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Predicting land-use change and its impact on the groundwater system of the Kleine Nete catchment, Belgium

机译:预测比利时Kleine Nete流域的土地利用变化及其对地下水系统的影响

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Land-use changes are frequently indicated to be one of the main human-induced factors influencing the groundwater system. For land-use change, groundwater research has mainly focused on the change in water quality thereby neglecting changes in quantity. The objective of this paper is to assess the impact of land-use changes, from 2000 until 2020, on the hydrological balance and in particular on groundwater quantity, as results from a case study in the Kleine Nete basin, Belgium. New is that this study tests a methodology, which couples a land-use change model with a water balance and a steady-state groundwater model. Four future land-use scenarios (A1, A2, B1 and B2) based on the Special Report on Emission Scenarios (SRES) are modelled with the CLUE-S model. Water balance components, groundwater level and baseflow are simulated using the WetSpass model in conjunction with a steady-state MODFLOW groundwater flow model. Results show that the average recharge decreases with 2.9, 1.6, 1.8 and 0.8% for scenario A1, A2, B1 and B2, respectively, over the 20 covered years. The predicted reduction in recharge results in a small decrease of the average groundwater level in the basin, ranging from 2.5 cm for scenario A1 to 0.9 cm for scenario B2, and a reduction of the baseflow with maximum 2.3% and minimum 0.7% for scenario A1 and B2, respectively. Although these averages appear to indicate small changes in the groundwater system, spatial analysis shows that much larger changes are located near the major cities in the study area. Hence, spatial planning should take better account of effects of land-use change on the groundwater system and define mitigating actions for reducing the negative impacts of land-use change.
机译:人们经常指出,土地利用变化是影响地下水系统的主要人为因素之一。对于土地利用变化,地下水研究主要集中在水质变化上,而忽略了数量变化。本文的目的是评估从2000年到2020年土地利用变化对水文平衡,尤其是对地下水量的影响,这是根据比利时克莱因内特盆地的案例研究得出的结果。新的是,这项研究测试了一种方法,该方法将土地利用变化模型与水平衡和稳态地下水模型结合在一起。使用CLUE-S模型对基于排放情景特别报告(SRES)的四个未来土地使用情景(A1,A2,B1和B2)进行建模。结合WetSpass模型和稳态MODFLOW地下水流模型对水平衡成分,地下水位和基流进行了模拟。结果表明,在20年覆盖的情况下,方案A1,A2,B1和B2的平均充值分别下降了2.9%,1.6%,1.8%和0.8%。预计补给量的减少会导致流域中的平均地下水位小幅下降,范围从方案A1的2.5厘米到方案B2的0.9厘米,并且方案A1的基流减少最大2.3%和最小0.7%和B2分别。尽管这些平均值似乎表明了地下水系统的微小变化,但空间分析表明,更大的变化位于研究区域的主要城市附近。因此,空间规划应更好地考虑土地利用变化对地下水系统的影响,并确定缓解措施,以减少土地利用变化的负面影响。

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