The coal reservoir is a kind of geologic body with considerable elasticity, and its response to stress is more sensitive than the routine ones. In the pool-forming process of the coalbed methane, (CBM) the action of many external geodynamic factors in the coal reservoir is represented by the ability of CBM's diffusion and migration in the coal reservoir. Therefore, the occurrence of the natural fissures in the coal reservoir becomes a key that determines whether the CBM pool can be formed or not. Based on the principle, the authors have designed a comprehensive method of physical modeling to study the elasticity of the coal matrix block with different coal ranks in the light of the solid to fluid coupling, have established the model of the volume deformation (selfadjusted elastic effect) of the coal reservoir under the condition of the effective stress-adsorption/desorption, and have obtained a correct understanding of the law of the elastic deformation. Afterwards, a new viewpoint, named as the self-closing elastic effect for forming the CBM pool in the high rank reservoir, is put forward, providing an initial point and a scientific basis for a further investigation into its dynamic factors, possible mechanism and role in the CBM energy-balancing system.Although the CBM pool-forming process is controlled by many geodynamic factors, its key depends on the relatively closed geological environment derived from a favorable match among these factors, in which the tectonic stress field, hydrodynamic field of groundwater, geothermal field and strata contribute to the formation of such environment. However, these factors first act on the coal reservoir itself, which is represented by the diffusing and migrating ability of CBM within the coal reservoir. Coal itself is quite unfavorable for CBM diffusion. Therefore, the occurrence of the natural fissures in the coal seam, especially the opening or closing extent of the natural fissures during the geological history, becomes a key factor that determines whether the CBM pool can be formed or not.Before being broken under stress, coal is a kind of elastic body with a rather compressible or swellable capacity. Taking as a kind of the organic reservoir mainly composed of organic matters, the response of the coal reservoir to stress is more sensitive than some routine ones such as sandstone and carbonate rock reservoirs. So the direct dynamic factors determining the opening or closing extent of the natural fissures in the coal reservoir include two aspects. The first is the effective stress, which is expressed as the pressure difference of the overall stress, being perpendicular to the fissure strike, to the fluid pressure in pores and fissures within the coal reservoir, and with increasing the effective stress the fissures are compressed so as to become narrow or even close. The second is the swelling-shrinking effect of the coal matrix block surrounded by natural fissures. The fissures becomes narrow due to the swelling effect derived from the absorbing gas, while the desorpt...