Enrichment conditions and resource potential of coal-rock gas in Ordos Basin, NW China

IF 7 Q1 ENERGY & FUELS Petroleum Exploration and Development Pub Date : 2024-10-01 DOI:10.1016/S1876-3804(25)60530-1
Xiaobing NIU , Liyong FAN , Xiaoxiong YAN , Guoxiao ZHOU , Hui ZHANG , Xueyuan JING , Mengbo ZHANG
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Abstract

To reveal the enrichment conditions and resource potential of coal-rock gas in the Ordos Basin, this paper presents a systematic research on the sedimentary environment, distribution, physical properties, reservoir characteristics, gas-bearing characteristics and gas accumulation play of deep coals. The results show that thick coals are widely distributed in the Carboniferous–Permian of the Ordos Basin. The main coal seams Carboniferous 5# and Permian 8# in the Carboniferous–Permian have strong hydrocarbon generation capacity and high thermal evolution degree, which provide abundant materials for the formation of coal-rock gas. Deep coal reservoirs have good physical properties, especially porosity and permeability. Coal seams Carboniferous 5# and Permian 8# exhibit the average porosity of 4.1% and 6.4%, and the average permeability of 8.7×10−3 μm2 and 15.7×10−3 μm2, respectively. Cleats and fissures are developed in the coals, and together with the micropores, constitute the main storage space. With the increase of evolution degree, the micropore volume tends to increase. The development degree of cleats and fissures has a great impact on permeability. The coal reservoirs and their industrial compositions exhibit significantly heterogeneous distribution in the vertical direction. The bright coal seam, which is in the middle and upper section, less affected by ash filling compared with the lower section, and contains well-developed pores and fissures, is a high-quality reservoir interval. The deep coals present good gas-bearing characteristics in Ordos Basin, with the gas content of 7.5–20.0 m3/t, and the proportion of free gas (greater than 10%, mostly 11.0%–55.1%) in coal-rock gas significantly higher than that in shallow coals. The enrichment degree of free gas in deep coals is controlled by the number of macropores and microfractures. The coal rock pressure testing shows that the coal-limestone and coal-mudstone combinations for gas accumulation have good sealing capacity, and the mudstone/limestone (roof)-coal-mudstone (floor) combination generally indicates high coal-rock gas values. The coal-rock gas resources in the Ordos Basin were preliminarily estimated by the volume method to be 22.38×1012 m3, and the main coal-rock gas prospects in the Ordos Basin were defined. In the central-east of the Ordos Basin, Wushenqi, Hengshan–Suide, Yan'an, Zichang, and Yichuan are coal-rock gas prospects for the coal seam #8 of the Benxi Formation, and Linxian West, Mizhi, Yichuan–Huangling, Yulin, and Wushenqi–Hengshan are coal-rock gas prospects for the coal seam #5 of the Shanxi Formation, which are expected to become new areas for increased gas reserves and production.
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中国西北部鄂尔多斯盆地煤岩气富集条件与资源潜力
为揭示鄂尔多斯盆地煤岩气的富集条件和资源潜力,本文对深部煤系的沉积环境、分布、物性、储层特征、含气特征和积气作用进行了系统研究。研究结果表明,厚煤广泛分布于鄂尔多斯盆地石炭-二叠系。石炭-二叠系主要煤层石炭5#、二叠8#煤层生烃能力强,热演化程度高,为煤岩气的形成提供了丰富的物质基础。深部煤储层具有良好的物理性质,尤其是孔隙度和渗透率。石炭纪 5# 煤层和二叠纪 8# 煤层的平均孔隙率分别为 4.1%和 6.4%,平均渗透率分别为 8.7×10-3 μm2 和 15.7×10-3 μm2。煤中裂隙和裂缝发育,与微孔一起构成了主要的储集空间。随着演化程度的增加,微孔体积也呈上升趋势。裂隙和裂缝的发育程度对渗透率有很大影响。煤储层及其工业成分在垂直方向上呈现明显的异质分布。位于中上段的亮煤层与下段相比,受灰渣充填影响较小,孔隙和裂隙发育,是优质的储层区间。鄂尔多斯盆地深部煤层具有良好的含气特征,含气量为 7.5-20.0 m3/t,煤岩气中游离瓦斯比例(大于 10%,大部分为 11.0%-55.1%)明显高于浅部煤层。深层煤中游离瓦斯的富集程度受大孔隙和微裂隙数量的控制。煤岩压力测试表明,煤-灰岩和煤-泥岩组合的瓦斯积聚具有良好的密封能力,泥岩/灰岩(顶板)-煤-泥岩(底板)组合一般显示出较高的煤岩瓦斯值。经体积法初步估算,鄂尔多斯盆地煤岩瓦斯资源量为 22.38×1012 立方米,并圈定了鄂尔多斯盆地主要煤岩瓦斯远景区。在鄂尔多斯盆地中东部,乌审旗、横山-绥德、延安、子长、伊川为本溪地层 8#煤层煤岩瓦斯远景区,林县西、米脂、伊川-黄陵、榆林、乌审旗-横山为山西地层 5#煤层煤岩瓦斯远景区,有望成为新的瓦斯增储上产地区。
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