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A NOVEL CALCULATION METHOD FOR TIGHT SANDSTONE PERMEABILITY USING ROCK CONDUCTIVITY

机译:一种利用岩导电导率的砂岩渗透性的一种新型计算方法

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The prediction of tight sandstone permeability is difficult due to the combined effects of regional tectonic setting, complex pore structure, formation anisotropy, strong heterogeneity and bound water. In order to solve this problem, this paper establishes a calculation model for the permeability of tight sandstone reservoirs from the micro-scale level, combined with the Hanai-Bruggeman equation and the Kozeny-Carman equation. The model well considers the effects of formation rock conductivity (Cs), particle conductivity (Cg), formation water conductivity (Cw) and cementation index (m) on rock permeability. The influence of rock conductivity on permeability was analyzed. The results showed that the permeability increases with the increase of rock conductivity. When the tight sandstone has a low conductivity, it has little effect on the permeability. On the contrary, the impact is greater. Finally, the model was applied to a low porosity and low permeability tight sandstone reservoir, which achieved good application results. The average absolute error of the reservoir permeability prediction was 0.035 mD. This study has certain reference value for the fine evaluation of tight sandstone reservoirs.
机译:由于区域构造凝固,复杂的孔隙结构,形成各向异性,强异质性和结合水的组合效应,砂岩渗透性的预测是困难的。为了解决这个问题,本文建立了砂岩储层从微尺度水平的渗透性的计算模型,结合了汉语 - Bruggean方程和Kozeny-Carman方程。该模型很好地考虑了形成岩导(Cs),颗粒导电性(CG),形成导水(CW)和胶结指数(M)对岩石渗透性的影响。分析了岩石电导率对渗透性的影响。结果表明,随着岩石电导率的增加,渗透性增加。当紧密砂岩具有低导电性时,它对渗透性几乎没有影响。相反,影响更大。最后,将该模型应用于低孔隙率和低渗透紧密砂岩储层,实现了良好的应用结果。储层渗透预测的平均绝对误差为0.035md。本研究具有一定的参考价值,用于砂岩储层的精细评估。

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