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研究生: 林群智
論文名稱: 大屯火山區溫泉水中化學特性對鈾/釷系列核種放射性不平衡之影響
指導教授: 朱鐵吉
口試委員:
學位類別: 博士
Doctor
系所名稱: 原子科學院 - 生醫工程與環境科學系
Department of Biomedical Engineering and Environmental Sciences
論文出版年: 2003
畢業學年度: 91
語文別: 中文
論文頁數: 134
中文關鍵詞: 火山溫泉放射性不平衡
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  • 中文摘要
    本研究針對大屯火山區溫泉中U/Th系列核種(包括:238U, 234U, 230Th, 226Ra, 232Th, and 228Th)進行分析,並分析採樣點環境之化學特性(如:酸鹼度、氧化還原電位及溫泉水中之Cl-、SO42- 濃度等),藉以探討放射性核種之遷移及其對放射性核種含量之變動的影響。

    研究結果顯示,溫泉水中U 、 Th之含量隨pH增加而遞減。234U/238U之放射活度比值(AR)可歸因於U(VI)之水解、α衰變核反跳及234U之選擇性瀝濾,然其不平衡現象並不明顯。而溫泉水中之230Th/234U, 226Ra/230Th和 228Th/232Th及底泥中230Th/234U, 226Ra/230Th, 228Ra/232Th, 228Th/228Ra 和228Th/232Th之放射活度比值均可見明顯之不平衡現象。

    溫泉水中之Cl-和SO42-離子可促進U和Th溶入水中。溫泉水中之230Th/234U AR (0.04–0.63)小於1,而底泥中之230Th/234U AR (1.13–1.52)大於1,此可歸因於234U和230Th溶解度的迥異。溫泉水中226Ra/230Th的AR (0.60–34.8)隨Cl-和SO42-濃度增加而下降,而底泥中226Ra/230Th的AR (1.57–21.5)則有相反之趨勢;此結果可歸因於230Th 與Cl-或SO42-的錯合及226Ra與(Ba,Pb)SO4的共沉澱反應。228Th/232Th 在溫泉水中之AR (1.01–12.0)和底泥中之AR(1.02–25.6)均偏離1,且與228Ra和(Ba,Pb)SO4之共沉澱及228Th之錯合有關。


    目錄 中文摘要 ………………………………………………………………...i 英文摘要 ………………………………………………………………..ii 謝誌 ………………………………………………………………….…iii 圖檢索目錄 …………………………………………………………….iv 表檢索目錄 ………………………………………………………….....ix 第一章 研究緣起 ………………………………………………….….1 第二章 文獻回顧 ……………………………………………….…….2 第三章 大屯火山群區簡介 ……………………………………….….6 3-1 大屯火山群的形成 ………………………………………….….6 3-2 溫泉的形成 ………………………………………………….…10 第四章 鈾/釷系列核種簡介 4-1 自然界的放射性核種 ………………………………………….12 4-1-1 235U衰變系列 ..……………………………………….…14 4-1-2 232Th衰變系列 ………………………………………….14 4-1-3 238U衰變系列 …………………………………………..15 4-2 鈾的基本性質 …………………………………………………19 4-3 釷的基本性質 …………………………………………………23 4-4 鐳的基本性質 ..………………………………………………..26 第五章 原理簡介 5-1 液體閃爍偵檢器 ………………………………………………29 5-2 α偵檢器 ………………………………………………………32 5-3 感應偶合電漿原子放射光譜儀 ..……………………………..34 5-3-1 導電偶電漿光源 ……………………………………….34 5-3-2 原子放射光譜法 ……………………………………….35 5-4 紫外線-可見光吸收光譜儀 …………………………………...36 5-5 高純鍺偵檢器 …………………………………………………39 第六章 實驗方法 6-1取樣地點 ……………………………………………………….41 6-2取樣與樣品之保存 …………………………………………….43 6-3鈾的分析方法 ………………………………………………….44 6-4釷的分析方法 ………………………………………………….51 6-5鐳的分析方法 ………………………………………………….56 6-6溫泉水中硫酸鹽的分析 ……………………………………….62 6-7溫泉水中氯離子的分析 ……………………………………….65 6-8樣品中主要離子之定量 ……………………………………….66 第七章 實驗結果與討論 7-1 各採樣點的化學性質特徵 ……………………………………68 7-1-1 SO42-的分析結果 ………………………………..……...73 7-1-2 Cl-的分析結果 ……………………………………..…..74 7-2 各採樣點溫泉水及底泥中U/Th系列核種之含量 ………….75 7-2-1 鈾之分析結果 ……………………………..…………..78 7-2-2 釷的分析結果 ………………………………………....80 7-2-3 鐳的分析結果 ………………………………………....81 7-3 溫泉水中U, Th及Ra隨pH變動的情形 …..…………..…..86 7-4溫泉中234U/238U活度比隨氧化還原電位(Eh) 變動的情形 …………………………………………………..95 7-5 底泥中之226Ra及228Ra的活度濃度均隨 SO42-濃度變動的情形 ……………………………….….…...99 7-6 溫泉水中230Th/234U之放射活度比值隨Cl-和 SO42-濃度變動的情形 ………………………………….…..100 7-7 226Ra/230Th的放射活度比值隨Cl-和SO42-濃度 變動的情形 …………………………………………….…..103 7-8 228Th/232Th的放射活度比值隨Cl-和SO42-濃度 變動的情形 ………………………………………………...104 第八章 結論 ........………………………………………………...108 參考文獻 ……………………………………………………………111 附錄A 以皇冠醚萃取鐳之方法探討 …………....………………..119 附錄B 個人著作 ………………………………………………….133

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