Parameterization of soil hydraulic parameters for HYDRUS-3D simulation of soil water dynamics in a drip-irrigated orchard

被引:0
|
作者
Domúnguez-Niño J.M. [1 ]
Arbat G. [2 ]
Raij-Hoffman I. [3 ]
Kisekka I. [3 ]
Girona J. [1 ]
Casadesús J. [1 ]
机构
[1] Programme on Efficient Use of Water in Agriculture, Institute of Agrifood Research and Technology (IRTA), Parc de Gardeny (PCiTAL), Fruitcentre, Lleida
[2] Department of Chemical and Agricultural Engineering and Technology, University of Girona, Campus Montilivi s/n, Girona
[3] Department of Land, Air and Water Resources/Biological and Agricultural Engineering, University of California Davis, One Shields Avenue, PES 1110, Davis, 95616, CA
来源
Domúnguez-Niño, Jesús María (jesus.dominguez@irta.cat) | 1600年 / MDPI AG, Postfach, Basel, CH-4005, Switzerland卷 / 12期
关键词
HYDRUS-3D; HYPROP; Neutron probe; Rosetta; Simulation; Soil water content; Soil wetting patterns; Tensiometer; WP4C;
D O I
10.3390/W12071858
中图分类号
学科分类号
摘要
Although surface drip irrigation allows an efficient use ofwater in agriculture, the heterogeneous distribution of soil water complicates its optimal usage. Mathematical models can be used to simulate the dynamics ofwater in the soil belowa dripper and promote: a better understanding, and optimization, of the design of drip irrigation systems, their improved management and their monitoring with soil moisture sensors. The aim of this paper was to find the most appropriate configuration of HYDRUS-3D for simulating the soil water dynamics in a drip-irrigated orchard. Special emphasis was placed on the source of the soil hydraulic parameters. Simulations parameterized using the Rosetta approach were therefore compared with others parameterized using that of HYPROP + WP4C. The simulations were validated on a seasonal scale, against measurements made using a neutron probe, and on the time course of several days, against tensiometers. The results showed that the best agreement with soil moisture measurements was achieved with simulations parameterized from HYPROP + WP4C. It further improved when the shape parameter n was empirically calibrated from a subset of neutron probe measurements. The fit of the simulations with measurements was best at positions near the dripper and worsened at positions outside its wetting pattern and at depths of 80 cm or more. © 2020 by the authors.
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