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A Method to Compute Water Saturation in Tight Rocks Accounting for Conductivity of Clay Minerals

机译:一种在粘土矿物电导率下计算紧密岩石中的水饱和的方法

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The objective of this paper is to determine the water saturation applying the Waxman-Smits equation and using mineralogy analysis obtained from XRD/CT scanning and resistivity data for a tight sandstone formation. Contrarious to using Archie's equation, the suggested approach takes conductivity into account and provides more accurate water saturation calculations, in order to correctly predict oil and gas in place. Accurate computing of the correlations between rock resistivity and fluid saturations is vital to constructing 2D and 3D models of water saturation to understand the effect of microstructure on petrophysical properties of tight formations. The negative charges on the surface of monoclinic and triclinic clay minerals, with layered silica tetrahedra in shale rocks, hold electric interactions with bipolar molecules of water and free cations. The presence of clays in tight gas sandstone reservoirs may lead to the overestimation of water saturation, if the mineralogy is not properly included into the computations. This implies that proper water saturation characterization of tight gas reservoirs could lead to an increase of evaluated hydrocarbon resources. Such an increase may be significant in large newly discovered tight rock gas bearing basins with multiple shaley-sand sweet spots. The case study in this paper shows a computational analysis made by comparing Archie versus Waxman-Smits equations. Results from tight rock samples illustrate a proportional relationship between the clay content and the quantity of exchangeable clay. A new term, named the clay factor, Cf, has been obtained from this linear relationship, and was found that it could possibly replace the BQV term in the Waxman-Smits equation. These results show a promising workflow method to calculate water saturation considering the conductivity and fraction volume of clay minerals. As the mineralogy of a rock can be accurately identified by high resolution imaging techniques, an approach based on mineralogy, as the proposed method can be utilized as a better way to compute saturation using modification of the Waxman-Smits model. Good assessment of saturation can have a large impact in the computation of transition zones and gas resources in tight rocks, revisiting volumes that were counted as water in past models.
机译:本文的目的是确定应用蜡烛式方程的水饱和度,并使用从XRD / CT扫描和电阻率数据获得的矿物学分析进行紧密砂岩地层。对着使用ARCHIE的方程来说,建议的方法考虑了导电性并提供更准确的水饱和度计算,以便正确预测油气和天然气。精确计算岩石电阻率和流体饱和之间的相关性对于构建2D和3D模型的水饱和度至关重要,以了解微观结构对紧密地层的岩石物理性质的影响。在页岩岩石中具有层状二氧化硅四边形的单斜晶和三晶粘土矿物表面的负电荷,与双极分子的水和自由阳离子保持电相互作用。如果矿物学未被正确包括在计算中,粘土中的粘土可能导致水饱和度的高估。这意味着紧密气体储层的适当水饱和度表征可能导致评估的碳氢化合物资源增加。这种增加可能在大型新发现的紧密岩石轴承盆地中具有多种,具有多个Shaley沙子甜点。本文的案例研究显示了通过比较Archie与Waxman-Smits方程来进行的计算分析。紧密岩石样品的结果说明了粘土含量与可交换粘土量之间的比例关系。从这种线性关系中获得了一个名为CLAY因子CF的新术语,并且发现它可能替换蜡烛 - SMITS方程中的BQV术语。这些结果表明,考虑粘土矿物的电导率和馏分体积的水饱和度,这些结果显示了有希望的工作流程方法。由于可以通过高分辨率成像技术准确地识别岩石的矿物,这是一种基于矿物学的方法,因为所提出的方法可以用作使用蜡烛模型的修改来计算饱和度的更好方法。良好的饱和度评估在紧张区域和气体资源的计算中可能具有很大的影响,在紧张的岩石中,重新探测在过去的模型中被计入水的体积。

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