中国煤岩气生成阶段及气藏成因类型OA
Generation stages and genetic types of coal-rock gas in China
根据煤演化过程中的分子结构跃变、生成烃类组成及储层特征变化规律,结合气藏生产特征,对中国煤岩气生成阶段及气藏成因类型进行研究.煤的生气过程可分为5个阶段:低煤阶生物气生成阶段(Ro<0.5%),中煤阶过渡型气生成阶段(0.5%≤Ro<0.8%),中煤阶成熟气生成阶段(0.8%≤Ro<1.3%),中煤阶高成熟气生成阶段(1.3%≤Ro<2.0%),高煤阶过成熟气生成阶段(Ro≥2.0%).基于气藏埋藏深度和成因来源,将其划分为3种类型,即浅层煤层气、深层煤岩气和他源型煤岩气.其中,深层煤岩气根据煤岩生烃演化阶段,进一步划分为4种类型:中煤阶过渡型煤岩气、中煤阶成熟煤岩气、中煤阶高成熟煤岩气和高煤阶过成熟煤岩气.煤岩从浅到深的动态演化过程中,经历了"生物气→过渡型气→湿气→干气"的成烃演化过程,以及"原生孔→割理发育→有机质孔达峰→致密脆化+裂隙张开"的成储演变序列,赋存状态从"吸附气绝对主导"逐步转变为"游离气占比持续增高",开发也从"需长期排水降压解吸"转变为"开井即见气、见气即高产"的模式.此外,还有一类来自外源的煤岩气,天然气来自下伏地层,煤岩煤阶低,储层发育,气藏受构造控制,游离气含量高,初期产量高.
Based on the molecular structure transitions,hydrocarbon composition,and reservoir characteristics changes during coal evolution,combined with the production characteristics of coal-rock gas,the generation stages and genetic types of coal-rock gas in China are investigated.The generation of coal-rock gas can be divided into five stages:low-coal-rank biogenic gas generation stage(Ro<0.5%),mid-coal-rank transitional gas generation stage(0.5%≤ Ro<0.8%),mid-coal-rank mature gas generation stage(0.8%≤ Ro<1.3%),mid-coal-rank high-maturity gas generation stage(1.3%≤ Ro<2.0%),and high-coal-rank overmature gas generation stage(Ro ≥2.0%).Based on the burial depth and gas origin,the gas reservoirs are divided into three types:shallow coalbed methane,deep coal-rock gas and exogenous coal-rock gas.According to the hydrocarbon generation stage of coal rock,deep coal-rock gas is further classified into:mid-coal-rank transitional coal-rock gas,mid-coal-rank mature coal-rock gas,mid-coal-rank high-maturity coal-rock gas,and high-coal-rank overmature coal-rock gas.During the dynamic evolution of coal rock from shallow to deep depths,the coal rock has experienced a hydrocarbon generation evolution sequence of"biogenic gas→transitional gas→wet gas→dry gas",and a process of"primary pores →cleat development →peak organic matter pores--densification and fracturing+fracture opening"of reservoirs formation.The occurrence state gradually shifts from"dominance of adsorbed gas"to"continuous increase in free gas proportion",and the development modes also transform from"long-term drainage and depressurization for desorption"to"high gas production upon well opening".In addition,there is another type of coal-rock gas which is externally sourced,with the natural gas originating from underlying strata.This type of coal-rock gas corresponds to low-rank coals with reservoir development,where gas was accumulated under the control of tectonics,with high-proportion free gas and high initial production.
张水昌;张斌;马行陟;唐勇;梁则亮;孙龙德
怀柔实验室新疆研究院,乌鲁木齐 830011||中国石油勘探开发研究院,北京 100083怀柔实验室新疆研究院,乌鲁木齐 830011||中国石油勘探开发研究院,北京 100083中国石油勘探开发研究院,北京 100083怀柔实验室新疆研究院,乌鲁木齐 830011怀柔实验室新疆研究院,乌鲁木齐 830011||新疆亚新煤层气投资开发(集团)有限责任公司,乌鲁木齐 830009怀柔实验室新疆研究院,乌鲁木齐 830011||中国石油天然气集团有限公司,北京 100007
能源科技
煤岩气煤层气煤阶划分方案生物成因气过渡型气他源型煤岩气煤岩气开发方式
coal-rock gascoalbed methanecoal rank classification schemebiogenic gastransitional gasexogenous coal-rock gascoal-rock gas development method
《石油勘探与开发》 2026 (3)
533-544,12
新型油气勘探开发国家科技重大专项"新疆地区中低煤阶煤岩气高效开发技术与集成示范"、"煤岩气成藏机理与煤岩气勘探新领域"项目(2024ZD1406000,2025ZD1404201)中国石油天然气集团有限公司科技项目(2025DJ102)
评论