...
首页> 外文期刊>Geophysical Prospecting >Seismic scale saturation relations in turbidite reservoirs undergoing waterflood
【24h】

Seismic scale saturation relations in turbidite reservoirs undergoing waterflood

机译:发生水驱的浊积岩储层中的地震标度饱和关系

获取原文
获取原文并翻译 | 示例
           

摘要

Estimates of the effective fluid modulus from seismic cannot be directly converted to the true pore-volume weighted mean saturation S_w determined from fluid flow principles by using the saturation laws currently in use. One of the reasons is that seismic waves sample the reservoir geology and production induced saturation heterogeneity in a different way from the fluids. This mismatch prevents accurate quantitative evaluation of saturation changes from 4D seismic analysis. To tackle this problem, a reservoir-related saturation law is developed for a turbidite reservoir - this geology being chosen because the architecture for a single sand package can be modelled as a stack of horizontal beds. An effective medium and perturbation theory are applied to the determination of the seismic properties of this model. This calculation provides a relationship that connects the true saturation S_w to the effective fluid modulus from seismic via statistical measures of the vertical spread of the porosity and saturation variations in the reservoir. These statistics can be extracted from the simulation model and if known, enable the new saturation law to deliver a significant improvement in accuracy when estimating S_w compared to other well-known laws. The relationship that has been developed also captures the effect of inter-bedded shales and can therefore be used to estimate true saturation in regions of the reservoir with moderate to low net-to-gross, provided the fraction of the shale component is known. In practice, the final choice of saturation law depends upon the reservoir information available, the assumptions that can be tolerated and the accuracy required in any particular reservoir characterization study.
机译:来自地震的有效流体模量的估计值不能通过使用当前使用的饱和定律直接转换为根据流体流动原理确定的真实孔隙体积加权平均饱和度S_w。原因之一是地震波以与流体不同的方式采样储层地质和生产引起的饱和非均质性。这种不匹配会阻止对4D地震分析进行饱和度变化的准确定量评估。为了解决这个问题,开发了与浊积岩储层相关的饱和度定律-之所以选择这种地质学,是因为单个砂包的结构可以建模为一堆水平床。有效的介质和摄动理论被应用于确定该模型的地震特性。该计算提供了一种关系,该关系通过对孔隙度的垂直扩展和储层中饱和度变化的统计度量将真实饱和度S_w与地震有效流体模量联系起来。可以从仿真模型中提取这些统计数据,并且如果已知的话,则与其他众所周知的定律相比,可以使新的饱和定律在估计S_w时在准确性方面有显着提高。所建立的关系还可以捕捉层间页岩的影响,因此,只要已知页岩成分的比例,就可以用来估算净中值至中值至低净值的储层区域的真实饱和度。实际上,饱和度定律的最终选择取决于可用的储层信息,可以容忍的假设以及任何特定储层特征研究中要求的精​​度。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号