Cryogenic Dark Matter Search Detector (CDMS)

A crystal cooled to one-hundredth of a degree above absolute zero, waiting in a former iron mine for a particle that has never been confirmed to exist.

The CDMS detectors record two independent signals whenever a particle collides inside them: the phonon energy (heat vibrations spreading through the crystal lattice) and the ionisation energy (free electrons and holes pulled through the crystal by an electric field). The ratio of these two signals cleanly separates nuclear recoils — the expected signature of a WIMP — from electron recoils caused by ordinary radioactive backgrounds. This dual-channel discrimination lets the experiment reject nearly all backgrounds on an event-by-event basis, rather than relying on shielding alone.

Each detector is a disk of high-purity germanium or silicon, 100 mm in diameter and 33 mm thick, cooled to roughly 15–50 mK inside a dilution refrigerator. Superconducting tungsten Transition Edge Sensors (TES) patterned photolithographically on both faces of the disk measure athermal phonons with eV-scale resolution. Interleaved photolithographic channels on the same faces collect ionisation charge. An applied electric field of a few to ~100 volts drifts charge carriers toward the collection electrodes; in the high-voltage (HV) operating mode the drifting charges generate additional Neganov–Trofimov–Luke phonons, amplifying the phonon signal and pushing the recoil threshold down toward 40–100 eV. A coincidence veto from surrounding shields and a 2-km overburden of rock suppress cosmic-ray muons to negligible levels.

In plain terms

Imagine a super-cold gem buried deep underground that can feel the difference between a feather tickling it and a gust of wind. It is waiting for an invisible particle from space to tap a single atom inside — and the faint warmth and tiny electric spark from that tap together identify what kind of thing hit it.

Also called: CDMS, SuperCDMS, iZIP detector, CDMSlite.

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A short history

The CDMS programme grew out of 1980s work at Stanford on cryogenic calorimeters. CDMS I ran at the shallow Stanford Underground Facility (17 mwe) from 1998 to 2002, demonstrating the dual phonon–ionisation technique in germanium and silicon. CDMS II relocated in 2003 to the Soudan Underground Laboratory in northern Minnesota (2090 mwe), operating a two-tower array of six germanium and six silicon detectors. Results published in 2004, 2009, and 2011 progressively set the world's best spin-independent WIMP–nucleon cross-section limits for WIMP masses above roughly 10 GeV/c². A 2013 silicon analysis with 140 kg-days of exposure found three WIMP-candidate events (expected background 0.41 events), stimulating substantial theoretical interest. SuperCDMS Soudan followed from 2011 to 2015 with improved 600-gram iZIP detectors, pioneering the CDMSlite low-threshold mode. The current phase, SuperCDMS SNOLAB, is being assembled 2 km underground at SNOLAB in Sudbury, Canada, with commissioning of 24 full-size detectors progressing in 2025–2026.

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