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+clear;
+clc;
+printf('FUNDAMENTALS OF HEAT AND MASS TRANSFER \n Incropera / Dewitt / Bergman / Lavine \n EXAMPLE 12.7 Page 759 \n')// Example 12.7
+
+// Spectral distribution of reflectivity
+// Total, hemispherical absorptivity
+// Nature of surface temperature change
+
+T = 500 ;//[K] temperature of surface
+e = .8;
+stfncnstt = 5.67*10^-8; //[W/m^2.K^4] Stefan-Boltzmann constant
+
+x=[0 6 8 16];
+y=[.8 .8 0 0];
+clf();
+plot2d(x,y,style=5,rect=[0,0,20,1]);
+
+
+xtitle("Spectral Distribution of reflectivity", "wavelength (micro-m)", "reflectivity");
+
+//From equation 12.43 and 12.44
+Gabs = {.2*500/2*(6-2)+500*[.2*(8-6)+(1-.2)*(8-6)/2]+1*500*(12-8)+500*(16-12)/2} ;//[w/m^2]
+G = {500*(6-2)/2+500*(12-6)+500*(16-12)/2} ;//[w/m^2]
+a = Gabs/G;
+
+//Neglecting convection effects net het flux to the surface
+qnet = a*G - e*stfncnstt*T^4;
+
+printf('\n Total, hemispherical absorptivity %.2f \n Nature of surface temperature change = %i W/m^2 \n Since qnet > 0, the sirface temperature will increase with the time', a,qnet); \ No newline at end of file