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首页> 外文期刊>Journal of Applied Geophysics >Quality-assured evaluation of effective porosity using fit-for-purpose estimates of clay-mineral volume fraction
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Quality-assured evaluation of effective porosity using fit-for-purpose estimates of clay-mineral volume fraction

机译:使用黏土矿物质体积分数的适合估计值,对有效孔隙度进行质量保证的评估

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Reservoirs that contain dispersed clay minerals traditionally have been evaluated petrophysically using either the effective or the total porosity system. The major weakness of the former is its reliance on "shale" volume fraction (V_(sh)) as a clay-mineral indicator in the determination of effective porosity from well logs. Downhole clay-mineral indicators have usually delivered overestimates of fractional clay-mineral volume (V_(cm)) because they use as a reference nearby shale beds that are often assumed to comprise clay minerals exclusively, whereas those beds also include quartzitic silts and other detritus. For this reason, effective porosity is often underestimated significantly, and this shortfall transmits to computed hydrocarbons in place and thence to estimates of ultimate recovery.The problem is overcome here by using, as proxy groundtruths, core porosities that have been upscaled to match the spatial resolutions of porosity logs. Matrix and fluid properties are established over clean intervals in the usual way. Log-derived values of V_(sh) are tuned so that, on average, the resulting log-derived porosities match the corresponding core porosities over an evaluation interval. In this way, V_(sh) is rendered fit for purpose as an indicator of clay-mineral content V_(cm) for purposes of evaluating effective porosity. The method is conditioned to deliver a value of effective porosity that shows overall agreement with core porosity to within the limits of uncertainty of the laboratory measurements. This is achieved through function-, reservoir- and tool-specific V_(sh) reduction factors that can be applied to downhole estimates of clay-mineral content over uncored intervals of similar reservoir character. As expected, the reduction factors can also vary for different measurement conditions. The reduction factors lie in the range of 0.29-0.80, which means that in its raw form, log-derived V_(sh) can overestimate the clay-mineral content by more than a factor of three. This exposition constitutes a major product of this paper.The implementation of the reduction factors demonstrably improves the evaluation of effective porosity from density, density-neutron and sonic logs, an exercise that also becomes more consistent across different tool types, with substantial reductions in uncertainty. This outcome brings petrophysics much closer to a verifiable equivalence of the effective and total porosity systems for enhanced quality assurance and thence a greater confidence in petrophysically-sourced reserves estimates.
机译:传统上,已使用有效孔隙度或总孔隙度系统对岩石中含有分散粘土矿物的储层进行了物性评估。前者的主要缺点是在确定测井有效孔隙度时,它依赖“页岩”体积分数(V_(sh))作为粘土矿物指标。井下粘土矿物指标通常提供了对粘土矿物体积分数(V_(cm))的高估,因为它们用作附近的页岩床的参考,这些页岩床通常被认为仅包含粘土矿物,而这些床也包含石英粉砂和其他碎屑。 。因此,有效孔隙率通常会被大大低估,这一缺口会传递到已计算出的碳氢化合物中,并进而传递到最终采收率的估算中。在此,通过使用已扩大规模以匹配空间的岩心孔隙度作为替代地基来克服这一问题。孔隙度分辨率。基质和流体特性是按常规方法在清洁间隔内确定的。调整V_(sh)的对数派生值,以使所得的对数派生孔隙率平均在评估间隔内与相应的岩心孔隙率匹配。以此方式,使V_(sh)适合作为目的,以作为评估有效孔隙率的粘土矿物含量的指标V_(cm)。该方法的条件是提供一个有效的孔隙率值,该值表明与岩心孔隙率的总体一致性在实验室测量结果的不确定性范围内。这是通过特定于功能,储层和工具的V_(sh)减少因子实现的,这些因子可用于在类似储层特征的无岩心区间内对粘土矿物含量进行井下估算。不出所料,减少因数也可能因不同的测量条件而异。还原因子在0.29-0.80范围内,这意味着以原始形式得到的对数派生的V_(sh)可能高估了粘土矿物含量的三倍以上。该说明构成了本文的主要成果。降低因子的实现明显改善了对密度,密度中子和声波测井的有效孔隙度的评估,该方法在不同工具类型之间也变得更加一致,并且不确定性大大降低。这一结果使岩石物理学更接近于有效孔隙度系统和总孔隙度系统的可验证等效性,从而提高了质量保证,因此对岩石物理来源的储量估算具有更大的信心。

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