Ongori Joash N, Lindsay Robert, Newman Richard T, Maleka Peane P
Department of Physics, University of the Western Cape, Private Bag X17, Bellville 7535, South Africa.
Department of Physics, University of the Western Cape, Private Bag X17, Bellville 7535, South Africa.
J Environ Radioact. 2015 Feb;140:16-24. doi: 10.1016/j.jenvrad.2014.10.012. Epub 2014 Nov 26.
The mining activities taking place in Gauteng province, South Africa have caused millions of tons of rocks to be taken from underground to be milled and processed to extract gold. The uranium bearing tailings are placed in an estimated 250 dumps covering a total area of about 7000 ha. These tailings dumps contain considerable amounts of radium and have therefore been identified as large sources of radon. The size of these dumps make traditional radon exhalation measurements time consuming and it is difficult to get representative measurements for the whole dump. In this work radon exhalation measurements from the non-operational Kloof mine dump have been performed by measuring the gamma radiation from the dump fairly accurately over an area of more than 1 km(2). Radon exhalation from the mine dump have been inferred from this by laboratory-based and in-situ gamma measurements. Thirty four soil samples were collected at depths of 30 cm and 50 cm. The weighted average activity concentrations in the soil samples were 308 ± 7 Bq kg(-1), 255 ± 5 Bq kg(-1) and 18 ± 1 Bq kg(-1) for (238)U, (40)K and (232)Th, respectively. The MEDUSA (Multi-Element Detector for Underwater Sediment Activity) γ-ray detection system was used for field measurements. The radium concentrations were then used with soil parameters to obtain the radon flux using different approaches such as the IAEA (International Atomic Energy Agency) formula. Another technique the MEDUSA Laboratory Technique (MELT) was developed to map radon exhalation based on (1) recognising that radon exhalation does not affect (40)K and (232)Th activity concentrations and (2) that the ratio of the activity concentration of the field (MEDUSA) to the laboratory (HPGe) for (238)U and (40)K or (238)U and (232)Th will give a measure of the radon exhalation at a particular location in the dump. The average, normalised radon flux was found to be 0.12 ± 0.02 Bq m(-2) s(-1) for the mine dump.
南非豪登省正在进行的采矿活动已导致数百万吨岩石从地下被开采出来,进行研磨和加工以提取黄金。含铀尾矿被放置在约250个废料堆中,总面积约7000公顷。这些尾矿堆含有大量镭,因此被确定为氡的主要来源。这些废料堆规模巨大,使得传统的氡析出测量耗时较长,而且很难获得整个废料堆具有代表性的测量结果。在这项工作中,通过在面积超过1平方千米的区域相当精确地测量废料堆的伽马辐射,对已停产的克鲁夫矿废料堆进行了氡析出测量。通过基于实验室和现场的伽马测量,由此推断出该矿废料堆的氡析出情况。在30厘米和50厘米深度采集了34个土壤样本。土壤样本中(238)U、(40)K和(232)Th的加权平均活度浓度分别为308±7贝克勒尔/千克、255±5贝克勒尔/千克和18±1贝克勒尔/千克。MEDUSA(水下沉积物活度多元素探测器)伽马射线探测系统用于现场测量。然后将镭浓度与土壤参数结合,使用不同方法(如国际原子能机构公式)来获取氡通量。还开发了另一种技术——MEDUSA实验室技术(MELT),用于绘制氡析出情况图,其依据是:(1)认识到氡析出不影响(40)K和(232)Th的活度浓度;(2)现场(MEDUSA)与实验室(高纯锗)对(238)U和(40)K或(238)U和(232)Th的活度浓度之比将给出废料堆中特定位置的氡析出量度。该矿废料堆的平均归一化氡通量为0.12±0.02贝克勒尔/平方米·秒。