https://www.selleckchem.com/pr....oducts/diabzi-sting-
Superhot geothermal environments in granitic crusts of approximately 400-500 °C are a frontier of geothermal energy. In the development of such environments, there is a concern of a reduction of permeability of fractured granite due to the formation of fine particles of amorphous silica induced by the phase change from subcritical water to supercritical water or superheated steam. However, the formation of silica particles and a resultant reduction in permeability have not been demonstrated to date. Therefore, ex
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