Moment analysis for modeling soil water distribution in furrow irrigation: Variable vs. constant ponding depths
Affiliation
Department of Soil, Water, and Environmental Sciences, College of Agriculture and Life Sciences, The University of ArizonaIssue Date
2021
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MDPI AGCitation
Kazemi, H., Sadraddini, A. A., Nazemi, A. H., & Sanchez, C. A. (2021). Moment analysis for modeling soil water distribution in furrow irrigation: Variable vs. Constant ponding depths. Water (Switzerland), 13(10).Journal
Water (Switzerland)Rights
Copyright © 2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Despite increasing use of pressurized irrigation methods, most irrigation projects world-wide still involve surface systems. Accurate estimation of the amount of infiltrating water and its spatial distribution in the soil is of great importance in the design and management of furrow irrigation systems. Moment analysis has previously been applied to describe the subsurface water distribution using input data from numerical simulations rather than field measured data, and as-suming a constant ponding depth in the furrow. A field experiment was conducted in a blocked-end level furrow at Maricopa Agricultural Center, Arizona, USA, to study the effect of time-variable ponding depths on soil water distribution and the resulting wetting bulb under real conditions in the field using moment analysis. The simulated volumetric soil water contents run with variable and constant (average) ponding depths using HYDRUS 2D/3D were almost identical, and both compared favorably with the field data. Hence, only the simulated soil water contents with variable ponding depths were used to calculate the moments. It was concluded that the fluctuating flow depth had no significant influence on the resulting time-evolving ellipses. This was related to the negligible 10-cm variation in ponding depths compared to the high negative matric potential of the unsaturated soil. © 2021 by the authors. Licensee MDPI, Basel, Switzerland.Note
Open access journalISSN
2073-4441Version
Final published versionae974a485f413a2113503eed53cd6c53
10.3390/w13101415
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Except where otherwise noted, this item's license is described as Copyright © 2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).