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  1. H150 博物館
  2. H150b 紀要
  3. 名古屋大学博物館報告
  4. 21

島根県仁多郡東出雲町横田地域の土壌の化学組成とたたら製鉄の関係

https://doi.org/10.18999/bulnum.021.03
6308d0f8-6426-432b-a4ef-adf2c5ca63eb
名前 / ファイル ライセンス アクション
bulnum_21_33.pdf bulnum_21_33.pdf (476.6 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2006-04-14
タイトル
タイトル 島根県仁多郡東出雲町横田地域の土壌の化学組成とたたら製鉄の関係
その他のタイトル
その他のタイトル The relation between the geochemistry of stream sediments and development of Tatara iron making in Yokota, Oku-Izumo, Shimane, Japan
著者 武邊, 勝道

× 武邊, 勝道

WEKO 11975

武邊, 勝道

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TAKEBE, Masamichi

× TAKEBE, Masamichi

WEKO 11976

TAKEBE, Masamichi

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鶴留, 浩和

× 鶴留, 浩和

WEKO 11977

鶴留, 浩和

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TURUDOME, Hirokazu

× TURUDOME, Hirokazu

WEKO 11978

TURUDOME, Hirokazu

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赤川, 史典

× 赤川, 史典

WEKO 11979

赤川, 史典

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AKAGAWA, Fuminori

× AKAGAWA, Fuminori

WEKO 11980

AKAGAWA, Fuminori

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山本, 鋼志

× 山本, 鋼志

WEKO 11981

山本, 鋼志

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YAMAMOTO, Koshi

× YAMAMOTO, Koshi

WEKO 11982

YAMAMOTO, Koshi

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吉田, 英一

× 吉田, 英一

WEKO 11983

吉田, 英一

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YOSHIDA, Hidekazu

× YOSHIDA, Hidekazu

WEKO 11984

YOSHIDA, Hidekazu

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抄録
内容記述 It is known that the technology and culture of “Tatara iron making” have developed in Okuizumo,
Shimane, Japan from ancient time. In order to clarify the relation between the development of
Tatara iron making and geochemical feature in the region, this study analyzed the chemistry of
stream sediments in Yokota, Okuizumo and made geochemical maps. The research area consists
mainly of felsic igneous rocks. The igneous rocks extend from northeast to southwest and show
parallel distribution with a few kilometers in width. The distribution of these rocks affects the
element compositions of stream sediments. The sediments from area, in which the Yokota
granodiorite is distributed, show high concentrations of Fe, MgO and CaO and low concentrations
of SiO2. The sediments from area composed of the other rocks show opposite geochemical features.
Stream sediments from Yokota area are entirely characterized by high Fe concentration. The average
Fe concentration is 7.1% and some samples show higher Fe concentration than 15%. The average
concentration is higher than twice of Fe concentration of JG-1a, JG-2, and JG-3. Samples, of which
magnetic component are removed, show lower Fe concentration than that of bulk ones. The removed
components of the samples show X-ray diffraction patterns with peaks of magnetite and hematite.
Therefore, the high Fe contents of the stream sediments are ascribed to high content of magnetite,
which is principal mineral for Tatara iron making. The enrichment of magnetite in Yokota may
play an important role in development of the industry. While, there is no distinct relation between
the distributions of Fe concentration and Tatara ruins in Yokota, suggesting additional requirements
for the development of Tatara iron making.
内容記述タイプ Abstract
内容記述
内容記述 国立情報学研究所で電子化したコンテンツを使用している。
内容記述タイプ Other
出版者
出版者 名古屋大学博物館
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
ID登録
ID登録 10.18999/bulnum.021.03
ID登録タイプ JaLC
ISSN(print)
収録物識別子タイプ ISSN
収録物識別子 13468286
書誌情報 名古屋大学博物館報告

巻 21, p. 33-41, 発行日 2005
フォーマット
application/pdf
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/6330
識別子タイプ HDL
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