石油与天然气地质2024,Vol.45Issue(6) :1590-1604.DOI:10.11743/ogg20240607

鄂尔多斯盆地上古生界本溪组8#煤岩煤岩气与致密砂岩气主要气藏特征对比

Comparison of main reservoir characteristics between deep coal-rock gas of the No.8 coal seam of the Upper Paleozoic Benxi Formation and tight sand gas reservoirs,Ordos Basin

李明瑞 史云鹤 范立勇 戴贤铎 荆雪媛 张沂
石油与天然气地质2024,Vol.45Issue(6) :1590-1604.DOI:10.11743/ogg20240607

鄂尔多斯盆地上古生界本溪组8#煤岩煤岩气与致密砂岩气主要气藏特征对比

Comparison of main reservoir characteristics between deep coal-rock gas of the No.8 coal seam of the Upper Paleozoic Benxi Formation and tight sand gas reservoirs,Ordos Basin

李明瑞 1史云鹤 2范立勇 2戴贤铎 2荆雪媛 2张沂3
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作者信息

  • 1. 低渗透油气田勘探开发国家工程实验室,陕西西安 710018;中国石油长庆油田公司勘探事业部,陕西西安 710018
  • 2. 低渗透油气田勘探开发国家工程实验室,陕西西安 710018;中国石油长庆油田公司勘探开发研究院,陕西西安 710018
  • 3. 中国石油长庆油田公司采气一厂,陕西西安 710018
  • 折叠

摘要

鄂尔多斯盆地长庆油田在盆内煤岩气领域取得了良好的勘探进展,发现CH4多以吸附态和游离态赋存于煤岩中,形成自生自储型煤岩气藏.针对上古生界本溪组8#煤岩为代表的煤岩气藏特征进行了深入研究.结果表明:鄂尔多斯盆地自上而下发育10套煤岩,其中5#和8#煤岩为主力煤岩,分布稳定,厚度大.本溪组煤岩气相较于浅层煤层气表现出"高压力、高温度、高含气、高饱和、高游离"等5高特征.气藏平均地层压力22~35 MPa,压力高但压力系数为1.0~1.1,为正常压力系统.气藏平均地层温度为67~92 ℃,地温梯度为29.4 ℃/km,属于正常地温梯度.气体组分中CH4含量平均值为96.92%,C2H6含量平均值为0.61%,C02含量平均值为0.85%,N2含量平均值为1.47%,为干气气藏.气藏地层水矿化度为41 644~89 776 mg/L,平均值为62 228 mg/L,为CaCl2型原生地层水,未受浅层水的影响.煤岩气试气产量高,生产阶段控压生产情况下产量稳定、压降速率低、稳产效果好.通过对煤岩气与苏里格气区石盒子组8段与山西组1段内致密砂岩气的系统性对比分析,发现两者在气藏类型、气藏压力和温度、气体成分、地层水性质及产能特征等主要气藏特征方面具有相似性,这个规律对后期煤岩气的大规模开发和建产具有指导意义.

Abstract

The Changqing Oilfield Company of PetroChina has achieved significant advances in exploring deep coal-rock gas within the Ordos Basin,discovering that methane(CH4)largely occurs in coals as both adsorbed and free gas,which contributes to the formation of self-sourced coal-rock gas reservoirs.In this study,we comprehensively investigate the characteristics of coal-rock gas reservoirs represented by the No.8 coal seam of the Benxi Formation.The results indicate that the Ordos Basin contains 10 coal seams from top to bottom.The Nos.5 and 8 coal seams,among others,predominate,exhibiting stable distribution and great thickness.Compared to shallow coalbed methane(CBM),the deep coal-rock gas occurring in the No.8 coal seam of the Paleozoic Benxi Formation is characterized by high formation pressure,high formation temperature,high gas content,high gas saturation,and high free gas content.Specifically,these coal-rock gas reservoirs exhibit average formation pressure ranging from 22 to 35 MPa,suggesting high formation pressure.However,their formation pressure coefficients vary between 1.0 and 1.1,indicating a normal pressure system.The coal-rock gas reservoirs present average formation temperatures ranging from 67 to 92 ℃ and an average geothermal gradient of 2.94 ℃/km,suggesting normal geothermal gradients.The composition of coal-rock gas in these reservoirs manifests an average CH4 content of 96.92%,average C2H6 content of 0.61%,average CO2 content of 0.85%,and average N2 content of 1.47%,establishing these reservoirs of dry gas type.The formation water in these reservoirs has total dissolved solids(TDS)concentrations ranging from 41 644 to 89 776 mg/L(average:62 228 mg/L),indicating primary CaCl2-rich formation water.Unaffected by shallow groundwater,the coal-rock gas reservoirs exhibited high gas production rates in tests and stable production at a low pressure drop rate.A systematic comparison between deep coal-rock gas reservoirs in the No.8 coal seam of the Benxi Formation and tight-sand gas reservoirs in the 8'h member of the Xiashihezi Formation(He 8 Member)and the 1st member of the Shanxi Formation(Shan 1 Member)in the Sulige gas field reveals similarities in major reservoir characteristics,including reservoir type,reservoir pressure and temperature,gas composition,formation water properties,and production capacity.These similarities will provide a valuable guide for future large-scale exploitation and production capacity construction of deep coal-rock gas.

关键词

气藏特征/致密砂岩气/煤岩气/煤岩/本溪组/鄂尔多斯盆地

Key words

tight-sand gas/coal-rock gas/gas reservoir characteristics/coal seam/Benxi Formation/Ordos Basin

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出版年

2024
石油与天然气地质
中国石油化工股份公司石油勘探开发研究院,中国地质学会石油地质专业委员会

石油与天然气地质

CSTPCDCSCD北大核心
影响因子:2.798
ISSN:0253-9985
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