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Estimation of Porosity, Permeability and Water Saturation in Tight Sandstone Reservoirs Based on Diagenteic Facies Classification Method: Case Studies of Chang 8 Formation in Northwest Ordos Basin

机译:基于仿真面分类方法的紧密砂岩储层孔隙,渗透性和水饱和度研究 - 以西北鄂尔多斯盆地昌8型形成的案例研究

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Porosity, permeability and water saturation cannot be effectively estimated from conventional logs by using the classical methods in tight sandstone reservoirs due to the complicated mineral components, pore structure and strong heterogeneity that caused by the diagenesis in the Chang 8 Formation of northwest Ordos basin, In this paper, based on the difference of diagenetic facies, effective formations are classified into three types, the relationships between conventional density log and core derived porosity, core derived porosity and permeability are established in every type of formation. In the meanwhile, the laboratory resistivity experimental results are also classified based on the diagenetic facies, and the cross plots of porosity and formation factor, water saturation and resistivity index are drawn to obtain the rock resistivity parameters, separately. These results illustrate that for formations with different diagenetic facies, the matrix densities are diverse, the relationships between core derived porosity and permeability are also different, and they contain different rock resistivity parameters. By using the diagenetic facies classification method and chart proposed by Xiao (2012), the effective Chang 8 Formation is classified into three types, and the corresponding models are applied to calculate porosity, permeability and water saturation. Comparisons of estimated porosity, permeability and water saturation by using the proposed techniques and the core derived results illustrate that the proposed techniques are valueable in tight sandstone reservoir parameters evaluation.
机译:孔隙度,渗透率和水饱和度不能被有效地从常规测井通过使用紧砂岩储层经典方法估计由于复杂的矿物成分,孔隙结构和非均质性强引起的在西北鄂尔多斯盆地,在长8形成成岩本文中,基于成岩相的不同,有效结构被分为三类,常规密度测井和核心衍生的孔隙率,芯衍生孔隙度和渗透率之间的关系被建立在每个类型的形成。在此期间,在实验室的电阻率的实验结果也被分类基于所述成岩相,和孔隙度和地层因素,水饱和度和电阻率指数的横地块被拉伸以得到岩石电阻率参数,另。这些结果说明,对于具有不同的成岩相地层中,基质密度是多种多样的,核心衍生孔隙度和渗透率之间的关系也不同,并且它们包含不同的岩石电阻率参数。通过使用由萧(2012)提出的成岩相分类方法和图表,该有效长8形成是分为三种类型,以及相应的模型用于计算孔隙度,渗透率和水饱和度。通过使用所提出的技术和芯衍生结果估计孔隙度,渗透率和水饱和度的比较示出了所提出的技术是在致密砂岩储层参数评价居停。

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