Fluid Dynamics - Using the Manometer Equation

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Homework Help Overview

The discussion revolves around the application of the manometer equation in fluid dynamics, specifically involving two water reservoirs open to the atmosphere and a U-shaped tube containing mercury. The participants are exploring how to determine the difference in elevation between the two water levels based on the height difference of mercury in the tube.

Discussion Character

  • Exploratory, Conceptual clarification, Assumption checking

Approaches and Questions Raised

  • Participants discuss isolating variables in the manometer equation and question the assumption that atmospheric pressure results in no pressure difference. There is also a suggestion to think about the pressures at various points in the manometer and how they relate to each other.

Discussion Status

Some participants have provided guidance on considering the pressures in equilibrium and how to relate them through the manometer. There are multiple interpretations of the problem being explored, particularly regarding the calculation of the height difference and the implications of the hydrostatic pressure involved.

Contextual Notes

There is a mention of specific densities for water and mercury, as well as the requirement for participants to show their attempts at solving the problem. The original poster's interpretation of the problem and the resulting calculations are also under discussion.

dylanwalt
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Homework Statement
The two water reservoirs shown in the figure are open to the atmosphere. The water has a density of 1.00 Mg/m°.
A u-shaped tube between the reservoirs contains incompressible mercury with a density of 13.60 Mg/m'.
The difference in height, d, of the mercury on either side of the u-shaped tube is 25.0 cm as shown.
What is the difference in elevation h?
Relevant Equations
(delta)P=pg(delta)h
I tried to use this equation, so I isolated the delta h because that is what im solving for and then I thought because the pressure on both ends of the reservoir is both atmospheric pressure the change in pressure is 0. This makes my entire equation 0 and thus height is 0 which is definitely not the case.
 

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Think of the two reservoirs as the right hand side and left hand side of an equation. In this instance the equation for pressure. You would put mercury's pressure on the right hand side.

P_h + Px + P25 = Pmerc + Px
 
Last edited:
dylanwalt said:
Homework Statement: The two water reservoirs shown in the figure are open to the atmosphere. The water has a density of 1.00 Mg/m°.
A u-shaped tube between the reservoirs contains incompressible mercury with a density of 13.60 Mg/m'.
The difference in height, d, of the mercury on either side of the u-shaped tube is 25.0 cm as shown.
What is the difference in elevation h?
Relevant Equations: (delta)P=pg(delta)h

I tried to use this equation, so I isolated the delta h because that is what im solving for and then I thought because the pressure on both ends of the reservoir is both atmospheric pressure the change in pressure is 0. This makes my entire equation 0 and thus height is 0 which is definitely not the case.
You appear to be using Bernoulli's between 1 and 3? While not wrong...it's not going to get you anywhere. You have to think about the pressures at the various points in the manometer. You can relate these from surface ##\enclose{circle}{\text{1}}## to surface ##\enclose{circle}{\text{3}}##.
 
Is it clear to you that, at the bottom of the blue section in either leg of the manometer, the pressures are equal (since there is only mercury of equal heights in the two legs below this level)?
 
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Yes it is clear to me, I worked it out. I used the idea that the pressure on the left is equal to the pressure on the right because the system is in equilibrium and then placed all the values in and got an answer of 3.15 meters.
 
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dylanwalt said:
Yes it is clear to me, I worked it out. I used the idea that the pressure on the left is equal to the pressure on the right because the system is in equilibrium and then placed all the values in and got an answer of 3.15 meters.
Welcome, @dylanwalt !

For homework questions, we require you to show your attempt to resolve the problem.

Another way to see it:
A hydrostatic pressure able to create a 0.25-meter column of mercury, will be able to induce a [(13.60 / 1.00) x 0.25]-meter column of water (which is not equal to answer C).
 
Lnewqban said:
A hydrostatic pressure able to create a 0.25-meter column of mercury, will be able to induce a [(13.60 / 1.00) x 0.25]-meter column of water (which is not equal to answer C).
To avoid possible confusion, it's worth noting that the question asks for the value of ##h##. But ##h## is not the length of a "[(13.60 / 1.00) x 0.25]-meter column of water".

So, unless I'm misunderstanding something, the OP has the correct answer (C, 3.15m in Post #5).

Minor edit made.
 
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