Feasibility analysis of using inverse modeling for estimating natural groundwater recharge from a large-scale soil moisture monitoring network

被引:45
作者
Wang, Tiejun [1 ]
Franz, Trenton E. [1 ]
Yue, Weifeng [1 ,2 ]
Szilagyi, Jozsef [1 ,3 ]
Zlotnik, Vitaly A. [4 ]
You, Jinsheng [1 ]
Chen, Xunhong [1 ]
Shulski, Martha D. [1 ]
Young, Aaron [1 ]
机构
[1] Univ Nebraska, Sch Nat Resources, Hardin Hall,3310 Holdrege St, Lincoln, NE 68583 USA
[2] Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China
[3] Budapest Univ Technol & Econ, Dept Hydraul & Water Resources Engn, Budapest, Hungary
[4] Univ Nebraska, Dept Earth & Atmospher Sci, 214 Bessey Hall, Lincoln, NE 68588 USA
基金
美国国家科学基金会;
关键词
Groundwater recharge; Inverse modeling; Vadose zone model; Soil moisture; Automated Weather Data Network; NEBRASKA SAND HILLS; HYDRAULIC CONDUCTIVITY; TEMPORAL STABILITY; WATER-BALANCE; EVAPOTRANSPIRATION; MODIS; FLOW; IMPACT; PRECIPITATION; DISTRIBUTIONS;
D O I
10.1016/j.jhydrol.2015.12.019
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Despite the importance of groundwater recharge (GR), its accurate estimation still remains one of the most challenging tasks in the field of hydrology. In this study, with the help of inverse modeling, long-term (6 years) soil moisture data at 34 sites from the Automated Weather Data Network (AWDN) were used to estimate the spatial distribution of GR across Nebraska, USA, where significant spatial variability exists in soil properties and precipitation (P). To ensure the generality of this study and its potential broad applications, data from public domains and literature were used to parameterize the standard Hydrus-1D model. Although observed soil moisture differed significantly across the AWDN sites mainly due to the variations in P and soil properties, the simulations were able to capture the dynamics of observed soil moisture under different climatic and soil conditions. The inferred mean annual GR from the calibrated models varied over three orders of magnitude across the study area. To assess the uncertainties of the approach, estimates of GR and actual evapotranspiration (ETa) from the calibrated models were compared to the GR and ETa obtained from other techniques in the study area (e.g., remote sensing, tracers, and regional water balance). Comparison clearly demonstrated the feasibility of inverse modeling and large-scale (>10(4) km(2)) soil moisture monitoring networks for estimating GR. In addition, the model results were used to further examine the impacts of climate and soil on GR. The data showed that both P and soil properties had significant impacts on GR in the study area with coarser soils generating higher GR; however, different relationships between GR and P emerged at the AWDN sites, defined by local climatic and soil conditions. In general, positive correlations existed between annual GR and P for the sites with coarser-textured soils or under wetter climatic conditions. With the rapidly expanding soil moisture monitoring networks around the globe, this study may have important applications in aiding water resources management in different regions. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:250 / 265
页数:16
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