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通过3H/3He确定的与补给时间相关的地下水水质趋势逆转的证明。

Demonstrating trend reversal of groundwater quality in relation to time of recharge determined by 3H/3He.

作者信息

Visser A, Broers H P, van der Grift B, Bierkens M F P

机构信息

Department of Physical Geography, Utrecht University, P.O. Box 80115, 3508 TC Utrecht, The Netherlands.

出版信息

Environ Pollut. 2007 Aug;148(3):797-807. doi: 10.1016/j.envpol.2007.01.027. Epub 2007 Mar 26.

Abstract

Recent EU legislation is directed to reverse the upward trends in the concentrations of agricultural pollutants in groundwater. However, uncertainty of the groundwater travel time towards the screens of the groundwater quality monitoring networks complicates the demonstration of trend reversal. We investigated whether trend reversal can be demonstrated by relating concentrations of pollutants in groundwater to the time of recharge, instead of the time of sampling. To do so, we used the travel time to monitoring screens in sandy agricultural areas in the Netherlands, determined by (3)H/(3)He groundwater dating. We observed that concentrations of conservative pollutants increased in groundwater recharged before 1985 and decreased after 1990. Thereby, we demonstrated trend reversal of groundwater quality. From this research we concluded that (3)H/(3)He dating can be used to facilitate (re)interpretation of existing groundwater quality data. The presented approach is widely applicable in areas with unconsolidated granular aquifers and large agricultural pressures on groundwater resources.

摘要

欧盟近期的立法旨在扭转地下水中农业污染物浓度上升的趋势。然而,地下水到达地下水质量监测网络监测井的运移时间存在不确定性,这使得趋势逆转的证明变得复杂。我们研究了是否可以通过将地下水中污染物的浓度与补给时间而非采样时间相关联来证明趋势逆转。为此,我们利用了通过³H/³He地下水测年法确定的荷兰沙质农业区地下水到达监测井的运移时间。我们观察到,保守性污染物在1985年之前补给的地下水中浓度增加,而在1990年之后浓度下降。由此,我们证明了地下水质量的趋势逆转。从这项研究中我们得出结论,³H/³He测年法可用于促进对现有地下水质量数据的(重新)解读。所提出的方法广泛适用于具有未固结粒状含水层且地下水受农业压力较大的地区。

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