Neutrinos are produced whenever particles undergo weak-interaction processes, especially beta decay, electron or positron capture, pion and muon decay, and nuclear fusion. Their sources can be organized into the following major categories.
Cosmic Neutrino Background
Relic neutrinos produced during the first second after the Big Bang
Sometimes called the cosmic relic neutrino background
Expected temperature today: approximately 1.95 K
Not yet directly detected
Primordial Nucleosynthesis Neutrinos
Produced during weak-interaction reactions in Big Bang nucleosynthesis
Diffuse Supernova Neutrino Background
The accumulated neutrino emission from all past core-collapse supernovae
Also called the supernova relic neutrino background
Early-Universe Particle Decays
Possible neutrinos from the decay of unstable primordial particles
Cosmic-String or Topological-Defect Neutrinos
Hypothetical ultra-high-energy neutrinos from cosmic strings, monopoles, or other defects
Neutrinos from Primordial Black Holes
Possible Hawking-radiation neutrinos from evaporating primordial black holes
Produced by nuclear fusion reactions in the Sun:
Proton–proton neutrinos
Pep neutrinos
Helium-3–proton, or hep, neutrinos
Beryllium-7 neutrinos
Boron-8 neutrinos
Nitrogen-13 neutrinos
Oxygen-15 neutrinos
Fluorine-17 neutrinos
The first five primarily originate from the proton–proton chain, while nitrogen-13, oxygen-15, and fluorine-17 neutrinos arise from the CNO cycle.
Hydrogen-fusion neutrinos
CNO-cycle neutrinos
Neutrinos from massive stellar cores
Thermal neutrinos from hot stellar interiors
Plasma-process neutrinos
Pair-annihilation neutrinos
Photoneutrinos
Bremsstrahlung neutrinos
Nuclear weak-decay neutrinos
Plasmon-decay neutrinos
Pair-annihilation neutrinos
Bremsstrahlung neutrinos
Neutrinos from accreting white dwarfs
Neutrinos from white-dwarf mergers
Beta-equilibrium neutrinos
Direct and modified Urca-process neutrinos
Neutrinos from neutron-star cooling
Neutrinos from neutron-star crust reactions
Neutrinos from superfluid-pair formation and breaking
Supernovae are intense sources of all neutrino flavors:
Electron neutrinos from neutronization
Electron antineutrinos from positron capture
Muon neutrinos and antineutrinos
Tau neutrinos and antineutrinos
Thermal neutrinos from the proto-neutron star
Neutrinos from shock propagation and stellar collapse
Neutrinos from direct stellar collapse into a black hole
Short-duration, high-luminosity neutrino bursts
Neutrinos from exceptionally energetic core-collapse explosions
Possible high-energy neutrinos from associated relativistic jets
Weak-interaction neutrinos from thermonuclear burning
Electron-capture neutrinos
Lower neutrino output than core-collapse supernovae
Neutrinos from radioactive nuclei and nuclear reactions
Possible high-energy neutrinos from shock-accelerated particles
Possible neutrinos from powerful shocks, dense circumstellar environments, or central engines
Thermal and nuclear-process neutrinos from massive stellar explosions
Binary neutron-star mergers
Neutron-star–black-hole mergers
Binary black-hole mergers with surrounding matter
White-dwarf mergers
Neutron-star–white-dwarf mergers
Post-merger hypermassive neutron stars
Black-hole accretion disks formed after mergers
These events may produce thermal MeV neutrinos and, where relativistic jets form, high-energy neutrinos.
