Global Antineutrino Map: Measuring Nuclear Reactor Emissions Worldwide

In summary, the scientists used geology models and data about nuclear reactors together with results from two neutrino detectors to produce a worldwide map of antineutrino emission. Man-made reactors are contributing 1% to the total emission, but the production is so localized it is clearly visible in many spots.
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A group of scientists used geology models and data about nuclear reactors together with results from two neutrino detectors to produce a worldwide map of antineutrino emission. Man-made reactors are contributing 1% to the total emission, but the production is so localized it is clearly visible in many spots.

Original publication
phys.org news

Next step: actually measure this...
Could be interesting to monitor nuclear reactors from everywhere in the world, but that would need a very good angular resolution of the detectors.

antinumap.jpg
 
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Likes Jeff Rosenbury, Astronuc, Greg Bernhardt and 2 others
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  • #2
mfb said:
A group of scientists used geology models and data about nuclear reactors together with results from two neutrino detectors to produce a worldwide map of antineutrino emission. Man-made reactors are contributing 1% to the total emission, but the production is so localized it is clearly visible in many spots.

Original publication
phys.org news

Next step: actually measure this...
Could be interesting to monitor nuclear reactors from everywhere in the world, but that would need a very good angular resolution of the detectors.

View attachment 88108

That's really neat! Thanks for sharing it.

Unfortunately, since this is what the sun looks like in neutrinos (in Super-K), I don't have too much hope of there being the resolution to measure this any time soon. :sorry:
solpic_1500d_2_1.jpg
 
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Why the huge difference (factor of 5) between land and sea?
 
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Vanadium 50 said:
Why the huge difference (factor of 5) between land and sea?
Presumably the differential distribution of U/Th in the oceanic vs continental crusts. Continental crusts are enriched in U/Th relative to the ocean. http://www.world-nuclear.org/info/Nuclear-Fuel-Cycle/Uranium-Resources/The-Cosmic-Origins-of-Uranium/
 
  • #5
Vanadium 50 said:
Why the huge difference (factor of 5) between land and sea?
Wikipedia says the continental crust is roughly 5 times as thick as the ocean crust. Could it be as simple as that?
 
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Lord Crc said:
Wikipedia says the continental crust is roughly 5 times as thick as the ocean crust. Could it be as simple as that?
Not really. It is a difference in elemental composition that matters. The continental crust is more enriched in the long-lived radioisotopes (U,Th,K).
 
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I suppose that bright dot on the US west coast isn't actually due to my watch with tritium tubes ...
 
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France is pretty high, which is not too surprising. A large part of western China and Mongolia is too.
 
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Hypatio said:
Not really. It is a difference in elemental composition that matters. The continental crust is more enriched in the long-lived radioisotopes (U,Th,K).
Why?

I can understand how dissolved uranium salts might tend to work their way out of the oceans, but the seeming abundance in stable precambrian rock seems odd. It would seem more likely to concentrate in volcanic/hotsprings areas. Over the long term it should wash out from wet stable geologies.
 
  • #11
Jeff Rosenbury said:
Why?

I can understand how dissolved uranium salts might tend to work their way out of the oceans, but the seeming abundance in stable precambrian rock seems odd. It would seem more likely to concentrate in volcanic/hotsprings areas. Over the long term it should wash out from wet stable geologies.
The answer is in the link I posted upthread. http://www.world-nuclear.org/info/Nuclear-Fuel-Cycle/Uranium-Resources/The-Cosmic-Origins-of-Uranium/

The present-day abundance of uranium in the 'depleted' mantle exposed on the ocean floor is about 0.004 ppm. The continental crust, on the other hand, is relatively enriched in uranium at some 1.4 ppm. This represents a 70-fold enrichment compared with the primitive mantle. In fact, the uranium lost from the 'depleted' oceanic mantle is mostly sequestered in the continental crust.

It is likely that the process or processes which transferred uranium from the mantle to the continental crust are complex and multi-step. However, for at least the past 2 billion years they have involved:

  1. formation of oceanic crust and lithosphere through melting of the mantle at mid-ocean ridges,
  2. migration of this oceanic lithosphere laterally to a site of plate consumption (this is marked at the surface by a deep-sea trench),
  3. production of fluids and magmas from the downgoing (subducted) lithospheric plate and overriding mantle 'wedge' in these subduction zones,
  4. transfer of these fluids/melts to the surface in zones of 'island arcs' (such as the Pacific's Ring of Fire),
  5. production of continental crust from these island arc protoliths, through remelting, granite formation and intra-crustal recycling.
 
