Shu LC, Jing YD, Huang XD, Yu ZB, Wang ZL (2012) On the development of improved empirical formulas for calculating the phreatic water evaporation for bare land. Rong LS, Shu LC, Wang MM, Deng ZB (2009) Study on estimation method of ecological water level of reasonable groundwater-case study on lower reaches of the Tarim river. ![]() Prakashan CV, Speelman S, van Huylenbroeck G (2013) Estimating the impact of water pricing on water use efficiency in semi-arid cropping system: an application of probabilistically constrained nonparametric efficiency analysis. Pan XF, Yan BX (2011) Effects of land use and changes in cover on the transformation and transportation of iron: a case study of the Sanjiang Plain, Northeast China. Luo YF, Mao YL, Peng SZ, Zheng Q, Wang WG, Jiao CY, Feng YH (2013) Modified Aver’yanov’s phreatic evaporation equations under crop growing. Liu CM, Zhang XY, You BZ (1998) Determination of daily evaporation and evapotranspiration of winter wheat field by large-scale weighting lysimeter and micro lysimeter. Li YF (2013) Study on the eco-environmental changes in Sanjiang Plain during recent years. Krause S, Heathwaite AL, Miller F (2007) Groundwater-dependent wetlands in the UK and Ireland: controls, functioning and assessing the likelihood of damage from human activities. Herrea-Pantoja M, Hiscock KM, Boar RR (2012) The potential impact of climate change on groundwater-fed wetlands in eastern England. Ge F, Wang Z (2004) The application and current condition of Lysimeter. Ĭrosbie RS, Scanlon BR, Mpelasoka FS, Reedy RC, Gates JB, Zhang L (2013) Potential climate change effects on groundwater recharge in the High Plains Aquifer, USA. Ĭarol E, Kruse E, Mancuso M (2013) Local and regional water flow quantification in groundwater-dependent wetlands. J Am Water Resour Assoc 49:519–533Ĭao YJ, Tang CY, Song XF, Liu CM, Zhang YH (2012) Characteristics of nitrate in major rivers and aquifers of the Sanjiang Plain. Knowledge of the variation and influence factors of EDSG for a certain plant system and the current shallow groundwater condition in the higher latitude region can be a key to the development of preventive actions for large quantity pumping groundwater and protection regional and sustainable development of irrigated agriculture.īeamer JP, Justin LH, Charles GM, Greg MP (2013) Estimation annual groundwater evaporation from phreatic in the great basin using land sat and flux tower measurements. We also identified an area of 3.86 × 10 10 m 2, which accounting for 35.3% of the entire Sanjiang Plain, has exceeded the ESGD by over exploited for years. ![]() ![]() Many factors including climate, soil parameters, vegetation and topography affected the EDSG. Spatially, the sites, which were in the northeast and center had the deepest and the shallowest EDSG, whereby, indicate that it has higher and lower pumping potential capacity. The study showed a large spatial variation of EDSG in the region. In this study, the ratio of actual groundwater depth and EDSG (RAE) method was used to understand the spatial variability of EDSG in the Sanjiang Plain, one of China’s largest grain production bases and China’s largest inland freshwater wetland region. ![]() Accurate estimation of extinction depth of shallow groundwater (EDSG) and identification of its influence factors are important for sustainable management of groundwater resources, ecological protection, and human health in intensively irrigated region.
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