不同饱和度区域的现代论证方法

Yu. A. Rozhitsin, V. Belkina
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引用次数: 0

摘要

过去 10 到 15 年间在西西伯利亚开发的大多数矿床都具有结构复杂和高度复杂且规模较小的特点。只有在充分和足够精确的模型基础上,才能有效地开发这些矿床。如果不全面分析各类地质和地球物理信息,有时还要分析储层流体的物理和化学性质,就不可能建立复杂矿床的详细和高精度模型。 本研究旨在通过全面分析,阐明别列戈沃耶油田 PK19 2 油层的地质结构。 通过扩大测井范围、根据地震数据绘制有效厚度和含沙量预测图以及增加区域和地方基准,可以明确碳氢化合物的分布区域,并表明该矿床不是一个单一的矿床,而是由三个在流体力学上分离的矿床组成。流体接触的显著差异间接证实了矿床的岩性分异。对储油层流体物理化学性质的分析表明,北部和南部储油层饱和的凝析油类型不同,密度也大相径庭。研究结果得出了以下结论:首先,澄清并详细说明了别列戈沃耶油田 PK19 2 地层矿床的结构;其次,澄清了储量;第三,证明了北部矿床的凝析油密度,因此,在国家天平上确定凝析油储量以及从该矿床开采凝析油在经济上是不切实际的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Modern approaches to the justification of zones with different saturation
   Most of the deposits that that have been developed in Western Siberia over the past 10 to 15 years are characterized by a complex and highly complex structure with small sizes. The effective development of such deposits is possible only on the basis of adequate and sufficiently accurate models. The construction of detailed and high-precision models of complex deposits is impossible without a comprehensive analysis of all types of geological and geophysical information, and in some cases, the physical and chemical properties of reservoir fluids.   The aim of the study is to clarify the geological structure of the PK19 2 formation of the Beregovoye field through a comprehensive analysis.   The use of an expanded well logging, predictive maps of effective thicknesses and sandiness according to seismic data and the justification of an increased set of regional and local benchmarks made it possible to clarify the area of hydrocarbon distribution and show that the deposit is not a single one, but consists of three hydrodynamically separated deposits. The lithological differentiation of the deposits is indirectly confirmed by a significant difference in fluid contacts. The discrepancy between the contacts of the northern and southern deposits is 6 m. An analysis of the physico-chemical properties of reservoir fluids has shown that the northern and southern deposits are saturated with condensates of different types and significantly different densities. The results of the work have enabled the following conclusions to be drawn: firstly, the structure of the PK19 2 formation deposits of the Beregovoye field has been clarified and detailed; secondly, the reserves have been clarified; and thirdly, it has been demonstrated that the condensate density of the northern deposit is such that setting condensate reserves on the state balance and their extraction from this deposit are economically impractical.
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