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Characterization and modelling of naturally occurring radioactive material releases from a phosphogypsum disposal area in Greece

机译:希腊磷酸缺口处理区自然发生的放射性物质释放的特征与建模

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At the north part of Greece a phosphate fertilizer industry is in operation since 1975. The produced 145 m3/h phosphogypsum (wet production 30% b.w) is deposited continuously near the industry, by the sea side, in a 6 basins (height: 2 -12m) open land disposal area of 563240 m~3. The underground clay layer is not uniform. Moreover, it has a slope and in some areas it disappears, so the vertical leakage is favored. The underground water pH is significantly low (min= 1.93), specially at the north part of the disposal. The low pH values are correlated with increased SO_4 and P_2O_5 concentrations. The underground water pollution is mainly due to underground phosphogypsum drainage water runoffs (10-20 m~3/h), mainly at north, east and south where water permeable layers at the underground water level exist. At the west side, the existing draining channel, the very low permeable layer (clay), the absence of a leakage point (based on piezoelectric measurements) and the direction (west to east) of the underground water flow, prevent the surface and underground runoffs. In order to evaluate the releases of the natural radionuclides from the disposal area to the nearby environment, phosphogypsum measurements with gamma spectrometry and determination of uranium isotopes & ~(226)Ra with alpha-spectrometry in underground and surface water samples collected from different sampling points, have been performed. The ~(238)U concentration in underground water varies from 120 up to 1060 mBq/l, while the ~(226) Ra from 8 up to 5880 mBq/l. High ~(238)U and ~(226) Ra concentrations have been observed at the north part of the disposal area. A model was applied for assessing the behavior of the natural radionuclides U and Ra in the surrounding environment of disposal phosphogypsum site. The model includes the performance assessment, obtaining the water flow and radiological parameters based on experimental data. From field and laboratory data, it has been possible to obtain parameters for the driving processes considered in the model, water fluxes, source term definition, and distribution coefficients. The model consider for both waters flows and mass balance of the radionuclides in a natural environment, provides assessments of radionuclides behavior in groundwater, surface water and including processes of radionuclide migration through land and water. The model has been implemented in a flexible software package RESRAD permits either deterministic or probabilistic calculations to be undertaken for the specific data of the site. In the presented work deterministic calculations will be presented.
机译:在希腊北部,自1975年以来磷肥工业处于运行中。由海面,6个盆地(高度:2)在行业附近封装生产的145m3 / h磷酸缺口(湿润30%BW)。(高度:2 -12m)开放式土地处置面积563240 m〜3。地下粘土层不均匀。此外,它具有斜坡,在一些区域消失,因此垂直泄漏是有利的。地下水pH值明显低(in = 1.93),特别是在北部处置。低pH值与增加的SO_4和P_2O_5浓度相关。地下水污染主要是由于地下磷光膏排水水径流(10-20米〜3 / h),主要在北,东部和南部,存在地下水位的透水层存在。在西侧,现有的排水通道,非常低的渗透层(粘土),缺少泄漏点(基于压电测量)和地下水流的方向(西向东),防止表面和地下径流。为了评估从处理区域到附近环境的自然放射性核素的释放,用γ光谱法测量γ光谱法测定α-光谱法从不同采样点收集的地下和表面水样中的α-光谱法测定,已经进行了。 〜(238)u浓度在地下水中的浓度可达120至1060 mbq / l,而〜(226)ra从8升至5880 mbq / l。高〜(238)u和〜(226)在处置区域的北部观察到ra浓度。应用模型用于评估自然放射性核素U和RA在处理磷酸缺口位点周围环境中的行为。该模型包括性能评估,基于实验数据获得水流和放射性参数。从场和实验室数据,已经可以获得在模型,水助量,源术语定义和分配系数中考虑的驱动过程的参数。该模型考虑到天然环境中放射性核素的水分和质量平衡,提供了地下水,地表水中放射性核素行为的评估,包括通过陆地和水的放射性核素迁移过程。该模型已经在灵活的软件包中实现,允许允许为站点的特定数据进行确定性或概率计算。在所呈现的工作中,将提出确定性计算。

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