Title of article
Measurement of 222Rn dissolved in water at the Sudbury Neutrino Observatory
Author/Authors
Blevis، نويسنده , , I and Boger، نويسنده , , J and Bonvin، نويسنده , , E and Cleveland، نويسنده , , B.T and Dai، نويسنده , , X and Dalnoki-Veress، نويسنده , , F and Doucas، نويسنده , , G and Farine، نويسنده , , J and Fergani، نويسنده , , H and Grant، نويسنده , , D and Hahn، نويسنده , , R.L and Hamer، نويسنده , , A.S and Hargrove، نويسنده , , C.K and Heron، نويسنده , , H and Jagam، نويسنده , , P and Jelley، نويسنده , , N.A and Jillings، نويسنده , , C and K، نويسنده ,
Pages
15
From page
139
To page
153
Abstract
The technique used at the Sudbury Neutrino Observatory (SNO) to measure the concentration of 222Rn in water is described. Water from the SNO detector is passed through a vacuum degasser (in the light water system) or a membrane contact degasser (in the heavy water system) where dissolved gases, including radon, are liberated. The degasser is connected to a vacuum system which collects the radon on a cold trap and removes most other gases, such as water vapor and N2. After roughly 0.5 tonnes of H2O or 6 tonnes of D2O have been sampled, the accumulated radon is transferred to a Lucas cell. The cell is mounted on a photomultiplier tube which detects the α-particles from the decay of 222Rn and its progeny. The overall degassing and concentration efficiency is about 38% and the single-α counting efficiency is approximately 75%. The sensitivity of the radon assay system for D2O is equivalent to ∼3×10−15 g U/g water. The radon concentration in both the H2O and D2O is sufficiently low that the rate of background events from U-chain elements is a small fraction of the interaction rate of solar neutrinos by the neutral current reaction.
Keywords
RADON , Radioactivity assay , Solar neutrino , SnO
Journal title
Astroparticle Physics
Record number
2022210
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