Multistep optimization of HyPix model for flexible vertical scaling of soil hydraulic parameters
Metadatos
Mostrar el registro completo del ítemEditorial
Elsevier
Materia
Variably saturated flow Vertical discretisation Multistep optimisation Inverse modelling Soil hydraulic properties Non-uniqueness Julia language
Fecha
2022-07-31Referencia bibliográfica
J.A.P. Pollacco... [et al.]. Multistep optimization of HyPix model for flexible vertical scaling of soil hydraulic parameters, Environmental Modelling & Software, Volume 156, 2022, 105472, ISSN 1364-8152, [https://doi.org/10.1016/j.envsoft.2022.105472]
Patrocinador
New Zealand Ministry of Business, Innovation and Employment throught the ‘Winning Against Wildings, C09X1611’; ‘Next Generation S-map, C09X1612’ research programmes; y University of Granada/CBUA, SpainResumen
Efficient simulation of water-flow processes in the vadose zone is crucial to increase agricultural productivity
within environmental limits. This requires deriving detailed soil hydraulic parameters of the soil profile that is
highly challenging, particularly for heterogeneous soils. We therefore developed an alternative indirect methodology to calibrate the hydraulic parameters from soil water content time series measured at multiple depths by
using the new physically based hydrological model HyPix.
We propose a novel, efficient, multistep optimization algorithm for layered soils that derives an optimal set of
hydraulic parameters for a desired number of soil layers. For each selected soil layer, HyPix derives five physical,
bimodal, Kosugi hydraulic parameters that describe the soil water retention and hydraulic conductivity by using
a novel algorithm that reduces the degree of sensitivity and freedom of the parameters. The optimization algorithm upscales the soil hydraulic parameters by gradually incorporating the soil heterogeneity. This method
overcomes the problems associated with optimization of the hydraulic parameters of each layer individually,
which leads to poor results because it does not represent the cohesive soil water dynamics across the unsaturated
zone.
We tested the method using soil water content measurements at different depths at five heterogeneous
experimental sites in New Zealand. We show how the accuracy of the simulated water balance components
increases with the number of soil layers. The multistep optimization upscales a detailed, layered profile of soil
hydraulic parameters into a model with fewer layers. The methodology developed provides an estimate of the
uncertainty of using a reduced number of soil layers. We also show that a pedological description can provide an
indication of the minimum soil layers of vertical discretization required to accurately compute the soil water
balance components.