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水辐射分解促进铀矿床围岩赤铁矿化蚀变的实验研究
引用本文:闵茂中,吴俊奇,戚成云,周云生.水辐射分解促进铀矿床围岩赤铁矿化蚀变的实验研究[J].铀矿地质,1992(1).
作者姓名:闵茂中  吴俊奇  戚成云  周云生
作者单位:南京大学地球科学系,南京大学地球科学系,南京大学地球科学系,南京大学地球科学系
摘    要:本文根据人工辐照含二价铁的水溶液实验结果,讨论水的辐射分解对铀矿床围岩红化蚀变的意义。铀矿床围岩中各种形式的水,当遭受辐射线长期辐照后,将发生辐射分解作用,析出许多自由基及其反应产物(H,H_3O~+,OH,HO_2,H_2,O_2,H_2O_2等),其最终结果是明显地增强周围介质的氧化性,这无论在氧化或弱还原条件下,都将使铀矿床围岩中广泛分布的二价铁氧化成三价铁,产生红化(赤铁矿化)围岩蚀变,利用这一原理可解释某些地质现象。

关 键 词:辐射分解  围岩蚀变  赤铁矿化  实验研究

EXPERIMENTAL STUDIES IN RADIOLYSIS OF WATER FACILITATING HEMATITIZATION OF HOSTROCKS IN URANIUM DEPOSITS
Min Maozhong,Wu Junchi,Qi Chengyun,Zhou Yinsheng.EXPERIMENTAL STUDIES IN RADIOLYSIS OF WATER FACILITATING HEMATITIZATION OF HOSTROCKS IN URANIUM DEPOSITS[J].Uranium Geology,1992(1).
Authors:Min Maozhong  Wu Junchi  Qi Chengyun  Zhou Yinsheng
Institution:Min Maozhong,Wu Junchi,Qi Chengyun,Zhou Yinsheng Department of Earth Sciences,Nanjing University
Abstract:The gamma irradiation experiments were performed. Water solution containing Fe_2SO_3,Na_2SO_3 was placed in a gamma field, having absorbed dose of 0,20, 60, 180, 500 KGy (during5d). The water solution in gamma field was disintegrated into hydrogen, oxygen and oxidi-zing compounds (e.g., H_2O_2) under the influence of ionizing radiation, called radiolysis.It was of particular concern because it produced an oxidizing environment and changed Fe~2+into Fe~(3+). The reaction culd happen in host rocks of uranium deposit and result in the for-mation of hematite, goethite etc,reddening host-rocks. Authors of this paper explain severalgeological phenomena with radiolysis, and suggest that radiolysis of water is an importantcause for hematitization of hostrocks in uranium deposits.
Keywords:Radiolysis  Alteration of host-rock  Hematitization  Experimental study
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