Discussion - Atmospheric Fogging in Underground Mine Airways – Technical Papers, MINING ENGINEERING, Vol. 35, No. 4, April 1983, pp. 336-342 – Gillies, A. D. S. and Schimmelpfennig, M. A.

The American Institute of Mining, Metallurgical, and Petroleum Engineers
M. J. McPherson
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
2
File Size:
117 KB
Publication Date:
Jan 1, 1984

Abstract

Having worked on the thermodynamics of air/liquid-water mixtures passing through the surface fans of deep mines, I find this paper of great interest and congratulate the authors on producing it. There are two matters, however, deserving discussion. First, the authors have described the classical theory of fog formation with fogging occurring at "supersaturation." In fact, the process of fog formation begins well below 100% humidity. The more strongly hygroscopic nuclei in the atmosphere will attract water molecules and begin to grow at a relative humidity perhaps as low as 70%. The process is a dynamic one with both condensation and evaporation taking place throughout the mixture on microscopic liquid surfaces. As saturation is approached, the rate of condensation accelerates rapidly producing the familiar reduction in visibility. Hygroscopic nuclei are present in all natural atmospheres and under the appropriate conditions of pressure and temperature, will produce clean fogs. However, if the air is polluted by particulates from combustion or other processes then the resultant coagulation with growing liquid particles may produce dense (and sometimes photochemical) smogs. It is this process that is likely to occur in underground mines when moist air is cooled below dew point. Second, the authors have summarized very well the individual measures that might alleviate the problem. In particular, I agree that neither heating nor refrigerating the air, by themselves, provides a satisfactory solution. However, there is a combination of these that provides a neat and effective control of fog formation. This involves a small, self-contained refrigeration unit within a duct but without the usual external heat rejection facility. The air is cooled below dew point and, hence, dehumidified on passing over the cold evaporator coils. The heat from the condenser is rejected back into the air down-stream from the water eliminator, as shown in [Fig. 1]. The duct configuration can be designed to create good mixing at the outlet.
Citation

APA: M. J. McPherson  (1984)  Discussion - Atmospheric Fogging in Underground Mine Airways – Technical Papers, MINING ENGINEERING, Vol. 35, No. 4, April 1983, pp. 336-342 – Gillies, A. D. S. and Schimmelpfennig, M. A.

MLA: M. J. McPherson Discussion - Atmospheric Fogging in Underground Mine Airways – Technical Papers, MINING ENGINEERING, Vol. 35, No. 4, April 1983, pp. 336-342 – Gillies, A. D. S. and Schimmelpfennig, M. A.. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1984.

Export
Purchase this Article for $25.00

Create a Guest account to purchase this file
- or -
Log in to your existing Guest account