Calibration of a two-dimensional root water uptake model

被引:247
作者
Vrugt, JA
Hopmans, JW [1 ]
Simunek, J
机构
[1] Univ Calif Davis, Hydrol Program, Dept Land Air & Water Resources, Davis, CA 95616 USA
[2] Univ Amsterdam, Inst Biodivers & Ecosyst Dynam, NL-1018 VZ Amsterdam, Netherlands
[3] Univ Calif Riverside, USDA, US Salin Lab, Riverside, CA 95207 USA
关键词
D O I
10.2136/sssaj2001.6541027x
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Although solutions of multidimensional transient water flow can be obtained by numerical modeling, their application may be limited in part as root water uptake is generally considered to be one-dimensional only. The objective of this study was to develop and test a two-dimensional root water uptake model, which can be incorporated into numerical multidimensional flow models. The two-dimensional uptake model is based on the model by Raats, but is extended with a radial component. Subsequently, the root water uptake model was incorporated into a two-dimensional flow model, and root water uptake parameters were optimized, minimizing the residuals between measured and simulated water content data. Water content was measured around a sprinkler-irrigated almond tree (Prunus laurocerasus M-J.Roem) for a 16-d period at 25 locations, following irrigation. To calibrate the flow and root water uptake model, a genetic algorithm (GA) was used to find the approximate global minimum of the optimized parameter space. The final fitting parameters were determined using the Simplex algorithm (SA). With the optimized root water uptake parameters, simulated and measured water contents during the 16-d period were in excellent agreement, with R-2 values generally ranging between 0.94 and 0.99 and a root mean squared error (RMSE) of 0.015 m(3) m(-3). The developed root water uptake model is extremely flexible and allows spatial variations of water uptake as influenced by nonuniform (drip irrigation) and uniform water application patterns.
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收藏
页码:1027 / 1037
页数:11
相关论文
共 38 条
[1]   Spatial and temporal distribution of soil water balance for a drip-irrigated almond tree [J].
Andreu, L ;
Hopmans, JW ;
Schwankl, LJ .
AGRICULTURAL WATER MANAGEMENT, 1997, 35 (1-2) :123-146
[2]  
[Anonymous], 1987, 121 USDA ARS US SAL
[3]  
[Anonymous], IGWMCTPS53 COL SCH M
[4]  
[Anonymous], CALIFORNIA IRRIGATIO
[5]  
Back T, 1996, EVOLUTIONARY ALGORIT
[6]   Maximum rooting depth of vegetation types at the global scale [J].
Canadell, J ;
Jackson, RB ;
Ehleringer, JR ;
Mooney, HA ;
Sala, OE ;
Schulze, ED .
OECOLOGIA, 1996, 108 (04) :583-595
[7]   A GENERAL MASS-CONSERVATIVE NUMERICAL-SOLUTION FOR THE UNSATURATED FLOW EQUATION [J].
CELIA, MA ;
BOULOUTAS, ET ;
ZARBA, RL .
WATER RESOURCES RESEARCH, 1990, 26 (07) :1483-1496
[8]   SIMULTANEOUS MODELING OF TRANSIENT 3-DIMENSIONAL ROOT-GROWTH AND SOIL-WATER FLOW [J].
CLAUSNITZER, V ;
HOPMANS, JW .
PLANT AND SOIL, 1994, 164 (02) :299-314
[9]   ROOTZONE PROCESSES AND THE EFFICIENT USE OF IRRIGATION WATER [J].
CLOTHIER, BE ;
GREEN, SR .
AGRICULTURAL WATER MANAGEMENT, 1994, 25 (01) :1-12
[10]  
Coelho FE, 1996, SOIL SCI SOC AM J, V60, P1039, DOI 10.2136/sssaj1996.03615995006000040012x