This article established groundwater flows differential equation mathematical model of San iiang Plain on the hydrology theory foundation, and used the analysis finite element method to liner change the differential e...This article established groundwater flows differential equation mathematical model of San iiang Plain on the hydrology theory foundation, and used the analysis finite element method to liner change the differential equation into the large-scale system of linear equations, it took linear equations as a part of constraint conditions of the optimized model, carried on the groundwater flow status equation and the optimized model the coupling, and carries on the solution with the Lingo software. The results indicated that this local shallow layer groundwater resources were rich and have the big development potential. But recent years water resources disposition was unreasonable and ground water mining quantity was oversized, these caused the region water flux to assume the drop tendency.展开更多
1. Introduction Sanjiang Plain is situated in northeast part of Heilongjiang Province in China. The area is 108,900km^2. The mountain and hill make up 39% and the plain makes up 61% in the whole plain area. The marshl...1. Introduction Sanjiang Plain is situated in northeast part of Heilongjiang Province in China. The area is 108,900km^2. The mountain and hill make up 39% and the plain makes up 61% in the whole plain area. The marshland is a special landscape of the plain. After the People’s Republic founding, the wasteland has been reclaimed 27,440,000ha. through three times of large scale reclaimation. The farmland has been enlarged three times in 35 years, in which the exploitation speed of state farm system is much faster than county system. Its farmland has been increased from original 7,267ha. to current 1,644,700ha.. The farmland increasing brings about raising of grain production to a great extent.展开更多
文摘This article established groundwater flows differential equation mathematical model of San iiang Plain on the hydrology theory foundation, and used the analysis finite element method to liner change the differential equation into the large-scale system of linear equations, it took linear equations as a part of constraint conditions of the optimized model, carried on the groundwater flow status equation and the optimized model the coupling, and carries on the solution with the Lingo software. The results indicated that this local shallow layer groundwater resources were rich and have the big development potential. But recent years water resources disposition was unreasonable and ground water mining quantity was oversized, these caused the region water flux to assume the drop tendency.
文摘1. Introduction Sanjiang Plain is situated in northeast part of Heilongjiang Province in China. The area is 108,900km^2. The mountain and hill make up 39% and the plain makes up 61% in the whole plain area. The marshland is a special landscape of the plain. After the People’s Republic founding, the wasteland has been reclaimed 27,440,000ha. through three times of large scale reclaimation. The farmland has been enlarged three times in 35 years, in which the exploitation speed of state farm system is much faster than county system. Its farmland has been increased from original 7,267ha. to current 1,644,700ha.. The farmland increasing brings about raising of grain production to a great extent.
