Civil Engineering Department, Faculty of Engineering, Minia University, Minia, 61111, Egypt.
Doctoral School of Earth Sciences, University of Pécs, Ifjúság útja 6, 7624, Pecs, Hungary.
Sci Rep. 2023 Mar 28;13(1):5061. doi: 10.1038/s41598-022-21259-4.
Land-use/land-cover (LULC) change is considered a key human factor influencing groundwater recharge in floodplains. Without accurate estimations, the impact of LULC change on water balance components may be either significantly understated or exaggerated. This paper assesses the impacts of LULC changes from 1990 to 2018 on water balance components and groundwater levels of the Drava floodplain, Hungary, where human interference has led to a critical environmental situation. In this study, a spatially-distributed water balance model (WetSpass-M), and a groundwater flow model (MODFLOW-NWT) were integrated to assess the impacts of LULC changes. The moderate expansion of built-up areas increased surface runoff, while the afforestation of arable land and meadows and the overgrowth of bare mudflats with willow shrubs increased evapotranspiration. As a consequence, total annual groundwater recharge decreased by 5.3 × 10 m in the floodplain with an average of 335 mm year and 317 mm year in 2012 and 2018, respectively. Moreover, an average groundwater level decline by 0.1 m is observed in the same period. Declined groundwater recharge, increased runoff, and evapotranspiration exerted a negative effect on water resources in the Drava basin. The approach tested in this paper allows temporal and spatial estimation of hydrological components under the changes of LULC, providing quantitative information for decision-makers and stakeholders to implement efficient and sustainable management of water resources in the Drava floodplain. The provided integrated model is also applicable to regionally.
土地利用/土地覆被(LULC)变化被认为是影响洪泛平原地下水补给的关键人为因素。如果没有准确的估计,LULC 变化对水量平衡组成部分的影响可能会被低估或夸大。本文评估了 1990 年至 2018 年 LULC 变化对匈牙利德拉瓦洪泛平原水量平衡组成部分和地下水位的影响,人类干扰导致了该地区的环境状况十分严峻。在这项研究中,一个空间分布式水量平衡模型(WetSpass-M)和一个地下水流动模型(MODFLOW-NWT)被集成,以评估 LULC 变化的影响。建成区适度扩张增加了地表径流量,而耕地、草地的造林以及柳树灌木对裸泥滩的过度生长增加了蒸散量。因此,洪泛平原的年总地下水补给量减少了 5.3×10 m,2012 年和 2018 年的平均地下水补给量分别为 335mm 年和 317mm 年。此外,同期观察到地下水位平均下降了 0.1 m。地下水补给减少、径流量增加和蒸散量增加对德拉瓦流域的水资源产生了负面影响。本文测试的方法允许在 LULC 变化下对水文组成部分进行时空估计,为决策者和利益相关者提供定量信息,以实现德拉瓦洪泛平原水资源的有效和可持续管理。所提供的综合模型也适用于区域。