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DEPLOYING A FIT-FOR-PURPOSE FORMATION EVALUATION PROGRAM TO DE-RISK TIGHT GAS SAND PLAYS

机译:部署适合于目的的形成评估计划,以防范耐气沙剧

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challenges for petrophysical analysis where uncertainties are often much larger when compared to the usual conventional reservoirs. These low porosity and permeability rocks are associated with complex mineralogical properties and require an integrated approach to better characterize the reservoir, starting from a fit-for-purpose logging suite, the acquisition of high quality core and the implementation of an optimised core analysis program. In this paper the authors discuss an approach used to de-risk a tight gas play, where they made particular use of NMR log and Dean-Stark analysis for porosity and water saturation model calibration. OBM drilling fluids could not be used due to environmental restrictions consequently Deuterium Oxide (commonly known as D2O) was used to dope the water based drilling mud, to discriminate between the volumes of mud filtrate and formation water within the formation. The formations intercepted by the boreholes proved to have similarities from a stratigraphic/geological point of view, but showed significant differences when seeking to define producible water volumes using NMR estimates of irreducible water saturation (Swi) and core derived water saturations. In Well#1 resistivity derived water saturations were low and very close to NMR irreducible water saturations suggesting little or no formation water should be produced. In contrast in Well#2, a much more conglomeratic rock, a discrepancy was observed between core derived water saturations and NMR irreducible water saturations suggesting that this formation was not a irreducible water saturation and would likely contain producible water. It was also noteworthy that there existed a salinity variation between the two wells, where in Well #2 for formation water was more “fresh-brackish” then in Well #1. Well #1 was subsequently fracture stimulated and produced a mixture of gas, condensate and water (assumed to be frac fluid - based on salinity measurement) and well#2 was put on hold based on high water saturation indication and complex conglomeratic rock matrix. Petrophysical analysis played a key role in enabling the business decision through the integration of advanced logging and core analysis.
机译:与通常的传统水库相比,岩石物理学分析的挑战往往更大。这些低孔隙率和渗透性岩石与复杂的矿物质特性相关,并且需要一种综合方法来更好地表征储层,从拟合目的的测井套件开始,采集高质量核心和优化的核心分析程序的实施。在本文中,作者讨论了一种用于使狭窄气体发挥的措施的方法,在那里他们对孔隙度和水饱和模型校准进行了特别使用NMR日志和Dean-STARK分析。由于环境限制,不能使用OBM钻井液,因此使用氘氧化氘(通常称为D2O)来掺杂水基钻井泥浆,以区分在地层内的泥浆滤液和形成水之间。由钻孔截取的形成被证明是与地层/地质观点的相似性,但是在寻求使用不可缩续的水饱和度(SWI)和核衍生的水饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和水饱和时具有显着差异。在井中#1电阻率衍生的水饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和饱和度很少或根本没有形成水。相反,在井#2中,在核心衍生的水饱和饱和饱和饱和和NMR不可缩水中观察到差异,表明这种形成不是不可缩短的水饱和度,并且可能含有可生布的水。还值得注意的是,两个孔之间存在盐度变化,在井#2中的井#2中的井#2。然后在井#1中更为“新鲜咸咸”。随后,#1随后抗损伤并产生气体,冷凝物和水的混合物(假设是基于盐度测量的Frac流体 - 基于高水饱和指示和复杂的砾岩岩基质保持井#2。岩石物理学分析在通过整合高级测井和核心分析来实现业务决策方面发挥了关键作用。

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