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A cylindrical bucket, open at the top, is 25.0 cm high and 10.0 cm in diameter. A circular hole with a cross-sectional area 1.50 cm2 is cut in the center of the bottom of the bucket. Water flows into the bucket from a tube above it at the rate of 2.40 x 10-4m3/s. How high will the water in the bucket rise?

Short Answer

Expert verified

Answer

The water rise in the bucket is 0.131m .

Step by step solution

01

Step-by-Step Solution Step 1: Identification of the given data

The given data can be listed below as,

  • The height of cylinder bucket is, h = 25.0 cm.
  • The diameter of cylinder bucket is, d1 = 10cm .
  • The cross-sectional area is, A2 = 1.50 cm2
  • The water flow rate is, QË™=2.40×10−4″¾3/s.
02

Determination of the water in the bucket rise

The water level in the bucket will rise in anticipation of the volume flow rate into the bucket, 2.40 x 10-4 m3/s is equal to the volume flow rate out the hole in the bottom.

The relation of Bernoulli’s equation is expressed as,

p1+12ÒÏv12+ÒÏgh1=p2+12ÒÏv22+ÒÏgh2.......(i)

Here,p1and p2 are the pressure at point 1 and point 2, v1 and v2 are velocity at the point 1 and point 2, ÒÏis the density of water and g is the gravitational acceleration.

The volume flow rate from bucket is equal to the volume flow rate out of hole is expressed as,

QË™=A2v22.40×10−4″¾3/s=A2v2v2=2.40×10−4″¾3/sA2

Here, A2 is the area at point 2, and v2 is the velocity at point 2.

Substitute 1.50 x 10-4m2 for A2 in the above equation.

v2=2.40×10-4″¾3/s1.50×10−4″¾2=1.6″¾/s

The area at point 1 (A1 ) is greater than the value of A2 i.e. A1>>A2, then 12ÒÏv12<<12ÒÏv22so neglected the term 12ÒÏv12 . Now, the value of h2 = 0 .because the height of point 2 from ground level is zero and p1=p2=p0(atmospheric pressure), these values put in equation. (I).

p0+ÒÏgh1=p0+12ÒÏv22+0ÒÏgh1=12ÒÏv22h1=v222g

Here, h1 is the height of water rise in the bucket.

Substitute 1.6 m/s for v2 and 9.81m/s2 for g in the above equation.

h1=1.6″¾/s22×9.81 m/s2=0.131″¾

Hence, the water rise in the bucket is 0.131m .

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