  • #12
e.bar.goum said:
The answer is in the link I posted upthread. http://www.world-nuclear.org/info/Nuclear-Fuel-Cycle/Uranium-Resources/The-Cosmic-Origins-of-Uranium/
I read that post. It just doesn't make sense to me.

If the salts are water soluble (at temperature) they would collect on land over time. If they aren't, they would collect in the ocean. But either way, stable wet areas like the Canadian Shield should be depleted (or at least neutral).

I don't blame the web site's authors. They didn't have access to a neat "Global Antineutrino Map" [:bow:] when they made their theory. But I wonder how the theory stacks up against new data.

Of course it's more likely I'm missing something, which is why I asked.
 
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This is keen and disappointing at the same time.

Keen because it is something I have not seen before. And at least somewhat interesting. Those hot-spots would seem to be interesting places to go look for interesting isotopes.

Disappointing because I thought it was going to be something very much more. When I was in grad school, round about 1983 or so, there was a proposal by a certain now-well-known physicist to build a really sensitive neutrino detector.

You have to recall that at the time there was a proposal in the USA for a thing called "The Strategic Defense Initiative" and immediately dubbed Star Wars. If you recall, that was a plan to build things that might hope to intercept incoming nuclear ballistic missiles. I don't have any idea if such a thing is possible, but that isn't the point. The point for this story is, during the construction of such a thing if it did indeed work, or was believed to work by the opposition, there would be a period during which opposition nuclear forces would be perceived to be losing their possible value. So there would be some pressure to "use it or lose it." Hence beginning to build such a thing might trigger a war.

Anyway, the neutrino detector proposal was to detect scattering modes of neutrinos that supposedly had a much higher cross section. And to detect them, the proposal was for a multi-tonne ultra-pure single crystal of Boron. The idea was, with such a crystal you could detect phonon modes that would be excited by scattering neutrinos. Meaning you could get, so it was hoped, a directional neutrino detector. That is, a neutrino telescope, possibly with a very interesting angular resolution. You might hope to see individual stars with it, for example.

During the Q&A period, an exchange somewhat like this occurred. (No I won't tell you who NI and LK were. At least one of them is dead anyway. 30 years is a long time in the life of a physics prof.)

NI: Could it detect nuclear reactors?
LK: Yes, quite likely.
NI: Such as on nuclear submarines?
LK: Yes, quite likely.
NI: In real time? Distance and direction?
LK: Yes, quite likely.
NI: So it's more destabilizing than Star Wars?
LK: If it gets me my funding, then I'm ok with that.

Note that the reason it would be destabilizing is because a large fraction of the world's nuclear weapon arsenal is located on submarines. The idea is that they are hard to detect and hard to locate accurately. So they would be hard to kill in a surprise attack. So if you started something, your opponent's nuclear subs would surface some time later and punish you. But if a neutrino telescope could tell you exactly where the subs were, you could spare a warhead for each one, and hope that a surprise attack could get away with little reprisal.

As far as I know the project was never done. I thought this might be it, but it is not.
 

1. What is a global antineutrino map?

A global antineutrino map is a visual representation of the distribution and intensity of antineutrinos around the world. Antineutrinos are subatomic particles that are produced in nuclear reactions, and their detection and mapping can provide valuable information about the Earth's interior and processes happening within it.

2. How is a global antineutrino map created?

A global antineutrino map is created by using data collected from antineutrino detectors located around the world. These detectors measure the number and energy of antineutrinos passing through the Earth's surface. This data is then analyzed and processed to create a map of the antineutrino flux, which is the number of antineutrinos passing through a specific area per unit of time.

3. What can a global antineutrino map tell us?

A global antineutrino map can tell us about the distribution of radioactive elements, such as uranium and thorium, within the Earth's interior. These elements produce antineutrinos as they decay, and their distribution can provide valuable insights into the composition and structure of the Earth's crust and mantle. Additionally, a global antineutrino map can also be used to monitor nuclear reactors and detect potential nuclear activity.

4. How accurate is a global antineutrino map?

A global antineutrino map is constantly being refined and improved as more data is collected and analyzed. The accuracy of the map depends on the sensitivity and precision of the detectors used, as well as the amount of data available. Generally, the map is most accurate in areas with a high concentration of detectors, such as North America and Europe, while other regions may have less precise data.

5. What are the potential applications of a global antineutrino map?

A global antineutrino map has a wide range of potential applications, including monitoring nuclear activity, studying the Earth's interior, and identifying potential locations for geothermal energy sources. It can also be used to improve our understanding of the Earth's formation and evolution, as well as provide valuable information for geological and geophysical studies.

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