High altitude balloon acceleration

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Discussion Overview

The discussion revolves around calculating the acceleration of a high altitude balloon at various altitudes, focusing on the forces acting on the balloon, including buoyant force and the mass of the helium. Participants explore the effects of changing air density and volume as the balloon ascends, as well as the implications of gravity at high altitudes.

Discussion Character

  • Technical explanation
  • Mathematical reasoning
  • Debate/contested

Main Points Raised

  • One participant calculates the net force on the balloon using the buoyant force and the mass of the balloon and payload, noting that the net force remains positive only up to about 55,000 feet.
  • Another participant points out that the buoyant force is dependent on the density of air and the volume of the balloon, which increases as the balloon ascends.
  • Concerns are raised about how to model the change in volume of the balloon as it rises, with one participant indicating that the mass of helium remains constant in their calculations.
  • Some participants mention the use of the ideal gas law to calculate the balloon's volume at different altitudes, but express confusion over why the buoyant force appears constant in their results.
  • There is a discussion about the effects of gravity at high altitudes, with some noting that gravity decreases slightly and that the composition of the atmosphere changes, potentially affecting buoyancy.
  • One participant questions the implications of a constant buoyant force, suggesting that it would lead to an unrealistic acceleration of the balloon.

Areas of Agreement / Disagreement

Participants express differing views on the behavior of buoyant force and the implications of constant values in their calculations. There is no consensus on how to accurately model the changes in volume and buoyancy as the balloon ascends.

Contextual Notes

Participants acknowledge limitations in their models, including assumptions about the behavior of the balloon and the effects of altitude on air density and gravity. The discussion remains open-ended regarding the mathematical modeling of these factors.

Who May Find This Useful

This discussion may be of interest to those involved in high altitude ballooning, atmospheric science, or anyone looking to understand the dynamics of buoyancy and acceleration in varying atmospheric conditions.

djdoug99
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I'm trying to calculate the acceleration of a high altitude balloon at different altitudes. In excel I've got the temperature, air pressure, and air density for a given altitude (thanks to NASA). Right now I am calculating the net force on the balloon with:

Fnet= Fb-Fm

Fb = Buoyant force = density of air*volume*9.81

Fm= (mass of balloon+mass of payload+(volume*density of helium))*9.81

For whatever volume I put in for the balloon I only get a positive net force until about 55,000 feet. I'm thinking it is because I am not taking into account the increase of air that will be displaced by the balloon as it gets higher and higher, but I am not sure how to model that mathematically. Any insight as to how to do this would be appreciated.
 
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Isn't the buoyant force: density of air*volume*9.81 ?

High altitude balloons will start out partially filled, so their volume will increase. What won't increase is the mass of the helium used. F_m will be a constant unless you let out helium
 
Yes it is. I guess I wasn't paying attention when I was typing that in. Its been fixed in the original post. I'm aware that the volume of the balloon will increase as it climbs which is my problem since the amount of air displaced will also increase. I just don't know how to model the change of volume. As for the helium, the mass of the helium in my excel sheet is constant (it uses the initial volume of the balloon)
 
bump.. or anyone have another idea how I can approximate the acceleration at various altitudes?
 
Im using these equations:
http://www.grc.nasa.gov/WWW/K-12/airplane/atmosmet.html

I'm still getting a constant buoyant force for some reason. If someone could take a look at my excel sheet that would be great. The ideal gas law is being used to calculate the baloons volume at different altitudes.

thank you
 

Attachments

djdoug99 said:
I'm still getting a constant buoyant force for some reason.
Maybe because it is correct? At least as long as the balloon can expand freely.
 
At very high altitudes, the strength of gravity will be a bit less. Eventually it's mostly helimum and hydrogen at the outer edges of the atmosphere without any of the heavier elements.
 
Jeff Reid said:
At very high altitudes, the strength of gravity will be a bit less. Eventually it's mostly helimum and hydrogen at the outer edges of the atmosphere without any of the heavier elements.
Yes, these a minor effects. But at some point the balloon is fully inflated, so it cannot reduce its density to float into less dense regions.
 
A.T. said:
Maybe because it is correct? At least as long as the balloon can expand freely.

But if it was constant than its acceleration would be constant so it would be going close to 300 m/s at a certain altitude. This of course is without the drag force accounted for.
 
  • #10
Jeff Reid said:
Eventually it's mostly helimum and hydrogen at the outer edges of the atmosphere without any of the heavier elements.

I don't think you'll get that far with a balloon.
 

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