深部煤层气储层气相赋存状态及控制因素定量分析——综合模型及其在临兴区块的应用

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2025-06-23 DOI:10.1155/gfl/5449100
Jian Wu, Songhang Zhang, Weiwei Chao, Tengfei Jia, Wenchun Peng, Zizhen Liu, Shilong Li
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引用次数: 0

摘要

深层煤层气是保障能源安全的重要资源。尽管局部深部煤层气开发取得了成功,但对含气量和赋存状态的认识不清仍然是制约深部煤层气综合开发的主要障碍。本研究利用保压取心和电缆取心含气量测试、等温吸附测试以及试井温度和压力数据建立方法模型。该模型对电缆取心获得的含气量进行了校正,确定了含气量的赋存状态。计算了吸附气含量、游离气含量、气水饱和度,并对控制因素进行了分析。结果表明,总含气量和吸附气含量高值区均集中在研究区西南部。煤的吸附能力受其变质程度的影响,是影响总瓦斯含量和吸附瓦斯含量的主要因素。游离气含量高值区主要集中在研究区西北边缘。影响游离气孔隙度差异的主要因素是煤的变质类型和惰质含量。受岩浆热变质作用影响的地区和惰质含量高的地区孔隙度较高。此外,压力,而不是温度,被认为是决定自由气体密度的主要因素。这些发现为获取深部煤层气含量和赋存状态,特别是研究深部煤层游离气含量提供了一种相对简单的间接方法。该方法旨在为临兴中段深部煤层气开发提供理论支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Quantitative Analysis of Gas Occurrence States and Its Controlling Factors in Deep CBM Reservoirs: An Integrated Model With Application in Linxing Block

Quantitative Analysis of Gas Occurrence States and Its Controlling Factors in Deep CBM Reservoirs: An Integrated Model With Application in Linxing Block

Deep coalbed methane (CBM) is a crucial resource for ensuring energy security. Despite some successful localized deep CBM developments, the unclear understanding of gas content and gas occurrence state remains a key obstacle to the comprehensive development of deep CBM. This study utilizes data from pressure-preserved coring and wireline coring gas content tests, isothermal adsorption tests, and well test temperature and pressure data to establish a methodological model. This model corrects the gas content obtained from wireline coring and determines the gas occurrence state. The gas content, including adsorbed and free gas content, and gas/water saturation were calculated, and the controlling factors were analyzed. The results reveal that the high values of total gas content and adsorbed gas content are concentrated in the southwestern part of the study area. The adsorption capacity of the coal, influenced by its degree of metamorphism, is identified as the primary factor affecting the total gas content and adsorbed gas content. Furthermore, the high values of free gas content are primarily concentrated at the northwestern edge of the study area. The main factors affecting the porosity difference of free gas are coal metamorphism type and inertinite content. Areas affected by magmatic thermal metamorphism and those with high inertinite content tend to have higher porosity. Additionally, pressure, rather than temperature, is identified as the main factor determining the density of free gas. These findings provide a relatively simple indirect method for obtaining deep CBM content and occurrence state, particularly for studying the free gas content in deep coal seams. This approach is aimed at offering theoretical support for the development of deep CBM in the middle Linxing block.

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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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