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首页> 外文期刊>Journal of Water Resource and Protection >Recycling Tailings Seepage Water for Diogo Heavy Minerals Mine Sustainability (Northern Senegal)
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Recycling Tailings Seepage Water for Diogo Heavy Minerals Mine Sustainability (Northern Senegal)

机译:迪奥戈重矿物矿山可持续性的回收尾矿渗水(塞内加尔北部)

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style="text-align:justify;"> The sandy Quaternary and the deep Maastrichtian aquifers located in the northern coastal zone of Senegal, from the locality of Kayar in the south to Saint-Louis in the north, constitute the main sources of water supply for urban and local needs as well as mining activities. The Quaternary aquifer that provides the water required for the irrigation of local farmlands, hosts a significant heavy mineral sands deposit currently being mined by the Grande Cote Operations (GCO). As a result of variable rainfall and increased water abstraction, this shallow aquifer has recorded a continuous water level decline since 1970, with potential negative effects on both the social and economic development of the region. The mining of heavy minerals (zircon, ilmenite, leucoxene and rutile) at GCO is realised through conventional dredging techniques that require large volumes of water (up to 60,000 m3/d). The water pumped by the dredge to enable the extraction of the heavy minerals, infiltrates into the shallow aquifer, runs-off into the dredge pond or evaporates. The objective of this study is to evaluate a water balance that enables the provision of a permanent water supply to the dredge pond, whilst minimising the risk of flooding of the cropping depressions adjacent to the mine site or drying out of the farming wells. The hydrodynamic model implemented for this purpose was calibrated and tested during the first year of operation. The Root Mean Squared Error (RMSE) obtained for the calibration is approximately 0.52 m. The predictions indicate a requirement for the system to recover part of the tailings infiltration through dewatering boreholes. The quantity of recycled water is estimated at 16,000 m3/d on average. The model simulations show an additional water requirement, extracted from the deep Maastrichtian aquifer, varying between 23,000 and 28,000 m3/d to achieve the optimum pond water level.
机译:style =“ text-align:justify;”>位于塞内加尔北部沿海地区的沙质第四纪和深层的马斯特里赫特含水层,从南部的凯亚尔地区到北部的圣路易斯,是主要来源满足城市和地方需求以及采矿活动的供水需求。第四纪含水层为当地农田的灌溉提供了所需的水,其中蕴藏着大量重矿物砂,目前正由格兰德科特行动公司(GCO)开采。由于降雨变化和取水量增加,自1970年以来,该浅层含水层的水位持续下降,对该地区的社会和经济发展均具有潜在的负面影响。通过常规挖泥技术需要大量的水(高达60,000 m 3 / d)来实现在GCO上开采重矿物(锆石,钛铁矿,白细胞和金红石)。挖泥机泵出的水能够提取重矿物质,渗入浅层含水层,流到挖泥机池中或蒸发。这项研究的目的是评估一种水平衡,该平衡能够为挖泥池提供永久性的供水,同时最大程度地减少了邻近矿区的作物洼地泛滥或耕作井变干的风险。为此,在运行的第一年对水动力模型进行了校准和测试。校准获得的均方根误差(RMSE)约为0.52 m。这些预测表明该系统需要通过脱水钻孔来回收部分尾矿渗透。平均回收水量估计为16,000 m 3 / d。模型模拟表明,从马斯特里赫特深层含水层提取的额外需水量在23,000至28,000 m 3 / d之间,以达到最佳池塘水位。

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