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A new method for estimating total organic carbon content from well logs

机译:一种从测井资料估算总有机碳含量的新方法

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With the booming exploration and development of unconventional hydrocarbon resources in source rocks, the estimation of total organic carbon (TOC) content from well logs has become increasingly important because of the significance of TOC in the formation evaluation of those resources. In this paper, a new log overlay method is developed to estimate the TOC content of source rocks with excess radioactivity, but containing little or no potassium feldspar. Specifically, on the basis of previous results of log responses of source rocks, it is believed that the natural gamma ray (GR) log responses of source rocks in the applicable conditions are predominantly contributed by clay minerals and organic matter. A practical clay indicator is established to reflect the clay content using density and neutron logs. The indicator is effective not only in nonsource rocks that contain oil or water but also in source rocks. Furthermore, a new method was developed by overlaying the properly scaled clay indicator curve on the GR curve. In nonsource rocks, including clay-rich rocks and reservoirs saturated with oil or water, the two curves overlie each other, whereas a separation between the curves occurs in organic-rich source rocks. The separation between the curves was defined and expressed and can be used to calculate the TOC consecutively after careful calibration with core data. This method has been successfully applied to two shale gas plays with high-maturity kerogen in the Sichuan Basin, China. In addition, a source rock with low-maturity kerogen was used to verify the new method for its effectiveness, reliability, and widespread adaptability.
机译:随着烃源岩非常规烃资源的勘探与开发的蓬勃发展,由于测井仪在这些资源的形成评价中具有重要意义,因此从测井中估算总有机碳含量变得越来越重要。本文提出了一种新的测井覆盖法来估算放射性过高但含钾长石少或不含钾长石的烃源岩的总有机碳含量。具体地,根据先前的烃源岩测井响应结果,可以认为,在适用条件下烃源岩的天然伽马射线(GR)测井响应主要由粘土矿物和有机质引起。建立了实用的黏土指示剂,以利用密度和中子测井来反映黏土含量。该指标不仅对含油或水的非烃源岩有效,而且对烃源岩也有效。此外,通过将适当比例的粘土指示剂曲线叠加在GR曲线上,开发了一种新方法。在非源岩中,包括富含粘土的岩石和充满油或水的储层,两条曲线相互重叠,而在富含有机物的源岩中则发生曲线间的分离。曲线之间的间距已定义并表示出来,可在对核心数据进行仔细校准后将其用于连续计算TOC。该方法已成功应用于中国四川盆地的两个含高成熟干酪根的页岩气层。此外,使用一种具有低成熟干酪根的烃源岩来验证这种新方法的有效性,可靠性和广泛的适应性。

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