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traits and structure regulate below-ground microclimate and microbial carbon cycling across spatial scales. You will combine controlled experiments, field observations, remote sensing data, ecosystem flux
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functionality in response to global changes and restoration efforts at large spatial and temporal scales is essential to understand where action is needed and to monitor restoration success. Developments in
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used in 3D groundwater flow simulations to predict BEP potential occurrence spatially. For this you can draw on the Dept. of Physical Geography’s unique expertise on geomorphology, geology and
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boils), and used in 3D groundwater flow simulations to predict BEP potential occurrence spatially. For this you can draw on the Dept. of Physical Geography’s unique expertise on geomorphology, geology and
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trace element distributions at high spatial resolution. The resulting data will be integrated into thermodynamic models (e.g. FACTSage-based approaches) to support process optimisation and control in