Repositorium für Publikationen und Forschungsdaten

Suchen Sie in der Research Collection der ETH Zürich nach wissenschaftlichen Publikationen und Forschungsdaten oder laden Sie selbst eigenen Forschungsoutput hoch. Weiterlesen

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ETH RDM Summer School 2024 für Nachwuchswissenschaftler:innen

Die ETH Research Data Management Summer School 2024 hat noch einige freie Plätze. Nutzen Sie die Gelegenheit und lernen Sie zwischen dem 10. und 14. Juni 2024 mehr über das Thema! Anmeldung und weitere Informationen

Coffee Lectures – das neue Programm ist da

In nur 15 Minuten: Holen Sie sich nützliche Tools und Themen, die Sie bei Ihrer täglichen Forschungsarbeit unterstützen – in den Coffee Lectures der ETH-Bibliothek. Weiterlesen

Fit im Forschungsdatenmanagement – Workshop-Reihe im Frühjahrssemester 2024

Machen Sie sich und Ihr Forschungsprojekt fit mit unserem Workshop-​Angebot zum Thema Forschungsdatenmanagement. Ab sofort können Sie sich für die Workshops im Frühjahrssemester 2024 anmelden. Weiterlesen

  

Neueste Publikationen 

  1. Water evaporation from bare soil 

    Lehmann P. (2023)
    Encyclopedia of Soils in the Environment, Second Edition
    Evaporation of water emitted from soil surfaces is a key process of the hydrologic cycle and the surface energy balance. It can be limited by the solar energy to vaporize water, the amount of precipitation, the soil hydraulic properties and surface characteristics (albedo, roughness, and presence of residues). Evaporation rates are large for wet soil surfaces with high atmospheric demand (controlled by energy, vapor pressure deficit, and ...
    Book Chapter

  2. Bioturbation—Physical processes 

    Ruiz S.; Hallett P.D.; Or D. (2023)
    Encyclopedia of Soils in the Environment, Second Edition
    Bioturbation is the physical movement of soil by fauna or plant roots. The primary goal of bioturbation is for organisms to access resources in soil such as food, plant nutrients and water. Bioturbation includes soil translocation by burrowing and ingestion, soil deformation by organism expansion, and soil stabilization by compounds secreted by organisms and their tissue. These processes are extremely important to the formation of soil ...
    Book Chapter

  3. Bioturbation—Physical processes 

    Ruiz S.; Hallett P.D.; Or D. (2023)
    Encyclopedia of Soils in the Environment, Second Edition: Volume 1-5
    Bioturbation is the physical movement of soil by fauna or plant roots. The primary goal of bioturbation is for organisms to access resources in soil such as food, plant nutrients and water. Bioturbation includes soil translocation by burrowing and ingestion, soil deformation by organism expansion, and soil stabilization by compounds secreted by organisms and their tissue. These processes are extremely important to the formation of soil ...
    Book Chapter

  4. Water evaporation from bare soil 

    Lehmann P. (2023)
    Encyclopedia of Soils in the Environment, Second Edition: Volume 1-5
    Evaporation of water emitted from soil surfaces is a key process of the hydrologic cycle and the surface energy balance. It can be limited by the solar energy to vaporize water, the amount of precipitation, the soil hydraulic properties and surface characteristics (albedo, roughness, and presence of residues). Evaporation rates are large for wet soil surfaces with high atmospheric demand (controlled by energy, vapor pressure deficit, and ...
    Book Chapter

  5. Accelerating rehabilitation through AR/VR solutions 

    Calderon-Sastre E.; Renganathan G.; Palani P.; et al. (2024)
    Smart VR/AR/MR Systems for Professionals
    Rehabilitation plays a crucial role in restoring or optimizing physical, mental, and social functions compromised by illness, injury, trauma, or aging. With an aging population, an increase in chronic diseases, and a shortage of rehabilitation professionals, the demand for rehabilitation services is growing. Furthermore, the COVID-19 pandemic has heightened the need for rehabilitation due to disabilities caused by the disease. This chapter ...
    Book Chapter

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