Abstract
The North China Plain (NCP) is one of the places where the groundwater is most over-exploited in the world. Currently, our understanding on the spatiotemporal variability of the cones of depression in this region is fragmentary. This study intends to simulate the cones of depression in the shallow aquifer across the entire NCP during the whole period from 1960 to 2011. During the simulation, the dominant role of anthropogenic activities is emphasized and carefully taken into account using a Neural Network Algorithm. The results show that cones of depression in the NCP were formed in 1970s and continuously expanded. Their centers were getting deeper with an increasing degree of groundwater exploitation. This simulation provides valuable insights for developing more sustainable groundwater management options after the implementation of the South-to-NorthWater Diversion Project (SNWDP), which is a very important surface water project in China in the near future. The numerical model in this paper is built by MODFLOW, with pumpage data completed by neural network algorithm and hydrogeological parameters calibrated by simulated annealing algorithm. Based on our long-term numerical model for regional groundwater flow in the NCP, one exploitation limitation strategy after the implementation of SNWDP is studied in this paper. The results indicate that the SNWDP is beneficial for groundwater recovery in the NCP. A number of immense groundwater cones will gradually shrink. However, the recovery of the groundwater environment in the NCP will require a long time.
Highlights
Water shortage is a common phenomenon due to increasing population, expanding areas of irrigated agriculture and growing economic development
Understanding of processes of groundwater depletion under anthropogenic activities and climate change is significantly important for sustainable groundwater utilization [4]
From the results of simulation, we can see that most of the cones of depression in shallow aquifers in the North China Plain (NCP) were located in the piedmont clinoplains and the western part of the flood plain, where most of the groundwater supply is from the shallow aquifers [10]
Summary
Water shortage is a common phenomenon due to increasing population, expanding areas of irrigated agriculture and growing economic development. Groundwater is of fundamental significance to meet the increasing water demand [1]. The total global groundwater depletion has increased from 126 km a−1 in 1960 to 283 km a−1 in 2000 in subhumid to arid areas [2], owing to increased groundwater abstraction, especially in the world’s major agricultural regions, including northwest. The efficiency of implementing groundwater protection or recovery measures needs quantitative appraisal of aquifer evolution based on reliable data [3] and based on the relationship among different aquifers [5]. Numerical modeling of groundwater flow can provide quantitative insight into sustainability [6]. The North China Plain (NCP) is an excellent example covering these issues
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