Skip to content

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

How we use AISend a correction

Photograph accompanying Real-time oxygen tracking shows hematite photocurrent overstates water splitting at low currents
Photo: imperial.ac.uk

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.

Compiled by The ScientistSomething wrong?How this is made

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.

Clarity's read

What the record supports and how the coverage leans. The claims behind it follow.

Reality

Evidence55
Adoption
Insufficient
Hype gap+10
Incentives
Insufficient
Confidence55
Why these scores

Claim ledger

Ranked by verification strength, evidence, and original report placement.

  1. [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.

    ReportedSupportedSource: phys.org report on Imperial College London studyView cited source
  2. [2]

    Hematite is one of the most widely studied materials in solar water splitting.

    ReportedSupportedSource: phys.orgView cited source
  3. [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).

    ReportedSupportedSource: phys.orgView cited source

Sources

1 independent publisher whose own reporting we read for this story.

  1. phys.org

    1 article · October 8, 2026

    Real-time oxygen measurements expose hidden losses in solar water splitting

Share your take

Let Clarity write the post for you.

Signed-in readers get a short post drafted on this story in the register they choose — narrative, analytical, or a direct position — editable to the last word before it goes anywhere. The share buttons at the top of this story work without an account.

Topics and entities

Follow any of these and your For You feed starts watching them — no settings page required.

Topics

Entities

Loading related stories