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Title: Change of pore properties during carbonization of coking coal

Journal Article · · Carbon; (United States)
 [1];
  1. Kuraray Engineering Co., Kurashiki, Japan

Porosimetry, sorption and density measurements are reported on two caking bituminous coals. West Virginia Jewel No. 2 medium volatile and a Pennsylvania Pittsburgh seam high volatile C, for final carbonization temperatures between 400 and 1000/sup 0/C. Samples were not confined and heating rates of 3 and 8.2%/min were employed. The medium volatile samples exhibit pronounced maxima in pore volume, pore surface area and porosity between 600 and 800/sup 0/C. These temperatures are unexpectedly greater than those at which maximum particle dilation and maximum rate of devolatilization occur. An explanation for this observation is that closed pores are created during carbonization below 600/sup 0/C which are opened when carbonization is carried to higher temperatures. Shape of the pore volume curves suggest new pore initiation, pore growth and pore shrinkage are the dominant processes operating, although collapse of the ultra micro pore structure seems to occur above 800/sup 0/C. A pore development model employing simple expressions for the three dominant processes successfully predicts the pore volume and surface area changes. Apparent activation energies derived from the model indicate that the rates of these dominant steps are controled by basicaly physical, not chemical, changes.

OSTI ID:
5254222
Journal Information:
Carbon; (United States), Vol. 18:2
Country of Publication:
United States
Language:
English