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Climate change impact on residual contaminants under sustainable remediation

机译:气候变化对可持续治理下残留污染物的影响

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This study investigates the potential impact of climate change on residual contaminants in vadose zones and groundwater. We assume that the effect of climate changes can be represented by perturbations in the natural recharge through the aquifer system. We perform numerical modeling of unsaturated/saturated flow and transport and consider different performance metrics: contaminant concentrations at observation wells and contaminant export at the site's boundary. We evaluate the effect of increasing and decreasing recharge as well as the impact of potential failure of surface capping structures employed to immobilize vadose zone contaminants. Our approach is demonstrated in a real case study by simulating transport of non-reactive radioactive tritium at the U.S. Department of Energy's Savannah River Site. Results show that recharge changes significantly affect well concentrations: after an initial slight dilution we identify a significant concentration increase at different observation wells some years after the recharge increase and/or the cap failure, as a consequence of contaminants' mobilization. This effect is generally emphasized and occurs earlier as the recharge increases. Under decreased aquifers' recharge the concentration could slightly increase for some years, due to a decrease of dilution, depending on the magnitude of the negative recharge shift. We identify trigger levels of recharge above which the concentration/export breakthrough curves and the time of exceedance of the Maximum Contaminant Level for tritium are remarkably affected. Moreover, we observe that the contaminant export at the control plane, identified as the risk pathway to the downgradient population, may only be minimally affected by shifts in the natural recharge regime, except for some extreme cases. We conclude that more frequent sampling and in-situ monitoring near the source zone should be adopted to better explain concentrations' anomalies under changing climatic conditions. Moreover, the maintenance of the cap is critical not only to sequester residual contaminants in the vadose zone, but also to reduce the uncertainty associated with future precipitation changes. Finally, realistic flow and transport simulations achieved through proper calibration processes, rather than conservative modeling, should be adopted to identify non-trivial trade-offs which enable better allocation of resources towards reducing uncertainty in decision making.
机译:这项研究调查了气候变化对渗流带和地下水中残留污染物的潜在影响。我们假设气候变化的影响可以通过含水层系统中自然补给的扰动来表示。我们对不饱和/饱和流和运输进行数值建模,并考虑不同的性能指标:观察井处的污染物浓度和站点边界处的污染物出口。我们评估增加和减少补给的效果,以及用于固定渗流带污染物的表面封盖结构潜在失效的影响。通过在美国能源部萨凡纳河站点模拟非反应性放射性tri的传输,在真实案例研究中证明了我们的方法。结果表明补给量的变化会显着影响孔的浓度:经过最初的轻微稀释后,由于污染物的迁移,我们发现补给量增加和/或瓶盖破裂数年后,不同观察井的浓度明显增加。通常会强调这种效果,并且随着补给的增加而更早地发生。在含水层补给量减少的情况下,由于稀释的减少,几年内浓度可能会略有增加,具体取决于负补给量变化的幅度。我们确定了补给的触发水平,在此之上,the的浓度/出口突破曲线和超过最大污染物水平的时间会受到显着影响。此外,我们观察到,在控制平面上的污染物出口(被认为是导致人口下降的风险途径),除了某些极端情况外,受自然补给制度变化的影响可能很小。我们得出结论,应采用更频繁的采样和在源区附近进行现场监测,以更好地解释气候条件变化下的浓度异常。此外,维持瓶盖不仅对于隔离渗流带中的残留污染物至关重要,而且对于减少与未来降水变化相关的不确定性也至关重要。最后,应该采用通过适当的校准过程而不是保守模型实现的现实流动和运输模拟,以识别非平凡的权衡取舍,从而可以更好地分配资源以减少决策的不确定性。

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