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| Funder | Formas |
|---|---|
| Recipient Organization | Swedish University of Agricultural Sciences |
| Country | Sweden |
| Start Date | Jan 01, 2023 |
| End Date | Dec 31, 2026 |
| Duration | 1,460 days |
| Number of Grantees | 5 |
| Roles | Co-Investigator; Principal Investigator |
| Data Source | Swedish Research Council |
| Grant ID | 2022-00307_Formas |
Severe droughts are expected to become more frequent in a future climate.
Water availability controls crop growth, which in turn has direct and indirect effects on flows of energy, water, carbon (C), and nutrients in the soil-plant system.
For grasslands, there are indications that drought may alter the partitioning of above- and below-ground production, with more C being allocated to the root system. Microbial carbon use efficiency (CUE) may also change in a warmer climate. The amount of root-derived C that can be stored in the soil therefor difficult to predict in a future climate climate.
Soil C models assume that the C supply from plants is a fixed input unaffected by climate.
On the other hand, the interactions between soil water dynamics and plant growth in existing crop models are generally poorly described, although they have a significant impact on C dynamics.
In this four-year project, we will develop a new model that will account for dynamic feedbacks between soil hydrology, plant growth, and microbial activity.
It will be tested against data from the Tereno-SoilCan lysimeter network in Germany and a field experiment in Sweden with grass subjected to drought and control treatments.
Swedish University of Agricultural Sciences
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