Researchers at Edith Cowan University in Western Australia have discovered that magnetite found within the state’s vast iron ore deposits can generate natural hydrogen when reacting with hot water deep underground, according to a recent statement from the university. This discovery of geological, or white, hydrogen offers a potential new low-emission energy source for industrial processes currently reliant on fossil fuels, as reported by bioengineer.org.
Magnetite Reactions and Geological Conditions
According to Edith Cowan University researchers, magnetite participates in oxidation-reduction reactions when exposed to hot water at temperatures of approximately 200 degrees Celsius under high pressure. Bioengineer.org notes that this process causes iron within the mineral to become more oxidized while water molecules are reduced, producing molecular hydrogen. To replicate hydrothermal environments found kilometers beneath the Earth’s surface, the research team exposed magnetite samples to these intense conditions for 60 days. The findings were published in the International Journal of Hydrogen Energy.
Subsurface Plumbing and Exploration Strategies
Research from the Edith Cowan University School of Engineering indicates that total magnetite abundance alone does not predict hydrogen production. According to findings covered by bioengineer.org, fluid accessibility through fractures, pores, and permeable pathways is critical because water must reach fresh mineral surfaces to sustain the reaction. Without connected channels and subsurface plumbing systems, impermeable rock bodies leave much of the magnetite chemically inaccessible. Consequently, future natural hydrogen exploration may focus heavily on mapping these pathways rather than just identifying mineral deposits.
Stimulating Production in Western Australia
Western Australia hosts some of the world’s largest banded iron formations, particularly across the Pilbara region. According to Edith Cowan University, researchers found that injecting a solution into these banded iron formations could significantly increase hydrogen production. Bioengineer.org reports that while industrial hydrogen is heavily used in chemical manufacturing and refining today, natural hydrogen accumulates over geological timescales, prompting scientists to evaluate how quickly reserves replenish and whether large-scale extraction can remain economically and environmentally sustainable.
Did You Know?
Natural hydrogen, often referred to as white or geological hydrogen, is produced entirely through natural underground chemical reactions between water and iron-bearing minerals in the Earth’s crust.
Frequently Asked Questions
What is natural hydrogen?
Natural hydrogen is a gas formed underground through chemical reactions between water and minerals like magnetite, differing from manufactured hydrogen produced using fossil fuels or renewable electricity.

How was the discovery made?
Researchers at Edith Cowan University tested magnetite samples at 200 degrees Celsius under high pressure for 60 days to simulate deep underground hydrothermal environments.
Where is magnetite abundant?
Magnetite is widely found in the banded iron formations of Western Australia, particularly across the Pilbara region.
Can hydrogen production be artificially increased?
According to Edith Cowan University researchers, injecting a solution into banded iron formations can significantly boost hydrogen generation rates.
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