Calculating Water Flow Speed at Points A and B: Pipe Branching Equations

In summary, the conversation discusses a problem involving a level pipe filled with water and two branching pipes with different cross sectional areas and a height difference. The question is how to find the water flow speed at two points in the main pipe. There is a suggestion to use an equation, but it is uncertain if the pressure in the pipes should be equal or if gravity should be taken into account.
  • #1
redshift
53
0
I've struggled with this since this morning with hardly any progress.
"There is a level pipe filled with water flowing through it. Branching off from this pipe are two pipes going perpendicularly upward, with a cross sectional area Sa, Sb, respectively, and there being a difference in water height of h. Find the water flow speed at points A and B."

Since no figures are given, I guess the answer is an equation. I also assume A and B are the points in the main pipe where the branches are.

Since the pressure should (i think) be equal in both branch pipes, even if their diameters are not the same, could A = [Sa(h)]/(Sb-Sa) and B = [Sb(h)]/(Sb-Sa)?

Regards
 
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  • #2
shouldn't the presser in the pipe that goes higher be less due to the need to overcome gravity for a longer period of time?
 
  • #3


Thank you for your question. Calculating water flow speed at points A and B in a branching pipe system can be a challenging task, but with the proper equations and understanding of fluid dynamics, it can be achieved. To start, we need to consider a few key factors that will affect the water flow speed at points A and B: the cross-sectional areas of each pipe (Sa and Sb), the difference in water height (h), and the pressure within the pipes.

First, we can use the Bernoulli's equation to determine the pressure at points A and B. This equation states that the total pressure at any point in a fluid system is equal to the sum of the static pressure, dynamic pressure, and hydrostatic pressure. In this case, the dynamic pressure (which is caused by the flow of water) will be the same at both points A and B, as they are at the same elevation in the main pipe. Therefore, we can simplify the equation to:

P + ρgh = constant

Where P is the static pressure, ρ is the density of water, g is the acceleration due to gravity, and h is the height of the water column.

Next, we can use the continuity equation, which states that the mass flow rate at any point in a system is constant. This means that the mass flow rate at point A must be equal to the mass flow rate at point B. We can express this as:

ρAv = ρBvB

Where A and B represent the cross-sectional areas at points A and B, and v and vB represent the water flow speed at those points.

Now, we can combine these equations to solve for the water flow speed at points A and B. First, we can rearrange the continuity equation to solve for vB:

vB = (Av)/(B)

Then, we can substitute this into the Bernoulli's equation:

P + ρgh = (ρAv)/(B)

Solving for v, we get:

v = √[(2gh)/(1-(A/B)^2)]

Therefore, the water flow speed at points A and B can be calculated using this equation. It is important to note that this equation assumes that the flow of water is steady and incompressible, and that there are no losses due to friction or other factors in the system.

I hope this explanation helps you understand the process for calculating water flow speed at points A and B in a branching pipe
 

1. What is "Stumped again: Water flow speed Q"?

"Stumped again: Water flow speed Q" is a phrase often used in the scientific community to describe a situation where scientists are unable to accurately measure the speed of water flow due to various factors such as turbulence, changing water levels, or equipment limitations.

2. Why is measuring water flow speed important?

Measuring water flow speed is important for a variety of reasons. It allows us to understand and predict the movement of water in rivers, streams, and oceans, which is crucial for managing water resources, predicting floods, and protecting ecosystems. It also helps in designing and maintaining infrastructure such as dams, bridges, and irrigation systems.

3. What factors can affect water flow speed?

There are several factors that can affect water flow speed, including the slope of the land, the depth and width of the water body, the roughness of the channel bottom, and the presence of obstacles such as rocks and vegetation. Water temperature and density also play a role in determining water flow speed.

4. How do scientists measure water flow speed?

There are various methods for measuring water flow speed, including using current meters, acoustic doppler current profilers, and stream gauges. These instruments measure the speed of water at a specific point or along a transect. Scientists can also use mathematical models to estimate water flow speed based on other factors such as water level and channel geometry.

5. Can water flow speed change over time?

Yes, water flow speed can change over time due to natural and human factors. For example, heavy rainfall can increase water flow speed, while drought conditions can decrease it. Human activities such as dam construction, land use changes, and water diversions can also impact water flow speed. It is important for scientists to regularly monitor and assess changes in water flow speed to better understand and manage water resources.

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