2023
DOI: 10.1080/10916466.2023.2175867
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NMR experiments on the migration characteristics of water in bedding-bearing low rank coal

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Cited by 2 publications
(3 citation statements)
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“…Once the residual pressure is removed, water enters the pores through spontaneous imbibition under the action of capillary forces. , When the direction of imbibition is consistent with the direction of CBM production, the capillary force is the driving force of CBM migration. Otherwise, it is resistance. , This resistance causes the retention of fracturing fluid, known as the water-blocking effect. , Therefore, water imbibition in coal seams is considered a key factor affecting CBM recovery, and understanding the transport mechanism of the water imbibition process in coal bodies is of great importance for CBM production. …”
Section: Introductionmentioning
confidence: 99%
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“…Once the residual pressure is removed, water enters the pores through spontaneous imbibition under the action of capillary forces. , When the direction of imbibition is consistent with the direction of CBM production, the capillary force is the driving force of CBM migration. Otherwise, it is resistance. , This resistance causes the retention of fracturing fluid, known as the water-blocking effect. , Therefore, water imbibition in coal seams is considered a key factor affecting CBM recovery, and understanding the transport mechanism of the water imbibition process in coal bodies is of great importance for CBM production. …”
Section: Introductionmentioning
confidence: 99%
“…Meanwhile, it has been observed that most of the studies tend to focus on cores in the field of petroleum engineering, with very few investigations into coal cores. 13,35 In this study, samples from the Datong, Duanshi, and Sihe coal mines in the Qinshui Basin and the Zhangjiamao coal mine in the Ordos Basin are selected as research objects. The samples were made into 25 mm diameter columns for spontaneous imbibition experiments at room temperature.…”
Section: Introductionmentioning
confidence: 99%
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