Hydrogen in Australian natural gas: occurrences, sources and resources

Водород в природном газе Австралии: проявления, источники и ресурсы
Christopher J. Boreham, Andrew Feitz, Dianne S. Edwards, Krystian Czado, Nadège Rollet, Liuqi Wang, S. van der Wielen, D.C. Champion, R.S. Blewett, Paul Henson
2021-06-29

abiogenic hydrogenhydrogen geochemistrynatural hydrogenserpentinizationwater radiolysis
Natural or native molecular hydrogen (H2) can be a major component in natural gas, and yet its role in the global energy sector’s usage as a clean energy carrier is not normally considered. Here, we update the scarce reporting of hydrogen in Australian natural gas with new compositional and isotopic analyses of H2 undertaken at Geoscience Australia. The dataset involves ~1000 natural gas samples from 470 wells in both sedimentary and non-sedimentary basins with reservoir rocks ranging in age from the Neoarchean to Cenozoic. Pathways to H2 formation can involve either organic matter intermediates and its association with biogenic natural gas or chemical synthesis and its presence in abiogenic natural gas. The latter reaction pathway generally leads to H2-rich (>10 mol% H2) gas in non-sedimentary rocks. Abiogenic H2 petroleum systems are described within concepts of source–migration–reservoir–seal but exploration approaches are different to biogenic natural gas. Rates of abiogenic H2 generation are governed by the availability of specific rock types and different mineral catalysts, and through chemical reactions and radiolysis of accessible water. Hydrogen can be differently trapped compared to hydrocarbon gases; for example, pore space can be created in fractured basement during abiogenic reactions, and clay minerals and evaporites can act as effective adsorbents, traps and seals. Underground storage of H2 within evaporites (specifically halite) and in depleted petroleum reservoirs will also have a role to play in the commercial exploitation of H2. Estimated H2 production rates mainly from water radiolysis in mafic–ultramafic and granitic rocks and serpentinisation of ultramafic–mafic rocks gives a H2 inferred resource potential between ~1.6 and ~58 MMm3 year-1 for onshore Australia down to a depth of 1 km. The prediction and subsequent identification of subsurface H2 that can be exploited remains enigmatic and awaits robust exploration guidelines and targeted drilling for proof of concept.
1
Abiogenic hydrogen generally produces hydrogen-rich gas exceeding 10 mol% H2 in non-sedimentary rocks.
2
Abiogenic hydrogen petroleum systems involve source, migration, reservoir, and seal elements, but require exploration strategies distinct from biogenic natural gas.
3
Hydrogen formation can involve organic intermediates associated with biogenic gas or chemical synthesis associated with abiogenic gas.
4
Hydrogen trapping and storage may involve fractured basement pore space, clay minerals, evaporites, halite formations, and depleted petroleum reservoirs; robust exploration guidelines remain lacking.
5
Onshore Australian hydrogen production potential to 1 km depth is estimated at approximately 1.6–58 MMm3 per year, mainly from radiolysis and serpentinization.
6
The study updates sparse knowledge of Australian natural-gas hydrogen using compositional and isotopic analyses of approximately 1,000 samples from 470 wells.

Hydrogen (H2) occurrences and petroleum systems in Australian natural gas across sedimentary and non-sedimentary basins

The sources, formation pathways, trapping mechanisms, and inferred resource potential of natural molecular hydrogen

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Publication Date
2021-06-29
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Authors
Christopher J. Boreham
Andrew Feitz
Dianne S. Edwards
Krystian Czado
Nadège Rollet
Liuqi Wang
S. van der Wielen
D.C. Champion
R.S. Blewett
Paul Henson
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