TY - JOUR
T1 - Hydro-pedotransfer functions
T2 - A roadmap for future development
AU - Weber, Tobias Karl David
AU - Weihermüller, Lutz
AU - Nemes, Attila
AU - Bechtold, Michel
AU - Degré, Aurore
AU - Diamantopoulos, Efstathios
AU - Fatichi, Simone
AU - Filipović, Vilim
AU - Gupta, Surya
AU - Hohenbrink, Tobias L.
AU - Hirmas, Daniel R.
AU - Jackisch, Conrad
AU - De Jong Van Lier, Quirijn
AU - Koestel, John
AU - Lehmann, Peter
AU - Marthews, Toby R.
AU - Minasny, Budiman
AU - Pagel, Holger
AU - Van Der Ploeg, Martine
AU - Shojaeezadeh, Shahab Aldin
AU - Svane, Simon Fiil
AU - Szabó, Brigitta
AU - Vereecken, Harry
AU - Verhoef, Anne
AU - Young, Michael
AU - Zeng, Yijian
AU - Zhang, Yonggen
AU - Bonetti, Sara
N1 - Publisher Copyright:
© 2024 Tobias Karl David Weber et al.
PY - 2024/7/29
Y1 - 2024/7/29
N2 - 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 research.
AB - 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 research.
KW - ITC-GOLD
KW - ITC-ISI-JOURNAL-ARTICLE
U2 - 10.5194/hess-28-3391-2024
DO - 10.5194/hess-28-3391-2024
M3 - Review article
AN - SCOPUS:85200401727
SN - 1027-5606
VL - 28
SP - 3391
EP - 3433
JO - Hydrology and earth system sciences
JF - Hydrology and earth system sciences
IS - 14
ER -