238 RADIATIVE HEAT TRANSFER
ǫ3
(1 −F2−2−F2−3F3−2)+F2−3F3−2
And the total flux is q3=−15.11 −3.61 =−18.72 W/cm2, which is the same as for a gray surface.
However, in order to reemit the absorbed source radiation (same in both cases), the surface must be a lot
PROGRAM SEMIGRXCHDF
IMPLICIT NONE
INTEGER,PARAMETER :: N=2
DOUBLE PRECISION :: A(N),F(N,N),EPS(2,N),HO(N),T(N),q(N),L1,L2
integer :: id(N),iclsd,i
! Dimensions
L1=3.1416*0.02
A(1)=L1 ! per unit depth
id(1)=0 ! q specified
A(2)=L2 ! per unit depth
id(2)=1 ! T specified
T(2)=300.D0 ! T in K
! View Factors; since configuration is open (iclsd=2), diagonal terms are also needed
iclsd=2
! Range 1&2 have same Fij for diffuse surfaces
F(1,1)=0.3634; F(1,2)=0.3183; F(2,2)=0.;
1 1307.2 0.0000E+00 0.0000E+00
2 300.0 -0.1872E+06 -0.7487E+04
More accurately, one should use emissive-power-weighted emittances, with ǫ1evaluated at 3000 K,
and ǫ2evaluated at a temperature close to the unknown T2(emission from A3at 300 K will be pretty
negligible). Thus, replacing the EPS line by