KLASIFIKASI PETROFISIKA TIPE BATUAN UNTUK MEMPREDIKSI KUALITAS RESERVOAR PASIR SERPIHAN PADA FORMASI TALANG AKAR, CEKUNGAN ONWJ

JGE Pub Date : 2020-01-17 DOI:10.23960/JGE.V4I3.1072
Feni Priyanka, Ordas Dewanto, B. Mulyatno, Riezal Ariffiandhany
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Abstract

Hydrocarbons were accumulated in reservoir, the reservoir has a lot of types depending on the geological conditions and the constituent mineral. In ONWJ basins, sub-basins Arjuna, Talang Akar Formation is sand splintersreservoir type. The presence of clay in a reservoir will reduce the resistivity and increase thesaturation, so it takes a multimineral analysis and the reservoir qualityclassification. In this study, physical properties (porosity, permeability, Rw, and saturation) and the quality of the reservoir can be identified through petrophysical analysis by utilizing log data and core analysis, and the rocktypeprediction(using R35 Winland or HFU method). In this study 5 wells (IX-A1, IX-13, IX-4, IX-7 and IX-8)used and found eight hydrocarbon zones, 6 are validated by the DST (drill steam test)data, androck type method that suitable is the method of HFU (hydraulic flow units) due to the coefficient of correlation between porosity and permeability shows a value of 0.75, based on the calculations, the eight types of rock is conclude, where the dominance of the rock typeis the type 12 with a pore size between 5-10 microns, type reservoir rocks in this study belong to the lithofacies distributary channel and mouthbar sand. By knowing the petrophysical property values, it can determine reservoir productivity and determine the zone eligible to be produced or not, by using curve SMLP (Stratigraphic Modified Lorenz Plot).
BATUNE类型的岩石分类以预测储层的质量PASIR更多陆地形成的信息,ONWJ生长
油气在储层中富集,根据地质条件和组成矿物的不同,储层类型繁多。在ONWJ盆地中,亚盆地Arjuna、Talang Akar组为砂屑伺服类型。储层中粘土的存在会降低电阻率并增加饱和度,因此需要进行多矿物分析和储层质量分类。在本研究中,储层的物理性质(孔隙度、渗透率、Rw和饱和度)和质量可以通过利用测井数据和岩心分析的岩石物理分析以及岩石类型预测(使用R35 Winland或HFU方法)来确定。在本研究中,使用了5口井(IX-A1、IX-13、IX-4、IX-7和IX-8)并发现了8个油气层,其中6口井通过DST(钻井蒸汽测试)数据进行了验证,由于孔隙度和渗透率之间的相关系数显示出0.75的值,因此适合采用HFU(水力流动单元)方法的岩石类型方法,岩石类型以孔隙大小在5-10微米之间的12型为主,本研究中的储层岩石类型属于岩相分流河道和河口坝砂。通过了解岩石物性值,可以通过使用SMLP曲线(地层改良洛伦兹图)来确定储层生产力,并确定是否符合生产条件的区域。
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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JGE
JGE
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22 weeks
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