Saturation Height Modelling for Tight Sandstone Reservoirs with Gas Diffusion Dynamics Taken into Account

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2023-10-03 DOI:10.1155/2023/5583636
Zhou Lyu, Zhilun Yang, Yuhong Hao, Shunzhi Yang, Liqiong Wang, Sen Chang, Xiaomin Xue, Jing Li
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Abstract

Interpreting and predicting the saturation of tight sandstone gas reservoirs are the key task to improve the reservoir development. The role of gas diffusion dynamics is stronger than that of buoyancy during the gas accumulation of tight sandstone reservoirs. In this study, a saturation height model that takes gas diffusion dynamics into account is proposed, which can complement logging saturation interpretation and provide a better practice in saturation prediction. Taking the study of the Sulige tight sandstone gas reservoir in China as an example, the saturation height model compares the controlling factors and uncertainties affecting the saturation distribution, characterizes the complex gas-water distribution, and determines the lower gas charging limits. This study concludes that the configuration between gas diffusion dynamics and reservoir capillary pressure controls the distribution of saturation. The buoyancy effect only serves to improve the saturation at regional uplifts with good petrophysical properties. The different saturation characteristics in the central, western, and eastern parts of the Sulige gas field are precisely caused by the different configurations of source rock quality and reservoir quality. This study provides a key reference for static model and development deployment.
考虑气体扩散动力学的致密砂岩储层饱和高度模型
致密砂岩气藏饱和度的解释和预测是提高储层开发水平的关键。在致密砂岩储层天然气成藏过程中,气体扩散动力学的作用大于浮力的作用。本文提出了一种考虑气体扩散动力学的饱和高度模型,可以作为测井饱和度解释的补充,为饱和度预测提供更好的实践。以中国苏里格致密砂岩气藏研究为例,利用饱和高度模型对比了影响饱和度分布的控制因素和不确定因素,刻画了复杂的气水分布特征,确定了气藏充注下限。研究认为,天然气扩散动力学与储层毛管压力之间的配置关系控制着饱和度的分布。浮力效应只在岩石物性较好的区域隆起处起到提高饱和度的作用。苏里格气田中部、西部和东部不同的饱和度特征,正是烃源岩质和储层质配置不同造成的。该研究为静态模型和开发部署提供了重要参考。
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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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