Research

Physics at the extremes

The group works on three experiments: one deep underground, one in the Antarctic ice and one on the Pacific seafloor.

Side view of the ATLAS detector in its underground cavern, with walkways and yellow access platforms.

At the Large Hadron Collider, CERN

ATLAS

One of the two general-purpose detectors at the LHC.

Photo: the ATLAS detector, by SimonWaldherr, CC BY-SA 4.0, via Wikimedia Commons

SFU physicists study the properties of the Higgs boson, search for new long-lived particles and other signs of physics beyond the Standard Model, and work on detector calibration and track reconstruction.

In 2012, ATLAS and its sister experiment CMS discovered the Higgs boson,2 the particle tied to the field that gives other fundamental particles their mass. It completed the Standard Model of particle physics, but the Standard Model still can't explain dark matter or why the universe is made of matter rather than antimatter. So ATLAS also hunts for new particles that could. ATLAS sees up to 1.7 billion proton collisions a second, and its trigger system keeps only the most promising: roughly one in a million.3

ATLAS event display: four red muon tracks leaving the collision point through the detector.
A Higgs boson candidate decaying through two Z bosons into four muons (red), recorded by ATLAS on 10 June 2012. The four muons together have a mass of 125 GeV, the mass of the Higgs boson. Image: ATLAS Collaboration, CC BY-SA 3.0, via Wikimedia Commons

How it works

Protons collide at the centre of ATLAS. Charged particles curve through the inner tracker, the calorimeters stop most of them and measure their energy, and a muon carries on to the outer muon chambers. Muon chambers Calorimeters Inner tracker Proton beams → ← Proton beams Muon Charged particle 1 2 3
AI-rtistic interpretation. The numbers match the steps.
  1. Protons collide

    Beams of protons from the Large Hadron Collider collide at the centre of ATLAS.

  2. Tracks are recorded

    Charged particles curve in the 2-tesla field of a solenoid magnet,4 and the inner tracker records their paths. The curvature gives their momentum. SFU helps build the new tracker.

  3. Energy is measured

    Calorimeters stop almost all particles and measure their energy. Muons get through and are measured again in the muon chambers; neutrinos escape unseen, showing up as missing momentum.

Video: CERN, 2016 · Watch on YouTube

Step inside ATLAS

A 360° look around the detector in its cavern, 100 metres below CERN. Drag the video, or move your phone, to look in any direction.

Video: CERN, edited by Prof. Bernd Stelzer to add the SFU Tier-1 centre, from his YouTube channel QuantumBernd · Watch on YouTube

From collision to data centre

Follow the data from the ATLAS and CMS detectors to the computers that store and analyze it, including the ATLAS Tier-1 centre here at SFU.

More about ATLAS computing at SFU →

Open to students

Research areas

Graduate students join the team's work in these areas, and usually combine a physics analysis with work on the detector itself.

  • The Higgs boson and new particlesMeasuring the properties of the Higgs boson and searching for new particles, such as long-lived particles or heavy resonances, often with machine learning.
  • Calibration and trackingCalibrating how the detector measures jets of particles, identifying tau leptons, and reconstructing the tracks of charged particles.
  • Building the new trackerAssembling and testing tracker petals for the High-Luminosity LHC with the SFU and TRIUMF team. More below.
  • Computing at scaleRunning analyses over petabytes of data on the ATLAS Tier-1 centre and national supercomputers.
~100of the 400 petals worldwide

The new ATLAS Inner Tracker (ITk)

For the High-Luminosity LHC, which is due to start around 2030 with about ten times as many collisions,5 ATLAS is replacing its whole inner detector with a new all-silicon tracker. The SFU and TRIUMF team was the first to produce a petal for installation (a wedge of silicon strip sensors for the tracker's end-caps) and plans to make about 100 of the 400 petals being produced worldwide.6

Video: Prof. Bernd Stelzer, from his YouTube channel QuantumBernd · Watch on YouTube

A petal up close

A look at an ITk petal: a wedge of silicon strip sensors, one of about 100 that the SFU and TRIUMF team is building for the new tracker's end-caps.

Where things stand

  1. 2008The LHC's first proton beams circulate, with ATLAS complete and ready.7
  2. 2010First collisions at 7 TeV, a record energy at the time.8
  3. July 2012ATLAS and CMS announce the discovery of the Higgs boson.2
  4. 2015–2018Run 2, at 13 TeV.9
  5. 2022–2026Run 3, at a record 13.6 TeV, ends on 27 June 2026 with ATLAS's largest dataset yet.10
  6. NowA long shutdown: ATLAS is being taken apart and rebuilt for the High-Luminosity LHC, and the first petals are going into the new tracker's end-caps. Meanwhile, the Run 3 data are analyzed.
  7. 2030Beams return for the High-Luminosity LHC, with about ten times as many collisions over its lifetime.5
46 mlong and 25 m across1
7,000 tabout the weight of the Eiffel Tower1
100 munderground, in a cavern at CERN1
The blue IceCube Laboratory building on stilts on the flat Antarctic snow, with a large orange hose reel for the drill in the foreground.

