Calculating the Drag Coefficient C D for a Cylinder in Cross Flow Theoretical Basis— Using Surface Pressure Measurements Consider the area element dA = LRd on the surface of the cylinder as shown below in Fig. 1. Fig. 1 Measuring the Surface Static Pressure Profile [1] The component of the pressure–area force on this element projected into the streamwise direction is dFD = Ps()dA cos = Ps()LR cosdwhere the dependence on is included explicitly to emphasize that Ps is not constant. Integrating over the entire surface of the cylinder to find the pressure drag, and recognizing the axisymmetric nature of the pressure distribution, we have F D 2 Ps LR cos d LD Ps cos d 0 (1) 0 Subtracting the constant approach static pressure P1 from the integrand does not change the magnitude of the drag force since a constant pressure force normal to the surface gives the zero vector when integrated over the cylinder surface. This is easily seen from P cosd 0 1 for P1 = constant. (2) 0 F D LD Ps P1 cosd 0 where D=2R. 1|Page (3) The drag coefficient then is formed by dividing both sides of the equation by the free-stream dynamic pressure 1 2 U21 and the projected area Aproj = LD FD CD 2 U 1 LD 2 0 Ps ( ) P1 cos d C P cos d U 12 2 (4) 0 Later, we will use this equation in conjunction with surface static pressure measurements to determine the cylinder drag coefficient. (Note: Since surface shear forces have been neglected here, this method ignores the skin friction contribution to the total drag.) Using Excel Spreadsheets The first thing that you must do is create a template with all measured parameters (i.e. D, T, Patm, Vel, , , etc.). Using this information, calculate the Reynolds number using the cylinder diameter as the characteristic length. Next, choose a characteristic interval over which to do the surface pressure measurements (and subsequent numerical integration). In this case, every 10 was chosen for convenience as seen in Fig. 2. Fig. 2 Excel Spreadsheet Template 2|Page Object Cylinder D (mm) 88.9 Theta (deg) Theta (rad) 0 0 10 0.1745329 20 0.3490659 30 0.5235988 40 0.6981317 50 0.8726646 60 1.0471976 70 1.2217305 80 1.3962634 90 1.5707963 100 1.7453293 110 1.9198622 120 2.0943951 130 2.268928 140 2.443461 150 2.6179939 160 2.7925268 170 2.970597 180 3.1415927 23.33 Vel (m/s) 8.55 Ps-P1 (H20) 0.063191732 0.053649902 -0.01595052 -0.1104126 -0.22920736 -0.36159261 -0.46394857 -0.48276774 -0.4508667 -0.42651367 -0.43103027 -0.42108154 -0.45676676 -0.44812012 -0.45607503 -0.42600505 -0.43094889 -0.51200358 -0.434611 Ps-P1 (Pa) 15.724631 13.350242 -3.969128 -27.47507 -57.03596 -89.97871 -115.449 -120.1319 -112.1937 -106.1337 -107.2576 -104.7819 -113.6618 -111.5102 -113.4897 -106.0071 -107.2373 -127.407 -108.1486 T1 Patm (mmHg) 746 Cp T1 (Celsius) 23.33 Integrand T1 mu air rho air (K) (Pa-s) (kg/m3) Re 296.48 1.84E-05 1.16791 48245.79 Weight Int*Wt Weight Cd Fig. 3 Excel Spreadsheet with Surface Pressure Measurements (shown in red) Fig. 4 Excel Spreadsheet with Calculated Cp Values 3|Page Int*Wt In Figure 3, the surface pressure measurements are added to the spreadsheet noting the units of the pressure transducer (i.e. in H2O) and making the conversion to SI units (if necessary). Next, the coefficient of pressure Cp is calculated which is equal to the measured pressure difference divided by the dynamic pressure. In Figure 4, the column ‘Integrand’ is equal to Cp multiplied by cos as shown in Equation (4). Using the trapezoidal rule to perform the numerical integration requires a weighting factor of 2 for all terms in the summation except the first and last term. If Simpson’s Rule is used instead, then the weighting factors follow the pattern 1, 4, 2, 4, 2,…, 2, 4, 2, 4, 1 as shown below. More specifically, applying Simpson’s rule results in the following formula for the integral over the interval: Simpson’s Rule Finally then, multiplying the integrand in column F by the appropriate weighting factor and summing up these terms results in the drag coefficient (i.e. CD) for the cylinder as shown in Figure 5. A Object Cylinder B D (mm) 88.9 Theta (deg) Theta (rad) 0 0 10 0.1745329 20 0.3490659 30 0.5235988 40 0.6981317 50 0.8726646 60 1.0471976 70 1.2217305 80 1.3962634 90 1.5707963 100 1.7453293 110 1.9198622 120 2.0943951 130 2.268928 140 2.443461 150 2.6179939 160 2.7925268 170 2.970597 180 3.1415927 C D E 23.33 Vel (m/s) 8.55 Patm (mmHg) 746 Ps-P1 (H20) 0.063191732 0.053649902 -0.01595052 -0.1104126 -0.22920736 -0.36159261 -0.46394857 -0.48276774 -0.4508667 -0.42651367 -0.43103027 -0.42108154 -0.45676676 -0.44812012 -0.45607503 -0.42600505 -0.43094889 -0.51200358 -0.434611 Ps-P1 (Pa) 15.724631 13.350242 -3.969128 -27.47507 -57.03596 -89.97871 -115.449 -120.1319 -112.1937 -106.1337 -107.2576 -104.7819 -113.6618 -111.5102 -113.4897 -106.0071 -107.2373 -127.407 -108.1486 Cp 0.368356925 0.312735741 -0.092978696 -0.643616559 -1.336094372 -2.107793829 -2.70444666 -2.814147289 -2.628189898 -2.486231353 -2.512559504 -2.454566414 -2.662582527 -2.612179535 -2.658550288 -2.483266471 -2.512085123 -2.9845687 -2.533432273 T1 F G H T1 (Celsius) 23.33 Fig. 5 Using the Trapezoidal Rule and Simpson’s Rule to Calculate CD References: [1] University of Illinois (UIUC) Fluid Mechanics Laboratory Manual 4|Page I J T1 mu air rho air (K) (Pa-s) (kg/m3) Re 296.48 1.84E-05 1.16791 48245.79 Trapezoidal Simpson Integrand Weight Int*Wt Weight Int*Wt 0.368356925 1 0.368357 1 0.368357 0.307984584 2 0.615969 4 1.231938 -0.087371393 2 -0.17474 2 -0.17474 -0.557388283 2 -1.11478 4 -2.22955 -1.02350767 2 -2.04702 2 -2.04702 -1.354863799 2 -2.70973 4 -5.41946 -1.352223216 2 -2.70445 2 -2.70445 -0.962494997 2 -1.92499 4 -3.84998 -0.45638039 2 -0.91276 2 -0.91276 -6.66183E-08 2 -1.3E-07 4 -2.7E-07 0.436301498 2 0.872603 2 0.872603 0.839511209 2 1.679022 4 3.358045 1.331291258 2 2.662583 2 2.662583 1.679076584 2 3.358153 4 6.716306 2.036567756 2 4.073136 2 4.073136 2.150571876 2 4.301144 4 8.602288 2.36058785 2 4.721176 2 4.721176 2.941041247 2 5.882082 4 11.76416 2.533432273 1 2.533432 1 2.533432 Cd 1.699881 1.720084
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