Impacts of water saving on groundwater balance in a large-scale arid irrigation district, Northwest China

被引:30
|
作者
Yue, Weifeng [1 ,3 ]
Liu, Xianze [1 ]
Wang, Tiejun [2 ,3 ]
Chen, Xunhong [3 ]
机构
[1] Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China
[2] Tianjin Univ, Inst Surface Earth Syst Sci, Tianjin 300072, Peoples R China
[3] Univ Nebraska, Sch Nat Resources, Hardin Hall,3310 Holdrege St, Lincoln, NE 68583 USA
基金
中国国家自然科学基金;
关键词
SURFACE-WATER; SOIL-MOISTURE; RECHARGE; MODEL; TABLE; BASIN; RESOURCES; SALINITY; DYNAMICS; EVAPOTRANSPIRATION;
D O I
10.1007/s00271-016-0504-x
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Water saving practices are essential for sustainable use of water resources in semiarid regions. To understand the impacts of different water saving measures on groundwater resources, the Hetao Irrigation District in Northwest China was chosen in this study. Based on the data from 1991 to 2010, a groundwater balance model was calibrated and validated. The simulation results showed that irrigation-induced infiltration (92 % of the total groundwater recharge) and groundwater evaporation (92 % of the total groundwater discharge) were the primary factors controlling groundwater table fluctuations during irrigation seasons. The impacts of different water saving scenarios on groundwater balance components were then evaluated. The results revealed that the conjunctive use of water resources was the most effective way to improve water use efficiency (reducing surface water diversions by 52 %) and the depth to groundwater table increased by up to 79 cm. However, deeper groundwater tables may have a negative effect on crop growth due to reduced upward fluxes of groundwater into root zones. Therefore, future studies are needed to evaluate the impacts of different water saving measures on both water resources and crop yields. The results of this study provide further insights into effectively managing water resources in water-limited agricultural areas.
引用
收藏
页码:297 / 312
页数:16
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