|
|
||||||||
a Dep. of Plants, Soils, and Biometeorology, 4820 Old Main Hill, Utah State Univ., Logan, UT 84322-4820
b Dep. of Soil and Water Sci., Faculty of Agricultural, Food, and Environmental Sci., POB 12, Rehovot 76100, Israel
* Corresponding author (ldud{at}cc.usu.edu)
Received 19 December 2002.
Because transpiration is often the largest component of the water budget in arid systems, the efficacy of computer simulation models as predictors of water and salt movement is predicated on their ability to predict transpiration. The objective of this study was to improve the root-sink term for water extraction and thus improve predictions of transpiration. The root-sink terms often use either a transpiration-apportioning (TA) empirical function for the plant response to the soil matric and osmotic potential or a potential-flow (PF) function. Three root-sink terms, a TA formulation, a PF formulation, and a combination of the two (PFTA, a TA function for computing water uptake in response to salinity and a PF function for computing water uptake in response to water availability) were coded into a simulation model, and model predictions were compared with field-collected data. When predicted and measured relative yields (yield/yieldmax) were compared, the PF produced the poorest agreement with data (y = 0.8741x + 0.0251), the TA gave better agreement (y = 0.9283x + 0.0476), and PFTA provided the best agreement (y = 0.9909x + 0.0430). The plant and plantsoil based formulation predicted the salinity profile at the end of the field experiment under conditions of high salinity (EC irrigation water = 6.0 dS m-1) and irrigation equal to potential evaporation. The plantsoil formulation was the better predictor under the same salinity condition with irrigation at 40% of potential evaporation. The simulated evolution of the water content and salinity profile across time was also examined.
Abbreviations: PF, potential-flow function PFTA, combination of potential-flow and transition-apportioning functions TA, transpiration-apportioning function
This article has been cited by other articles:
![]() |
L. M. Dudley, A. Ben-Gal, and N. Lazarovitch Drainage Water Reuse: Biological, Physical, and Technological Considerations for System Management J. Environ. Qual., September 2, 2008; 37(5_Supplement): S-25 - S-35. [Abstract] [Full Text] [PDF] |
||||
![]() |
E. Segal, T. Kushnir, Y. Mualem, and U. Shani Water Uptake and Hydraulics of the Root Hair Rhizosphere Vadose Zone J., August 1, 2008; 7(3): 1027 - 1034. [Abstract] [Full Text] [PDF] |
||||
![]() |
L. M. Dudley, A. Ben-Gal, and U. Shani Influence of Plant, Soil, and Water on the Leaching Fraction Vadose Zone J., April 14, 2008; 7(2): 420 - 425. [Abstract] [Full Text] [PDF] |
||||
![]() |
H. Fujimaki, Y. Ando, Y. Cui, and M. Inoue Parameter Estimation of a Root Water Uptake Model under Salinity Stress Vadose Zone J., January 23, 2008; 7(1): 31 - 38. [Abstract] [Full Text] [PDF] |
||||
![]() |
T. H. Skaggs, P. J. Shouse, and J. A. Poss Irrigating Forage Crops with Saline Waters: 2. Modeling Root Uptake and Drainage Vadose Zone J., June 21, 2006; 5(3): 824 - 837. [Abstract] [Full Text] [PDF] |
||||
![]() |
U. Shani, A. Ben-Gal, and L. M. Dudley Environmental Implications of Adopting a Dominant Factor Approach to Salinity Management J. Environ. Qual., August 9, 2005; 34(5): 1455 - 1460. [Abstract] [Full Text] [PDF] |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Journal of Natural Resources and Life Sciences Education |
Soil Science Society of America Journal | ||||
| Journal of Plant Registrations | Journal of Environmental Quality |
The Plant Genome | |||