1. 河南理工大学能源科学与工程学院,河南 焦作 454000煤炭安全生产与清洁高效利用省部共建协同创新中心,河南,焦作,454000
2. 煤炭安全生产与清洁高效利用省部共建协同创新中心,河南 焦作 454000山西潞安金源煤层气开发有限责任公司,山西,长治,046000
3. 山西潞安金源煤层气开发有限责任公司,山西 长治 046000河南理工大学安全科学与工程学院,河南,焦作,454000
4. 河南理工大学安全科学与工程学院,河南,焦作,454000
[ "倪小明(1979—),男,博士,教授,主要从事煤系气地质与勘探开发方面的科研与教学工作。地址:河南省焦作市高新区世纪大道2001号,邮政编码:454000。E-mail:nxm1979@126.com" ]
纸质出版:2024
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倪小明, 冯冬, 郝少伟, 等. 五里堠井田煤系气合采产气来源及贡献判识[J]. 油气藏评价与开发, 2024,14(6):952-958.
NI Xiaoming, FENG Dong, HAO Shaowei, et al. Gas source and contribution identification for coal measure gas commingled production in Wulihou mining area[J]. Petroleum Reservoir Evaluation and Development, 2024, 14(6): 952-958.
倪小明, 冯冬, 郝少伟, 等. 五里堠井田煤系气合采产气来源及贡献判识[J]. 油气藏评价与开发, 2024,14(6):952-958. DOI: 10.13809/j.cnki.cn32-1825/te.2024.06.017.
NI Xiaoming, FENG Dong, HAO Shaowei, et al. Gas source and contribution identification for coal measure gas commingled production in Wulihou mining area[J]. Petroleum Reservoir Evaluation and Development, 2024, 14(6): 952-958. DOI: 10.13809/j.cnki.cn32-1825/te.2024.06.017.
查明煤系气合采时的产气来源及产气贡献能为合采方案制定奠定基础。以潞安矿区五里堠井田的煤系气勘探开发资料为基础,开展了3+4号煤系地层、15号煤层中CH
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气体的碳、氢同位素测试,结合二元气体分源模型,判识出6口合采井的产气来源及占比。基于突变理论,考虑影响煤系气产量的含气性、渗透性和解吸性等因素,计算出3口合采井中3+4号煤系气和15号煤层气的产气量贡献。结果表明:多产气层气体的碳、氢同位素值存在差异时,可以据此判识各产气层的来源及占比。当3+4号煤系地层稳定产气但15号煤层未解吸时,产出的气体均来源于3+4号煤系地层;当3+4号煤系地层和15号煤层均稳定产气时,3+4号煤系地层产气来源占42%~45%,15号煤层产气来源占55%~58%。基于突变理论计算出的3口合采井的产量劈分系数与实验测试结果相差不大,印证了该方法的可行性。该成果为准确判识该井田煤系气合采产层来源及贡献提供了方法和依据。
Determining the gas source and contribution in coal measure gas commingled production lays the foundation for developing commingled production schemes. Based on coal measure gas exploration and development data from the Wulihu mining area in the Lu’an mining area
carbon and hydrogen isotope tests of CH
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from the No. 3+4 coal measure strata and the No. 15 coal seam were conducted. Using a binary gas source model
the gas source and proportions of six commingled wells were identified. Additionally
considering factors such as gas content
permeability
and desorption capacity
the production contributions of gas from the No. 3+4 coal meas
ure strata and the No. 15 coal seam in three commingled wells were calculated based on catastrophe theory. The results showed that when isotopic differences in carbon and hydrogen values were observed between multiple gas-producing layers
these differences could be used to determine the source and proportion of gas from each layer. When the No. 3+4 coal measure strata consistently produced gas while the No. 15 coal seam did not desorb gas
the produced gas entirely originated from the No. 3+4 coal measure strata. When both the No. 3+4 coal measure strata and the No. 15 coal seam stably produced gas
the gas productions were 42%-45% and 55%-58%
respectively. The production split coefficients calculated based on catastrophe theory closely matched experimental results
confirming the feasibility of this method. This study provides a method and reference for accurately identifying gas sources and contributions in coal measure gas commingled production for this mining area.
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