Supernova remnants
Pulsars
Pulsar wind nebulae
Magnetars
Soft gamma repeaters
Binary-star systems
X-ray binaries
High-mass X-ray binaries
Low-mass X-ray binaries
Microquasars
Accreting neutron stars
Accreting stellar-mass black holes
Colliding-wind binary systems
Young stellar objects
Stellar clusters
Massive star-forming regions
Molecular clouds illuminated by cosmic rays
Galactic Centre
Fermi bubbles
Galactic cosmic-ray interactions
Nova remnants
Galactic PeVatrons
High-energy neutrinos are generally produced when accelerated hadrons interact through:
Proton–proton interactions
Proton–photon interactions
Nucleus–nucleus interactions
Photodisintegration and subsequent particle decay
Blazars
Flat-spectrum radio quasars
BL Lacertae objects
Radio galaxies
Seyfert galaxies
Quasars
Low-luminosity active galactic nuclei
AGN jets
AGN cores
AGN coronae
AGN accretion disks
Long-duration gamma-ray bursts
Short-duration gamma-ray bursts
Low-luminosity gamma-ray bursts
Choked-jet gamma-ray bursts
Shock-breakout gamma-ray bursts
Failed gamma-ray bursts
Stars disrupted by supermassive black holes
Jetted tidal disruption events
Non-jetted tidal disruption events
Starburst galaxies
Ultra-luminous infrared galaxies
Luminous infrared galaxies
Galaxy clusters
Galaxy groups
Intergalactic shocks
Fast blue optical transients
Luminous fast blue optical transients
Fast radio burst environments
Extragalactic magnetar flares
Changing-look active galactic nuclei
Black-hole accretion transients
Atmospheric neutrinos are produced when cosmic rays strike nuclei in Earth’s atmosphere.
Charged pions
Charged kaons
Muons
Charmed mesons
Other short-lived hadrons
Conventional atmospheric neutrinos
Prompt atmospheric neutrinos
Electron neutrinos and antineutrinos
Muon neutrinos and antineutrinos
Tau neutrinos produced through oscillations
Neutrinos from cosmic-ray air showers
Atmospheric neutrinos cover energies from hundreds of MeV to beyond the PeV scale.
The Sun
Cosmic-ray interactions in the solar atmosphere
Solar flares
Coronal mass-ejection environments
Cosmic-ray interactions with the Moon
Cosmic-ray interactions with planetary atmospheres
Cosmic-ray interactions with asteroids or other solid bodies
Possible neutrinos from dark-matter annihilation inside the Sun
Possible neutrinos from dark-matter annihilation inside planets
Solar-atmospheric neutrinos differ from ordinary solar-fusion neutrinos because they originate from cosmic-ray collisions near the solar surface.
Electron antineutrinos produced by radioactive decay inside Earth, principally from:
Uranium-238 decay chain
Thorium-232 decay chain
Potassium-40 decay
Uranium-235 decay chain
Rubidium-87 decay
Major terrestrial regions include:
Continental crust
Oceanic crust
Upper mantle
Lower mantle
Possible deep-Earth reservoirs
Rocks
Soil
Minerals
Ocean water
Groundwater
Atmospheric radionuclides
Radioactive isotopes in living organisms
Cosmic-ray-induced atmospheric neutrinos
Neutrinos from radioactive atmospheric isotopes
Possible low-intensity neutrinos associated with photonuclear reactions
Beta-decay neutrinos from unstable isotopes generated by lightning
Living organisms contain naturally radioactive isotopes.
Sources include:
Potassium-40 beta decay
Carbon-14 beta decay
Other trace radioactive isotopes
The human body therefore emits a small number of electron antineutrinos, mainly from potassium-40 beta decay.
Nuclear reactors are powerful sources of electron antineutrinos.
Commercial power reactors
Research reactors
Naval propulsion reactors
Small modular reactors
Fast breeder reactors
Molten-salt reactors
Experimental reactors
Isotope-production reactors
Natural nuclear reactors, such as the ancient Oklo reactors
Neutron-rich fission fragments undergo beta-minus decay:
[
(A,Z)\rightarrow(A,Z+1)+e^-+\bar{\nu}_e
]
Major fission parents include:
Uranium-235
Uranium-238
Plutonium-239
Plutonium-241
Produced when proton beams strike a target and generate pions and kaons.
