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首页> 外文期刊>Applied Magnetic Resonance >Calculation of Irreducible Water Saturation (S_(wirr)) from NMR Logs in Tight Gas Sands
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Calculation of Irreducible Water Saturation (S_(wirr)) from NMR Logs in Tight Gas Sands

机译:从致密气砂中的NMR测井计算不可还原的水饱和度(S_(wirr))

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摘要

It is difficult to calculate irreducible water saturation (S_(wirr)) from nuclear magnetic resonance (NMR) logs in tight gas sands due to the effect of diffusion relaxation on the NMR T_2 spectrum at present. By combining with classical Timur and Schlumberger-Doll Research (SDR) models, a novel model of calculating S wirr is derived. The advantage of this novel model is that S_(wirr) can be calculated without a T_2 cutoff, and all input information can be acquired from NMR logs accurately. With the calibration of 36 core samples, which were drilled from Xujiahe Formation in Bao-jie region of Triassic, Sichuan basin, southwest China, the values of these statistic model parameters are defined. Field examples of tight gas sands show that the proposed model is reliable. The S_(wirr) calculated with the proposed model match well with core analyzed results both in tight gas formations and water-saturated layers, the absolute error is in the range of ±4%. The calculated results by using 20.75 ms as the T_2 cutoff are accurate in water-saturated layers but are overestimated in gas-bearing intervals. Defining 33 ms as the T_2 cutoff is unusable both in gas-bearing and water layers.
机译:目前,由于扩散弛豫对NMR T_2光谱的影响,很难从致密气砂中的核磁共振(NMR)测井图中计算出不可还原的水饱和度(S_(wirr))。通过结合经典的帖木儿和斯伦贝谢娃娃研究(SDR)模型,得出了计算s wirr的新模型。这种新颖模型的优点是可以在没有T_2截止的情况下计算S_(wirr),并且可以从NMR测井中准确获取所有输入信息。通过对西南盆地四川三叠系宝界地区须家河组钻探的36个岩心样品进行标定,确定了这些统计模型参数的取值。致密气砂的现场实例表明,该模型是可靠的。用该模型计算的S_(wirr)在致密气层和水饱和层中均与岩心分析结果吻合良好,绝对误差在±4%范​​围内。以20.75 ms作为T_2截止值的计算结果在水饱和层中是准确的,但在含气层中被高估了。将T_2截止时间定义为33 ms在含气层和水层均不可用。

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