Gouy Balance Nonlinear Slope (Magnetic Susceptibility Lab)

In summary, the speaker is analyzing data for a physical chemistry magnetic susceptibility lab and is having trouble linearizing the graphs of force vs. current. They have tried plotting force vs. current squared and fitting a second degree polynomial, but the results are still non-linear. Possible explanations for this include a non-linear relationship between current and magnetic field, non-linear properties of the magnetic core material, an incorrect experimental setup, or a changing magnetic susceptibility of the sample.
  • #1
djh101
160
5
I am currently analyzing my data for the physical chemistry magnetic susceptibility lab. All the data is giving nice, smooth graphs for force vs. current, but I am unable to linearize them.

[itex]F = \frac{1}{2}\chi\mu_{0}AH^{2}[/itex]

I have plotted force vs. current and force vs. current squared (current should be proportional to field, so using current shouldn't affect the slope). The former gives an upward moving curve while the latter gives a downward moving curve, so neither is linear. However, fitting a second degree polynomial gives a very good fit to the former (R2 = .997) and a near perfect fit to the latter (R2 = .999). What might be a possible explanation for the nonlinearity?

The only thing I can think of would be an inaccurate current reading, but even doubling the current (making it higher than the current setting, which was already higher than the actual current) doesn't completely kill of the nonlinearity. Any ideas?

http://onlinesciencetools.com/_miscfiles/nicl2.png
 
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  • #2
It is possible that the nonlinearity is due to a non-linear relationship between current and the magnetic field. This could be caused by the magnetic core material having non-linear properties, or due to the experimental setup. For example, if the wire is wound too tightly, it can cause a non-linear relationship between the current and the magnetic field. It is also possible that the nonlinearity is due to the fact that the magnetic susceptibility of the sample is changing with the increasing field strength, which would cause a non-linear response in the force measurement.
 

1. What is a Gouy Balance Nonlinear Slope?

A Gouy Balance Nonlinear Slope is a laboratory technique used to measure the magnetic susceptibility of a substance. This method involves measuring the weight of a sample in both the presence and absence of a magnetic field, and then using this data to calculate the magnetic susceptibility of the sample.

2. How does a Gouy Balance Nonlinear Slope work?

In a Gouy Balance Nonlinear Slope, a sample is placed in a test tube and suspended between two magnetic poles. The weight of the sample is measured in both the presence and absence of a magnetic field. The difference in weight between the two measurements is used to calculate the magnetic susceptibility of the sample.

3. What is the purpose of a Gouy Balance Nonlinear Slope in a magnetic susceptibility lab?

The purpose of a Gouy Balance Nonlinear Slope is to accurately measure the magnetic susceptibility of a substance. This information can be used to study the magnetic properties of a material and its potential applications, such as in electronics or materials science.

4. What factors can affect the accuracy of a Gouy Balance Nonlinear Slope measurement?

The accuracy of a Gouy Balance Nonlinear Slope measurement can be affected by several factors, including the uniformity of the magnetic field, the temperature of the sample, and the precision of the equipment used. Additionally, the sample itself can affect the accuracy if it is not homogenous or if it contains impurities.

5. Are there any limitations to using a Gouy Balance Nonlinear Slope for measuring magnetic susceptibility?

While a Gouy Balance Nonlinear Slope is a commonly used method for measuring magnetic susceptibility, it does have some limitations. It is not suitable for samples with high magnetic susceptibility, as the weight differences may be too small to accurately measure. Additionally, this method cannot provide information on the anisotropy of a sample's magnetic properties.

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