Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor

A substantial number of models predicting the soil moisture characteristic curve (SMC) from particle size distribution (PSD) data underestimate the dry range of the SMC especially in soils with high clay and organic matter contents. In this study, we applied a continuous form of the PSD model to pre...

Full description

Bibliographic Details
Main Authors: F. Meskini-Vishkaee, M. H. Mohammadi, M. Vanclooster
Format: Article
Language:English
Published: Copernicus Publications 2014-10-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/18/4053/2014/hess-18-4053-2014.pdf
id doaj-ac62210a99094c25b533fa754006f9c4
record_format Article
spelling doaj-ac62210a99094c25b533fa754006f9c42020-11-24T20:46:01ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382014-10-0118104053406310.5194/hess-18-4053-2014Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factorF. Meskini-Vishkaee0M. H. Mohammadi1M. Vanclooster2Department of Soil Science, Faculty of Agriculture, University of Zanjan, Zanjan, IranDepartment of Soil Science, Faculty of Agriculture, University of Zanjan, Zanjan, IranEarth and Life Institute, Environmental Sciences, Univ. Catholique de Louvain, Croix du Sud 2, Bte 2, 1348 Louvain-la-Neuve, BelgiumA substantial number of models predicting the soil moisture characteristic curve (SMC) from particle size distribution (PSD) data underestimate the dry range of the SMC especially in soils with high clay and organic matter contents. In this study, we applied a continuous form of the PSD model to predict the SMC, and subsequently we developed a physically based scaling approach to reduce the model's bias at the dry range of the SMC. The soil particle packing density was considered as a metric of soil structure and used to define a soil particle packing scaling factor. This factor was subsequently integrated in the conceptual SMC prediction model. The model was tested on 82 soils, selected from the UNSODA database. The results show that the scaling approach properly estimates the SMC for all soil samples. In comparison to the original conceptual SMC model without scaling, the scaling approach improves the model estimations on average by 30%. Improvements were particularly significant for the fine- and medium-textured soils. Since the scaling approach is parsimonious and does not rely on additional empirical parameters, we conclude that this approach may be used for estimating SMC at the larger field scale from basic soil data.http://www.hydrol-earth-syst-sci.net/18/4053/2014/hess-18-4053-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author F. Meskini-Vishkaee
M. H. Mohammadi
M. Vanclooster
spellingShingle F. Meskini-Vishkaee
M. H. Mohammadi
M. Vanclooster
Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor
Hydrology and Earth System Sciences
author_facet F. Meskini-Vishkaee
M. H. Mohammadi
M. Vanclooster
author_sort F. Meskini-Vishkaee
title Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor
title_short Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor
title_full Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor
title_fullStr Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor
title_full_unstemmed Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor
title_sort predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2014-10-01
description A substantial number of models predicting the soil moisture characteristic curve (SMC) from particle size distribution (PSD) data underestimate the dry range of the SMC especially in soils with high clay and organic matter contents. In this study, we applied a continuous form of the PSD model to predict the SMC, and subsequently we developed a physically based scaling approach to reduce the model's bias at the dry range of the SMC. The soil particle packing density was considered as a metric of soil structure and used to define a soil particle packing scaling factor. This factor was subsequently integrated in the conceptual SMC prediction model. The model was tested on 82 soils, selected from the UNSODA database. The results show that the scaling approach properly estimates the SMC for all soil samples. In comparison to the original conceptual SMC model without scaling, the scaling approach improves the model estimations on average by 30%. Improvements were particularly significant for the fine- and medium-textured soils. Since the scaling approach is parsimonious and does not rely on additional empirical parameters, we conclude that this approach may be used for estimating SMC at the larger field scale from basic soil data.
url http://www.hydrol-earth-syst-sci.net/18/4053/2014/hess-18-4053-2014.pdf
work_keys_str_mv AT fmeskinivishkaee predictingthesoilmoistureretentioncurvefromsoilparticlesizedistributionandbulkdensitydatausingapackingdensityscalingfactor
AT mhmohammadi predictingthesoilmoistureretentioncurvefromsoilparticlesizedistributionandbulkdensitydatausingapackingdensityscalingfactor
AT mvanclooster predictingthesoilmoistureretentioncurvefromsoilparticlesizedistributionandbulkdensitydatausingapackingdensityscalingfactor
_version_ 1716813370058866688