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回填铀矿井下尾矿的氡逸出。

Radon emanation from backfilled mill tailings in underground uranium mine.

机构信息

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

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

出版信息

J Environ Radioact. 2014 Apr;130:15-21. doi: 10.1016/j.jenvrad.2013.12.017. Epub 2014 Jan 9.

Abstract

Coarser mill tailings used as backfill to stabilize the stoped out areas in underground uranium mines is a potential source of radon contamination. This paper presents the quantitative assessment of radon emanation from the backfilled tailings in Jaduguda mine, India using a cylindrical accumulator. Some of the important parameters such as (226)Ra activity concentration, bulk density, bulk porosity, moisture content and radon emanation factor of the tailings affecting radon emanation were determined in the laboratory. The study revealed that the radon emanation rate of the tailings varied in the range of 0.12-7.03 Bq m(-2) s(-1) with geometric mean of 1.01 Bq m(-2) s(-1) and geometric standard deviation of 3.39. An increase in radon emanation rate was noticed up to a moisture saturation of 0.09 in the tailings, after which the emanation rate gradually started declining with saturation due to low diffusion coefficient of radon in the saturated tailings. Radon emanation factor of the tailings varied in the range of 0.08-0.23 with the mean value of 0.21. The emanation factor of the tailings with moisture saturation level over 0.09 was found to be about three times higher than that of the absolutely dry tailings. The empirical relationship obtained between (222)Rn emanation rate and (226)Ra activity concentration of the tailings indicated a significant positive linear correlation (r = 0.95, p < 0.001). This relationship may be useful for quick prediction of radon emanation rate from the backfill material of similar nature.

摘要

用作地下铀矿采空区回填的较粗磨矿尾矿是氡污染的潜在来源。本文使用圆柱形累积器对印度贾杜达铀矿回填尾矿的氡逸出进行了定量评估。在实验室中测定了影响氡逸出的一些重要参数,如尾矿中的(226)Ra 活度浓度、体密度、体孔隙率、含水量和氡逸出因子。研究表明,尾矿的氡逸出率在 0.12-7.03 Bq m(-2) s(-1)之间变化,几何平均值为 1.01 Bq m(-2) s(-1),几何标准偏差为 3.39。在尾矿含水量达到 0.09 之前,氡逸出率逐渐增加,之后由于氡在饱和尾矿中的扩散系数较低,逸出率逐渐开始随饱和度下降。尾矿的氡逸出因子在 0.08-0.23 之间变化,平均值为 0.21。含水量超过 0.09 的尾矿的逸出因子比绝对干燥尾矿的逸出因子高约三倍。在尾矿的(222)Rn 逸出率与(226)Ra 活度浓度之间获得的经验关系表明存在显著的正线性相关(r = 0.95,p < 0.001)。这种关系可能有助于快速预测类似性质的回填材料的氡逸出率。

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