的井有潜在的钻探风险。

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