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Hydro-pedotransfer functions : A roadmap for future development

Authors :
Weber, Tobias Karl David
Weihermüller, Lutz
Nemes, Attila
Bechtold, Michel
Degré, Aurore
Diamantopoulos, Efstathios
Fatichi, Simone
Filipović, Vilim
Gupta, Surya
Hohenbrink, Tobias L.
Hirmas, Daniel R.
Jackisch, Conrad
de Jong Van Lier, Quirijn
Koestel, John
Lehmann, Peter
Marthews, Toby R.
Minasny, Budiman
Pagel, Holger
van der Ploeg, Martine
Shojaeezadeh, Shahab Aldin
Svane, Simon Fiil
Szabó, Brigitta
Vereecken, Harry
Verhoef, Anne
Young, Michael
Zeng, Yijian
Zhang, Yonggen
Bonetti, Sara
Weber, Tobias Karl David
Weihermüller, Lutz
Nemes, Attila
Bechtold, Michel
Degré, Aurore
Diamantopoulos, Efstathios
Fatichi, Simone
Filipović, Vilim
Gupta, Surya
Hohenbrink, Tobias L.
Hirmas, Daniel R.
Jackisch, Conrad
de Jong Van Lier, Quirijn
Koestel, John
Lehmann, Peter
Marthews, Toby R.
Minasny, Budiman
Pagel, Holger
van der Ploeg, Martine
Shojaeezadeh, Shahab Aldin
Svane, Simon Fiil
Szabó, Brigitta
Vereecken, Harry
Verhoef, Anne
Young, Michael
Zeng, Yijian
Zhang, Yonggen
Bonetti, Sara
Source :
ISSN: 1027-5606
Publication Year :
2024

Abstract

Hydro-pedotransfer functions (PTFs) relate easy-to-measure and readily available soil information to soil hydraulic properties (SHPs) for applications in a wide range of process-based and empirical models, thereby enabling the assessment of soil hydraulic effects on hydrological, biogeochemical, and ecological processes. At least more than 4 decades of research have been invested to derive such relationships. However, while models, methods, data storage capacity, and computational efficiency have advanced, there are fundamental concerns related to the scope and adequacy of current PTFs, particularly when applied to parameterise models used at the field scale and beyond. Most of the PTF development process has focused on refining and advancing the regression methods, while fundamental aspects have remained largely unconsidered. Most soil systems are not represented in PTFs, which have been built mostly for agricultural soils in temperate climates. Thus, existing PTFs largely ignore how parent material, vegetation, land use, and climate affect processes that shape SHPs. The PTFs used to parameterise the Richards-Richardson equation are mostly limited to predicting parameters of the van Genuchten-Mualem soil hydraulic functions, despite sufficient evidence demonstrating their shortcomings. Another fundamental issue relates to the diverging scales of derivation and application, whereby PTFs are derived based on laboratory measurements while often being applied at the field to regional scales. Scaling, modulation, and constraining strategies exist to alleviate some of these shortcomings in the mismatch between scales. These aspects are addressed here in a joint effort by the members of the International Soil Modelling Consortium (ISMC) Pedotransfer Functions Working Group with the aim of systematising PTF research and providing a roadmap guiding both PTF development and use. We close with a 10-point catalogue for funders and researchers to guide review processes and rese

Details

Database :
OAIster
Journal :
ISSN: 1027-5606
Notes :
application/pdf, Hydrology and Earth System Sciences 28 (2024) 14, ISSN: 1027-5606, ISSN: 1027-5606, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1462289877
Document Type :
Electronic Resource