World's Major Observatories

Nine major detectors spanning five continents, three oceans, and two polar ice sheets.

Active
IceCube
📍 South Pole, Antarctica

World's largest neutrino detector. 5,160 DOMs on 86 strings. Detected first PeV astrophysical neutrinos in 2013.

Technology Ice Cherenkov
Volume / Mass 1 km³
Underground 1,450–2,450 m
Operational Since 2010
↗ Official Website
Active
Super-Kamiokande
📍 Kamioka, Japan

50,000-ton water Cherenkov detector. Confirmed atmospheric neutrino oscillations in 1998, Nobel Prize 2015.

Technology Water Cherenkov
Volume / Mass 50,000 tons
Underground 1,000 m
Operational Since 1996
↗ Official Website
Active
SNO+
📍 Sudbury, Ontario, Canada

Successor to SNO. Now filled with liquid scintillator for solar, reactor, and double beta decay physics.

Technology Liquid Scintillator
Volume / Mass 1,000 tons
Underground 2,100 m
Operational Since 2013
↗ Official Website
Building
KM3NeT
📍 Mediterranean Sea

Deep-sea neutrino telescope with two sites: ARCA (astrophysical) off Sicily, ORCA (oscillations) off France.

Technology Sea Cherenkov
Volume / Mass 1 km³
Underground 3,500 m
Operational Since 2016
↗ Official Website
Building
DUNE
📍 Lead, South Dakota, USA

Fermilab's flagship experiment. 1,300 km baseline from Fermilab. Targets CP violation, mass ordering, proton decay.

Technology Liquid Argon TPC
Volume / Mass 40,000 tons
Underground 1,500 m
Operational Since 2020
↗ Official Website
Building
Hyper-Kamiokande
📍 Kamioka, Japan

Super-K's 5× larger successor. 260,000 tons ultra-pure water. Primary target: CP violation with T2HK beam.

Technology Water Cherenkov
Volume / Mass 260,000 tons
Underground 650 m
Operational Since 2020
↗ Official Website
Complete
Borexino
📍 Gran Sasso, Italy

First real-time spectroscopy of sub-MeV solar neutrinos. Detected pp, pep, CNO, and geoneutrino signals.

Technology Liquid Scintillator
Volume / Mass 300 tons
Underground 1,400 m
Operational Since 2007
↗ Official Website
Active
Baikal-GVD
📍 Lake Baikal, Russia

Gigaton Volume Detector in the world's deepest freshwater lake. Expanding to 1 km³ sensitivity.

Technology Water Cherenkov
Volume / Mass 0.5 km³
Underground 1,200 m
Operational Since 2021
↗ Official Website
Building
JUNO
📍 Jiangmen, China

Largest liquid scintillator detector. 53 km from reactors. Will determine mass ordering with sub-percent precision.

Technology Liquid Scintillator
Volume / Mass 20,000 tons
Underground 700 m
Operational Since 2022
↗ Official Website

How We Detect the Invisible

Four main detection strategies, each optimised for different neutrino energies and physics goals.

💡

Cherenkov Radiation

When a neutrino interacts with water or ice and produces a charged particle moving faster than light in that medium, a cone of blue light is emitted — analogous to a sonic boom for light. This Cherenkov ring is detected by arrays of photomultiplier tubes. The technique works at many energy scales, from MeV solar neutrinos to PeV astrophysical ones.

USED BY: SUPER-K, ICECUBE, KM3NET, BAIKAL-GVD, HYPER-K

Liquid Scintillation

A neutrino interaction in an organic liquid causes a tiny flash of light (scintillation). This gives superior energy resolution and lower detection thresholds than Cherenkov, making it ideal for reactor, solar, and geo-neutrinos. The key challenge is extreme radiopurity.

USED BY: BOREXINO, SNO+, KAMLAND, JUNO
🔵

Liquid Argon TPC

Neutrino interactions in liquid argon produce ionisation electrons and scintillation light. The electrons drift in an electric field to fine wire grids, producing beautiful 3D images of particle tracks — like a digital bubble chamber with millimetre resolution. Best for detailed event reconstruction and νe appearance.

USED BY: DUNE, MICROBOONE, ICARUS, ARGONCUBE
🏔️

Radiochemical Detection

Pioneered by Ray Davis with 615 tons of perchloroethylene, solar neutrinos transform Cl into radioactive Ar atoms which are extracted and counted. The GALLEX/GNO and SAGE experiments used gallium. Slow but sensitive to the lowest-energy pp neutrinos. Davis won the Nobel Prize 2002 for this method.

USED BY: HOMESTAKE, SAGE, GALLEX/GNO

Why Go Underground?

Neutrino detectors must be shielded from cosmic rays — high-energy particles from space that create thousands of muons per second passing through any detector at the surface. Even a single misidentified muon can mimic a neutrino signal.

Rock, water, or ice overburden reduces the cosmic ray muon flux by many orders of magnitude. At SNOLAB (2,100 m underground), the muon rate is reduced by a factor of ~50 million compared to the surface — leaving only a handful per day to contend with.

The material surrounding the detector must also have ultra-low radioactivity — trace uranium, thorium, and potassium produce backgrounds that can mimic neutrino signals. This drives extraordinary purity requirements, down to parts per trillion.

DEPTH COMPARISON
WIPP (US)
650 m salt
Kamioka Mine
1,000 m
Gran Sasso
1,400 m rock
IceCube (bottom)
2,450 m ice
SNOLAB
2,100 m rock
Baikal-GVD
1,366 m H₂O
KM3NeT
3,500 m sea