Integrated Formation Evaluation Using Novel Neutron Correction in the Presence of Trace Elements

Hao Zhang, Nora Alarcon, F. Mendez
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Abstract

The estimation of formation porosity in particular and formation volumetrics in general are key to any reservoir evaluation as they establish the hydrocarbon storage capacity. Compensated neutron porosity is one of the most common measurements incorporated in any log-based volumetric analysis. However, this type of measurement is strongly affected by the presence of trace elements, especially in clay rich formations. Trace elements, such as boron and gadolinium, have very high neutron capture cross-sections and absorb large amounts of thermal neutrons in the formation. Whenever these elements are present in concentrations exceeding just a few parts per million they have a significant effect on overall thermal neutron capture, yielding high apparent neutron porosity. When the measurement is included in an integrated log analysis system, this results in inaccurate formation porosity and matrix volumes. A reliable neutron porosity correction method is therefore needed to improve petrophysical evaluation in in such logging environments. In this work, an integrated model is proposed to correct the compensated neutron response using pulsed neutron spectroscopy measurements and other conventional log data. A joined inversion method is implemented which obtains an improved neutron response by removing the undesirable contributions by the trace elements which are not a part of the formation petrophysical model. The proposed model is validated, by applying it to several data sets from different shale plays in North America and Latin America, and comparing the results against core analysis data. Due to presence of rich trace elements in the formation, without the correction model, the original processing results indicate up to 50% higher formation porosity when compared with core measurements. After applying the proposed correction, the porosity comparison is dramatically improved, matching the reference core porosity. The proposed model offers an effective, integrated analysis method, in challenging unconventional clay-rich shale environments, for correct estimation of formation porosity and volumes of mineral constituents.
微量元素存在下新型中子校正综合地层评价
储层孔隙度和储层体积的估算是储层评价的关键,因为它们决定了储层的储油能力。补偿中子孔隙度是测井体积分析中最常用的测量方法之一。然而,这种类型的测量受到微量元素存在的强烈影响,特别是在富含粘土的地层中。微量元素,如硼和钆,具有很高的中子俘获截面,并在地层中吸收大量的热中子。当这些元素的浓度超过百万分之几时,它们就会对整个热中子捕获产生重大影响,产生高的表观中子孔隙率。当测量包含在综合测井分析系统中时,会导致地层孔隙度和基质体积不准确。因此,需要一种可靠的中子孔隙度校正方法来改善这种测井环境下的岩石物性评价。在这项工作中,提出了一个综合模型,利用脉冲中子谱测量和其他常规测井数据来校正补偿的中子响应。采用联合反演方法,通过去除不属于地层岩石物理模型的微量元素的不良贡献,获得了更好的中子响应。通过将该模型应用于北美和拉丁美洲不同页岩区的多个数据集,并将结果与岩心分析数据进行比较,验证了该模型的有效性。由于地层中存在丰富的微量元素,在没有校正模型的情况下,原始处理结果表明,与岩心测量结果相比,地层孔隙度高出50%。应用所提出的校正方法后,孔隙度对比得到显著改善,与参考岩心孔隙度相匹配。该模型为具有挑战性的非常规富泥页岩环境提供了一种有效的综合分析方法,可以正确估计地层孔隙度和矿物成分体积。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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