How is the wavelength of emitted EM radiation measured?

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Discussion Overview

The discussion revolves around the measurement of the wavelength of emitted electromagnetic (EM) radiation, particularly focusing on the historical and technical aspects of measuring frequencies, the definition of the second based on caesium-133, and the implications of temperature on these measurements. Participants explore various methods and instruments used for measuring wavelengths and frequencies across different portions of the EM spectrum.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Historical

Main Points Raised

  • Some participants discuss the historical context of measuring the frequency of radiation, noting that atomic clocks utilize the frequency of caesium-133 to define the second.
  • There is mention of various measurement methods for different frequencies, with optical frequencies being easier to measure using interference techniques, while GHz frequencies can be measured using digital counters.
  • Some participants suggest that the choice of 0 K in the definition of the second is to avoid Doppler broadening effects, although it is acknowledged that absolute zero cannot be practically achieved.
  • One participant notes that while temperature does not affect the radiation emitted, atomic motion at temperatures above 0 K leads to Doppler shifts that complicate frequency measurements.
  • There is a discussion about the need to correct for gravitational time dilation when measurements are made at different altitudes, although some participants express uncertainty about its relevance to the official definition of the second.
  • Some participants propose that precise frequency measurements require feedback loops to stabilize oscillators and reduce random perturbations, emphasizing the complexity of achieving high accuracy.
  • Others mention that while the caesium-133 definition is precise, there are ongoing efforts to develop even more accurate standards using optical frequencies or nuclear transitions.

Areas of Agreement / Disagreement

Participants express a range of views on the measurement methods and implications of temperature on radiation emission. There is no clear consensus on the necessity of corrections for gravitational time dilation, and discussions about the accuracy of different measurement techniques highlight ongoing debates in the field.

Contextual Notes

Some limitations are noted regarding the practical impossibility of achieving absolute zero and the challenges posed by Doppler effects at non-zero temperatures. Additionally, the discussion reflects varying levels of accuracy achievable with different measurement techniques and the historical evolution of these methods.

PainterGuy
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Hi,

Since 1967, the second has been defined as exactly "the duration of 9,192,631,770 periods of the radiation corresponding to the transition between the two hyperfine levels of the ground state of the caesium-133 atom" (at a temperature of 0 K). This length of a second was selected to correspond exactly to the length of the ephemeris second previously defined. Atomic clocks use such a frequency to measure seconds by counting cycles per second at that frequency. Radiation of this kind is one of the most stable and reproducible phenomena of nature. The current generation of atomic clocks is accurate to within one second in a few hundred million years.
Source: https://en.wikipedia.org/wiki/Second#"Atomic"_second

How were such huge number of periods per second measured originally? Was an instrument such as Michelson interferometer used? I think it was Albert Michelson who invented the interferometer to make calculations of wavelength and frequency of EM waves.

Another related question is that why the temperature of 0 K was chosen since 0 Kelvin couldn't be achieved practically. I understand that the atoms must be at complete rest while emitting the radiation but the problem is that absolute rest state is not possible so how do they go around this problem practically?

I'd really appreciate if you could help me with the queries above. Thank you.
 
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That's a very wide open question as the different frequencies suit different measurement methods. Wavelength is easiest to measure at optical frequencies, using easy to measure mechanical quantities and interference as a 'lever' to magnify a tiny distance (wavelength) into a large fringe separation.(Michelson and all the others)
Wavelength can be measured by looking at standing wave patterns on transmission lines (several MHz up to several Ghz). Very limited accuracy but better than nothing and all you could do when valves were struggling with frequencies above a few hundreds of MHz. In fact it's all historical.

BUT the possible accuracy of Frequency / Time measurement can take you into much much higher accuracy for Frequency measurement, once the electronics can handle it. Frequency and time are quantities that can be measured with much greater accuracy than any others. (1 in 1012 is easy in the Lab)
 
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These are GHz frequencies, not optical frequencies, so I think the frequencies are simply measured with digital counters that count the number of cycles.
 
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phyzguy said:
These are GHz frequencies, not optical frequencies, so I think the frequencies are simply measured with digital counters that count the number of cycles.

You can take an optical frequency source and mix it with another optical frequency (laser local oscillator) to produce a microwave signal, which can be measured with a 'counter'. The accuracy will depend on the accuracy and noise of the local oscillator - as always in any heterodyne system.
'Counting the number of cycles' is not necessarily as simple as just that.
 
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sophiecentaur said:
That's a very wide open question as the different frequencies suit different measurement methods. Wavelength is easiest to measure at optical frequencies, using easy to measure mechanical quantities and interference as a 'lever' to magnify a tiny distance (wavelength) into a large fringe separation.(Michelson and all the others)

Thank you. I agree with you. I had optical frequencies in mind when I asked this question but didn't realize that "9,192,631,770 periods of the radiation corresponding to the transition between the two hyperfine levels of the ground state of the caesium-133 atom" correspond to radio waves portion of EM spectrum. The 9,192,631,770 periods of the radiation per second is equivalent to frequency of 9.19263177 GHz. I checked online and there are radio interferometers like the shown below.

