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Petrophysical characterization of high-rank coal by nuclear magnetic resonance: a case study of the Baijiao coal reservoir SW China

机译:核磁共振表征高品位煤的岩石物理特征-以中国西南白jia煤储层为例

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摘要

To better apply nuclear magnetic resonance (NMR) to evaluate the petrophysical characterization of high-rank coal, six anthracite samples from the Baijiao coal reservoir were measured by NMR. The porosity, T2 cutoff value, permeability and pore type were analysed using the transverse relaxation time (T2) spectrum before and after centrifugation. The results show that the T2 spectrum of water-saturated anthracite can be divided into a discontinuous and continuous trimodal distribution. According to the connectivity among pores, three T2 spectrum peaks were identified at the relaxation times of 0.01–1.7 ms, 1.7–65 ms and greater than 65 ms, which correspond to the micropores (less than 100 nm), mesopores (100–1000 nm) and macropores (greater than 1000 nm), respectively. Based on the T2 cutoff value, we divided the T2 spectrum into two parts: bound fluid and free fluid. By comparing two classic permeability models, we proposed a permeability model to calculate the permeability of anthracite. This result demonstrates that NMR has great significance to the exploration of coal reservoirs and to the understanding of the development of coalbed methane.
机译:为了更好地利用核磁共振(NMR)评估高级煤的岩石物理特征,通过NMR测量了六角白煤储层的六个无烟煤样品。使用离心前后的横向弛豫时间(T2)光谱分析孔隙率,T2临界值,渗透率和孔类型。结果表明,水饱和无烟煤的T2光谱可分为不连续和连续三峰分布。根据孔之间的连通性,在0.01–1.7 ms,1.7–65 ms和大于65 ms的弛豫时间确定了三个T2谱峰,分别​​对应于微孔(小于100 nm),中孔(100–1000)纳米)和大孔(大于1000纳米)。基于T2截止值,我们将T2频谱分为两部分:结合流体和自由流体。通过比较两种经典的渗透率模型,我们提出了一种渗透率模型来计算无烟煤的渗透率。这一结果表明,核磁共振对煤储层的勘探和对煤层气发育的认识具有重要意义。

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