DETERMINING OF FORMATION WATER SATURATION TO ESTIMATE REMINING HYDROCARBON SATURATION IN THE X LAYER Y FIELD

R. Sitaresmi, G. Wijanarko, P. Wijayanti, Danaparamita Kusumawardhani
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引用次数: 2

Abstract

Efforts are made to find the remaining hydrocarbons in the reservoir, requiring several methods to calculate the parameters of reservoir rock characteristics. For this reason, logging and core data are required. The purpose of this research is to estimate the Remaining Hydrocarbon Saturation that can be obtained from log data and core data. With several methods used, can determine petrophysical parameters such as rock resistivity, shale volume, effective porosity, formation water resistivity, mudfiltrate resistivity and rock resistivity in the flushed zone (Rxo) and rock resistivity in the Uninvaded Zone which will then be used to calculate the Water Saturation value Formation (Sw) and Mudfiltrat Saturation. (Sxo) In this study four exploratory wells were analyzed. Shale volume is calculated using data from Gamma Ray Log while effective Porosity is corrected for shale volume. Rw value obtained from the Pickett Plot Method is 0.5 μm. The average water saturation by Simandoux Method were 33.6%, 43.4%, 67.0% and 39.7% respectively in GW-1, GW-2, GW-3 and GW-4 wells. While the average water saturation value by the Indonesian Method were 43.9%, 48.8%, 72.3% and 44% respectively in GW-1, GW-2, GW-3 and GW-4 wells. From comparison with Sw Core, the Simandoux Method looks more appropriate. Average mudfiltrate (Sxo) saturation by Simandoux Method were 65.5%, 68.2%, 77.0% and 64.6% respectively in GW-1, GW-2, GW-3 and GW wells -4. Remaining Hydrocarbon Saturation (Shr) was obtained by 34.5%, 31.8, 23%, 35.4% of the results of parameters measured in the flushed zone namely Rxo, Rmf and Sxo data. For the price of Moving Hydrocarbons Saturation or production (Shm) is 31.9%, 24.8%, 10%, 24.9% in wells GW-1, GW-2, GW-3 and GW-4.
通过测定地层含水饱和度来估计x层y油田的矿物烃饱和度
为了寻找储层中的剩余烃,需要几种方法来计算储层岩石特征参数。因此,需要日志记录和核心数据。本研究的目的是利用测井资料和岩心资料估算剩余烃饱和度。通过使用多种方法,可以确定岩石物理参数,如岩石电阻率、页岩体积、有效孔隙度、地层水电阻率、淹水带(Rxo)的泥浆电阻率和岩石电阻率,以及未侵水带的岩石电阻率,然后用于计算地层含水饱和度(Sw)和泥浆饱和度(Sw)。本研究对4口探井进行了分析。利用伽马射线测井数据计算页岩体积,同时根据页岩体积校正有效孔隙度。Pickett Plot Method测得的Rw值为0.5 μm。西芒杜法计算的GW-1、GW-2、GW-3和GW-4井平均含水饱和度分别为33.6%、43.4%、67.0%和39.7%。而GW-1井、GW-2井、GW-3井和GW-4井的平均含水饱和度分别为43.9%、48.8%、72.3%和44%。与Sw Core相比,Simandoux Method看起来更合适。Simandoux法测定的GW-1、GW-2、GW-3和GW -4井的平均泥浆饱和度分别为65.5%、68.2%、77.0%和64.6%。剩余烃饱和度(Shr)分别为冲洗带实测参数Rxo、Rmf和Sxo数据的34.5%、31.8%、23%和35.4%。在GW-1、GW-2、GW-3和GW-4井中,移动烃饱和度或产量(Shm)分别为31.9%、24.8%、10%和24.9%。
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