Mumtaz Saqib, Streten Claire, Parry David L, McGuinness Keith A, Lu Ping, Gibb Karen S
Charles Darwin University, Darwin, NT, Australia.
Australian Institute of Marine Science, Darwin, NT, Australia.
J Environ Radioact. 2015 Nov;149:121-8. doi: 10.1016/j.jenvrad.2015.07.014. Epub 2015 Jul 30.
Ranger Uranium Mine (RUM) is situated in the wet-dry tropics of Northern Australia. Land application (irrigation) of stockpile (ore and waste) runoff water to natural woodland on the mine lease is a key part of water management at the mine. Consequently, the soil in these Land Application Areas (LAAs) presents a range of uranium (U) and other metals concentrations. Knowledge of seasonal and temporal changes in soil U and physicochemical parameters at RUM LAAs is important to develop suitable management and rehabilitation strategies. Therefore, soil samples were collected from low, medium, high and very high U sites at RUM LAAs for two consecutive years and the effect of time and season on soil physicochemical parameters particularly U and other major solutes applied in irrigation water was measured. Concentrations of some of the solutes applied in the irrigation water such as sulphur (S), iron (Fe) and calcium (Ca) showed significant seasonal and temporal changes. Soil S, Fe and Ca concentration decreased from year 1 to year 2 and from dry to wet seasons during both years. Soil U followed the same pattern except that we recorded an increase in soil U concentrations at most of the RUM LAAs after year 2 wet season compared to year 2 dry season. Thus, these sites did not show a considerable decrease in soil U concentration from year 1 to year 2. Sites which contained elevated U after wet season 2 also had higher moisture content which suggests that pooling of U containing rainwater at these sites may be responsible for elevated U. Thus, U may be redistributed within RUM LAAs due to surface water movement. The study also suggested that a decrease in U concentrations in LAA soils at very high U (>900 mg kg(-1)) sites is most likely due to transport of particulate matter bound U by surface runoff and U may not be lost from the surface soil due to vertical movement through the soil profile. Uranium attached to particulate matter may reduce its potential for environmental impact. These findings suggest that U is effectively adsorbed by the soils and thus land application may serve as a useful tool for U management in the wet-dry tropics of northern Australia.
兰杰铀矿(RUM)位于澳大利亚北部干湿季分明的热带地区。将堆存(矿石和废料)径流废水通过土地灌溉的方式应用于矿区租赁地上的天然林地,是该矿水资源管理的关键部分。因此,这些土地应用区域(LAA)的土壤呈现出一系列不同的铀(U)和其他金属浓度。了解兰杰铀矿土地应用区域土壤中铀和理化参数的季节性及时间变化,对于制定合适的管理和修复策略至关重要。因此,连续两年从兰杰铀矿土地应用区域的低、中、高和极高铀含量场地采集土壤样本,并测定时间和季节对土壤理化参数(特别是灌溉水中的铀和其他主要溶质)的影响。灌溉水中施用的一些溶质,如硫(S)、铁(Fe)和钙(Ca)的浓度呈现出显著的季节性和时间变化。两年间,土壤中的硫、铁和钙浓度从第1年到第2年,以及从旱季到雨季均呈下降趋势。土壤铀含量也呈现相同模式,只是与第2年旱季相比,我们记录到在第2年雨季之后,兰杰铀矿大部分土地应用区域的土壤铀浓度有所增加。因此,这些场地从第1年到第2年土壤铀浓度并未显著下降。在第2个雨季之后铀含量升高的场地,其土壤湿度也较高,这表明这些场地含铀雨水的汇集可能是导致铀含量升高的原因。因此,由于地表水的流动,铀可能在兰杰铀矿土地应用区域内重新分布。该研究还表明,在极高铀含量(>900 mg kg⁻¹)场地的土地应用区域土壤中铀浓度降低,最有可能是由于地表径流携带了与颗粒物结合的铀,并且铀可能不会因通过土壤剖面的垂直移动而从表层土壤中流失。附着在颗粒物上的铀可能会降低其对环境的潜在影响。这些发现表明,铀能被土壤有效吸附,因此土地灌溉应用可能是澳大利亚北部干湿季分明的热带地区铀管理的一种有效手段。