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CALCULATED DETERMINATION OF VARIABLE WETTABILITY IN THE MIDDLE BAKKEN AND THREE FORKS, WILLISTON BASIN, USA

机译:计算中间Bakken可变润湿性的测定,美国威利斯顿盆地

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The determination of oil in place can be problematic informations with varying wettability using resistivitybased saturation models. This is because the Archie nsaturation exponent increases as wettability goes from 1)water wet to 2) mixed wet to 3) oil wet. The MiddleBakken and Three Forks in the Williston Basin are bothin this category and are formations with highly varyingwettability.In this study, we examined a combination of triplecombo, NMR, dielectric, and core data to determinewettability and the Archie n. By examining fluidcomposition as a function of T2 or T1 distribution, wecould examine wettability as a function of mineralogy(including clay), porosity, pore size, and depth. Theadvantage of this technique over using special coreanalysis is 1) reduced cost, 2) a continuous measurementwith depth, and 3) the ability to determine these valuesin-situ. The inherent changes in fluid properties resultingfrom core extraction, the changes in wettability becauseof core cleaning, and the uncertainty in measuring coreat reservoir conditions is effectively eliminated with thistechnique.Our results show that the Middle Bakken is mixed wetwith intervals that are more oil wet. It was determinedthat as a result of the increased carbonate and chloritecontent in the Three Forks, this formation is more oil wetthan the Middle Bakken. In both formations, the cleanestintervals are the most oil wet. Using the calculatedvariable n, a favorable comparison with core SCAL andsaturations was obtained, and will be shown in the paper.CRIM inversion of dielectric data, which gives a totallyindependent determination of bulk volume water,confirms the water volumes calculated with the variablen resistivity model.
机译:油状物的测定可以是有问题的使用电阻率的不同润湿性的形成基于饱和模型。这是因为ARCHIE N.随着润湿性从1开始,饱和度指数增加水湿至2)混合湿至3)油湿润。中间Bakken和Williston Basin中的三叉都是在此类别中,是具有高度变化的地层润湿性。在这项研究中,我们检查了三联人的组合用于确定的组合,NMR,介电和核心数据润湿性和Archie n。通过检查液体组成作为T2或T1分布的功能,我们可以作为矿物学的功能来检查润湿性(包括粘土),孔隙率,孔径和深度。这这种技术使用特殊核心分析为1)降低成本,2)连续测量深度和3)确定这些值的能力原位。液体性质的固有变化从核心提取,润湿性的变化,因为核心清洁,以及测量核心的不确定性在储层条件下有效地消除了技术。我们的结果表明,中间Bakken混合湿润间隔更加湿润。它是确定的这是由于碳酸盐和亚氯酸盐增加三叉中的内容,这种形成更加湿润比中间的bakken。在两个地层中,最干净间隔是最具湿的。使用计算出变量n,与核心尺度有利的比较获得饱和,并将在纸中显示。压力介质数据的反转,它完全介绍独立测定散装量水,确认用变量计算的水量n电阻率模型。

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