Wang Ning, Du Yi, Fu Changqing, Ma Xicong, Zhang Xin, Wang Jiayi, Wang Ning
National and Local Joint Engineering Research Center for Carbon Capture Utilization and Sequestration & State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China.
Shaanxi Key Laboratory for Carbon Neutral Technology, Northwest University, Xi'an 710069, China.
ACS Omega. 2023 Sep 8;8(37):33526-33542. doi: 10.1021/acsomega.3c03534. eCollection 2023 Sep 19.
The comprehension of the mechanisms governing spontaneous water imbibition in gas-water systems plays a significant role in the operation of hydraulic fracturing and the development of coalbed methane (CBM). In this study, nuclear magnetic resonance (NMR) techniques were used to investigate the pore structure and fluid behavior of different rank coal samples during spontaneous imbibition. Analyses were conducted on the 1D NMR spectrum, 2D NMR - spectrum, and layer division spectra to achieve accurate and detailed information about the internal pore structure of coal and the characteristics of fluid transport during spontaneous imbibition. Low-rank coal exhibits good pore connectivity and favorable pore sorting characteristics, indicating favorable reservoir conditions. High-rank coal has larger pore spaces and highly developed micropores, which are highly beneficial for gas adsorption. However, its poor pore sorting characteristics and connectivity limit the migration and diffusion of fluids within the reservoir. The imbibition capacity follows a specific order of contribution, with small pores (10-50 nm) having the most significant role, followed by micropores (2-10 nm), ultramicropores ( < 2 nm), mesopores (50-1000 nm), macropores (1000-10,000 nm), and microfractures ( ≥ 10,000 nm). Low-rank coal stands out due to the restricted development of ultramicropores and small pores, leading to a different contribution of imbibition capacity compared to other samples, where macropores and microfractures dominate over all pore types. The coal reservoirs with favorable pore sorting characteristics and pore connectivity tend to exhibit a tendency toward rapid saturation and attainment of a prompt stable state during the hydraulic fracturing process. Finally, the mechanism of the late retreat effect of imbibition and the laws governing different coal ranks, pore structures, and fluid transport were discussed. This study offers comprehensive analyses of the mechanism of coal spontaneous imbibition and the characteristic laws of fluid seepage, providing insights into the optimization of CBM recovery and reservoir management.
理解气水系统中自发吸水的控制机制对水力压裂作业和煤层气(CBM)开发具有重要作用。在本研究中,利用核磁共振(NMR)技术研究了不同煤阶煤样在自发吸水过程中的孔隙结构和流体行为。对一维核磁共振谱、二维核磁共振谱和分层谱进行了分析,以获取关于煤内部孔隙结构和自发吸水过程中流体传输特性的准确详细信息。低阶煤具有良好的孔隙连通性和有利的孔隙分选特征,表明储层条件良好。高阶煤具有较大的孔隙空间和高度发达的微孔,这对气体吸附非常有利。然而,其较差的孔隙分选特征和连通性限制了储层内流体的运移和扩散。吸水能力遵循特定的贡献顺序,小孔(10 - 50 nm)起最主要作用,其次是微孔(2 - 10 nm)、超微孔(< 2 nm)、中孔(50 - 1000 nm)、大孔(1000 - 10000 nm)和微裂缝(≥ 10000 nm)。低阶煤因超微孔和小孔发育受限而突出,导致其吸水能力的贡献与其他样品不同,在其他样品中,大孔和微裂缝在所有孔隙类型中占主导地位。具有良好孔隙分选特征和孔隙连通性的煤储层在水力压裂过程中往往呈现快速饱和并迅速达到稳定状态的趋势。最后,讨论了吸水后期后退效应的机制以及不同煤阶、孔隙结构和流体传输的规律。本研究对煤自发吸水机制和流体渗流特征规律进行了全面分析,为煤层气采收率优化和储层管理提供了见解。