张松航, 唐书恒, 孟尚志, 信迪, 张远远, 王希栋. 煤储层含水性及其对煤层气产出的控制机理[J]. 煤炭学报, 2023, 48(S1): 171-184. DOI: 10.13225/j.cnki.jccs.2022.0122
引用本文: 张松航, 唐书恒, 孟尚志, 信迪, 张远远, 王希栋. 煤储层含水性及其对煤层气产出的控制机理[J]. 煤炭学报, 2023, 48(S1): 171-184. DOI: 10.13225/j.cnki.jccs.2022.0122
ZHANG Songhang, TANG Shuheng, MENG Shangzhi, XIN Di, ZHANG Yuanyuan, WANG Xidong. Water-bearing characteristics of coal reservoirs and its control mechanism on coalbed methane production[J]. Journal of China Coal Society, 2023, 48(S1): 171-184. DOI: 10.13225/j.cnki.jccs.2022.0122
Citation: ZHANG Songhang, TANG Shuheng, MENG Shangzhi, XIN Di, ZHANG Yuanyuan, WANG Xidong. Water-bearing characteristics of coal reservoirs and its control mechanism on coalbed methane production[J]. Journal of China Coal Society, 2023, 48(S1): 171-184. DOI: 10.13225/j.cnki.jccs.2022.0122

煤储层含水性及其对煤层气产出的控制机理

Water-bearing characteristics of coal reservoirs and its control mechanism on coalbed methane production

  • 摘要: 煤储层的含水性不仅决定了煤层气吸附成藏理论的应用,影响储层改造措施的选取,也决定了对煤层气产出过程的认识。针对煤层的含水性,煤层气地质学认为煤储层基本饱和水,而瓦斯地质学在瓦斯含量计算和瓦斯渗流中基本没考虑水的影响,相当于认为煤储层饱和气。从煤层水来源、煤储层埋藏及热演化史的角度阐述了煤储层含水性的变化,分析现今煤储层可能存在饱和水、超低饱和含水、不饱和含水和不含水4种状态。煤储层热演化生烃及其造成的储层润湿性的改变,先存气体对后期水侵作用的影响是影响储层现今含水性的关键因素。由于我国构造运动复杂,多发生后期水侵,"大孔裂隙饱和水、小微孔饱和气"可能为多数煤储层气、水赋存状态。这种气、水赋存状态,可以有效回应煤层气地质理论中"煤储层饱和水,兰氏吸附理论不适用"的论点,同时也决定了在煤储层含气性分析中应该考虑毛管力的影响。此外,煤储层为低孔、低渗储层,早期的排采阶段一般为单相水流,煤层气的排采过程需要确定并考虑启动压力梯度的影响。综上所述,开展煤-水-甲烷条件下的煤储层润湿性研究,生烃作用及先存气体对储层含水性的影响研究,重新认识煤储层的含水性,并基于此进一步刻画煤层气的赋存和产出过程,可能是解决我国煤层气,特别是中、高煤阶煤层气低产问题的一把钥匙。

     

    Abstract: Water-bearing characteristics of original coal reservoir not only determine the application of coalbed methane(CBM) adsorption and accumulation theory,but also affect the selection of reservoir reconstruction measures, and the understanding of the CBM production process. Regarding the water-bearing properties of coal seams, in the coalbed methane geology,it believes that coal reservoirs are basically saturated with water,while in the coal gas geology,it basically does not consider the influence of water in gas content calculation and gas seepage,which is equivalent to thinking that coal reservoirs are saturated with gas. From the perspective of coal seam water source,coal reservoir burial and thermal evolution history, the changes of water bearing in coal reservoirs are expounded. According to the analysis, there may be four states in the present coal reservoir, i. e., saturated water, ultra-low saturated water,unsaturated water and no water. The influence of pre-existing gas on later water invasion,the change of reservoir wettability reduced by the thermal evolution and hydrocarbon generation of coal reservoir are the key factors affecting the water bearing of the reservoir. Due to the complexity of tectonic movement in China and the frequent occurrence of late water intrusion,"saturated water in large pores and fractures and saturated gas in small pores" may be the occurrence state of most coal reservoir gas and water. This state of occurrence of gas and water can effectively explain the argument that " saturated water in coal reservoir is not applicable to the Lan's adsorption theory" in the geological theory of coalbed methane,and it also determines that the influence of capillary force should be considered in the analysis of gas content of coal reservoir. In addition,the coal reservoir is a low-porosity and low-permeability reservoir,and the early stage of drainage and production is generally single-phase flow,so the drainage and production process of coalbed methane needs to determine and consider the influence of start-up pressure gradient. To sum up,it should carry out the study on the wettability of coal reservoir under the condition of coal-water-methane, study the influence of hydrocarbon generation and pre-existing gas on reservoir water content,and re-recognize the water bearing capacity of coal reservoir. Based on the studies above,to further describe the occurrence and production process of coalbed methane may be a key to solve the problem of low production of coalbed methane,especially medium and high rank coalbed methane in China.

     

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