3DMGAR: A Transient Quasi-3D Point-Source Green–Ampt Infiltration and Redistribution Model

Although Richards’ equation (RE) generally provides a good description of infiltration and water redistribution in soils, its numerical solutions can be computationally intensive or suffer from numerical instability and require extensive soil data. Simplified physically based approaches are often us...

Full description

Bibliographic Details
Main Authors: Leslie C. Gowdish, Rafael Muñoz-Carpena
Format: Article
Language:English
Published: Wiley 2018-12-01
Series:Vadose Zone Journal
Online Access:https://dl.sciencesocieties.org/publications/vzj/articles/17/1/180032
id doaj-94b95951e22e474fb564003eb55991e7
record_format Article
spelling doaj-94b95951e22e474fb564003eb55991e72020-11-25T02:58:16ZengWileyVadose Zone Journal1539-16632018-12-0117110.2136/vzj2018.02.00323DMGAR: A Transient Quasi-3D Point-Source Green–Ampt Infiltration and Redistribution ModelLeslie C. GowdishRafael Muñoz-CarpenaAlthough Richards’ equation (RE) generally provides a good description of infiltration and water redistribution in soils, its numerical solutions can be computationally intensive or suffer from numerical instability and require extensive soil data. Simplified physically based approaches are often used in many practical settings after validation against RE used as a benchmark. The purpose of this research was to develop and test an approximated physical model for simulating transient point-source infiltration and redistribution in a quasi three-dimensional flow domain. An existing three-dimensional Green–Ampt model that simulates only the infiltration phase is extended based on the one-dimensional modified Green–Ampt with redistribution (MGAR) method to calculate the three-dimensional soil water redistribution phase between point-source events. Comparison with the HYDRUS-2D numerical solution of RE showed the proposed model (3DMGAR) to provide satisfactory results for a broad range of soils. The ability of 3DMGAR to accurately and robustly simulate infiltration and redistribution for point-source water application time series is particularly important for cases with difficult Richards solutions, such as in sandy soils, to improve water application efficiency and decrease chemical leaching in many settings like crop fertigation, waste water disposal, and mitigation of climate-induced coastal salinization.https://dl.sciencesocieties.org/publications/vzj/articles/17/1/180032
collection DOAJ
language English
format Article
sources DOAJ
author Leslie C. Gowdish
Rafael Muñoz-Carpena
spellingShingle Leslie C. Gowdish
Rafael Muñoz-Carpena
3DMGAR: A Transient Quasi-3D Point-Source Green–Ampt Infiltration and Redistribution Model
Vadose Zone Journal
author_facet Leslie C. Gowdish
Rafael Muñoz-Carpena
author_sort Leslie C. Gowdish
title 3DMGAR: A Transient Quasi-3D Point-Source Green–Ampt Infiltration and Redistribution Model
title_short 3DMGAR: A Transient Quasi-3D Point-Source Green–Ampt Infiltration and Redistribution Model
title_full 3DMGAR: A Transient Quasi-3D Point-Source Green–Ampt Infiltration and Redistribution Model
title_fullStr 3DMGAR: A Transient Quasi-3D Point-Source Green–Ampt Infiltration and Redistribution Model
title_full_unstemmed 3DMGAR: A Transient Quasi-3D Point-Source Green–Ampt Infiltration and Redistribution Model
title_sort 3dmgar: a transient quasi-3d point-source green–ampt infiltration and redistribution model
publisher Wiley
series Vadose Zone Journal
issn 1539-1663
publishDate 2018-12-01
description Although Richards’ equation (RE) generally provides a good description of infiltration and water redistribution in soils, its numerical solutions can be computationally intensive or suffer from numerical instability and require extensive soil data. Simplified physically based approaches are often used in many practical settings after validation against RE used as a benchmark. The purpose of this research was to develop and test an approximated physical model for simulating transient point-source infiltration and redistribution in a quasi three-dimensional flow domain. An existing three-dimensional Green–Ampt model that simulates only the infiltration phase is extended based on the one-dimensional modified Green–Ampt with redistribution (MGAR) method to calculate the three-dimensional soil water redistribution phase between point-source events. Comparison with the HYDRUS-2D numerical solution of RE showed the proposed model (3DMGAR) to provide satisfactory results for a broad range of soils. The ability of 3DMGAR to accurately and robustly simulate infiltration and redistribution for point-source water application time series is particularly important for cases with difficult Richards solutions, such as in sandy soils, to improve water application efficiency and decrease chemical leaching in many settings like crop fertigation, waste water disposal, and mitigation of climate-induced coastal salinization.
url https://dl.sciencesocieties.org/publications/vzj/articles/17/1/180032
work_keys_str_mv AT lesliecgowdish 3dmgaratransientquasi3dpointsourcegreenamptinfiltrationandredistributionmodel
AT rafaelmunozcarpena 3dmgaratransientquasi3dpointsourcegreenamptinfiltrationandredistributionmodel
_version_ 1724707429934956544