首页> 外文会议>SPWLA annual logging symposium >QUANTITATIVE METHOD FOR ESTIMATING TOTAL ORGANIC CARBON AND POROSITY, AND FOR DIAGNOSING MINERAL CONSTITUENTS FROM WELL LOGS IN SHALE-GAS FORMATIONS
【24h】

QUANTITATIVE METHOD FOR ESTIMATING TOTAL ORGANIC CARBON AND POROSITY, AND FOR DIAGNOSING MINERAL CONSTITUENTS FROM WELL LOGS IN SHALE-GAS FORMATIONS

机译:页岩气地层测井中有机碳和孔隙度估算及矿质成分定量分析方法

获取原文

摘要

Reliable estimates of shale properties are critical for detecting perforation zones or candidates for hydro-fracturingjobs. Current methods for in-situ lithological and petrophysical assessment of organic shales are largely based onqualitative responses and empirical formulas. Even core-based measurements can be inconsistent and inaccuratewhen evaluating clay minerals and other grain constituents.We introduce a new method for organic-shale evaluation based on well logs to estimate total porosity, total organiccarbon (TOC) and volumetric/weight concentrations of mineral/fluid constituents. After detecting bed boundaries,the first step of the method is to perform separate inversion of individual well logs to estimate bed properties such asdensity, migration length, electrical conductivity, PEF (Photo Electric Factor), and Th (Thorium), U (Uranium), andK (Potassium) volumetric concentrations. Next, a multi-layer petrophysical model specific to organic shale isconstructed with an initial guess obtained from conventional petrophysical interpretation or XRD (X-RayDiffraction) data; bed properties are calculated with the initial layer-by-layer values. Final estimates of organic shaleproperties are obtained by progressively minimizing the difference between calculated and measured bed properties.A unique advantage of this method is the possibility of implicitly correcting for shoulder-bed effects in well logs,which are prevalent in shale-gas plays. Another advantage is the possibility of calculating accurate well-logresponses for specific petrophysical, mineral, fluid, and kerogen properties.Examples are described of the successful application of the new organic-shale evaluation method in the Haynesvilleshale-gas formation. This formation includes complex solid compositions and thin beds where rapid depth variationsof both mineral/fluid constituents are commonplace. Comparison of estimates for total porosity, total watersaturation, and TOC obtained using (a) conventional commercial software, (b) our organic-shale evaluation method,and (c) core/XRD measurements, indicates an improvement of more than 50% in estimates of total porosity andwater saturation when calculated with the newly developed method. The estimated TOC is also in agreement withcore laboratory measurements.
机译:对页岩性质的可靠估计对于检测射孔区或水力压裂候选物至关重要 职位。目前对有机页岩进行岩性和岩石物理评估的方法主要基于 定性反应和经验公式。甚至基于核的测量也可能不一致和不准确 在评估粘土矿物和其他谷物成分时。 我们介绍了一种基于测井曲线的有机页岩评估新方法,以估算总孔隙度,总有机质 碳(TOC)和矿物质/流体成分的体积/重量浓度。在检测到床边界之后, 该方法的第一步是对单个测井曲线进行单独的反演,以估算诸如 密度,迁移长度,电导率,PEF(光电系数),Th(T),U(铀)和 K(钾)体积浓度。接下来,建立有机页岩特有的多层岩石物理模型 根据常规岩石物理解释或XRD(X射线 衍射数据);用初始的逐层值计算床性质。有机页岩的最终估算 通过逐步最小化计算出的和测量的床层特性之间的差异来获得床层特性。 这种方法的独特优势是可以隐式校正测井中的肩床效应, 在页岩气中普遍存在。另一个优点是可以计算准确的测井曲线 对特定的岩石物理,矿物,流体和干酪根特性的响应。 举例说明了新的有机页岩评估方法在海恩斯维尔的成功应用 页岩气形成。这种地层包括复杂的固体成分和薄层,深度变化很快 两种矿物/流体成分都很常见。总孔隙率,总水量估算值的比较 饱和度,以及使用(a)常规商业软件,(b)我们的有机页岩评估方法获得的TOC, (c)岩心/ XRD测量表明,总孔隙率估算值提高了50%以上; 用新开发的方法计算出的水饱和度。估计的TOC也与 核心实验室测量。

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