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BERNOULLI'S PRINCIPLE
v1
v2
Ground (h = 0)
h1
h2
P1
P2
As the water loses elevation from the high end
of the pipe to the low end, it gains velocity.
To find the exact value of any parameter,
we apply the Bernoulli equation to two points
anywhere along the same streamline.
streamline
h1 = 250 m
P1 = atmospheric
h2 = 0 m
P2 = atmospheric
The water at the top of the reservoir starts at rest,
so v1 is zero, and the first term drops out.
Since the final height (h2) is also zero, this term
drops out, too.
Lastly, P1 = P2, which is atmospheric pressure,
so these terms drop out as well.
Plugging in the remaining the known parameters:
ρwater g (250 m) = ½ ρwater v2
2
Now the ρwater terms can be cancelled out.
Using g = 9.8 m/s2 and solving for v2, we have
v2 = sqrt (2*9.8 m/s2 * 250 m)
v2 = 70 m/s

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Cub bernoulli lesson01_bernoulliflowgraphics_v3_sas

  • 2. v1 v2 Ground (h = 0) h1 h2 P1 P2 As the water loses elevation from the high end of the pipe to the low end, it gains velocity. To find the exact value of any parameter, we apply the Bernoulli equation to two points anywhere along the same streamline. streamline
  • 3. h1 = 250 m P1 = atmospheric h2 = 0 m P2 = atmospheric The water at the top of the reservoir starts at rest, so v1 is zero, and the first term drops out. Since the final height (h2) is also zero, this term drops out, too. Lastly, P1 = P2, which is atmospheric pressure, so these terms drop out as well. Plugging in the remaining the known parameters: ρwater g (250 m) = ½ ρwater v2 2 Now the ρwater terms can be cancelled out. Using g = 9.8 m/s2 and solving for v2, we have v2 = sqrt (2*9.8 m/s2 * 250 m) v2 = 70 m/s

Editor's Notes

  • #3: Bernoulli’s Principle lesson
  • #4: Bernoulli’s Principle lesson