In the Antarctic ice, at the South Pole

IceCube

The IceCube Neutrino Observatory: a cubic kilometre of ice turned into a neutrino telescope.

Photo: the IceCube Lab at the South Pole, with the hose reel used for drilling. U.S. Geological Survey, public domain, via USGS

IceCube is P‑ONE's older sibling: the same idea, in ice instead of seawater. SFU's Professor Darren Grant was spokesperson of the IceCube Collaboration from 2017 to 2021,2 and also works on P‑ONE.

Neutrinos barely interact with matter, so they reach us straight from the most violent places in the universe, such as the surroundings of supermassive black holes, without being absorbed or deflected. IceCube was the first detector to see high-energy neutrinos from beyond our solar system, opening up neutrino astronomy.3 Its densely instrumented DeepCore region, and now the Upgrade, also make it a precision experiment on the neutrinos themselves.

The IceCube Lab lit red by its safety lights under a starry polar night sky, with the Milky Way overhead and green aurora to the right.
The IceCube Lab in the South Pole winter, under the Milky Way and the southern lights. The sensors are buried in the ice below. Photo: John Hardin, CC BY 4.0, via Wikimedia Commons

How it works

A neutrino coming up through the Earth interacts deep in the Antarctic ice and makes a muon. The muon gives off Cherenkov light, which the nearby optical modules on strings frozen into the ice detect. Their signals go up the cables to the IceCube Lab on the surface. Antarctic ice IceCube Lab Neutrino (invisible) Muon Cherenkov light 1,450 m Optical modules 2,450 m 1 2 3
AI-rtistic interpretation, not to scale. The numbers match the steps.
  1. A neutrino interacts

    Now and then a neutrino interacts in the ice or the rock below, producing charged particles such as a muon. Many come up through the Earth, which blocks every other kind of particle.

  2. Light is made

    Those particles travel faster than light does in ice, so they give off faint blue Cherenkov light, which carries far through the deep, very clear ice.

  3. Modules detect it

    Each optical module records the light with a 25 cm photomultiplier tube,1 then digitizes and time-stamps it and sends it up the cable to the IceCube Lab on the surface.

Video: Vedant Basu and Jennifer Wang, IceCube/NSF

Drilling into the South Pole

This time-lapse shows the drill site being moved into position at the South Pole for the IceCube Upgrade. Crews used a 5-megawatt hot-water drill to melt holes about 2.4 km deep into the ice, about three days per hole,7,8 then lowered the new strings of sensors into them before the water froze again.

Open to students

Research areas

Students join an international collaboration of more than 450 people from 58 institutions in 14 countries,6 working in areas like these.

  • Neutrino astronomyFinding the sources of high-energy cosmic neutrinos, such as the active galaxy NGC 1068, alone or with telescopes that see light and gravitational waves.
  • Neutrino oscillationsMeasuring how neutrinos made in the atmosphere change type as they cross the Earth, with DeepCore and the new Upgrade.
  • Dark matter and new physicsSearching neutrino data for signs of dark matter and other physics beyond the Standard Model.
  • Reconstruction and calibrationWorking out each neutrino's direction and energy from the light in the sensors, often with machine learning, and mapping how light travels through the ice. More below.
600+new sensors and calibration devices

The IceCube Upgrade

In the 2025/26 South Pole season, five new strings went into the ice at the bottom centre of IceCube, far more densely instrumented than the originals. Their new sensors, including multi-photomultiplier modules, are two to three times as sensitive. The Upgrade will sharpen measurements of neutrino oscillations, and its calibration devices will map the ice so precisely that 15 years of archived data can be reanalyzed. It also tests sensor designs for IceCube-Gen2.7

Where things stand

  1. December 2010The 86-string detector is completed at the South Pole.1
  2. 2013First evidence of high-energy neutrinos from beyond the solar system.3
  3. 2018A neutrino is traced to a flaring blazar, TXS 0506+056: the first evidence of a source.4
  4. 2022Evidence of neutrinos from the active galaxy NGC 1068.5
  5. 2025/26The IceCube Upgrade: five new, densely instrumented strings with more than 600 new sensors and calibration devices, at the bottom centre of the detector.7
  6. October 2026Francis Halzen, IceCube's principal investigator, receives the Nobel Prize in Physics.9
  7. NowCommissioning the Upgrade's new instruments, which will sharpen oscillation measurements and how well the ice is understood.
  8. After thatThe proposed IceCube-Gen2, with eight times IceCube's instrumented volume.7
1 km³of ice instrumented with sensors1
5,160optical modules on 86 strings1
1,450–2,450 mdepth of the sensors1
A tall metal frame holding the coiled P-ONE detector line being lowered into the water between two docks.

In the deep Pacific, off Vancouver Island

P‑ONE

The Pacific Ocean Neutrino Experiment: a planned neutrino telescope anchored to the deep seafloor.

