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首页> 外文期刊>Hydrology and Earth System Sciences >Mass transport of contaminated soil released into surface water by landslides (G?ta River, SW Sweden)
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Mass transport of contaminated soil released into surface water by landslides (G?ta River, SW Sweden)

机译:由滑坡释放到地表水中的受污染土壤的大规模运输(瑞典西南部Gta河)

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摘要

Landslides of contaminated soil into surface water represent an overlooked exposure pathway that has not been addressed properly in existing risk analysis for landslide hazard, contaminated land, or river basin management. A landslide of contaminated soil into surface water implies an instantaneous exposure of the water to the soil, dramatically changing the prerequisites for the mobilisation and transport of pollutants. In this study, an analytical approach is taken to simulate the transport of suspended matter released in connection with landslides into rivers. Different analytical solutions to the advection-dispersion equation (ADE) were tested against the measured data from the shallow rotational, retrogressive landslide in clayey sediments that took place in 1993 on the G?ta River, SW Sweden. The landslide encompassed three distinct events, namely an initial submerged slide, followed by a main slide, and a retrogressive slide. These slides generated three distinct and non-Gaussian peaks in the online turbidity recordings at the freshwater intake downstream the slide area. To our knowledge, this registration of the impact on a river of the sediment release from a landslide is one of few of its kind in the world and unique for Sweden. Considering the low frequency of such events, the data from this landslide are highly useful for evaluating how appropriate the ADE is to describe the effects of landslides into surface water. The results yielded realistic predictions of the measured variation in suspended particle matter (SPM) concentration, after proper calibration. For the three individual slides it was estimated that a total of about 0.6% of the total landslide mass went into suspension and was transported downstream. This release corresponds to about 1 to 2% of the annual suspended sediment transport for that river stretch. The studied landslide partly involved an industrial area, and by applying the analytical solution to estimate the transport of metals in the sediments, it was found that landslides may release a significant amount of pollutants if large contaminated areas are involved. However, further studies are needed to develop more detailed descriptions of the transport processes. There is also a need to increase the knowledge on possible environmental consequences in the near and far field, in a short- and long-time perspective. In summary, the release of pollutants should not be neglected in landslide risk assessments.
机译:被污染土壤滑入地表水的滑坡代表了一种被忽视的暴露途径,在现有的滑坡灾害,受污染土地或流域管理风险分析中并未适当解决。被污染的土壤滑入地表水中意味着水瞬间暴露在土壤中,从而极大地改变了污染物迁移和运输的前提条件。在这项研究中,采用一种分析方法来模拟与滑坡有关的悬浮物向河流的迁移。根据1993年在瑞典西南部Gta河上发生的黏性沉积物中的浅层旋转逆行滑坡的测量数据,测试了对流扩散方程(ADE)的不同解析解。滑坡包括三个不同的事件,即最初的淹没滑坡,随后的主滑坡和倒退滑坡。这些幻灯片在幻灯片区域下游的淡水进水口的在线浊度记录中生成了三个不同的非高斯峰。据我们所知,这种滑坡释放出的泥沙对河流的影响的记录是世界上为数不多的此类记录之一,并且在瑞典是独一无二的。考虑到此类事件发生的频率较低,来自该滑坡的数据对于评估ADE是否恰当地描述滑坡对地表水的影响非常有用。经过适当的校准,结果得出了对悬浮颗粒物(SPM)浓度测量变化的现实预测。对于这三个单独的滑坡,估计滑坡总质量中约有0.6%进入了悬浮状态并被输送到下游。该释放量相当于该河段每年悬浮泥沙输送量的1-2%。所研究的滑坡部分涉及工业区,通过应用分析解决方案估算沉积物中金属的运移,发现如果涉及大污染区,滑坡可能释放出大量污染物。但是,需要进一步的研究来发展对运输过程的更详细的描述。从短期和长期的角度来看,还需要增加对近场和远场可能的环境后果的认识。总之,在滑坡风险评估中不应忽略污染物的释放。

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