A Comparative Investigation of Various Pedotransfer Functions and Their Impact on Hydrological Simulations

Soil hydraulic properties, which are basically saturated and unsaturated hydraulic conductivity and water retention characteristics, remarkably control the main hydrological processes in catchments. Thus, adequate parameterization of soils is one of the most important tasks in physically based catch...

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Main Authors: Hadis Mohajerani, Sonja Teschemacher, Markus C. Casper
Format: Article
Language:English
Published: MDPI AG 2021-05-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/10/1401
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spelling doaj-1b8d7cf88f164fa78b0be99594bfbc172021-06-01T00:18:24ZengMDPI AGWater2073-44412021-05-01131401140110.3390/w13101401A Comparative Investigation of Various Pedotransfer Functions and Their Impact on Hydrological SimulationsHadis Mohajerani0Sonja Teschemacher1Markus C. Casper2Department of Physical Geography, Faculty VI, University of Trier, Universitätsring 12, 54296 Trier, GermanyDepartment of Physical Geography, Faculty VI, University of Trier, Universitätsring 12, 54296 Trier, GermanyDepartment of Physical Geography, Faculty VI, University of Trier, Universitätsring 12, 54296 Trier, GermanySoil hydraulic properties, which are basically saturated and unsaturated hydraulic conductivity and water retention characteristics, remarkably control the main hydrological processes in catchments. Thus, adequate parameterization of soils is one of the most important tasks in physically based catchment modeling. To estimate these properties, the choice of the PTFs in a hydrological model is often made without taking the runoff characteristics of the catchment into consideration. Therefore, this study introduces a methodology to analyze the sensitivity of a catchment water balance model to the choice of the PTF. To do so, we define 11 scenarios including different combinations of PTFs to estimate the van Genuchten parameters and saturated hydraulic conductivity. We use a calibrated/validated hydrological model (WaSiM-ETH) as a baseline scenario. By altering the underlying PTFs, the effects on the hydraulic properties are quantified. Moreover, we analyze the resulting changes in the spatial/temporal variation of the total runoff and in particular, the runoff components at the catchment outlet. Results reveal that the water distribution in the hydrologic system varies considerably amongst different PTFs, and the water balance components are highly sensitive to the spatial structure of soil hydraulic properties. It is recommended that models be tested by careful consideration of PTFs and orienting the soil parameterization more towards representing a plausible hydrological behavior rather than focusing on matching the calibration data.https://www.mdpi.com/2073-4441/13/10/1401pedotransfer functionssoil hydraulic parameterizationcatchment water balancerunoff componentshydrologic modelingspatial pattern comparison
collection DOAJ
language English
format Article
sources DOAJ
author Hadis Mohajerani
Sonja Teschemacher
Markus C. Casper
spellingShingle Hadis Mohajerani
Sonja Teschemacher
Markus C. Casper
A Comparative Investigation of Various Pedotransfer Functions and Their Impact on Hydrological Simulations
Water
pedotransfer functions
soil hydraulic parameterization
catchment water balance
runoff components
hydrologic modeling
spatial pattern comparison
author_facet Hadis Mohajerani
Sonja Teschemacher
Markus C. Casper
author_sort Hadis Mohajerani
title A Comparative Investigation of Various Pedotransfer Functions and Their Impact on Hydrological Simulations
title_short A Comparative Investigation of Various Pedotransfer Functions and Their Impact on Hydrological Simulations
title_full A Comparative Investigation of Various Pedotransfer Functions and Their Impact on Hydrological Simulations
title_fullStr A Comparative Investigation of Various Pedotransfer Functions and Their Impact on Hydrological Simulations
title_full_unstemmed A Comparative Investigation of Various Pedotransfer Functions and Their Impact on Hydrological Simulations
title_sort comparative investigation of various pedotransfer functions and their impact on hydrological simulations
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-05-01
description Soil hydraulic properties, which are basically saturated and unsaturated hydraulic conductivity and water retention characteristics, remarkably control the main hydrological processes in catchments. Thus, adequate parameterization of soils is one of the most important tasks in physically based catchment modeling. To estimate these properties, the choice of the PTFs in a hydrological model is often made without taking the runoff characteristics of the catchment into consideration. Therefore, this study introduces a methodology to analyze the sensitivity of a catchment water balance model to the choice of the PTF. To do so, we define 11 scenarios including different combinations of PTFs to estimate the van Genuchten parameters and saturated hydraulic conductivity. We use a calibrated/validated hydrological model (WaSiM-ETH) as a baseline scenario. By altering the underlying PTFs, the effects on the hydraulic properties are quantified. Moreover, we analyze the resulting changes in the spatial/temporal variation of the total runoff and in particular, the runoff components at the catchment outlet. Results reveal that the water distribution in the hydrologic system varies considerably amongst different PTFs, and the water balance components are highly sensitive to the spatial structure of soil hydraulic properties. It is recommended that models be tested by careful consideration of PTFs and orienting the soil parameterization more towards representing a plausible hydrological behavior rather than focusing on matching the calibration data.
topic pedotransfer functions
soil hydraulic parameterization
catchment water balance
runoff components
hydrologic modeling
spatial pattern comparison
url https://www.mdpi.com/2073-4441/13/10/1401
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