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首页> 外文期刊>Journal of Hydrology >Modelling spatial variability and uncertainty of cadmium leaching to groundwater in an urban region
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Modelling spatial variability and uncertainty of cadmium leaching to groundwater in an urban region

机译:城市地区地下水中镉淋溶的空间变异性和不确定性建模

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Over the last century, soils in the region of Nordenham in northern Germany received high loads of heavy-metals by air-borne immissions from a close-by metal smelter. Based on measured soil properties and cadmium contamination data the leaching of Cd to groundwater was predicted for Nordenham using a numerical transport model based on the convection-dispersion equation. The main objective in this study was to account for the spatial variability and uncertainty of Cd sorption controlling soil properties (pH, organic carbon content) and to analyze their propagation into the variance of area-related model outputs, i.e. Cd breakthrough concentrations at the groundwater surface. For this purpose a nested Monte-Carlo method was combined with deterministic numerical 1D simulations of Cd leaching. The transport model was parameterized without any parameter fitting involved. The validity of the model was verified by retrospective simulations from the initial operation of the smelter until the year of soil sampling. Forecast simulations were run for a period of 200 years. Predicted local scale Cd breakthrough concentrations at the groundwater surface were evaluated by spatial aggregation for single blocks at the field scale, yielding area-related concentrations with associated uncertainties from imprecise knowledge on local soil properties. Significant exceedance of the limit of the German drinking water ordinance of 5 mu g L-1 is observed on approximately 90% of the study area with the average point in time of limit value exceedance being the year 2066 and a 90% prediction interval of 2049-2092. At the end of the simulation period, Cd concentrations at the groundwater surface still increase on large parts of the study area. The spatially averaged Cd concentration is 19.89 mu g L-1 with a 90% prediction interval of 15.28-24.69 mu g L-1. Locally, however, concentrations larger than 60 mu g L-1 may be reached. Prediction uncertainty is only moderate and does not question the exceedance of the limit value on the majority of the regarded plots even for spatially averaged concentrations, unless measures to prevent leaching are taken, such as an increase of soil pH by liming.
机译:上个世纪,德国北部诺德纳姆(Nordenham)地区的土壤由于附近一家金属冶炼厂的空运污染物而承受了重金属的高负荷。根据测得的土壤性质和镉污染数据,使用基于对流扩散方程的数值传输模型,预测了诺登汉姆(Nordenham)镉向地下水的浸出。这项研究的主要目的是说明控制土壤吸附镉特性(pH,有机碳含量)的空间变异性和不确定性,并分析其传播到与区域有关的模型输出的变异中,即地下水中的镉突破浓度。表面。为此,将嵌套蒙特卡洛方法与Cd浸出的确定性数值一维模拟相结合。对运输模型进行参数化,不涉及任何参数拟合。该模型的有效性通过从冶炼厂开始运营到土壤采样年的回顾性模拟得到了验证。预测模拟运行了200年。通过对田间尺度的单个区块进行空间聚集,评估了地下水表面预测的局部Cd突破浓度,并从对当地土壤特性的不确切了解中得出了与区域相关的浓度以及相关的不确定性。在大约90%的研究区域中观察到明显超过了德国饮用水条例5微克L-1的限值,限值平均值的平均时间点是2066年,而90%的预测间隔是2049年-2092。在模拟期结束时,在研究区域的大部分地区,地下水表面的Cd浓度仍在增加。 Cd的空间平均浓度为19.89μg L-1,90%的预测间隔为15.28-24.69μg L-1。但是,局部浓度可能达到大于60μg L-1。预测不确定性仅是中等程度的,即使对于空间平均浓度而言,也绝不怀疑大多数考虑地块的极限值是否超出限值,除非采取了防止淋溶的措施,例如通过石灰增加土壤pH值。

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