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  1. 原著論文

Distribution of rare earth elements, thorium and uranium in Gulf of Thailand's sediment

https://repo.qst.go.jp/records/47159
https://repo.qst.go.jp/records/47159
755e6464-d09e-42a0-bc92-8b3bb47e7427
Item type 学術雑誌論文 / Journal Article(1)
公開日 2015-07-22
タイトル
タイトル Distribution of rare earth elements, thorium and uranium in Gulf of Thailand's sediment
言語
言語 eng
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 journal article
アクセス権
アクセス権 metadata only access
アクセス権URI http://purl.org/coar/access_right/c_14cb
著者 Kritsananuwat, Rawiwan

× Kritsananuwat, Rawiwan

WEKO 471244

Kritsananuwat, Rawiwan

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Kumar, Sahoo Sarata

× Kumar, Sahoo Sarata

WEKO 471245

Kumar, Sahoo Sarata

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Fukushi, Masahiro

× Fukushi, Masahiro

WEKO 471246

Fukushi, Masahiro

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Chanyotha, Supitcha

× Chanyotha, Supitcha

WEKO 471247

Chanyotha, Supitcha

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Rawiwan Kritsananuwat

× Rawiwan Kritsananuwat

WEKO 471248

en Rawiwan Kritsananuwat

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サフー サラタ クマール

× サフー サラタ クマール

WEKO 471249

en サフー サラタ クマール

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抄録
内容記述タイプ Abstract
内容記述 Distribution of rare earth elements (REEs), thorium and uranium in fifty-four marine sediments collected from five selected areas along the Gulf of Thailand are discussed in this paper. These areas have been selected as potential sites to set up thermal and nuclear power plants. Concentration of elements was determined using inductively coupled plasma mass spectrometry (ICP-MS). Absolute concentrations of REEs, Th and U show a sample-to-sample variation and may be due to different geological characteristic of area as well as grain size effect. Total REE concentrations (not including Y) range between 9 μg/g and 210 μg/g. The chondrite-normalized REEs patterns of all samples are similar to Post Archaean Australian Shale (PAAS) and average Upper Continental Crust (UCC), with LREEs enrichment relative to HREEs (LaN/YbN = 6.5 – 29.3), fairly flat HREEs patterns (GdN/YbN = 1.0 – 3.8) and ubiquitous negative Eu-anomaly (Eu/Eu* = 0.3 – 0.7). Th concentrations (1 – 28 μg/g) are relatively higher than those of uranium (0.4 – 4 μg/g). Th/U ratios (1.5z – 9.9) are higher than the average upper crust. These results are consistent with terrigenous sediments that formed from the weathering and erosion of felsic rocks.
書誌情報 Environmental Earth Sciences

巻 73, 号 7, p. 3361-3374, 発行日 2014-08
出版者
出版者 Springer-Verlag Berlin Heidelberg
ISSN
収録物識別子タイプ ISSN
収録物識別子 1866-6280
DOI
識別子タイプ DOI
関連識別子 10.1007/s12665-014-3624-8
関連サイト
識別子タイプ URI
関連識別子 1866-6299
関連名称 1866-6299
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