WINTER-REGIME THERMAL RESPONSE OF HEATED STREAMS

THE INCREASE IN WATER TEMPERATURE IN NATURAL STREAMS DUE TO WASTE HEAT DISPOSAL FROM THERMAL POWER PLANTS LEADS TO EXTENSIVE ICE-FREE REACHES DURING WINTER PERIODS. IT IS SHOWN THAT THE SURFACE HEAT EXCHANGE BETWEEN WATER AND THE ATMOSPHERE CAN BE EXPRESSED, FOR MOST PRACTICAL PURPOSES, AS A LINEAR FUNCTION OF THE WATER TEMPERATURE. USING THIS APPROXIMATION, A CLOSED-FORM SOLUTION OF THE ONE-DIMENSIONAL UNSTEADY CONVECTION-DIFFUSION EQUATION IS DEVELOPED TO PREDICT TEMPERATURE DISTRIBUTIONS IN STREAMS AND THE LENGTHS OF ICE-FREE DOWNSTREAM FROM THE THERMAL DISCHARGE SECTIONS. /ASCE/

  • Supplemental Notes:
    • PROC PAPER 10479 3 APP
  • Authors:
    • Paily, P P
    • Macagno, E O
    • Kennedy, J F
  • Publication Date: 1974-4

Media Info

  • Features: Figures; References; Tables;
  • Pagination: p. 531-51
  • Serial:

Subject/Index Terms

Filing Info

  • Accession Number: 00204550
  • Record Type: Publication
  • Files: TRIS
  • Created Date: Jul 16 1974 12:00AM