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BODIUM team

interdisciplinary cooperation

The BODIUM model depicts the soil as a system with all relevant physical, chemical and biological processes and their interrelationships. Therefore, interdisciplinary collaboration between different scientists is particularly important for its development.

Biogeochemical processes

The availability of nutrients in the soil depends largely on the soil texture and the organic matter (humus) that builds up as a result of dying roots and organic fertilizers. Bacteria and fungi live either in competition or in symbiosis with the plant roots and are the main drivers of humus dynamics in BODIUM. These processes release nutrients for plant growth but also produce CO2 and N2O emissions.

just

Christopher Just (TUM)

c.just@tum.de

Tel.: +49 (0) 8161 71 5381

platzhalter profil

Julius Diel (UFZ)

julius.diel@ufz.de

Tel.: +49 (0) 341 6025 2448

Sara König (UFZ)

sara.koenig@ufz.de

Tel.: +49(0)341 6025 2347

lukas

Lucas Kanagarajah (UFZ)

lucas.kanagarajah@ufz.de

Tel.: +49 (0) 341 6025 4215

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Soil biodiversity

Many processes in the soil are driven by biology: Earthworms loosen the soil and feed it with organic matter. Microorganisms metabolize this organic matter, make nutrients available and utilize unused nutrients and pollutants. Plants influence the soil through their root growth, as well as by absorbing water and nutrients. In order to simulate soil functions such as carbon storage, nutrient cycling or water filtration and balance under changing conditions, these processes must be integrated into systemic models such as BODIUM.

gabriel salako

Gabriel Salako 
(Senckenberg)

gabriel.salako@sencken
berg.de

Tel: +49 (0) 3581 4760-5170

andre zaytsev

Andrey Zayetsev
(Senckenberg)

andrey.zaytsev@sencken
berg.de

Bibiana Betancur Corredor (Senckenberg)

bibiana.betancurcorredor@ senckenberg.de
Tel: +49 (0) 35814760-5592

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Soil structure

The soil structure has an influence on the water and gas balance, root growth and biological turnover. It is influenced by biological processes, soil tillage and physical processes. The structure is not static, as is assumed in many soil physics models. It changes over the years depending on management and can also show changes within a year. BODIUM integrates the dynamic structure and can therefore map the effects of different soil management practices.

Hans-Jörg Vogel (UFZ)

email: hans-joerg.vogel@

ufz.de
Tel: +49 (0)341 6025 4404

Ulrich Weller (UFZ)

email: ulrich.weller@ufz.de

Tel:+49(0)341 6025 4410

oliverheller

Olivier Heller (Agroscope)

email: olivier.heller@

agroscope.admin.ch

Tel: +41 58 485 67 41

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Regionalization

The regionalization of soil information in Germany is an important element of the BODIUM model. The properties of soils and thus their functions can differ greatly from site to site. High-resolution, site-specific soil information is required in order to apply the BODIUM model throughout Germany. Therefore, data science approaches for the identification of spatial patterns and the designation of soil functional process units were developed. Each of these spatial units contains information regarding the soil properties that are necessary as input parameters for the BODIUM model. In addition, an informative approach based on the soil overview map of Germany BÜK200 will be developed.

ließ

Mareike Ließ (HSWT)

mareike.liess@hswt.de
Tel: +49 9826 654-248

Karin Schmelmer (BGR)

karin.schmelmer@bgr.de

Tel: +49 511-643-3293

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