CORDIS Project
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This project explores the chemical weathering of silicate rocks, a process crucial for nutrient cycling and climate regulation. By studying the interaction of water with rocks, it aims to understand how these processes influence carbon cycles and ecosystem health.
The chemical dissolution (weathering) of continental silicate rocks is a crucial Earth System process that makes nutrients available to ecosystems and consumes atmospheric CO2, affecting Earth’s climate and habitability.
The mechanistic controls on chemical weathering are still poorly understood, partly due to lack of integration between geochemical and hydrological concepts.
Here, I propose to test a key hypothesis that silicate weathering fluxes are primarily controlled by how long water spend…
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