Sources include:
Pion-decay beams
Kaon-decay beams
Muon-decay beams
On-axis neutrino beams
Off-axis neutrino beams
Wide-band beams
Narrow-band beams
Neutrino factories
Muon-storage rings
Beta beams
Decay-at-rest sources
Decay-in-flight sources
Stopped-pion sources
Spallation neutron sources
Beam-dump facilities
Collider-generated neutrinos
Forward neutrinos at particle colliders
Proton–proton collisions
Proton–antiproton collisions
Heavy-ion collisions
Electron–positron collisions
Decays of heavy-flavor hadrons
Decays of W and Z bosons
Tau-lepton decays
Top-quark decays
Beta-minus decay sources
Beta-plus decay sources
Electron-capture sources
Neutron-activated isotopes
Radioisotope neutrino generators
Artificial calibration sources
Intense electron-capture sources
Intense beta-decay antineutrino sources
Examples of useful source isotopes include:
Chromium-51
Argon-37
Cerium-144
Praseodymium-144
Strontium-90
Yttrium-90
Lithium-8
Helium-6
Atmospheric nuclear explosions
Underground nuclear explosions
Underwater nuclear explosions
Nuclear weapon tests
Fission explosions
Thermonuclear fusion explosions
They generate intense, short-duration electron-antineutrino emissions, mainly from radioactive fission products.
Nuclear beta decay
Electron capture
Positron emission
Nuclear fission
Neutron activation
Muon capture
Pion capture
Fusion reactions
Spallation reactions
Photodisintegration products
Heavy-ion collisions
Radioactive decay chains
Cosmic rays can produce neutrinos through interactions with:
Earth’s atmosphere
The solar atmosphere
Interstellar gas
Molecular clouds
Stellar winds
Supernova ejecta
Accretion disks
Radiation fields
Cosmic microwave background photons
Extragalactic background light
Galaxy-cluster gas
Planetary surfaces
The Moon
Asteroids
Intergalactic matter
Cosmogenic neutrinos are produced when ultra-high-energy cosmic rays interact with background radiation.
Interactions with the cosmic microwave background
Interactions with extragalactic background light
Photopion production
Neutron beta decay
Nuclear photodisintegration
They are also called:
GZK neutrinos
Ultra-high-energy cosmogenic neutrinos
Their expected energies may extend from PeV to EeV and beyond.
These remain hypothetical or unconfirmed.
Dark-matter annihilation in the Sun
Dark-matter annihilation in Earth
Dark-matter annihilation in the Galactic Centre
Dark-matter annihilation in dwarf spheroidal galaxies
Dark-matter annihilation in galaxy clusters
Dark-matter particle decay
Sterile-neutrino dark-matter decay
Dark-matter interactions with stars
Dark-matter capture in neutron stars
Dark-matter decay throughout the Universe
Sterile-neutrino decay
Heavy neutral lepton decay
Axion-like particle conversion or decay chains
Supersymmetric particle decay
Leptoquark decay
Grand-unified-theory particle decay
Topological defects
Cosmic strings
Magnetic monopole annihilation
Superheavy dark-matter decay
Evaporating black holes
Extra-dimensional particle processes
Lorentz-violation-induced particle decay
Secret neutrino interactions
Neutrinos from exotic compact objects
Beta-minus decay → electron antineutrinos
Beta-plus decay → electron neutrinos
Electron capture → electron neutrinos
Nuclear fusion → mainly electron neutrinos
Nuclear fission → mainly electron antineutrinos
Charged-pion decay
Charged-kaon decay
Muon decay
Tau-lepton decay
Charm-hadron decay
Bottom-hadron decay
Proton–proton interactions
Proton–photon interactions
Nucleus–nucleus interactions
Nucleus–photon interactions
Electron–positron pair annihilation
Plasmon decay
Photoneutrino emission
Bremsstrahlung
Recombination neutrino emission
Urca processes
The principal sources of neutrinos can therefore be summarized as:
Big Bang and cosmological relics
The Sun and other stars
Supernovae and stellar explosions
Neutron stars and compact-object mergers
Galactic cosmic accelerators
Extragalactic cosmic accelerators
Cosmic-ray interactions
Earth’s atmosphere
Radioactive decay inside Earth
Nuclear reactors
Particle accelerators
Laboratory radioactive sources
Nuclear explosions
Living organisms
Cosmogenic interactions
Dark matter and other hypothetical exotic phenomena