石家庄市平原区地下水位变化特征分析及预测研究
[Abstract]:For a long time, with the rapid development of China's economy, water resources are increasingly short, especially in North China. In order to meet the needs of regional social development, the groundwater in North China has been overexploited for many years, which has caused serious environmental problems. The plain area of Shijiazhuang City is a typical area of overmining groundwater resources in North China Plain. Due to the long-term over-exploitation of groundwater and the imbalance of recharge and drainage, the groundwater level in Shijiazhuang Plain has dropped rapidly, and a number of underground water funnels have been formed in the area. In recent decades, the scale of groundwater funnel has become larger and caused geological environmental problems such as ground fissure, collapse and so on. In view of the situation that the groundwater level in Shijiazhuang City is constantly falling and the scope of the groundwater drop funnel is increasing, Shijiazhuang City has carried out comprehensive treatment of groundwater overmining. There are two main ways to control the situation. One is to strengthen the construction of the supporting project of the South-to-North Water transfer Project. To make full use of the Yangtze River water allocated by the South-to-North Water transfer to replace the groundwater mined in the water-receiving area, second, to implement groundwater pressure mining, and to combine water saving in construction, water saving and agronomic water saving through strengthening the construction of water-saving projects. Improve the efficiency and efficiency of industrial and agricultural water use, save groundwater resources and reduce groundwater exploitation. By collecting the historical data of groundwater level, groundwater exploitation, rainfall, gross national product (GNP) and so on from 1980 to 2015 in Shijiazhuang Plain area, this paper deals with the historical variation characteristics and rainfall of groundwater level and groundwater exploitation in Shijiazhuang Plain area. The relationship between gross national product (GNP) and groundwater level is analyzed. By using multivariate linear regression analysis and genetic BP neural network algorithm, the prediction model of groundwater buried depth in Shijiazhuang plain area was constructed, and the average groundwater buried depth in Shijiazhuang plain area was simulated. After comparing the simulation results of the two prediction models, The genetic BP neural network prediction model was selected to forecast and analyze the average buried depth of groundwater in Shijiazhuang Plain area in 2016-2021 under the conditions of comprehensive treatment of groundwater overexploitation and no comprehensive treatment of groundwater overexploitation. There are great differences in the speed and range of groundwater level decline in different regions of Shijiazhuang Plain area. In the west, north, northeast and southwest of Shijiazhuang, the decrease of groundwater level is relatively small, but in the middle, there is no significant difference between the two regions. In the south and east of China, the groundwater level has declined greatly, and the southeastern region is the most serious. By comparison, it is found that comprehensive treatment of groundwater overmining in Shijiazhuang City can effectively reduce the rate of groundwater level decline, and obtain better treatment effect in the future.
【学位授予单位】:华北水利水电大学
【学位级别】:硕士
【学位授予年份】:2017
【分类号】:P641.2
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