• Papers

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• [1] Using pedotransfer functions in vadose zone models for estimating groundwater recharge in semiarid regions.
• [2] Using grain-size distribution methods for estimation of air permeability
• • [3] Field observations of regional controls of soil hydraulic properties on soil moisture spatial variability in different climate zones
  • [4] Assessing impacts of water saving on groundwater balance in a large-scale arid irrigation district, northwest China
  • [5] Assessing soil effects on temporal stability of absolute soil moisture content and soil moisture anomaly under different climatic conditions
  • [6] Evaluation of ecohydrologic model parsimony at local and regional scales in a semiarid grassland ecosystem
  • [7] Quantifying the impact of groundwater depth on evapotranspiration in a semi arid grassland region
  • [8] Impacts of devegetation on the temporal evolution of soil saturated hydraulic conductivity in a vegetated sand dune area
  • [9] Incorporation of globally available datasets into the cosmic-ray neutron probe method for estimating field scale soil water content
  • [10] Controls of soil hydraulic characteristics on modeling groundwater recharge under different climatic conditions
  • [11] Verification of numerical solutions of the Richards equation using a traveling wave solution
  • [12] Investigating soil controls on soil moisture spatial variability: numerical simulations and field observations
  • [13] Combined analysis of soil moisture measurements from roving and fixed cosmic-ray neutron probes for multi-scale real-time monitoring.
  • [14] A complementary relationship between actual and potential evapotranspiration and soil effects
  • [15] Feasibility analysis of using inverse modeling for estimating field-scale evapotranspiration in maize and soybean fields from soil water content monitoring networks
  • [16] Modeling the impacts of soil hydraulic properties on temporal stability of soil moisture under a semi-arid climate
  • [17] Spatial distributions of surface-layer saturated hydraulic conductivity and controlling factors on dam farmlands
  • [18] Spatiotemporal patterns of water table fluctuations and evapotranspiration induced by riparian vegetation in a semi-arid area
  • [19] Feasibility analysis of using inverse modeling for estimating natural groundwater recharge from a large-scale soil moisture monitoring network.
  • [20] Field evidence of a negative correlation between saturated hydraulic conductivity and soil carbon in a sandy soil.
  • [21] On the role of groundwater and soil texture in the regional water balance: An investigation of the Nebraska Sand Hills, USA
  • [22] Effect of vegetation on the temporal stability of soil moisture in grass-stabilized semi-arid sand dunes
  • [23] Using pedotransfer functions in vadose zone models for estimating groundwater recharge in semiarid regions
  • [24] Spatial trends in saturated hydraulic conductivity of vegetated dunes in the Nebraska Sand Hills: effects of depth and topography
  • [25] Interpretation of hydrologic trends from a water balance perspective: The role of groundwater storage in the Budyko hypothesis
  • [26] Feasibility analysis of using inverse modeling for estimating natural groundwater recharge from a large-scale soil moisture monitoring network.
  • [27] Spatiotemporal patterns of water table fluctuations and evapotranspiration induced by riparian vegetation in a semi-arid area.
  • [28] Combined analysis of soil moisture measurements from roving and fixed cosmic-ray neutron probes for multi-scale real-time monitoring.
  • [29] A complementary relationship between actual and potential evapotranspiration and soil effects.
  • [30] Effect of vegetation on the temporal stability of soil moisture in grass-stabilized semi-arid sand dunes.
  • [31] Modeling the impacts of soil hydraulic properties on temporal stability of soil moisture under a semi-arid climate.
  • [32] Interpretation of hydrologic trends from a water balance perspective: The role of groundwater storage in the Budyko hypothesis. W
  • [33] Controls of soil hydraulic characteristics on modeling groundwater recharge under different climatic conditions.
  • [34] Field evidence of a negative correlation between saturated hydraulic conductivity and soil carbon in a sandy soil.
  • [35] On the role of groundwater and soil texture in the regional water balance: An investigation of the Nebraska Sand Hills, USA.
  • [36] Spatial trends in saturated hydraulic conductivity of vegetated dunes in the Nebraska Sand Hills: effects of depth and topography.
  • [37] Investigating soil controls on soil moisture spatial variability: numerical simulations and field observations.
  • [38] On the use of the similar media concept for scaling soil air permeability
  • [39] Factors influencing the manganese release from the soils of a reservoir shore
  • [40] Evaluating climate and soil effects on regional soil moisture spatial variability using EOFs
  • [41] Evaluating controls of soil properties and climatic conditions on the use of an exponential filter for converting near surface to root zone soil moisture contents
  • [42] Implementation of evapotranspiration data assimilation with catchment scale distributed hydrological model via an ensemble Kalman filter
  • [43] A case study of field-scale maize irrigation patterns in Western Nebraska: Implications to water managers and recommendations for hyper-resolution land surface modelling