Isotopic Anomalies of Xenon from Tellurium minerals
スポンサーリンク
概要
- 論文の詳細を見る
Xenon extracted from old tellurium minerals were analyzed with a high-sensitivity mass spectrometer. Old tellurium minerals of different four localities were used in the experiments, that is, tetradymite(Bi<SUB>2</SUB> Te<SUB>2</SUB>S)from the Oya mine, tellurobismuthite(Bi<SUB>2</SUB> Te<SUB>3</SUB>)from the Suwa mine, tellurium mineral(AgAuTe+Te)from the Rendai-ji mine and native tellurium(Te)from the Teine mine. In heating the sample minerals, the temperature was raised stepwise typically by100°C and kept constant for a hour. Rare gases extracted at step of extraction temperature were purified and then sealed up in the respective ampoul. Large excesses in<SUP>129</SUP>Xe, <SUP>130</SUP>Xe and<SUP>131</SUP>Xe extracted from the Oya tellurium mineral and in<SUP>130</SUP>Xe from the Suwa tellurium mineral were found definitely. Their origins were discussed on the basis of the isotopic amonalies patterns as well as experimental and theoretical considerations on the nuclear reaction relating to the relevant isotopis of xenon. The<SUP>130</SUP>Xe-excess was attributed to doubleβ-decay of<SUP>130</SUP>Te. A mall excess in<SUP>128</SUP>Xe was interested in relation to double β-decay of<SUP>128</SUP>Te. Several nuclear processes which could contribute to<SUP>128</SUP>Xe were discussed on the available data. Concerning the isotopic amonalies in<SUP>129</SUP>Xe and<SUP>131</SUP>Xe, the ratio <SUP>129</SUP>Xe-excess/<SUP>130</SUP>Xe-excess(m=129 and 131)seems to decrease and the ratio<SUP>129</SUP>Xe-excess/<SUP>131</SUP>Xe-excess seems to increase with the increasing tellurium concentration for the Oya tellurium minerals. We may be able to look for a solution of the amonalies in either the epithermal neutron captures on<SUP>128</SUP>Te and on<SUP>130</SUP>Te or both the(μ<SUP>-</SUP>, n)reaction of<SUP>130</SUP>Te and the themal neutron captures on<SUP>128</SUP>Te and on<SUP>130</SUP>Te, where the neutrons can be produced by the(μ<SUP>-</SUP>, n)reactions and the(α, n)recations on the environmental rocks. In order to understand the above results on the ratio between Xe-excess, we may have to take into account the competition process between between the neutron captures on<SUP>128</SUP>Te and on<SUP>130</SUP>Te and the neutron adsorptions by the associated impurities, and the(a, n)reactions on<SUP>126</SUP>Te and on<SUP>128</SUP>Te respectively.
- 日本質量分析学会の論文
著者
-
Ogata K
Department Of Applied Biochemistry Faculty Of Applied Biological Science Hiroshima University
-
Takaoka N.
Department Of Earth And Planetary Sciences Faculty Of Science Kyushu University
-
Takaoka N
Department of Physics, Faculty of Science Osaka University
関連論文
- Noble gases in the Kobe CK4 carbonaceous chondrite
- Isotopic Anomalies of Xenon from Tellurium minerals