西南石油大学学报(自然科学版) ›› 2020, Vol. 42 ›› Issue (1): 57-68.DOI: 10.11885/j.issn.1674-5086.2018.10.10.03

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Fractal Characteristics of Coal Rock Pores in the Baliancheng Mining Area, Hunchun Basin

WANG Youzhi   

  1. Exploration and Development Research Institute of Daqing Oilfield Company Ltd., PetroChina, Daqing, Heilongjiang 163712, China
  • Received:2018-10-10 Online:2020-02-10 Published:2020-02-10

Abstract: Pore structure characteristics of coal rocks are important parameters for evaluating coal seam storage capacity and selecting fracturing layers. Low temperature nitrogen adsorption, nuclear magnetic resonance (NMR) technology, and argon ion polishing imaging enabled quantitative characterization of the pore heterogeneity by fractal theory were used to examine the influencing factors of fractal dimensions. The organic pores of the coal rocks from the Baliancheng mining area comprised mainly of plant tissue, intergranular, and gas pores, whereas the mineral pores were composed of dissolution and clay mineral pores. The type I curve indicated that the coal rock developed slit-like and wedge-shaped holes, while the type II curve indicated the development of bottle-shaped pores. The NMR bimodal T2 spectrum showed that the adsorption pores were developed only to a limited degree with poor connectivity. The trimodality indicated the development of weep holes and fissures under good pore percolation conditions. When the pore diameter ranged between 2 and 100 nm, the water content and specific surface area were positively correlated with D1, whereas D2 was positively correlated with the ash content and negatively correlated with average pore size. When the pore diameter was between 0.1 and 10.0 μm, DN1 obtained by NMR was positively correlated with the surface area of the pores and DN2 was positively correlated with the volume of the percolation pores. In addition, DM and the fractal dimension Dc of the dissolution pores were largely controlled by the clay mineral and feldspar contents, respectively. Therefore, coal layers exhibiting a nitrogen adsorption type I curve and trimodal nuclear magnetic T2 map are conducive to the development of coalbed methane.

Key words: pore structure, fractal dimension, nitrogen adsorption, nuclear magnetic resonance, argon ion polishing, Hunchun Basin

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