○Jackson Ezekiel Birore1[Student presentation: Master’s course], Yuna Nakazawa1, Natsuo Okada1, Angesom Gebretsadik1, Yoko Ohtomo1, Yohuei Kawamura1
(1. Hokkaido University )
司会:パク イルファン(北海道大学)
Keywords:Mbinga coal, Trace elements, Mineralogy, Environmental risk, Acid mine drainage
Coal is a complex mixture of organic matter and mineral phases, both of which can host toxic and trace elements. Understanding their mode of occurrence is essential for assessing environmental risks associated with coal mining and utilization. This study investigates the mineralogical composition and trace element distribution in the Mbinga bituminous coal deposit, located in the Ngaka coalfield of the Ruhuhu Basin in Tanzania. Optical microscopy and field-emission electron probe microanalysis (FE-EPMA) were used to characterize mineral phases and their chemical compositions.The dominant minerals identified include pyrite, barite, rutile, zircon, and rare earth element (REE)-bearing phosphates. Trace elements that were observed in minerals include: nickel (Ni), copper (Cu), scandium (Sc), platinum (Pt), aluminum (Al), chromium (Cr), calcium (Ca), and hafnium (Hf); and REE-phosphates, which are enriched in cerium (Ce), lanthanum (La), neodymium (Nd), and yttrium (Y), with significant thorium (Th) and praseodymium (Pr). These results highlight the diverse modes of trace element occurrence in coal, which has implications for environmental pollution during coal combustion, handling, and waste disposal. The presence of pyrite also suggests a risk of acid mine drainage. Understanding these mineralogical and chemical relationships provides a foundation for designing appropriate mitigation strategies, such as pre-combustion coal cleaning and post-combustion gas treatment technologies.
講演PDFファイルダウンロードパスワード認証
講演集に収録された講演PDFファイルのダウンロードにはパスワードが必要です。
現在有効なパスワードは、[資源・素材学会会員専用パスワード]です。
※[資源・素材学会会員専用パスワード]は【会員マイページ】にてご確認ください。(毎年1月に変更いたします。)
[資源・素材学会会員専用パスワード]を入力してください