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author | priyanka | 2015-06-24 15:03:17 +0530 |
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committer | priyanka | 2015-06-24 15:03:17 +0530 |
commit | b1f5c3f8d6671b4331cef1dcebdf63b7a43a3a2b (patch) | |
tree | ab291cffc65280e58ac82470ba63fbcca7805165 /405/CH7/EX7.10/7_10.sce | |
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-rwxr-xr-x | 405/CH7/EX7.10/7_10.sce | 31 |
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diff --git a/405/CH7/EX7.10/7_10.sce b/405/CH7/EX7.10/7_10.sce new file mode 100755 index 000000000..66ba1e547 --- /dev/null +++ b/405/CH7/EX7.10/7_10.sce @@ -0,0 +1,31 @@ +clear;
+clc;
+printf("\t\t\tExample Number 7.10\n\n\n");
+// heat transfer across water layer
+// Example 7.10 (page no.-346-347)
+// solution
+
+L = 0.5;// [m] length of square plate
+d = 0.01;// [m] seperation between square plates
+T1 = 100;// [degree F] temperature of lower plate
+T2 = 80;// [degree F] temperature of upper plate
+// we evaluate properties at mean temperature of 90 degree F and obtain, for water
+k = 0.623;// [W/m degree celsus]
+// and the following term is particularly useful in obtaining the product GrPr
+// g*Beta*rho^(2)*Cp/(mu*k) = 2.48*10^(10) [1/m^(3) degree celsius]
+// the Grashof-prandtl number product is now evaluated using the plate spacing of 0.01 m as the characterstic dimension
+K = 2.48*10^(10);// [1/m^(3) degree celsius]
+Gr_into_Pr = K*(T1-T2)*(5/9)*d^(3);
+// now, using equation 7-64 and consulting table 7-3(page no.-344) we obtain
+C = 0.13;
+n = 0.3;
+m = 0;
+// therefore, equation (7-64) becomes
+Ke_by_K = C*Gr_into_Pr^(n);
+// the effectve thermal conductivity is thus
+ke = k*Ke_by_K;// [W/m degree celsius]
+// and the heat transfer is
+A = L^(2);// [square meter] area of plate
+q = ke*A*(T1-T2)*(5/9)/d;// [W]
+printf("heat lost by the lower plate is %f W",q);
+
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