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Titlebook: Uranium geochemistry, mineralogy, geology, exploration and resources; Published for the In Benedetto Vivo,Felice Ippolito,P. R. Simpson Boo

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書目名稱Uranium geochemistry, mineralogy, geology, exploration and resources
副標(biāo)題Published for the In
編輯Benedetto Vivo,Felice Ippolito,P. R. Simpson
視頻videohttp://file.papertrans.cn/944/943837/943837.mp4
圖書封面Titlebook: Uranium geochemistry, mineralogy, geology, exploration and resources; Published for the In Benedetto Vivo,Felice Ippolito,P. R. Simpson Boo
描述turning points that, in the course of a few years, have made this The uranium minerals that today are at the centre of worldwide metal an essential raw material. attention were unknown until 1780, when Wagsfort found a First, the destructive property of fission reactions made uranium a metal of fundamental strategic importance, increas- pitchblende sample in 10hanngeorgenstadt. This discovery passed unnoticed, however, since Wags fort thought that it ing research in some nations, but the revolution came with the plan for the real possibility of utilizing chain reactions for contained a black species of a zinc mineral-hence the n‘:lme ‘pitchblende‘ (= pitch-like blende). Seven years later, Klaproth, energy production in place of conventional fuels. while examining the mineral, noted that it contained an oxide Since that time a ‘uranium race‘ has been in progress in many countries-often justified by the well-founded hope of of an unknown metal, which he called ‘uranium‘ in honour of the planet Uranus, recently discovered by Herschel. Klaproth becoming self-sufficient with regard to energy, or at least of also believed that he had separated the metal, but, in fact, the paying off a pa
出版日期Book 1984
關(guān)鍵詞chemistry; exploration; geochemistry; geology; mineral; mineralogy; economic geology; mineral resources
版次1
doihttps://doi.org/10.1007/978-94-009-6060-2
isbn_softcover978-94-009-6062-6
isbn_ebook978-94-009-6060-2
copyrightThe Institution of Mining and Metallurgy 1984
The information of publication is updating

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Geochemical behaviour of uranium in the supergene environment,Uranium (symbol U; atomic number 92) and 14 other elements (from actinium to lawrencium) form the actinide series. Uranium—from the Latin .—was named in 1790 by Klaproth after Herschel had discovered the planet with the same name.
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Uranium deposits in Italy,Uranium exploration in Italy was begun in the early 1950s by private companies, which evaluated known radioactive occurrences. In 1954 two state-owned organizations—the Comitato Nazionale Ricerche Nucleari (CNRN) and the Ente Nazionale Idrocarburi (ENI)—became active in the exploration field and, a few years later, were the sole operators.
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History of radioactivity,ochronology, it was found to be an important heat source within the planets and it produced small changes in the isotopic composition of some elements, which enabled us to trace geochemical processes back to the earth’s past. Moreover, radioactive processes are a source of energy for human beings.
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Geochemistry of uranium in the hydrographic network,carried out. Uranium contents are determined in both elements of the hydrographic network—liquid and solid. For regional surveys hydrogeochemistry is best suited for elements that produce very soluble complexes—for example, uranium. At this stage no other elements are assayed, uranium being its own best tracer in water.
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Uranium deposits of the world, excluding Europe,ons of selected deposits of each major type. Descriptions of geology, mineralogy, genesis and economics of each type of deposit precede summaries of selected occurrences of most types. The locations of described deposits are shown in Fig. 1.
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