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铀成矿作用、核废物地球化学处置与吸附作用的关系
引用本文:张景廉.铀成矿作用、核废物地球化学处置与吸附作用的关系[J].铀矿地质,1989,5(3):158-163.
作者姓名:张景廉
作者单位:不详
摘    要:在不同类型的工业铀矿床的矿石中,吸附状态的铀占了很大的比重,铁钛氢氧化物、硅胶、粘土、有机质等是常见的主要吸附剂。本文利用朗缪尔等温式、弗仑德里奇等温式、D-R等温式,讨论了粘土矿物(主要是高岭土、蒙脱石)对溶液中铀的吸附作用,对吸附作用在铀成矿作用、核废物处置中的意义作了详细的讨论,认为吸附作用是一种重要的成矿作用。

关 键 词:吸附作用  铀成矿作用  核废物处置  等温式

THE RELATIONSHIP BETWEEN URANIUM MINERALIZATION, NUCLEAR WASTE GEOCHEMICAL DISPOSAL AND ADSORPTION OF URANIUM
Zhang Jinglian.THE RELATIONSHIP BETWEEN URANIUM MINERALIZATION, NUCLEAR WASTE GEOCHEMICAL DISPOSAL AND ADSORPTION OF URANIUM[J].Uranium Geology,1989,5(3):158-163.
Authors:Zhang Jinglian
Institution:Zhang Jinglian
Abstract:Uranium as an adsorptive form accounts for a large proportion in the uranium ores of different type economic deposits. A variety of adsorbents including Fe and Ti hydroxides, amorphous silica, clays and organic matter are recognized. Adsorption of U from solutions on clay minerals (kaolinite, montmorillonite) is discussed by using Langmuir, Freundlich and D-R isotherms in this paper. The relationship between U mineralization, nuclear waste disposal and adsorption of U is discussed in detail. It is considered that adsorption is an important mineralization for U and some other deposits (e.g.Au, REE etc).
Keywords:Adsorption  U mineralization  Nuclear waste disposal  Isotherm  
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