1590198974072.png
I'd appreciate if you could comment on the following. Thanks a lot!

PainterGuy said:
Another related question is that why the temperature of 0 K was chosen since 0 Kelvin couldn't be achieved practically. I understand that the atoms must be at complete rest while emitting the radiation but the problem is that absolute rest state is not possible so how do they go around this problem practically?
 
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If the measurement is made near Earth you will also need to correct for gravitational time dilation at that location.
 
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PainterGuy said:
Summary:: I was thinking about the measurement instruments used to find the wavelength and frequency of EM waves. I was looking at the problem in historical perspective.

Another related question is that why the temperature of 0 K was chosen since 0 Kelvin couldn't be achieved practically.
Temperature actually makes no difference to the radiation an atom emits, but at temperatures above 0K the atom is moving, which means that the radiation you receive is Doppler shifted. That means that the frequency you receive isn't quite at the frequency standard. So the specification of 0K is meant to close off ambiguity from the Doppler effect.

In practice, you are correct that it is impossible to get to 0K, but we can cool to fractions of a Kelvin. And I think you can correct for the Doppler effect a bit - you know the distribution of velocities of atoms in a gas at a known temperature, so you know what the Dopplered distribution of frequencies should look like, so you can work out which part of the radiation is non-Dopplered and use that as your time standard.
 
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Baluncore said:
If the measurement is made near Earth you will also need to correct for gravitational time dilation at that location.

I had thought about it. I don't think that the official definition mentions anything related to the time dilation or any specific point or location where the measurement should be taken. I understand that the second would be elongated if the measurement is taken, say, at moon, but strangely I didn't come across anything related to the time dilation.

The definition is:
the duration of 9,192,631,770 periods of the radiation corresponding to the transition between the two hyperfine levels of the ground state of the caesium-133 atom at a temperature of 0 K.
 
PainterGuy said:
I don't think that the official definition mentions anything related to the time dilation or any specific point or location where the measurement should be taken.
As long as the emission and reception happen at the same height you don't have to worry about it. It's also a very small effect - just about detectable with great care - in a lab setting, whereas Doppler broadening is a large issue unless you insist on cryogenic temperatures.
 
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Ibix said:
And I think you can correct for the Doppler effect a bit - you know the distribution of velocities of atoms in a gas at a known temperature,
Any precise frequency measurement uses a feedback loop of some kind to lock an oscillator to the source frequency and to reduce random perturbations. Feedback loop all have a low pass filter to 'slow down' the response of the feedback loop. In order to get a reliable measure of frequency in the order of say, 1 part in 1012 (and even a hundred times better) the time constant must be well in excess of 1012 cycles of the comparison frequency. Needless to say, the equipment needs to be switched on for hours - probably even days - to eliminate thermal variations.
 
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  • #11
The Cs-133 definition for the second is very precise. Of course you have to do it at absolute 0 temperature to avoid the Doppler broadening of the resonance to reduce it to the "natural line width", which is very small. On the other hand this hyperfine transition is not the most accurate thinkable definition, and metrologists work on even better standards using optical frequencies either from other atomic transitions. Due to the higher frequency they can get more accurate. Another path is to use nuclear transitions. Here the problem is that usually the frequencies are too high (in the X-ray or ##\gamma##-ray realm) which are hard to get stabilized in a "laser-type" system. Most accurate are frequency combs using a mode-locked laser. There's however a promising candidate, the Thorium-229 isomer transition, which is in the UV range (~150 nm), which can be stabilized using a frequency comb. The advantage of using a nuclear transition as compared to a atomic transistion is that it's much more insensitive to external perturbations.

https://en.wikipedia.org/wiki/Nuclear_clock
https://en.wikipedia.org/wiki/Mode-locking
 
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  • #12
vanhees71 said:
There's however a promising candidate, the Thorium-229 isomer transition

If we could find it. There are several technical difficulties with nuclear clocks, but one fundamental one is that the uncertainty on the transition energy is ~1015 times larger than the width. That's a lot of places to look!
 
  • #13
It's measured! The accuracy is however not competitive with atomic clocks yet.

https://www.gsi.de/en/start/news/details/2019/09/11/auf_dem_weg_zur_kernuhr0.htm
https://arxiv.org/abs/1905.06308
 
  • #14
vanhees71 said:
It's measured!

Yay!

vanhees71 said:
The accuracy is however not competitive with atomic clocks yet.

That is true. It's good to 2%, or about half an hour per day. It's not competitive with a mechanical clock yet, but one needs to start somewhere. [no pun intended]Time will tell.[/no pun intended]
 
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  • #15
It's been measured twice: https://arxiv.org/abs/1902.04823 This is perhaps more interesting as it allows one to create the metastable state without knowing the exact frequency. In principle, one could pump it with x-rays and look for the VUV line from the decay. In practice it is not anywhere near this simple.

There sill be a seminar on this soon at CERN. Those with CERN credentials can find it.
 
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