LIU Mei-ying,MIN Lei-lei,SHEN Yan-jun
China Rural Water and Hydropower. 2017, (8):
80-85.
Download PDF
(
)
Knowledge map
 
Save
The Hebei Plain is one of the region with serious contradiction between supply and demand of water resources in China. Based on the daily data of groundwater depth collected in 11 monitoring sites from 2008 to 2014, this paper analyzed shallow groundwater dynamic variations in different regions of the Hebei Plain. The results showed that the average groundwater depths gradually decreased from the region of the piedmont plain to the region of the central plain, due to difference in groundwater exploitation. The fluctuation of inter annual groundwater level was no more than 3 meters in the region of the central plain. The groundwater level gradually decreased in the region of the piedmont plain. But it rose in some special area close to the reservoir because the increase of water storage of the reservoir and the decrease of the wheat planted area and the increase of precipitation. In the piedmont plain, the highest water level of these observed sites were in the period from February to March and the lowest were in the period from July to August, respectively. Meanwhile, highest water level in the period from April to June and lowest in September in the region of the central plain, respectively. The duration, changing rates and intra-annual distributions of the period of water level increase and decrease with great variations, due to the spatial differences of groundwater exploitation, land use, topography and landform, etc.