Coals are fossilized plant material plus inorganic silt deposited in irregular layers and containing l-20% void space which provides a medium which is porous to gas flow. Gas flows have been measured using discs of coal cut from several coal seams. Observed flow phenomena include molecular diffusion
Gas transport through sections of solid coal
β Scribed by F.S. Karn; R.A. Friedel; B.M. Thames; A.G. Sharkey Jr
- Book ID
- 103088837
- Publisher
- Elsevier Science
- Year
- 1970
- Tongue
- English
- Weight
- 391 KB
- Volume
- 49
- Category
- Article
- ISSN
- 0016-2361
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β¦ Synopsis
Measurements were made for helium and methane flowing through thin discs of coal. Flow increased with pressure differential and temperature. At room temperature the flows along the bedding plane were: helium, 873 :< lO-'O cm2 s-l atm-l, and methane 1.2 x 10mro cm2 s-l atm-l. Flow rates were 50"/, lower across the bedding plane of the coal than along the coal seam. Activation energies were 3.9 kcal mol-1 (16.3 kJ mol-1) for helium and 13.6 kcal molm1(57.0 kJ mol-l) for methane for flow measured either along or across the bedding plane.
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## Abstract Transport rates were measured by monitoring the pressure decay between two reservoirs connected by a polyethylene membrane. The diffusion equation was integrated to obtain a relation between the pressure difference across the reservoirs and the time, with solubility, expressed by Henry'