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Primary Drainage Relative Permeability in Hydrocarbon Reservoirs Interpreted Using Digital Rock Physics

机译:使用数字岩体物理解释的烃储层中的初级排水相对渗透性

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We apply multi-scale interrogation of complex carbonate reservoir rocks from whole core – plug – micro – nano scale,and then work backwards to upscale and integrate the properties to an acceptable 3D representation. This is achieved through imaging at different resolutions: for each image an equivalent network model is constructed. The smaller-scale networks are upscaled to generate effective properties for input into a plug-scale network representation of the rock. We study 54 samples from three reservoir zones of a Lower Cretaceous reservoir. Using the Dunham rock classification scheme we see a range of rock types from grainstone to mudstone-dominated. For primary drainage,the higher quality grain-dominated samples show better connectivity and a higher oil relative permeability than the poorer quality rocks. However,for waterflooding the situation is reversed: the better quality rocks tend to be more oil-wet,with a large water relative permeability which leads to early breakthrough and a poor local displacement efficiency. In contrast,the mudstones are mixed-wet and more poorly connected,which impedes the movement of water,leading to a more favourable local recovery. This study demonstrates how employing the state-of-the-art in multi-scale imaging and modeling,the behavior of complex carbonates can be quantified and interpreted,allowing an assessment of recovery based on pore structure and facies type.
机译:我们从整个核心插头微纳米秤上涂抹复杂碳酸盐储层岩石的多尺度询问,然后向后工作以高档,并将属性集成到可接受的3D表示。这通过以不同的分辨率进行成像来实现:对于每个图像,构造了等效网络模型。较小的网络被升级为生成有效属性,以输入岩石的插头级网络表示。我们研究了来自下白垩纪储层的三个水库区域的54个样品。使用Dunham Rock Classification Schements,我们看到一系列岩石从晶石到泥岩主导的岩石类型。对于初级排水,更高质量的谷物主导的样品显示出更好的连接性和比较差的质量岩石更高的油相对渗透性。然而,对于水顶来说,情况逆转:更好的质量岩石往往更加润湿,具有大的水相对渗透性,导致早期突破和局部位移效率差。相比之下,泥岩是混合湿润的,连接更差,阻碍了水的运动,导致局部恢复更有利。本研究表明如何在多尺度成像和建模中采用最先进的方式,可以量化和解释复合碳酸盐的行为,从而评估基于孔结构和相型的恢复。

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