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  1. B. 理工学域; 数物科学類・物質化学類・機械工学類・フロンティア工学類・電子情報通信学類・地球社会基盤学類・生命理工学類
  2. b 20. 紀要
  3. The science reports of Kanazawa University(金沢大学理科報告)
  4. 49巻

Biomineralization of radioactive sulfide minerals in strong acidic Tamagawa Hot Springs

https://doi.org/10.24517/00011132
https://doi.org/10.24517/00011132
ece11efc-e1b7-47c7-aae9-11d9d2f68d0e
名前 / ファイル ライセンス アクション
AA00835991-49-01_02-001.pdf AA00835991-49-01_02-001.pdf (83.9 MB)
license.icon
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2017-10-03
タイトル
タイトル Biomineralization of radioactive sulfide minerals in strong acidic Tamagawa Hot Springs
言語
言語 eng
キーワード
主題Scheme Other
主題 Radioactive sulfides
キーワード
主題Scheme Other
主題 strong acidic hot springs
キーワード
主題Scheme Other
主題 high ƒタ-ray
キーワード
主題Scheme Other
主題 barite
キーワード
主題Scheme Other
主題 gypsum
キーワード
主題Scheme Other
主題 sulfur
キーワード
主題Scheme Other
主題 orpiment
キーワード
主題Scheme Other
主題 Hokutolite
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ departmental bulletin paper
ID登録
ID登録 10.24517/00011132
ID登録タイプ JaLC
著者 Tazaki, Kazue

× Tazaki, Kazue

WEKO 15698
e-Rad 80211358

Tazaki, Kazue

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Watanabe, Hiroaki

× Watanabe, Hiroaki

WEKO 17423

Watanabe, Hiroaki

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著者別表示 田崎, 和江

× 田崎, 和江

WEKO 164
e-Rad 80211358
研究者番号 80211358

田崎, 和江

Search repository
提供者所属
内容記述タイプ Other
内容記述 Department of Earth Sciences, Kanazawa University
提供者所属
内容記述タイプ Other
内容記述 Department of Earth Sciences, Kanazawa University
書誌情報 Science reports of the Kanazawa University = 金沢大学理科報告

巻 49, 号 1-2, p. 1-24, 発行日 2005-01-01
ISSN
収録物識別子タイプ ISSN
収録物識別子 0022-8338
その他の識別子
内容記述タイプ Other
内容記述 AA00835991
抄録
内容記述タイプ Abstract
内容記述 Bioaccumulation of radioactive sulfide minerals by bacteria in strong acidic hot spring water was found at Tamagawa Hot Springs, Akita prefecture in Japan. The hot spring water produces Hokutolite of radioactive minerals containing high radium and radon. The ƒタ-ray measurements of sediments and biofilms indicate 1850-2420 and 5700 cpm, respectively, which are 50-100 times higher than that of the water and the air (50-90 cpm). The characteristics of hot spring water show pH (1.2), Eh (140 mV), EC (29mS/cm), DO (0.8 mg/l), and water temperature (99.5 Ž), indicating extremely strong acidic and reducing conditions. The hot spring water contains mainly HCl associated with high concentrations of Ca^<2+>, Al^<3+>, Fe^<2+>, HSO_4 and SO_4^<2->. SEM-EDX and TEM demonstrate some insight into how microorganisms affect the chemistry and microbiological characteristics of the strong acidic surroundings with high S, As, Ba, and Ca contents in biofilms. Especially SEM-EDX, ED-XRF, and STEM-EDX elemental content maps illustrate the distribution of sulfur-bearing compounds of barite (BaSO_4), gypsum (CaSO_4 E2H_2O), elemental sulfur (S) and orpiment (As_2S_3) in the reddish orange biofilms. The presence of a hydrogen sulfide-rich (H_2S) thermal spring and gypsum deposits suggest the volatilization of H_2S from the spring water, oxidation of the H_2S gas to sulfuric acid, and reaction of the sulfuric acid. TEM micrographs of bacteria in the biofilms reveal in detail the intimate connections between biological and mineralogical processes that the cells are entirely accumulated with spherical grains, 100 `200 nm in diameter. The relationship among sulfide minerals, such as barite, gypsum, sulfur, orpiment, and Hokutolite, associated with bacteria implies that heavy metals have been transported from strong acidic hot spring water to sediments through bacterial metabolism. It is possible that the capability of radioactive sulfide biofims for heavy metal immobilization can be used to counteract the disastrous effects of radio nuclide polluted water and radio pharmaceutical medical treatment.
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