Hostname: page-component-848d4c4894-wg55d Total loading time: 0 Render date: 2024-05-28T23:22:51.738Z Has data issue: false hasContentIssue false

University of Tokyo Radiocarbon Measurements V

Published online by Cambridge University Press:  18 July 2016

Hiromi Kobayashi
Affiliation:
Carbon Dating Laboratory, University of Tokyo, Tokyo, Japan†
Taeko Hirose
Affiliation:
Carbon Dating Laboratory, University of Tokyo, Tokyo, Japan†
Miyoi Sugino
Affiliation:
Carbon Dating Laboratory, University of Tokyo, Tokyo, Japan†
Naotune Watanabe
Affiliation:
Carbon Dating Laboratory, University of Tokyo, Tokyo, Japan†
Rights & Permissions [Opens in a new window]

Extract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Most of the 14C measurements reported here were made between August 1970 and August 1972. Chemical treatment of samples and counting technique remain as described previously (R, 1968, v 10, p 144–148; 1971, v 13, p 97–102). We have added Houtermans-Oeschger type multi-anode anticoincidence gas proportional counter, manufactured by Tokyo Atomic, Japan. The central counter tube, which has several small holes, 5mm diam, is made of aluminized polyethylene foil, 0.06mm thick, with 72mm inside diam and 300mm sensitive length. The external counter tube is made of stainless steel 4mm thick, with 93mm inside diam and 350mm length. The anode wires of both counters are also made of stainless steel 0.05mm diam. The counters are surrounded by a paraffin shield 50mm thick and encased in a 250mm shield of steel on all sides. Acetylene is used as the counting gas at 753.3mm Hg (22 ± 1°C). Counting rates of background and 95% activity of NBS oxalic acid standard were 1.25 ± 0.02cpm and 14.39 ± 0.12cpm, respectively.

Type
Research Article
Copyright
Copyright © The American Journal of Science 

References

Broecker, W S et al., 1968, Milankovich hypothesis supported by precise dating of coral reefs and deep-sea sediments: Science, v 159, p 297300.Google Scholar
Egami, N, Fukai, S, and Masuda, S, 1965, Dailaman I; 1966, Dailaman II: Inst Oriental culture, Univ Tokyo.Google Scholar
Fukai, S and Ikeda, J, 1971, Dailaman IV: Inst Oriental culture, Univ Tokyo.Google Scholar
Izumi, S and Terada, K, 1972, Excavation at Kotosh, Peru, 1963 and 1966, Univ Tokyo.Google Scholar
Kigoshi, Kunihiko, 1967, Gakushuin natural radiocarbon measurements VI: Radiocarbon, v 9, p 4362.Google Scholar
Kobayashi, H, Matsui, Y, and Suzuki, H, 1971, University of Tokyo radiocarbon measurements IV: Radiocarbon, v 13, p 97102.CrossRefGoogle Scholar
Núñez, A L, 1965, Estudios arqueologicos, v 1, Univ Chile.Google Scholar
Sato, J, Sato, T, Otomori, Y, and Suzuki, H, 1969, University of Tokyo radiocarbon measurements II: Radiocarbon, v 11, p 509514.CrossRefGoogle Scholar
Segerstrom, K, 1964, Quaternary geology of Chile: brief outline: Geol Soc America Bull, v 75, p 157170.Google Scholar
Sono, T and Fukai, S, 1968, Dailaman III: Inst Oriental culture, Univ Tokyo.Google Scholar
Suzuki, H and Takai, F (ed), 1973, The Palaeolithic site at Douara cave in Syria, p 143150.Google Scholar
Yamasaki, F, Hamada, T, and Fujiyama, C, 1964, RIKEN natural radiocarbon measurements I: Radiocarbon, v 6, p 112115.Google Scholar
Yamasaki, F, Hamada, T, and Fujiyama, C, 1966, RIKEN natural radiocarbon measurements II: Radiocarbon, v 8, p 324339.Google Scholar