JGE Pub Date : 2020-01-17 DOI:10.23960/JGE.V5I1.1133
F. Tarigan, Ordas Dewanto, Karyanto Karyanto, R. C. Wibowo, Andika Widyasari
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引用次数: 1

摘要

在进行岩石物理分析时,每种性质都有许多方法。因此,有必要确定适用于研究领域的每种岩石物理性质的精确方法,以避免解释时的不规则性。岩石物性由体积页岩、孔隙度、含水饱和度等组成。本研究使用了FBT01、FBT02、FBT03、FBT04、FBT05和FBT06六口井的数据,并辅以FBT03中的岩心数据。岩心数据被用作岩石物理分析的参考,因为它被认为代表或接近现场的实际储层条件。本研究区域位于南苏门答腊盆地“FBT”油田的Talangakar组。根据照片岩心和岩性,最适合“FBT”现场条件的体积页岩法是伽马射线中子密度法。至于有效孔隙度,最适合该领域的方法是中子密度声波法。油水接触有助于确定油气储量。在FBT01、FBT02、FBT03、FBT04、FBT05和FBT06的2277.5英尺、2226.5英尺、2312.5英尺、2331英尺、2296英尺和2283.5英尺深度处获得油水接触。FBT油田Talangakar组的油水接触深度差异是由地下结构引起的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ANALISIS PETROFISIKA UNTUK MENENTUKAN OIL-WATER CONTACT PADA FORMASI TALANGAKAR, LAPANGAN “FBT”, CEKUNGAN SUMATRA SELATAN
In conducting petrophysics analysis, there are many methods on each property. Therefore, it is necessary to determine the exact method on each petrophysical property suitable for application in the field of research in order to avoid irregularities at the time of interpretation. The petrophysical property consists of volume shale, porosity, water saturation, etc. This research used six well data named FBT01, FBT02, FBT03, FBT04, FBT05, and FBT06 and also assisted with core data contained in FBT03. Core data used as a reference in petrophysical analysis because it was considered to have represented or closed to the actual reservoir conditions in the field. The area in this research was in Talangakar Formation, "FBT" Field, South Sumatra Basin. The most suited volume shale method for “FBT” field condition was gamma ray-neutron-density method by seeing its photo core and lithology. As for the effective porosity, the most suited method for the field was neutron-density-sonic method by its core. Oil-water contact was useful to determine the hydrocarbon reserves. Oil-water contact was obtained at a depth of 2277.5 feet on FBT01, 2226.5 feet on FBT02, 2312.5 feet on FBT03, 2331 feet on FBT04, 2296 feet on FBT05, and 2283.5 feet on FBT06. The oil-water contact depth differences at Talangakar formation in FBT field caused by structure in subsurface.
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JGE
JGE
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