Abstract
Flowability of gas and water through low-permeability coal plays crucial roles in coalbed methane (CBM) recovery from coal reservoirs. To better understand this phenomenon, experiments examining the displacement of water by gas under different displacement pressures were systematically carried out based on nuclear magnetic resonance (NMR) technology using low-permeability coal samples of medium-high coal rank from Yunnan and Guizhou, China. The results reveal that both the residual water content (Wr) and residual water saturation (Sr) of coal gradually decrease as the displacement pressure (P) decreases. When P is 0–2 MPa, the decline rates of Wr and Sr are fastest, beyond which they slow down gradually. Coal samples with higher permeability exhibit higher water flowability and larger decreases in Wr and Sr. Compared with medium-rank coal, high-rank coal shows weaker fluidity and a higher proportion of irreducible water. The relationship between P and the cumulative displaced water content (Wc) can be described by a Langmuir-like equation, Wc = WLP/(PL + P), showing an increase in Wc in coal with an increase in P. In the low-pressure stage from 0 to 2 MPa, Wc increases most rapidly, while in the high-pressure stage (P > 2 MPa), Wc tends to be stable. The minimum pore diameter (d′) at which water can be displaced under different displacement pressures was also calibrated. The d′ value decreases as P increases in a power relationship; i.e., d′ the coal gradually decreases with the gradual increase in P. Furthermore, the d′ values of most of the coal samples are close to 20 nm under a P of 10 MPa.
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Financial support for this work was provided by the National Natural Science Foundation of China (Grant No. 41772155), and the Advanced Basic Research Projects of China National Petroleum Corporation (2019B-4910).
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Yang, M., Yang, Z., Sun, B. et al. A study on the flowability of gas displacing water in low-permeability coal reservoir based on NMR technology. Front. Earth Sci. 14, 673–683 (2020). https://doi.org/10.1007/s11707-020-0837-x
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DOI: https://doi.org/10.1007/s11707-020-0837-x