长石溶解对致密砂岩储层孔隙结构和特征的影响:中国鄂尔多斯盆地东北缘案例研究

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2024-09-02 DOI:10.1155/2024/9069384
Yanhe Zhu, Zhigang Zhao, Xin Li, Chang Liu, Shanshan Yu, Yuanyuan Lu, Xuejia Du
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引用次数: 0

摘要

鄂尔多斯盆地是中国主要的致密产气盆地。在强异质物性背景下,致密储层仍存在高孔隙度和高渗透率的 "甜点"。长石溶解对孔隙度/渗透率有显著影响,但其成因机制尚不清楚,制约了对有效储层的预测。本文研究了长石溶解的成因及其对储层异质性的影响。以鄂尔多斯盆地东北缘主要产气地层石炭-二叠系地层为研究对象。通过薄片观察、物性测试、包裹体、同位素和产能分析等方法,研究了长石溶解机理及其对致密砂岩储层的积极改造作用。结果表明,目标砂岩主要由石英岩和长石岩组成。约 98.6% 的样本渗透率小于 1 mD,89.7% 的样本孔隙度小于 10%。致密储层内的高孔隙度/渗透率空间以溶蚀孔隙为主,占总孔隙空间的 80% 以上。溶解矿物主要与长石有关,长石溶解量与孔隙度和渗透率呈正相关。根据石英杂生和绿泥石(与长石溶解有关)的流体化学信息,长石溶解孔隙是由有机质热成熟产生的有机酸造成的。根据生产数据,当孔隙度和渗透率分别小于 7% 和 0.1 mD 时,单井无法实现日产量。然而,一旦超过这个孔隙度/渗透率临界值,生产能力就会成倍提高。此外,当长石溶解的表层孔隙度超过 7% 时,大多数孔隙度和渗透率值都超过了允许生产率的临界值,这表明广泛的长石溶解是致密油藏有效开发储层空间的有利因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Influence of Feldspar Dissolution on the Pore Structure and Characteristics of a Tight Sandstone Reservoir: A Case Study From the Northeast Margin of Ordos Basin, China

Influence of Feldspar Dissolution on the Pore Structure and Characteristics of a Tight Sandstone Reservoir: A Case Study From the Northeast Margin of Ordos Basin, China

The Ordos Basin is the main tight gas-producing basin in China. Under the background of strong heterogeneous physical property, there is still high porosity and permeability “sweet spot” in tight reservoirs. Feldspar dissolution exerts a significant effect on porosity/permeability, while its genetic mechanism is unclear, which restricts the prediction of effective reservoir. In this paper, genesis of feldspar dissolution and its effect on reservoir heterogeneity were studies. Carboniferous-Permian Formation, which is the main gas-producing strata in northeast margin of Ordos Basin, is taken as the target. Based on the methods of thin section observation, physical property test, inclusion, isotope and productivity analysis, mechanism of feldspar dissolution, and its positive modification to tight sandstone reservoir are studied. The results show that the target sandstone is dominantly made up of litharenite and feldspathic litharenite. About 98.6% of the samples possess permeability less than 1 mD, while 89.7% of the samples possess porosity less than 10%. The high porosity/permeability space within tight reservoirs is dominated by dissolved pores, accounting for more than 80% of the total pore space. The dissolution minerals are mainly associated with feldspar, and the amount of feldspar dissolution is positively correlated with porosity and permeability. According to the fluid chemical information of quartz overgrowth and ankerite (related to feldspar dissolution), feldspar dissolved pores are caused by organic acid derived from the thermal maturity of organic matter. According to production data, no daily production can be achieved in single well, when the porosity and permeability are less than 7% and 0.1 mD, respectively. However, once it exceeds this porosity/permeability threshold value, the production capacity is exponentially improved. Furthermore, when surface porosity of feldspar dissolution exceeds 7%, most values of the porosity and permeability exceed the threshold values of the allowable productivity, indicating that extensive feldspar dissolution is favorable factor for effective reservoir space development in tight reservoirs.

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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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