Soil water retention and hydraulic conductivity measured in a wide saturation range

Publikation: Beitrag in FachzeitschriftForschungsartikelBeigetragenBegutachtung

Beitragende

  • Tobias L. Hohenbrink - , Technische Universität Braunschweig, Deutscher Wetterdienst (Autor:in)
  • Conrad Jackisch - , Technische Universität Bergakademie Freiberg, Karlsruher Institut für Technologie (Autor:in)
  • Wolfgang Durner - , Technische Universität Braunschweig (Autor:in)
  • Kai Germer - , Johann Heinrich von Thünen Institute (Autor:in)
  • Sascha C. Iden - , Technische Universität Braunschweig (Autor:in)
  • Janis Kreiselmeier - , Professur für Standortslehre und Pflanzenernährung, Johann Heinrich von Thünen Institute (Autor:in)
  • Frederic Leuther - , Helmholtz-Zentrum für Umweltforschung (UFZ), Universität Bayreuth (Autor:in)
  • Johanna C. Metzger - , Universität Hamburg, Friedrich-Schiller-Universität Jena (Autor:in)
  • Mahyar Naseri - , Technische Universität Braunschweig, Johann Heinrich von Thünen Institute (Autor:in)
  • Andre Peters - , Technische Universität Braunschweig (Autor:in)

Abstract

Soil hydraulic properties (SHPs), particularly soil water retention capacity and hydraulic conductivity of unsaturated soils, are among the key properties that determine the hydrological functioning of terrestrial systems. Some large collections of SHPs, such as the UNSODA and HYPRES databases, have already existed for more than 2 decades. They have provided an essential basis for many studies related to the critical zone. Today, sample-based SHPs can be determined in a wider saturation range and with higher resolution by combining some recently developed laboratory methods. We provide 572 high-quality SHP data sets from undisturbed, mostly central European samples covering a wide range of soil texture, bulk density and organic carbon content. A consistent and rigorous quality filtering ensures that only trustworthy data sets are included. The data collection contains (i) SHP data, which consist of soil water retention and hydraulic conductivity data, determined by the evaporation method and supplemented by retention data obtained by the dewpoint method and saturated conductivity measurements; (ii) basic soil data, which consist of particle size distribution determined by sedimentation analysis and wet sieving, bulk density and organic carbon content; and (iii) metadata, which include the coordinates of the sampling locations. In addition, for each data set, we provide soil hydraulic parameters for the widely used van Genuchten-Mualem model and for the more advanced Peters-Durner-Iden model. The data were originally collected to develop and test SHP models and associated pedotransfer functions. However, we expect that they will be very valuable for various other purposes such as simulation studies or correlation analyses of different soil properties to study their causal relationships. The data are available at 10.5880/fidgeo.2023.012 (Hohenbrink et al., 2023).

Details

OriginalspracheEnglisch
Seiten (von - bis)4417-4432
Seitenumfang16
FachzeitschriftEarth system science data
Jahrgang15
Ausgabenummer10
PublikationsstatusVeröffentlicht - 6 Okt. 2023
Peer-Review-StatusJa

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