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First Integrated Petrophysical Characterization in Limestone in Ecuador: M1 and M2 Limestones, Puma Field

机译:厄瓜多尔石灰岩中的首次综合岩石物理特征:M1和M2石灰岩,彪马田

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The first integrated characterization of limestone in Ecuador was performed in the Ml and M2 limestones in the Puma field of the Oriente basin. The characterization was performed by using available information from open hole logs and by applying the dual porosity methodology, which requires the use of porosity curves, including density, neutron, and sonic. The method used enabled estimates to be made of secondary porosity, "variable M" system cementation exponent fracture porosity, fracture intensity index, and effective porosity of the system. The effective porosity model was calibrated with nuclear magnetic resonance (NMR) logs. The results were validated with pressure transient analysis (PTA), which confirmed the dual porosity system and fracture system properties, and identified the λ and ω parameters. The petrophysical interpretation of the M2 limestone is characterized as a unit of good thickness with an interconnected pay zone, accurate fracture intensity for the entire section, and excellent effective porosity estimate (fracture plus matrix porosity). Because the matrix has connected effective porosity and includes the presence of fractures, this unit, according to the Nelson classification of fractured natural reservoirs (NFR), may be a Type II. The M2 limestone is thicker than the Ml; its fracture intensity index and its correspondent matrix effective porosity are greater than Ml (NFR type I). PTA through A and ω values confirmed the classification of the reservoirs. This paper describes the first integrated petrophysical evaluation for Ml and M2 limestones in the Oriente basin of Ecuador. This evaluation involves a dual porosity characterization in which the connected porosity system helped to reduce the uncertainty in the original oil-in-place estimate. The method used could be applied in other Oriente basin fields to assess the potential of carbonate reservoirs.
机译:在东方盆地彪马领域的M1和M2灰岩进行石灰石在厄瓜多尔的第一个集成的特征。表征通过使用从裸眼井测井可用的信息和通过将双孔隙度的方法,这需要使用孔隙度曲线,包括密度,中子和声波的执行。该方法中使用能够进行次生孔隙的估计“变量M”系统胶结指数裂缝孔隙度,断裂强度指数,并且该系统的有效孔隙率。有效孔隙率模型用核磁共振(NMR)测井校准。将结果与压力瞬变分析(PTA),这证实了双孔隙度系统和断裂系统性能进行了验证,并确定了λ和ω参数。的M2石灰石的岩石物理解释的特征为良好的厚度的单元和一个互连油层,对于整个部分准确断裂强度,以及优异的有效孔隙度估计(断裂加基质孔隙率)。因为矩阵具有连接有效孔隙度,并且包括裂缝的存在,此单元,根据断裂天然水库的纳尔逊分类(NFR),可以是II型。的M2石灰石比ML厚;其断裂强度指数和其对应的矩阵的有效孔隙度大于ml的(NFR I型)。 PTA通过A和ω值确认了水库的分类。本文介绍了在厄瓜多尔的东方盆地M1和M2灰岩第一综合岩石物理评价。该评估涉及双重孔隙特征,其中,连通孔隙度系统有助于减少在原油就地估计的不确定性。所用的方法可以在其他东方盆地领域得到应用,以评估碳酸盐岩储层的潜力。

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