首页 | 本学科首页   官方微博 | 高级检索  
     

原地浸出采铀元素的迁移与沉淀
引用本文:周锡堂,阙为民,胡鄂明,周泉,苏学斌.原地浸出采铀元素的迁移与沉淀[J].铀矿冶,2000,19(2):78-83,115.
作者姓名:周锡堂  阙为民  胡鄂明  周泉  苏学斌
作者单位:1. 中南工学院,湖南,衡阳,421001
2. 核工业溶浸采矿技术重点实验室,湖南,衡阳,421001
摘    要:原地浸出来采铀就是要在含矿含水层人为地选成有利元素迁移的地球化学环境,通过元素的为断迁移、沉淀和溶解,实现铀的浸出。本文结合地浸采铀工艺特点,对原地浸出采铀元素的迁移、元素的沉淀以及影响元素的因素进行了分析探讨。

关 键 词:原地浸出  采铀  元素迁移  沉淀

ELEMENT MIGRATION AND SEDIMENTATION OF IN-SITU URANIUM LEACHING
ZHOU Xi-tang,QUE Wei-min,HU E-ming,ZHOU Quan,SU Xue-bin.ELEMENT MIGRATION AND SEDIMENTATION OF IN-SITU URANIUM LEACHING[J].Uranium Mining and Metallurgy,2000,19(2):78-83,115.
Authors:ZHOU Xi-tang  QUE Wei-min  HU E-ming  ZHOU Quan  SU Xue-bin
Abstract:In situ leaching is the reverse process to the natural sedimentation of minerals.Under man made geochemical environments favourable to element migration in confined and mineralized aquifer,in situ leaching of uranium accomplishes through constant migration, se dimentation and dissolution of element.Combining with fundamental characteristics of in situ uranium leaching,the element migration and sedimentation are discussed.The factors which influence the element migration of in situ leaching are also discussed.
Keywords:in  situ leaching  element migration  sedimentation  factors of influence  
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号