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heat, fluid flow pathways, and recharge mechanisms and fluid chemical composition. These factors control the precipitation, dissolution and alteration of minerals, which can clog up wells (e.g
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has the potential to provide a long-term, sustainable source of low-carbon heat. However, the long-term performance can depend on complex interactions between geology, fluid flow and water–rock
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morphology be used to predict belowground water use and root-zone water dynamics? Can mechanistic models be used to predict how different tree-based farming systems influence water stress and water
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