Methods of Division of Development Unit for Thick Carbonate Reservoir—A Case Study of the Mishrif Formation, A Oilfield, Middle East

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geofluids Pub Date : 2024-11-08 DOI:10.1155/2024/7361600
Fengfeng Li, Yong Li, Jiaheng Chen, Lei Li, Lixin Ren, Lei Meng, Wenyu Wang, Yang Wan, Yuedong Lu, Haowei Chen
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Abstract

This paper is aimed at introducing a method for the division of development units of thick carbonate reservoirs. This method consists of eight steps, ranked according to impact weight, each of which is independent but intrinsically linked. When there is a conflict between studies in different steps, the results of the previous step take precedence. (1) Pressure is the most important and reliable data. When the wells with an abnormal pressure gradient in the same interval account for more than 60%, further division of the reservoir is appropriate. (2) Baffles are the second most important and reliable basis. When there are continuous baffles or poor reservoirs that encounter more than 80% wells, it is appropriate to further divide reservoirs. (3) Without the two mentioned above, but with an unconformity surface or discontinuity surface between two sequences, it is appropriate to treat these two sequences as two development units. (4) Without the three mentioned above, if the permeability above and below the sequence boundary differs by 10 or more times, reservoirs above and below the sequence boundary are appropriate as distinct development units. (5) When the thickness, continuity, distribution pattern, and microstructure of two adjacent sequences are significantly different, it is appropriate to treat these two sequences as two development units. (6) If the development units are based on sequences, check for homogeneity within the stratigraphy. If depositional facies or physical property discontinuities are present, the sequence would be reconsidered for subdivision. (7) The reserves in each development unit should account for more than 20% of that of the whole reservoir. (8) When the division of the development units is complete, it needs to be examined to ensure that there is a consistent structure, fluid property, and free water level. If inconsistencies exist, then subdivision is considered. The method was successfully applied to A oilfield, Central Arabian Basin, in combination with the cores, cast thin sections, regular or special core analysis, wireline logging data from 450 wells, formation pressure from 63 wells, and more than 100 wells with a production logging test. The Mishrif reservoir was divided into four development units, in which different well patterns and well types were deployed. The improved development effect proves that the division of development units for thick bioclastic limestone reservoir is reasonable.

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厚碳酸盐岩储层开发单元划分方法--中东 A 油田 Mishrif 油层案例研究
本文旨在介绍一种划分厚碳酸盐岩储层开发单元的方法。该方法由八个步骤组成,根据影响权重进行排序,每个步骤都是独立的,但又有内在联系。当不同步骤的研究结果发生冲突时,前一步骤的结果优先。(1) 压力是最重要、最可靠的数据。当同一区间压力梯度异常的井占 60%以上时,应进一步划分油藏。(2) 挡板是第二重要和可靠的依据。当遇到 80%以上的井有连续挡板或储层不良时,宜进一步划分储层。(3)没有上述两种情况,但两个层序之间有不整合面或不连续面,宜将这两个层序作为两个开发单元。(4) 没有上述三种情况,如果层序边界上下的渗透率相差 10 倍或 10 倍以上,则层序边界上下的储层宜作为不同的开发单元。(5) 当相邻两个层序的厚度、连续性、分布模式和微观结构有明显差异时,宜将这两个层序作为两个开发单元。(6) 如果开发单元以序列为基础,则应检查地层内部的同质性。如果存在沉积面或物理性质的不连续性,则应重新考虑序列的划分。(7) 每个开发单元的储量应占整个储层储量的 20%以上。(8) 开发单元划分完成后,需要对其进行检查,以确保结构、流体性质和自由水位一致。如果存在不一致,则考虑进行细分。该方法结合岩心、铸薄切片、常规或特殊岩心分析、450 口井的有线测井数据、63 口井的地层压力以及 100 多口井的生产测井测试,成功应用于阿拉伯盆地中部的 A 油田。Mishrif 油藏被划分为四个开发单元,其中部署了不同的井型和井种。开发效果的改善证明,对厚生物碎屑岩石灰岩储层划分开发单元是合理的。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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