Gravitational Acceleration and Rising Objects

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Discussion Overview

The discussion revolves around the challenges of measuring gravitational acceleration using a sounding balloon payload designed to ascend to 100,000 feet. Participants explore the mathematical and experimental considerations involved in distinguishing between proper acceleration and coordinate acceleration, as well as the implications of using various sensors for accurate measurements.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Experimental/applied

Main Points Raised

  • One participant suggests that the payload's proper acceleration can be measured directly, while the GPS-derived coordinate acceleration should be subtracted to find the change in gravitational acceleration.
  • Another participant points out that when the accelerometer is accelerated upwards, it will register an increase in gravitational acceleration, similar to feeling heavier in an elevator, implying that subtracting GPS acceleration could yield gravitational acceleration.
  • Concerns are raised about the potential for noise in the data to obscure the small differences in measurements, particularly when the balloon reaches terminal velocity and experiences lateral accelerations due to wind.
  • A different perspective emphasizes the limitations of using GPS data for acceleration calculations, advocating for a localized model of gravity and suggesting the use of filtering techniques like Kalman filters for better accuracy.
  • Questions are raised regarding the necessity of including a magnetometer in the setup, given the use of a single-axis accelerometer.

Areas of Agreement / Disagreement

Participants express differing views on the best approach to measuring gravitational acceleration, with some advocating for the use of GPS data and others cautioning against its reliability. There is no consensus on the optimal methodology or the effectiveness of the proposed equipment.

Contextual Notes

Participants note potential limitations such as the noise in measurements, the localized nature of gravity at high altitudes, and the challenges posed by the equipment's accuracy and weight constraints.

Jason0725
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So I'm performing an experiment at my university in which we've got to construct a sounding balloon payload to measure the relative changes in gravity for up to 100,000 feet. I'm having a bit of trouble, however, sorting out the math and such.

So the payload is rising, and its position will be tracked by GPS. We've also got a gyroscope, magnetometer, and single-axis accelerometer that we're planning on using to calculate the payload's accelerations.

My dilemma is this: I believe the payload's accelerations would be the "proper acceleration," and the acceleration calculated from the GPS data would be the "coordinate acceleration." So then I could get my change in gravitational acceleration by getting the downward component of my payload's proper acceleration and subtracting the coordinate acceleration from that, right? But the coordinate acceleration would be upward, opposite the gravitational acceleration I'm trying to measure.

Advice would be much obliged.
 
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Suppose the accelerometer on the balloon is a spring balance with a lump of lead attached. When it's sitting in the lab the spring balance is measuring the gravitational acceleration.

If the balance is accelerated upwards, the reading on the balance will increase, just as one feels heavier in an elevator accelerating up. So, presumably, if you subtract the GPS acceleration, you'll get the gravitational acceleration.

The problem is that the difference will be very small and probably smaller than your error bars.
 
Just thinking... a rising balloon may only accelerate for a few seconds before attaining a terminal velocity through the air. Then that velocity may change slowly with changes in density. If the measuring package is suspended from the balloon, there may be lateral accelerations to account for because of winds.

I tend to agree that the noise in the data may overcome the measurement.

Do you have access to a small rocket?
 
Jason0725 said:
So the payload is rising, and its position will be tracked by GPS. We've also got a gyroscope, magnetometer, and single-axis accelerometer that we're planning on using to calculate the payload's accelerations.

My dilemma is this: I believe the payload's accelerations would be the "proper acceleration," and the acceleration calculated from the GPS data would be the "coordinate acceleration."
I don't think you want to use an acceleration calculated from GPS data. It's going to be noisy.

With a balloon that goes up to 100,000 feet you are only going to get a very localized picture of Earth's gravity field. So use a localized model. You aren't chasing after extreme accuracy with the kinds of equipment you can put on a balloon. This suggests a simple localized and linearized model of gravity: Some acceleration at ground level less a free air correction.

Rather than using canned values, you are trying to back out the ground level acceleration and the free air correction. Some kind of least squares filter would work quite nicely here, either a Kalman filter or a batch least squares. With this, all you need from your GPS is the height above the reference ellipsoid.

I have doubts that a simple one-shot balloon experiment with presumably cheap and lightweight equipment will get you anything beyond this.

Why the magnetometer? That seems out of kilter given that you are only using a single axis accelerometer.
 

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