Ultramafic rocks are igneous formations that constitute a significant part of the Earth's mantle and crust. Characterized by high iron and magnesium content and low silica levels, these rocks act as a chemical battery, reacting readily with underground water through a process called serpentinization.
Serpentinisation occurs when water infiltrates Ultramafic rocks, initiating chemical reactions that produce hydrogen gas. This exothermic process not only generates heat but also continuously releases hydrogen over geological timescales, offering a sustainable and environmentally friendly hydrogen source.
Decahydron is the global leader in natural hydrogen exploration within ultramafic rock formations. Our extensive expertise in ultramafic rock and fluid interactions, backed by proprietary intellectual property, positions us at the forefront of this innovative energy solution.
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