RARE EARTH ELEMENTS SURFACE DISTRIBUTION IN WAYANG WINDU GEOTHERMAL FIELD
Rare Earth Elements are important for modern uses such as liquid crystal display (LCD), magnet, gadget, and so on. The potential of Rare Earth Elements (REE) in geothermal fields worldwide has been researched recently. The previous researches in Wayang Windu geothermal field include samples taken fr...
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id-itb.:440442019-10-01T13:53:56ZRARE EARTH ELEMENTS SURFACE DISTRIBUTION IN WAYANG WINDU GEOTHERMAL FIELD Xaverius Bimantara, Fransiskus Indonesia Final Project geothermal, ICP-MS, rare earth elements INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/44044 Rare Earth Elements are important for modern uses such as liquid crystal display (LCD), magnet, gadget, and so on. The potential of Rare Earth Elements (REE) in geothermal fields worldwide has been researched recently. The previous researches in Wayang Windu geothermal field include samples taken from fresh lava basement and springs. This research focus on 41 altered soil samples to initiate the analysis of rare earth surface occurrence by using analytical method of Inductively Coupled Plasma Mass Spectrometry (ICP-MS); 25 of grab samples and 16 of hand augers at 1-3 depth. The preparations of ICP-MS such as: solving agents used are HF and HNO3 mixing, filtering, and diluting by ultra pure water. Rare earth element anomaly is distributed towards northeastern and southeastern area influenced by high grade samples coded K29 and K22 respectively, where lineaments, craters and hot springs manisfestations occur. text |
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Rare Earth Elements are important for modern uses such as liquid crystal display (LCD), magnet, gadget, and so on. The potential of Rare Earth Elements (REE) in geothermal fields worldwide has been researched recently. The previous researches in Wayang Windu geothermal field include samples taken from fresh lava basement and springs. This research focus on 41 altered soil samples to initiate the analysis of rare earth surface occurrence by using analytical method of Inductively Coupled Plasma Mass Spectrometry (ICP-MS); 25 of grab samples and 16 of hand augers at 1-3 depth. The preparations of ICP-MS such as: solving agents used are HF and HNO3 mixing, filtering, and diluting by ultra pure water. Rare earth element anomaly is distributed towards northeastern and southeastern area influenced by high grade samples coded K29 and K22 respectively, where lineaments, craters and hot springs manisfestations occur. |
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Final Project |
author |
Xaverius Bimantara, Fransiskus |
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Xaverius Bimantara, Fransiskus RARE EARTH ELEMENTS SURFACE DISTRIBUTION IN WAYANG WINDU GEOTHERMAL FIELD |
author_facet |
Xaverius Bimantara, Fransiskus |
author_sort |
Xaverius Bimantara, Fransiskus |
title |
RARE EARTH ELEMENTS SURFACE DISTRIBUTION IN WAYANG WINDU GEOTHERMAL FIELD |
title_short |
RARE EARTH ELEMENTS SURFACE DISTRIBUTION IN WAYANG WINDU GEOTHERMAL FIELD |
title_full |
RARE EARTH ELEMENTS SURFACE DISTRIBUTION IN WAYANG WINDU GEOTHERMAL FIELD |
title_fullStr |
RARE EARTH ELEMENTS SURFACE DISTRIBUTION IN WAYANG WINDU GEOTHERMAL FIELD |
title_full_unstemmed |
RARE EARTH ELEMENTS SURFACE DISTRIBUTION IN WAYANG WINDU GEOTHERMAL FIELD |
title_sort |
rare earth elements surface distribution in wayang windu geothermal field |
url |
https://digilib.itb.ac.id/gdl/view/44044 |
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