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首页> 外文期刊>Journal of geophysics and engineering >Cation exchange capacity (Q(v)) estimation in shaly sand reservoirs: case studies in the Junggar Basin, northwest China
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Cation exchange capacity (Q(v)) estimation in shaly sand reservoirs: case studies in the Junggar Basin, northwest China

机译:泥质砂岩储层阳离子交换能力(Q(v))估算:以中国准gar尔盆地为例

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摘要

Cation exchange capacity (Qv) is a key parameter in resistivity-based water saturation models of shaly sand reservoirs, and the accuracy of Qv calculation is crucial to the prediction of saturations of oil and gas. In this study, a theoretical expression of Qv in terms of shaly sand permeability (Kshaly-sand), total porosity (phi(t)), and salinity of formation water (S) is deduced based on the capillary tube model and the physics volume model. Meanwhile, the classical Schlumberger-Doll research (SDR) model has been introduced to estimate Kshaly-sand. On this basis, a novel technique to estimate Qv from nuclear magnetic resonance (NMR) logs is proposed, and the corresponding model is also established, whose model parameters are calibrated by laboratory Qv and NMR measurements of 15 core samples from the Toutunhe formation of the Junggar Basin, northwest China. Based on the experimental data sets, this technique can be extended to reservoir conditions to estimate continuous Qv along the intervals. The processing results of field examples illustrate that the Qv calculated from field NMR logs are consistent with the analyzed results, with the absolute errors within the scope of +/-0.1 mmol cm(-3) for the majority of core samples.
机译:阳离子交换容量(Qv)是基于电阻率的泥质砂岩储层水饱和度模型中的关键参数,Qv计算的准确性对于预测油气饱和度至关重要。在这项研究中,根据毛细管模型和物理量推导了Qv的理论表达式,表示为页岩砂渗透率(Kshaly-sand),总孔隙率(phi(t))和地层水盐度(S)。模型。同时,引入了经典的斯伦贝谢娃娃研究(SDR)模型来估计Kshaly沙地。在此基础上,提出了一种新的从核磁共振(NMR)测井曲线估算Qv的技术,并建立了相应的模型,该模型的模型参数通过实验室Qv和NMR测量校正了图顿河地层的15个岩心样品。准gar尔盆地,中国西北。基于实验数据集,可以将该技术扩展到储层条件,以沿该区间估算连续的Qv。现场实例的处理结果表明,从现场NMR测井得出的Qv与分析结果一致,大多数核心样品的绝对误差在+/- 0.1 mmol cm(-3)范围内。

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