Field evaluation of a multicomponent solute transport model in soils irrigated with saline waters

被引:146
作者
Ramos, T. B. [1 ]
Simunek, J. [2 ]
Goncalves, M. C. [1 ,3 ]
Martins, J. C. [3 ]
Prazeres, A. [3 ]
Castanheira, N. L. [3 ]
Pereira, L. S. [1 ]
机构
[1] Univ Tecn Lisboa, Inst Agron, CEER Biosyst Engn, P-1349017 Lisbon, Portugal
[2] Univ Calif Riverside, Dept Environm Sci, Riverside, CA 92521 USA
[3] Inst Nacl Recursos Biol, L INIA, Estacao Agron Nacl, P-2784505 Oeiras, Portugal
关键词
HYDRUS-1D; Field experiment; Modeling; Soil salinity; Osmotic stress; Nitrogen leaching; SUBSURFACE DRIP IRRIGATION; SHALLOW GROUNDWATER; SALT ACCUMULATION; NITROGEN; CONDUCTIVITY; FERTIGATION; BASIN; CROP;
D O I
10.1016/j.jhydrol.2011.07.016
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Soil salinization, sodification, and non-point source pollution are among the most important and widespread environmental problems in agricultural regions with scarce water resources. Models evaluating these environmental problems should therefore consider an integrated approach to avoid favoring one problem over the other. The HYDRUS-1D software package was used to simulate water movement and solute transport in two complex experiments carried out under field conditions in Alvalade and Mitra, Portugal. The experiments involved irrigating maize with synthetic saline irrigation waters blended with fresh irrigation waters and waters with different nitrogen concentrations. The major ion chemistry module of HYDRUS-1D was used to model water contents (RMSE <= 0.04 cm(3) cm(-3)), the overall salinity given by the electrical conductivity of the soil solution (ECSW) (RMSE <= 2.35 dS m(-1)), the concentration of soluble cations Na+ (RMSE <= 13.86 mmol((c)) L-1), Ca2+ (RMSE <= 5.66 mmol((c)) L-1), Mg2+ (RMSE <= 4.16 mmol((c)) L-1), and SAR (RMSE <= 6.27 (mmol((c)) L-1)(0.5)) in different experimental plots. RMSE were always lower for the soil with coarse texture of Mitra. The standard HYDRUS solute transport module was used to model N-NH4+ (RMSE <= 0.07 mmol((c)) L-1) and N-NO3- (RMSE <= 2.60 mmol((c)) L-1) concentrations in the soil solution while either including or neglecting the effects of the osmotic stress on nutrient uptake. The model was able to successfully simulate root water and nutrient uptake reductions due to osmotic stress. Consequently, modeled fluxes of N-NH4+ and N-NO3- leached from the soil profiles increased due to the effects of the salinity stress on water and nutrient uptake. Possible causes of disagreements between the modeling and experimental data are discussed. HYDRUS-1D proved to be a powerful tool for analyzing solute concentrations related to overall soil salinity and nitrogen species. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:129 / 144
页数:16
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