...
首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Combined simulation and inversion of SP and resistivity logs for the estimation of connate-water resistivity and Archie's cementation exponent
【24h】

Combined simulation and inversion of SP and resistivity logs for the estimation of connate-water resistivity and Archie's cementation exponent

机译:结合SP和电阻率测井的模拟和反演估算原生水电阻率和Archie胶结指数

获取原文
获取原文并翻译 | 示例
           

摘要

Knowledge of initial water saturation is necessary to estimate original hydrocarbon in place. A reliable assessment of this petrophysical property is possible when rock-core measurements of Archie's parameters, such as saturation exponent n and cementation exponent m, are available. In addition, chemical analysis of formation water is necessary to measure connate-water resistivity R-w. Such measurements are seldom available in most applications; if they are available, their reliability may be questionable. We describe a new inversion method to estimate R,, and Archie's cementation exponent from the combined use of borehole spontaneous-potential (SP) and raw array-induction resistivity measurements acquired in water-bearing depth intervals. Combined inversion of resistivity and SP measurements is performed assuming a piston-like invasion profile. In so doing, the reservoir is divided into petrophysical layers to account for vertical heterogeneities. Inversion products are values of invaded and virgin formation resistivity, radius of invasion, and static spontaneous potential (SSP). Connate-water resistivity is calculated by assuming membrane and diffusion potentials as the main contributors to the SSP. Archie's or dual-water equations enable the estimation of m. The new combined estimation method has been successfully applied to a data set acquired in a clastic formation. Data were acquired in a high permeability and moderately highsalt-concentration reservoir. Values of R. and m yielded by the inversion are consistent with those obtained with a traditional interpretation method, thereby confirming the reliability of the estimation. The method is an efficient, rigorous alternative to conventional interpretation techniques for performing petrophysical analysis of exploratory and appraisal wells wherein rock-core measurements may not be available.
机译:初始含水饱和度的知识对于估算到位的原始碳氢化合物很有必要。当可以使用阿奇参数的岩心测量值(例如饱和指数n和胶结指数m)进行可靠的评估时,就可以对该岩石物理性质进行可靠的评估。另外,对地层水的化学分析对于测量原生水电阻率R-w是必要的。这种测量在大多数应用中很少可用。如果可用,其可靠性可能会令人怀疑。我们描述了一种新的反演方法,通过结合使用钻孔自发势能(SP)和在含水深度间隔中获得的原始阵列感应电阻率测量值来估算R和Archie的胶结指数。假设活塞状的侵入剖面,进行电阻率和SP测量的组合反演。在这种情况下,储层被划分为岩石物理层,以解决垂直非均质性问题。反演产物是已侵入和原始地层的电阻率,侵入半径和静态自发电势(SSP)的值。通过假设膜和扩散电位是SSP的主要贡献者来计算天然水电阻率。通过阿奇或双重水方程,可以估算m。新的组合估计方法已成功应用于碎屑岩层中采集的数据集。在高渗透率和中等高盐浓度的储层中采集数据。反演得到的R.和m的值与用传统解释方法获得的值一致,从而证实了估计的可靠性。该方法是常规解释技术的一种有效,严格的替代方法,用于对可能无法获得岩心测量值的勘探和评估井进行岩石物理分析。

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