Chlorine-36 in granite samples from the Hiroshima A-bomb site

Abstract

36 Cl is a long-lived radioisotope, which, because it is created mainly through a thermal neutron capture process by 35 Cl, may be used to estimate the strength of thermal neutron flux from A-bombs or nuclear fuel facilities. The 36 Cl contents in granite samples from the Hiroshima A-bomb site have been measured by the Cl-36 accelerator mass spectrometry (AMS) system at the University of Tsukuba. The 36 Cl/Cl ratios deduced from the 36 Cl measurements are compared with independent evaluations based upon the Dosimetry System 2002 (DS02) of the radiation doses received by the survivors of the Hiroshima A-bomb. The measurements corresponded well up to a ground distance of 1100 m, which proved the effectiveness of the DS02. Measurements of the 36 Cl/Cl ratio of unexposed granite samples were 1.92 × 10 −13 on average, and because the measured ratio for samples at a ground distance of 1163 m was 2.50 × 10 −13 , the assessment of the neutron flux by the 36 Cl measurements of samples beyond about 1100 m is not practical. This limitation arises from the inability to distinguish bomb-induced Cl-36 from activation due to ambient sources.