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Oxygen Theory of Combustion

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The oxygen theory of combustion holds that burning is a chemical combination of a substance with oxygen drawn from the air, not the release of a fire-like substance as phlogiston theory had claimed. Antoine Lavoisier built the case through sealed vessel experiments in which he weighed everything before and after combustion, showing that the total mass never changed and that metals gained exactly the mass of the oxygen they had combined with. His 1783 paper Reflections on Phlogiston presented the theory as a direct replacement, and it explained the weight gain phlogiston theory could not.

Facts
Proposed YearSourced to the subject's own account
1783 1
Proposed BySourced to the subject's own account
Antoine Lavoisier 1
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The Fire That Wasn't There

This article records tradition as it has been passed down and reported. Its sources are not yet part of the atlas's verified catalogue.

For most of the eighteenth century, chemists explained burning with phlogiston, a fire-like substance they held every combustible material contained and released into the air as it burned. Johann Joachim Becher first sketched the idea in 1667 as terra pinguis, a fatty earth given off by burning matter, and Georg Ernst Stahl renamed and systematized it as phlogiston around 1703. The theory organized a great deal of real chemistry correctly: it explained why a candle goes out in a sealed jar, phlogiston released by the flame saturates the enclosed air until it can absorb no more, and why charcoal, mostly phlogiston by this account, burns down to almost nothing. What it could not explain was why metals gain weight when they burn, when a substance is released, the remainder should weigh less, not more, and by the mid-eighteenth century this was a well-known, unresolved problem sitting inside the theory's own logic.

The experiment that would end up deciding the question was not designed to test phlogiston theory at all. On 1 August 1774, the English clergyman and chemist Joseph Priestley heated red mercuric oxide with a burning lens and isolated a colorless gas that made a candle burn unusually brightly and let a mouse breathe far longer than ordinary air allowed. Working entirely within phlogiston theory himself, Priestley called it dephlogisticated air, air that had been stripped of its own phlogiston and could therefore absorb an unusually large amount more. That October he described the experiment to Antoine Lavoisier in Paris, who repeated it.

Lavoisier read the same result completely differently. Working with sealed vessels and a precise balance, weighing everything before and after combustion, he showed that the total mass in a sealed system never changed, and that a burning metal gained exactly the mass of the gas it had combined with, not lost some invisible substance. His 1783 paper, Reflections on Phlogiston, presented combustion as a chemical combination with this gas, which he named oxygen, and proposed it as a direct replacement for phlogiston theory, one that explained the weight gain the older theory never could.

The most striking part of the story is that Priestley, whose own experiment supplied the decisive fact, never accepted Lavoisier's reinterpretation of it. He defended phlogiston theory for the rest of his life, publishing arguments for it even as the wider chemical community moved to Lavoisier's account through the 1780s and 1790s. The data that ended phlogiston theory and the chemist who generated it belonged, to the end, to two different sides of the argument.

Cross-Tradition Connections

Anticipated By

Phlogiston theory correctly identified combustion as a real chemical transformation and organized a century of experimental chemistry, but could not explain why metals gain weight when they burn. Joseph Priestley's own 1774 isolation of oxygen, read by him within phlogiston theory as dephlogisticated air, supplied the experimental fact that Antoine Lavoisier reinterpreted through careful mass measurements as combination with a gas drawn from the air; Lavoisier's 1783 Reflections on Phlogiston presented oxygen theory as phlogiston theory's replacement, explaining the weight gain the older theory could not.

Belongs To

Chemistry, Disciplines

Proposed By

Tested By

Joseph Priestley's 1 August 1774 isolation of the gas he called dephlogisticated air is the same experimental result Antoine Lavoisier reinterpreted, through his own sealed-vessel mass measurements, as evidence for combustion as combination with a gas drawn from the air; the experiment supplied the raw finding, and Lavoisier's reinterpretation of it built the theory.

Source Oxygen (Britannica)
Sources
1. Antoine Lavoisier (Wikipedia)
Phlogiston Theory (Wikipedia)
WikipediaAnticipated By: Phlogiston TheoryView the Source
Oxygen (Britannica)
Encyclopaedia BritannicaTested By: Discovery of OxygenView the Source
Dissenting Readings (1 dissenting reading)
Anticipated By: Phlogiston Theory

Priestley isolated the gas this transition turns on, on 1 August 1774, but he never accepted Antoine Lavoisier's reinterpretation of it. Working from phlogiston theory himself, he called the gas dephlogisticated air and defended phlogiston theory for the rest of his life after visiting Lavoisier in Paris that October and watching him repeat and reinterpret the same experiment. Carried here as the documented historical position of the very chemist whose own data the rival theory was built from, not as a claim that his reading was correct.

A dissenting reading, from Joseph PriestleyJoseph Priestley (Britannica), Encyclopaedia Britannica

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