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Abstract
First operational results from the Homestake chlorine experiment: 615 tons of tetrachloroethylene 1,478 m underground, sensitive to the reaction νe + ³⁷Cl → ³⁷Ar + e⁻. The measured capture rate is approximately 2.5 solar-neutrino units, significantly below the Standard Solar Model prediction of roughly 8 SNU.
Significance in the evidence base
First announcement of the solar neutrino deficit — the 'solar neutrino problem' — which persisted for thirty years and drove theoretical work on both solar physics and neutrino oscillation. Resolved in 2001 by SNO's measurement of the total flavor-summed solar flux.
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The chlorine technique
The reaction proposed by Pontecorvo in 1946, , has a threshold of 0.814 MeV, making it sensitive to the high-energy tail of the solar neutrino spectrum — primarily B and CNO-cycle neutrinos. The daughter Ar decays back to Cl with a 35-day half-life by electron capture, releasing 2.82 keV Auger electrons that can be counted in a low-background proportional chamber.
Davis’s approach was to run the target — tetrachloroethylene (C₂Cl₄, used commercially as cleaning fluid) — for ~2 months, then sweep the dissolved argon out of the tank with helium, cryogenically trap it, and count the Ar decays over the following months in a shielded low-activity proportional counter.
The 1968 result
Three runs completed in the 1967–1968 period gave a measured capture rate of roughly Ar atoms per day, corresponding to solar-neutrino units (1 SNU = captures per target atom per second). John Bahcall’s contemporaneous Standard Solar Model predicted approximately 8 SNU.
The factor-of-three discrepancy was immediately recognized as either:
- A solar-physics problem: the central solar temperature might be lower than assumed, suppressing B production
- A particle-physics problem: solar might transform into something the detector could not see
- An experimental problem: subtle systematics in the extraction or counting
Option 3 was methodically excluded by repeated cross-checks and refinements. Options 1 and 2 remained live for three decades.
Three decades of puzzle
Davis continued the measurement at Homestake for nearly thirty years, refining systematics and accumulating runs. The deficit persisted at about one-third of the Standard Solar Model prediction, robust to all experimental improvements.
Independent experiments using different targets — SAGE and GALLEX with gallium (sensitive to lower-energy pp neutrinos), Kamiokande and Super-Kamiokande with water Cherenkov detectors — each also found deficits, though with different magnitudes reflecting their different energy ranges.
The pattern — deficit present at all energies but with energy-dependent magnitude — was eventually recognized as the signature of MSW oscillation in the Sun.
Resolution
The 2001–2002 SNO measurements, enabled by a heavy-water target that could separate charged-current from neutral-current channels, showed that the total flavor-summed B neutrino flux matched the Standard Solar Model. The electron-neutrino fraction was about one-third — perfectly consistent with the deficit Davis had measured for thirty years. Two-thirds of the solar had transformed into and in flight.
Davis received the 2002 Nobel Prize in Physics, sharing it with Masatoshi Koshiba (Kamiokande) and Riccardo Giacconi (X-ray astronomy). He was 88 at the time of the award.
The Homestake measurements remain the canonical example of how a persistent, carefully controlled experimental anomaly can eventually force a rewriting of fundamental physics — in this case the recognition that neutrinos have mass.