Choice of Pedotransfer Functions Matters when Simulating Soil Water Balance Fluxes-Reference-Cited by-同舟云学术

Choice of Pedotransfer Functions Matters when Simulating Soil Water Balance Fluxes

Published:2021-03 Issue:3 Volume:13 Page:
ISSN:1942-2466
Container-title:Journal of Advances in Modeling Earth Systems
language:en
Short-container-title:J Adv Model Earth Syst

Author:

Weihermüller Lutz¹²^ORCID,Lehmann Peter³^ORCID,Herbst Michael¹^ORCID,Rahmati Mehdi⁴^ORCID,Verhoef Anne⁵^ORCID,Or Dani³⁶^ORCID,Jacques Diederick⁷^ORCID,Vereecken Harry¹²^ORCID

Affiliation:

1. Agrosphere Institute IBG 3, Forschungszentrum Jülich GmbH Jülich Germany

2. International Soil Modeling Consortium (ISMC) Jülich Germany

3. Department of Environmental Systems Science ETH Zurich Zurich Switzerland

4. Department of Soil Science and Engineering University of Maragheh Maragheh Iran

5. Department of Geography and Environmental Science University of Reading Reading UK

6. Division of Hydrologic Sciences (DHS)—Desert Research Institute Reno NV USA

7. Belgian Nuclear Research Centre SCK CEN Institute for Environment Health and Safety (EHS) Mol Belgium

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Environmental Chemistry,Global and Planetary Change

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020MS002404

Reference77 articles.

1. Estimating Soil Water Characteristics from Simpler Properties or Limited Data

2. Alastal K.(2012).Oscillatory flows and capillary effects in partially saturated and unsaturated porous media: Applications to beach hydrodynamics. (Ecoulements oscillatoires et effets capillaires en milieux poreux partiellement saturés et non satu‐rés: Applications en hydrodynamique côtière). Doctoral thesis of Institut National Polytech. de Toulouse/niv. de Toulouse. Institut de Mécanique des Fluides de Toulouse.

3. The concept of field capacity revisited: Defining intrinsic static and dynamic criteria for soil internal drainage dynamics

4. A SIMPLE METHOD FOR DETERMINING UNSATURATED CONDUCTIVITY FROM MOISTURE RETENTION DATA

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