Photo: the first P-ONE line being lowered for testing at Granville Island, June 2026. Simon Fraser University, from SFU News

SFU's Professor Matthias Danninger is the scientific spokesperson of the P‑ONE collaboration.1,2 SFU also built precision calibration detectors and high-power light emitters that measure how light travels through the seawater.

P‑ONE uses the same technique as IceCube, but in the deep ocean. Its site in the northeast Pacific sees a different part of the sky to IceCube, so the two complement each other, and it can plug into Ocean Networks Canada's existing seafloor network for power and data.3 The ocean also brings its own challenges: the lines sway in the currents, and the water glows faintly from radioactive potassium and bioluminescent sea life.3

Glass sphere optical modules on the P-ONE line, seen just below the water surface.
Modules on the first line under water during the June 2026 test. Each optical module's glass sphere holds 16 small photomultiplier tubes, eight in each half, that pick up faint flashes of light.4 Photo: Simon Fraser University, from SFU News

How it works

A neutrino interacts in the water and makes a muon. The muon gives off Cherenkov light, which forms a cone behind it, and the optical modules inside the cone detect the light. Neutrino (invisible) Muon Cherenkov light Optical modules 1 2 3
AI-rtistic interpretation. The numbers match the steps.
  1. A neutrino interacts

    Now and then a neutrino interacts in the seawater or the seafloor rock, producing charged particles such as a muon.

  2. Light is made

    Those particles travel faster than light does in water, so they give off faint blue Cherenkov light in a cone, at about 42° to their path.

  3. Modules detect it

    Optical modules spaced along mooring lines about one kilometre long pick up the light.2 When and where it arrives shows the particle's direction and energy.

Video: SFU Communications & Marketing, from SFU News

Watch the first line go into the water

In June 2026, P‑ONE‑1 was lowered into the harbour at Granville Island in Vancouver for its last test before deployment. It spent more than 12 hours in cold seawater, and every system worked.6

Read the Q&A: what is a neutrino telescope, and why was one tested in a Vancouver harbour? →

Open to students

Research areas

P‑ONE is a young experiment, so students help shape it: from building hardware to simulating the detector and analyzing its very first data.

  • CalibrationBuilding precision detectors and high-power light emitters that measure how light travels through the seawater.
  • Acoustic positioningTracking where every module is as the lines sway in the currents, using sound signals from transceivers on the seafloor.
  • Ocean backgroundsModelling the faint glow from potassium-40 and bioluminescent sea life, so it can be told apart from neutrino signals.
  • Building the linesTesting components and assembling detector lines in the TRIUMF cleanroom. More below.
TRIUMFwhere P‑ONE's lines are built

Building P‑ONE in Vancouver

P‑ONE's detector lines are put together in the cleanroom at TRIUMF, Canada's particle accelerator centre, where SFU group members work on hardware, integration and assembly. Parts arrive from Canada, the US and Europe, including SFU's calibration instruments. Each one is tested, then mounted on the kilometre-long backbone cable, and every power and optical-fibre connection is checked as the line comes together. P‑ONE‑1 was completed this way in April 2026.5 Next, the demonstrator's four lines will be assembled and tested at TRIUMF in 2027–2028.

Where things stand

  1. April 2026The first line, P‑ONE‑1, is fully assembled and integrated in the cleanroom at TRIUMF.5
  2. June 2026Wet test at Granville Island in Vancouver: over 12 hours in cold seawater, with every system working.6
  3. NextDeployment about 2,700 metres down in the Cascadia Basin, on a new 30 km cable extension from Ocean Networks Canada's NEPTUNE observatory.2,6 Data-taking starts straight away.
  4. 2027–2028The four lines of a demonstrator are assembled and tested at TRIUMF.
  5. After thatIf funded, a full detector of around 100 lines.2
~2,700 mdepth of the seafloor at the site2
~1 kmlength of each line; the first carries 20 modules4
4lines in the planned demonstrator

SFU and TRIUMF

TRIUMF, Canada's particle accelerator centre in Vancouver, began in 1968 as the TRI-University Meson Facility of UBC, the University of Victoria and SFU. SFU is still one of its 21 member universities,1 and the group works with TRIUMF on two of its three experiments.

ATLAS

Canada's ATLAS Tier-1 data centre was at TRIUMF from 2007 to 2018, then moved to SFU's Burnaby campus in 2019, where TRIUMF runs it.2 A consortium of ten institutions led by SFU and TRIUMF operates it, and it supplies about 10% of ATLAS's Tier-1 computing worldwide.2,3 SFU and TRIUMF also build petals together for the new ATLAS tracker.4

The new tracker   Computing at SFU

P‑ONE

P‑ONE's detector lines are assembled and tested in TRIUMF's cleanroom: P‑ONE‑1 in 2026, and the demonstrator's lines in 2027–2028.5 TRIUMF also provides site infrastructure in Vancouver, and P‑ONE's data acquisition system is largely a TRIUMF deliverable.6

Building the lines at TRIUMF

Want to work on ATLAS, IceCube or P‑ONE?

Students in the group analyze data, build detectors and learn large-scale computing.

How to join