Characteristics of in-situ stress distribution and its significance on the coalbed methane (CBM) development in Fanzhuang-Zhengzhuang Block, Southern Qinshui Basin, China

In-situ stress is a vital index on the coal reservoir permeability and coalbed methane (CBM) development. Based on 41 sets of well test data at depths (h) of 353-1273 m in Fanzhuang-Zhengzhuang Block, the distribution of in-situ stress was analyzed systematically and its effect on coal permeability was also addressed. Results show that stress fields could convert in the vertical and four ranges corresponding to the certain depth can be characterized: the sigma(H) > sigma(v) > sigma(h) type mainly occurs in the shallow and deep coal seams (< 600 m and > 825 m); From 600 to 725 m, a stress transition zone can be observed (sigma(H) approximate to sigma(v) > sigma(h)); The sigma(v) > sigma(H) > sigma(h) type is dominant within depth from 725 to 825 m. With the increase of depth, well testing permeability (k) exhibits a trend of decrease (h < 600 m, 0.055 < k < 0.91mD) - increase (600 < h < 825 m, 0.02 < k < 1.13 mD) - decrease (h > 825 m, k < 0.1 mD), the essence of which is the open and closure of pores and fractures under the control of stress regime and vertical belting. Meanwhile, the correlation between gas content and depth was also illustrated, which shows two trends at the depth of 200-825 m (increase) and 825-1400 m (decrease), respectively. Generally, the coal reservoir deeper than 825 m is characterized by high in situ stress, low permeability and low gas resource, meaning that the geological conditions for CBM development deteriorate. The gas/water production of 500 CBM wells also indicates that the gas recovery rate in deeper coal seams is poorer than that in shallower coal seams. Therefore, a series of corresponding methods for these deep CBM (> 825 m) should be taken in the future CBM development strategy.