The Comparation of Water Saturation Approaches to Reveal a Low Resistivity Reservoir Potential Case in Gumai Formation, South Sumatra Basin

Dhea Adisty Pratami, S. Winardi, S. S. Surjono, W. Atmoko
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Abstract

The LRLC reservoir zone has been identified in SN-3 well, at the DAP-1 interval on Gumai Formation. This interval has a low resistivity value from 3-5 ohm.m and the drill stem test (DST) results show oil with gas without water. This study is objected to identify the causes of LRLC reservoir in gumai formation and finding a suitable sw calculation method. Some data such as well logs, reports, cores, and XRD are used to calculate petrophysical parameters such as Vsh, Phie, and Sw, and would be validated by DST data. Water saturation (Sw) calculations from Archie and the CEC method (Waxman Smits, Dual Water, Juhasz) were performed and the results were compared. The results showed that the main cause of the DAP-1 interval LRLC zone was the presence of clay minerals consisting of mixed layers (Illite/smectite). These clay minerals will be associated with high cation exchange capacity (CEC) values, with the value 70 (meq/100g), which can increase conductivity and reduce resistivity values. Based on lumping the more optimistic results of sw calculation from Waxman Smits Sw method (Sw based on CEC method). The DST data on the SN-3 well does not have water test data, so the calculation of the Sw value that is close to the Swirr value is considered the most suitable Sw for the low resistivity reservoir conditions of the Gumai Formation in the study area. The best practice for low resistivity reservoir for suitable petrophysical calculation is necessary to pay attention to the rock lithology conditions, the presence of mineral clay, and determining suitable Sw appropriate to the reservoir conditions
比较水饱和度方法,揭示南苏门答腊盆地古迈地层的低电阻率储层潜力案例
SN-3 井在古迈地层的 DAP-1 层段发现了 LRLC 储油层。该区间的电阻率值较低,为 3-5 欧姆.米,钻杆测试(DST)结果显示油气共存,不含水。本研究旨在确定古迈地层 LRLC 储层的成因,并找到合适的 Sw 计算方法。一些数据(如测井记录、报告、岩心和 XRD)被用来计算岩石物理参数,如 Vsh、Phie 和 Sw,并通过 DST 数据进行验证。根据 Archie 和 CEC 方法(Waxman Smits、Dual Water、Juhasz)进行了水饱和度(Sw)计算,并对结果进行了比较。结果表明,DAP-1 区间 LRLC 区的主要原因是存在由混合层(伊利石/直闪石)组成的粘土矿物。这些粘土矿物具有较高的阳离子交换容量(CEC)值(70(meq/100g)),可增加电导率并降低电阻率值。根据 Waxman Smits Sw 方法(基于 CEC 方法的 Sw)计算出的较为乐观的 Sw 结果。由于 SN-3 井的 DST 数据中没有水测试数据,因此计算出的 Sw 值接近 Swirr 值,被认为是最适合研究区古迈地层低电阻率储层条件的 Sw 值。低电阻率储层岩石物理计算的最佳做法是关注岩石岩性条件、矿物粘土的存在,并确定适合储层条件的合适 Sw 值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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