著者

永田 和宏 松原 章浩 國分(齋藤) 陽子 中村 俊夫

出版者

一般社団法人 日本鉄鋼協会

雑誌

鉄と鋼 (ISSN:00211575)

巻号頁・発行日

vol.102, no.12, pp.736-741, 2016 (Released:2016-11-30)

参考文献数

15

被引用文献数

2 2

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Steel of Japanese swords has been produced with Tatara process from iron sand and charcoal. Carbon dissolved in steel was absorbed from wooden charcoal fuel during the production of the steel. From the decay of 14C activity in the steel, the 14C age of Japanese sword can be determined. The 14C ages of 4 Japanese swords were measured with accelerator mass spectrometry and calibrated to calendar years. Each 14C age provided plural calendar year periods with definite probabilities, and one of the periods agreed with the production year of each sword that was determined from the sword master’s name cut in the grip of his sword after taking the age range of charcoal used for steel production and usage for several generations of the same names of sword masters into account.

著者

生田 正文 丹羽 正和 檀原 徹 山下 透 丸山 誠史 鎌滝 孝信 小林 哲夫 黒澤 英樹 國分(齋藤) 陽子 平田 岳史

出版者

一般社団法人 日本地質学会

雑誌

地質学雑誌 (ISSN:00167630)

巻号頁・発行日

vol.122, no.3, pp.89-107, 2016-03-15 (Released:2016-06-21)

参考文献数

67

被引用文献数

11

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既往文献の火山ガラス屈折率データからは識別が困難であった桜島の歴史時代の噴火(文明,安永,大正)軽石について,本研究では火山ガラスの水和部と未水和部とを区別して屈折率測定を行い,斜方輝石の屈折率も含めてそれぞれの軽石に違いがあることを見出した.一方,宮崎平野南部で掘削したコアに含まれる軽石濃集層に対して鉱物組成分析,火山ガラスの形態分類や屈折率測定,斜方輝石の屈折率測定,および炭質物の放射性炭素年代測定を行い,本研究による歴史時代の桜島噴火起源の軽石の分析と比較した.また,それぞれの火山ガラスについてレーザーアブレーション誘導結合プラズマ質量分析法による主成分・微量元素同時分析を行った.その結果,軽石濃集層は桜島文明テフラに対比されることが判明した.桜島文明テフラは,軽石の状態で宮崎平野南部まで到達していた可能性が高い.

著者

永田 和宏 古主 泰子 松原 章浩 國分(齋藤) 陽子 中村 俊夫

出版者

一般社団法人 日本鉄鋼協会

雑誌

鉄と鋼 (ISSN:00211575)

巻号頁・発行日

vol.105, no.4, pp.488-491, 2019 (Released:2019-03-31)

参考文献数

16

被引用文献数

1 1

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The Japanese nails had been produced by the traditional ironmaking way of Tatara until the Edo period since the late of 6 Century. The Tatara is characterized as the ironmaking using very fine iron sand as the resources and is distinguished from the pre-modern ironmaking way in Europe using lump iron ore. The quality of the Japanese nails is affected from steel produced by Tatara in each age. The 14C ages of 3 Japanese nails were measured with accelerator mass spectrometry and calibrated to calendar years. Each 14C age provided plural calendar year periods with definite probabilities, and one of the periods determined in comparison with the history of temples and their repair records. The production ages of nails used in the Daibutuden of the Todaiji temple, the living quarters of the Manshuin temple and the Zaoudo of the Yoshino-Kinpusenji temple are before 1692, the 12 Century and before 1592, respectively, when they were repaired or reconstructed.

著者

山田 隆二 木村 誇 苅谷 愛彦 佐野 雅規 對馬 あかね 李 貞 中塚 武 國分(齋藤) 陽子 井上 公夫

出版者

公益社団法人 砂防学会

雑誌

砂防学会誌 (ISSN:02868385)

巻号頁・発行日

vol.73, no.5, pp.3-14, 2021-01-15 (Released:2022-01-17)

参考文献数

46

被引用文献数

1

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Establishing chronologies for large-scale landslides is crucial to understand the cause of the mass movements and to take measures against potential hazards in future. We discuss the applicability of dating methods for determining landslide chronologies in relation to the type of samples and the stratigraphic setting of sampling location. Case studies are carried out with fossil wood samples buried in the deposits of large-scale landslides in two areas of the Japanese Alps region in historic times ; Dondokosawa rock avalanche (DRA) and Ohtsukigawa debris avalanche (ODA). Ages are determined by accelerator mass spectrometry radiocarbon dating and dendrochronological analysis using the oxygen isotope composition of tree ring cellulose. We report seven radiocarbon ages and five dendrochronology data for the wood samples taken from outcrops and excavated trenches in the lacustrine sediments of dammed lakes formed by DRA, and two radiocarbon ages and two dendrochronology data for wood samples of ODA. Two sets of data for DRA are crosschecked independently to ensure the accuracy of results. Most of ages in the DRA area are concordant with the period of AD 887 Ninna (Goki-Shichido) mega-earthquake as proposed in previous studies. In the ODA area, ages are not concentrated in a specific period. When the preservation condition of buried wood trunks is good enough to date the exact or approximate tree-death years dendrochronologically, it is possible to estimate landslide occurrence periods in further detail by comparing the landslide chronology with historical records of heavy rainfall and large earthquakes.