Two large reservoirs with a difference in water level of 27 m are connected by a pipeline that splits into two branches (as in Fig. 6.7) after a distance of 10 km. Ignoring minor losses, calculate the discharge in each of the three pipelines if the details of the pipelines are:
pipeline 123 Diameter (m) 0.900.750.60 Length (km) 102123λ0.040.070.05Applying the Bernoulli equation to a streamline joining the surface of the reservoirs via pipes 1 and 2, ignoring minor losses: Z=λ1L1V12/2gD1+λ2L2V22/2gD2 where Z = 27 m. Thus:
27=[0.04×10000×V12/19.62×0.9]+[0.07×21000×V22/19.62×0.75]27=22.653V12+99.898V22 (1)
Applying the Bernoulli equation to a streamline joining the surface of the reservoirs via pipes 1 and 3, ignoring minor losses: Z=λ1L1V12/2gD1+λ3L3V32/2gD3 where Z = 27 m again. Thus:
27=22.653V12+[0.05×23000×V32/19.62×0.60] so:
27=22.653V12+97.689V32 (2)
Subtracting equation (2) from equation (1) gives: 0=99.898V22+97.689V32.
Thus V32=(99.898/97.689)V22 givingV3=1.011V2 (3)
Applying the continuity equation: Q1=Q2+Q3 or D12V1=D22V2+D32V3.
Thus 0.92V1=0.752V2+0.62V3 giving 0.81V1=0.563V2+0.36V3. Now substituting for V3 from equation (3): 0.81V1=0.563V2+0.36(1.011V2) thus 0.81V1=0.927V2 or V1=1.144V2 (4)
Substituting for V1 in equation (1): 27=22.653(1.144V2)2+99.898V22
27=129.545V22 thus V2=0.457 m/s.
Substituting for V2 in equation (4) gives V1 = 0.523 m/s.
Substituting for V2 in equation (3) gives V3 = 0.462 m/s.
Thus Q1=(π×0.92/4)×0.523=0.333 m3/s. Q2=(π×0.752/4)×0.457=0.202 m3/s.
Q1=(π×0.62/4)×0.462=0.131 m3/s.