Science1 publisherNot yet confirmed elsewhere2 min readPublished
Real-time oxygen tracking shows hematite photocurrent overstates water splitting at low currents
Imperial College London researchers measuring oxygen live found hematite converts about 80% of charge to oxygen only once surface charge builds. At lower currents much of it feeds competing surface reactions, so current alone overstates the oxygen.
The Scientist · Science desk

What happened
- The team adapted an electrochemical mass spectrometer at the Royce at Imperial facility to work under light, logging photocurrent and oxygen from one sample at the same time.
- The same selectivity switch appeared when the researchers drove hematite electrically in the dark, with no light at all.
- The work, led by Flurin Eisner and Daniele Benetti with Ifan Stephens and James Durrant, is published in the Journal of the American Chemical Society.
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Why it matters
- constraint On hematite, an oxygen efficiency computed from photocurrent at low current can only be treated as a ceiling until a direct gas measurement confirms it.
- decision Groups ranking candidate photoanodes on current alone now have to decide whether to add product detection, because equal currents need not mean equal oxygen.
- precedent The team's next tests on other metal oxides, and on carbon dioxide and nitrogen reduction, will show whether the current-as-product shortcut fails beyond hematite.
Photoelectrochemists commonly read current as a count of product. The phys.org report calls that assumption widespread, and the Imperial results challenge it [8]. If every charge crossing a hematite surface ended up in an oxygen molecule, current and oxygen would be the same number. The Imperial measurements say they are not, at least at low current. In that range, much of the charge went into competing surface reactions [5].
The dark run is the experiment's control. The switch still appeared with the light off [7], so illumination drops out of the explanation. The team attributes the behaviour to hematite itself [7].
Past the switch, once enough positive charge had built up at the surface, oxygen-production efficiency rose to around 80% [6]. Even at that best reported point, roughly a fifth of the charge went somewhere other than oxygen [13]. The phys.org account does not give the efficiency below the switch, the current at which it occurs, or what the competing surface reactions produce.
Catching the gap took oxygen detection sensitive enough for slow reactions [9]. "Its sensitivity allowed us to measure oxygen at reaction rates where current alone would have given an incomplete picture," said Eisner, now at Queen Mary University of London [10][3]. Ifan Stephens of Imperial's Department of Materials credited the mix of methods. "It is amazing to see how multiple techniques together, in this case electrochemistry, operando optical spectroscopy and electrochemical mass spectrometry, can make us rethink our mechanistic understanding of a reaction," he said [11]. The paper's title ties oxygen selectivity to the reaction order of water oxidation on hematite photoanodes [4].
The thing this doesn't tell you is how much a working device is affected. The losses sit at low current [5]. So the error in a current-only oxygen figure depends on where in its operating range a photoanode runs. I'd expect low-current comparisons between materials to be the most distorted and high-current device figures less so, on the condition that the switch holds across the hematite preparations other groups make. That condition carries weight because hematite is one of the most widely studied materials in solar water splitting [2].
What to watch
- The JACS paper's figures for oxygen efficiency below the switch and the current where it occurs; together they set the size of the overcount.
- Whether other hematite groups reproduce the selectivity switch on their own electrode preparations.
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- [1]
A technique developed at Imperial College London measures oxygen production in real time; the researchers found electrical current did not always correspond to oxygen generation in hematite.
- [2]
Hematite is one of the most widely studied materials in solar water splitting.
- [3]
The study was led by Flurin Eisner, formerly a research fellow in Imperial's Department of Materials and now at Queen Mary University of London, together with Daniele Benetti of Imperial's Department of Chemistry; collaborators included Ifan Stephens (Materials) and James Durrant (Chemistry).
- [4]
The research is published in the Journal of the American Chemical Society (2026) as 'Linking Oxygen Evolution Selectivity to Water Oxidation Reaction Order on Hematite Photoanodes by Operando Photoelectrochemical Mass Spectrometry'.
- [5]
The team identified a 'selectivity switch': at low current levels, much of the electrical charge was diverted into competing surface reactions rather than oxygen production.
- [6]
Once enough positive charge accumulated at the hematite surface, oxygen generation became far more efficient, with oxygen-production efficiency rising to around 80%.
- [7]
The same behaviour was observed when the reaction was driven electrically in the dark, suggesting it is a fundamental property of hematite rather than specific to light-driven reactions.
- [8]
The findings challenge the widespread assumption that electrical current always reflects how much oxygen is being produced.
- [9]
The researchers adapted an electrochemical mass spectrometry system at the Royce at Imperial facility in White City into a photoelectrochemical mass spectrometry (PEC-MS) platform that operates under illumination, measures oxygen in real time with high sensitivity, and simultaneously records photocurrent from the same sample.
- [10]
"Its sensitivity allowed us to measure oxygen at reaction rates where current alone would have given an incomplete picture."
- [11]
"It is amazing to see how multiple techniques together, in this case electrochemistry, operando optical spectroscopy and electrochemical mass spectrometry, can make us rethink our mechanistic understanding of a reaction."
- [12]
The team plans to apply the approach to other metal-oxide materials and to a wider range of energy-conversion reactions, including carbon dioxide and nitrogen reduction.
- [13]
Even after the selectivity switch, about 20% of the charge did not go into oxygen production.
Sources
1 independent publisher whose own reporting we read for this story.
- phys.orgReal-time oxygen measurements expose hidden losses in solar water splitting
1 article · October 8, 2026
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Topics
- Green HydrogenFollow
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- Royce at ImperialFollow
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