478 research outputs found
Partitioning of trace elements and rare earth elements between titanite and major rock-forming minerals in eclogite and clinopyroxenite from the northeastern Shandong Peninsula, eastern China
第2回極域科学シンポジウム/第31回極域地学シンポジウム 11月17日(木) 国立極地研究所 2階大会議
Hydrothermal Treatment of Hokkaido Peat - An Application of FTIR and 13C NMR Spectroscopy on Examining of Artificial Coalification Process and Development
Abukuma and Sanbagawa metamorphic belts in the Kanto district
'29th IGC field trip guide book' vol.5, C08: [Editors] Hirokazu Kato, Harufumi Noro「IGC巡検ガイドブック」 第5巻: [編者] 加藤 碵一, 野呂 春
関東山地三波川変成帯の岩石学的研究
京都大学0048新制・課程博士理学博士甲第3247号理博第905号新制||理||491(附属図書館)UT51-60-G336京都大学大学院理学研究科地質学鉱物学専攻(主査)教授 坂野 昇平, 教授 森本 信男, 教授 亀井 節夫学位規則第5条第1項該当Kyoto UniversityDFA
Removal Of Lead (Pb2+) From Aqueous Solutions By Natural Bentonite
The aim of the present work is to investigate the ability of natural bentonite (untreated) from Pacitan, East Java to remove lead ions from aqueous solution. The bentonite has specific surface area and cation exchange capacity of 27.52 m2 g−1 and 65.20 meq/100 gr of bentonite, respectively. Towards this aim, batch adsorption experiments were carried out and the effect of various parameters on this removal process has been investigated. The effects of pH, grain size of bentonite, adsorption time and lead ion concentration on the adsorption process were examined. The optimum pH for adsorption was found to be 9, with the finer grain size of bentonite is more effective. In adsorption studies, residual lead ions concentration reached equilibrium in a duration of 24 hours. Adsorption of lead on bentonite appeared to follow Freundlich isotherm. Our results demonstrate that the adsorption process was mostly dominated by ion exchange process. Keywords: Removal, lead, aqueous solution, natural bentonite, adsorption
Development of an Ultra-SensitiveEnzyme Immunoassay for Insulin and Its Application to the Evaluation of Diabetic Risk by Analysis of Morning Urine
COPPER (Cu2+) REMOVAL FROM WATER USING NATURAL ZEOLITE FROM GEDANGSARI, GUNUNGKIDUL, YOGYAKARTA
Development of indusrialization and urbanization not only increase economic growth but also contribute to the environmental degradation, especially contamination of heavy metals in water. In other side, there are many geological materials have capability to immobilize heavy metals. Therefore, the objective of this research is to know the maximum capacity of natural zeolite from Trembono area, Gunung Kidul regency to immobilize copper (Cu2+) from water and to understand their mechanism. This experiment was carry out by a batch test. The result showed that the maximum capacity of zeolite to immobilize Cu (qmax) is 63,69 mmolCu/kg Zeolite according to Langmuir adsorption equilibrium model. In addition, the capability to immobilize Cu will increases due to decreasing the grain size. The result of this research can be used as an alternative for waste water treatment, especially Cu.
Keywords: Removal, copper (Cu2+), natural zeolite, Langmuir isother
Crust-mantle interactions during subduction of oceanic & continental crust. 10th International Eclogite Conference, Courmayeur (Aosta, Italy) - Post-conference excursions: September 9-10, 2013
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