Model for Nonlinear Root Water Uptake Parameter

• Published in: Journal of irrigation and drainage engineering Vol. 138; no. 10; pp. 905 - 917
• Main Authors: Shankar, Vijay, Hari Prasad, K. S, Ojha, C. S. P, Govindaraju, Rao S
• Format: Journal Article
• Language: English
• Published: Reston, VA American Society of Civil Engineers 01.10.2012
• Subjects: Agricultural and forest climatology and meteorology. Irrigation. Drainage; Agricultural and forest meteorology; Agronomy. Soil science and plant productions; Biological and medical sciences; Fundamental and applied biological sciences. Psychology; General agronomy. Plant production; Irrigation. Drainage; Technical Papers; Water balance and requirements. Evapotranspiration; Irrigation; Parameters; Root; Simulation models; Soil moisture; Hydraulics; Crops; Water use; Modeling; Transpiration; Evapotranspiration; Soil water; Nonlinearity; Water absorption; Simulation model; Root uptake
• ISSN: 0733-9437; 1943-4774
• DOI: 10.1061/(ASCE)IR.1943-4774.0000469

AbstractAn empirical relationship is developed for the nonlinear root water uptake parameter in the O-R moisture uptake model from easily measurable plant physiological parameters, such as maximum daily transpiration, maximum root depth, and time to attain the maximum transpiration. A nondimensional parameter, termed specific transpiration, that involves the plant physiological parameters is used in this empirical relationship. Data for determining this relationship are obtained by minimizing the deviations between the field observed moisture depletions of 28 crops reported in the literature, and the Richards equation–based numerically simulated soil moisture depletions combined with the moisture uptake model accounting for root water uptake. In addition to cross-validation, field experiments on three Indian crops (maize, Indian mustard, and wheat) are conducted to further validate the proposed empirical relationship. Comparisons of model predictions with field observations of soil moisture profiles and moisture depletions in different layers of the root zone show good agreement during different stages of crop growth. The results highlight the utility of the developed equation for modeling root water uptake over a wide range of crops.