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评估低品位地下铀矿矿体和尾矿回填氡的逸出。

Assessment of (222)Rn emanation from ore body and backfill tailings in low-grade underground uranium mine.

机构信息

Department of Mining Engineering, Indian School of Mines, Dhanbad, 826 004, India.

Environmental Assessment Division, Bhabha Atomic Research Centre, Trombay, Mumbai, 400 085, India.

出版信息

Environ Sci Pollut Res Int. 2014 Feb;21(3):2305-2312. doi: 10.1007/s11356-013-2137-4. Epub 2013 Sep 21.

Abstract

This paper presents a comparative study of (222)Rn emanation from the ore and backfill tailings in an underground uranium mine located at Jaduguda, India. The effects of surface area, porosity, (226)Ra and moisture contents on (222)Rn emanation rate were examined. The study revealed that the bulk porosity of backfill tailings is more than two orders of magnitude than that of the ore. The geometric mean radon emanation rates from the ore body and backfill tailings were found to be 10.01 × 10(-3) and 1.03 Bq m(-2) s(-1), respectively. Significant positive linear correlations between (222)Rn emanation rate and the (226)Ra content of ore and tailings were observed. For normalised (226)Ra content, the (222)Rn emanation rate from tailings was found to be 283 times higher than the ore due to higher bulk porosity and surface area. The relative radon emanation from the tailings with moisture fraction of 0.14 was found to be 2.4 times higher than the oven-dried tailings. The study suggested that the mill tailings used as a backfill material significantly contributes to radon emanation as compared to the ore body itself and the (226)Ra content and bulk porosity are the dominant factors for radon emanation into the mine atmosphere.

摘要

本文对印度贾杜达地下铀矿中矿石和回填尾矿的氡逸出进行了对比研究。考察了表面积、孔隙率、(226)Ra 和含水量对氡逸出率的影响。研究表明,回填尾矿的体孔隙率比矿石高出两个数量级以上。从矿体和回填尾矿中得出的氡逸出率的几何平均值分别为 10.01×10(-3)和 1.03 Bq m(-2) s(-1)。观察到氡逸出率与矿石和尾矿中(226)Ra 含量之间存在显著的正线性相关性。对于归一化的(226)Ra 含量,由于更高的体孔隙率和表面积,尾矿的氡逸出率比矿石高 283 倍。发现含水量为 0.14 的尾矿的相对氡逸出率比烘干的尾矿高 2.4 倍。研究表明,与矿体本身相比,用作回填材料的尾矿对氡逸出的贡献显著,而(226)Ra 含量和体孔隙率是氡逸入矿井大气的主要因素。

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