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Applications of 2D-NMR maps and geometric pore scale modeling for petrophysical evaluation of a gas well

机译:二维核磁共振图谱和几何孔隙尺度模型在气井物性评价中的应用

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This paper presents the petrophysical evaluation of a gas reservoir from the Gulf of San Jorge basin, Argentina, by means of two-dimensional nuclear magnetic resonance (2D-NMR) maps and a geometric pore scale modeling of the NMR response of the wetting phase. The reservoir contains gas and irreducible water saturation at the top with a sharp transition into the water zone. The well has been logged with conventional tools such as gamma ray, neutron, density, and also the MRExplorer~(SM) (MREX~(SM)) to acquire the NMR data for determining the irreducible water saturation. Data from special core analysis, scanning electron microscopy, thin sections, and capillary pressure tests have also been acquired. The core-log evaluation shows a very good agreement between the laboratory and log field data, especially in terms of irreducible water saturation, porosity, and permeability, which was also modeled using the Timur-Coates equation for purposes of field delivery. The 2D-NMR maps as Tl vs. T2 apparent (T2_(app)) and diffusivity vs. T2 intrinsic (T2i_(int)) from both hydrocarbon and water zone lead to characterize the clay-bound and capillary-bound water and the under-called porosity due to the low hydrogen index of the gas. We use a pore scale model to quantify the effect of pendular water on T2 distribution.rnThe methodology is based on constructing physically representative model rocks numerically, which allows precise geometric description of pore space. Unlike many other approaches to pore-level modeling, this approach introduces no adjustable parameters and can be used to produce quantitative, a priori predictions of the rock macroscopic behavior.
机译:本文通过二维核磁共振(2D-NMR)图和润湿相NMR响应的几何孔隙尺度模型,对阿根廷圣豪尔赫盆地海湾的一个气藏进行了岩石物性评价。储层顶部含有气体和不可还原的水饱和度,并急剧过渡到水区。该井已用常规工具(例如,伽马射线,中子,密度)以及MRExplorer(SM)(MREX((SM)))进行了测井,以获取NMR数据以确定不可还原的水饱和度。还获得了来自特殊岩心分析,扫描电子显微镜,薄片和毛细管压力测试的数据。核心测井评估表明实验室数据和测井数据之间有很好的一致性,特别是在不可减少的水饱和度,孔隙度和渗透率方面,这也使用Timur-Coates方程进行了建模以用于现场输送。烃和水区的2D-NMR图谱分别为T1对T2表观(T2_(app))和扩散率对T2本征(T2i_(int)),从而表征了黏土结合水和毛细管结合水以及由于气体的氢指数低,因此称为“孔隙率”。我们使用孔隙尺度模型来量化水对T2分布的影响。该方法基于以数值方式构造具有物理代表性的模型岩石,从而可以对孔隙空间进行精确的几何描述。与孔隙水平建模的许多其他方法不同,该方法不引入可调整的参数,可用于生成岩石宏观行为的定量先验预测。

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