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H₂, CO, and CO₂ — The Gas Signature of Early-Stage Thermal Runaway

By Engineering — Sensing · May 21, 2026 · 8 min read

The gas-phase signature of a stressed Li-ion cell has a specific order and a specific tempo. Knowing it tells you what to sense, where, and when.

Peer-reviewed work on Li-ion off-gas signatures has converged on a consistent picture in the last five years. Electrolyte VOCs come first, then hydrogen as the SEI breaks down, then CO and CO₂ as the runaway propagates, then HF as the electrolyte salt decomposes. The sequence is the detector's map.

The signature in order

  • Carbonate solvent VOCs (DMC, EMC, EC) — first to appear, dominated by the electrolyte composition.
  • H₂ — released as the solid-electrolyte interphase breaks down, before any visible smoke.
  • CO and CO₂ — produced as the organic electrolyte decomposes at higher temperature.
  • HF — onset roughly coincident with the first audible vent, often the lethal exposure for crew.

Why H₂ is the most useful primary

Hydrogen is small, fast-diffusing, and not present in significant background concentration on a vehicle deck. Catalytic and electrochemical H₂ sensors with ppm-level sensitivity exist at marine-rated prices. The detection window is wide enough to catch the event before audible venting in bench conditions.

~2–8 min
H₂ lead time over visible smoke (bench, sealed chamber)
< 5 ppm
Sensor sensitivity required for early-stage detection
< 1 min
HF onset relative to first audible vent — too late for crew action

Where gas-only fails on a vehicle deck

Mechanical ventilation, large open volumes, and the residual VOC background from cold ICE engines means a deck-level H₂ trip can be late or absent at typical ventilation rates. The detection architecture has to either localise the sensor close to the source (impractical at scale) or fuse gas signal with thermal signal. We do the second.

Gas sensing is information, not localisation. It tells you the deck has a problem. Thermal sensing tells you which vehicle. The fusion of both is the layer that holds up at sea.
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