'Significant concentrations' of natural hydrogen detected at Australia's first exploration well — raising hopes of world-first commercial exploitation
Brisbane-based Gold Hydrogen confirms ‘active hydrogen system’ with H2 concentrations of 73.3%, with discovery of helium adding to potential value of site
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It also discovered “a relatively high concentration of helium”, which it describes as “a rare and valuable resource” that if found in commercial grades and quantities “could be a significant value-add” to its Ramsay project.
Gold Hydrogen drilled to a depth of 1,005 metres at its Ramsay 1 exploration well, and found “widespread connected fracture systems within the target formations”, which were “essential for the migration of hydrogen from the deeper source to shallow zones from which it can be potentially be extracted”.
Concentrations of hydrogen were at their highest — 73.3% — at a depth of 240 metres, which was consistent with findings from unsuccessful oil drilling at the same site in 1931.
However, the amount of natural hydrogen present under the ground — and therefore whether it is commercially exploitable — is still to be determined.
“The results remain preliminary in nature and further ongoing evaluation of the well and sampling data will be required to reduce the remaining uncertainties around the vertical and lateral distribution of the natural hydrogen,” said Gold Hydrogen. “However, the Company is pleased that these preliminary results support its ongoing work in discovering Australia’s first natural hydrogen field.”
A gas sample taken from Ramsay 1 at a depth of 892 metres contained 3.6% helium and 96.4% nitrogen.
“This suggests that the basement [layer of rock] is generating helium in significant amounts, and that the overlying weathered zone [ie, containing decaying rock] may act as a reservoir retaining the helium in commercial concentrations,” said Gold Hydrogen.
“Helium is a valuable and rare commodity, and its unique properties gives it a widespread usage in themedical industry, as well as for scientific research, space exploration, diving and energy industry applications. There is no way to manufacture helium artificially, and its price fluctuates based on global demand and declining supply. Helium currently trades upwards of US$600/MCF [million cubic feet], which is up to 200 times more than LNG [liquefied natural gas].”
Gold Hydrogen managing director Neil McDonald said: “It is incredible It is incredibly exciting that we have replicated the results of 100 years ago at 240m. With the additional find of helium, which could be a significant value-add to the project, we view these results as being better than planned.”
(Copyright)Key natural hydrogen production processes, environments and locations
There are six known ways in which hydrogen is produced naturally:
Serpentinisation
In which the mineral olivine located in mid-ocean ridges or ophiolites (a geological formation where sections of the Earth’s mantle rise above sea level) is weathered to form hydrogen-rich fluids. This has been seen in the Semail ophiolite, in the Hajar Mountains of Oman. Under pressure and high temperatures, water can react with these iron-rich rocks to produce H2.
Radiolysis of water
Radioactive elements in the Earth’s crust — for example in crystalline basement rocks with high content of uranium, thorium or potassium — decompose water molecules trapped in causing a hydrogen pocket, as happened in South Australia.
Deep degassing
In which “primary” hydrogen (a single hydrogen atom attached to a single carbon atom) escapes from deep within the Earth’s crust. This has been seen in Nebraska, in the US.
Iron reduction and sulphur oxidation
Ferric iron in a black smoker (a subsea hydrothermal vent formed from iron sulphide deposits) is reduced to ferrous iron and hydrogen sulphides.
Thermal decomposition of organic matter
In which ammonium compounds located in deep sendiments decompose under high temperatures to form hydrogen and nitrogen, for example in hydrogen-nitrogen gas seeps in Oman.
Biological activity
Hydrogen is produced by microbes living in the Earth’s crusts, usually co-existing with hydrogen-consuming microbes and found via sediment or aquifers. This has been observed in the coal beds of the Powder River Basin in Montana, US.