| Note [22] | |
C. Webster, page 448, {a} attribue la première relation de cette expérience à Étienne Noël : {b} During the course of his development of the aether hypothesis, Étienne Noël, who had been Descartes’ teacher at La Flèche, found that the introduction of a small volume of air caused a greater reduction in the mercury level than the same volume of water, when introduced above the mercury in the Torricelian experiment. This was a paradoxical result, since water was at least 400 times as dense as air. The depression of the mercury level was therefore not a manifestation of weight alone. Noël explained the paradox by proposing that the depression in the level was caused by the aether, which was present to a much greater extent in air than in water. However, the significance of this experiment was not in its conclusion, which, like other aether explanations was a problem of speculative rather than experimental physics, but in providing the basis for quantitative methods of measuring the degree of expansion of a volume of air. |
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Jean Pecquet et la Tempête du chyle (1651-1655), édité par Loïc Capron. – Paris : Bibliothèque interuniversitaire de santé, 2018. –
Texte : Jean Pecquet Dissertatio anatomica de circulatione sanguinis et motu chyli (1651) Chapitre viii, note 22. Adresse permanente : https://numerabilis.u-paris.fr/editions-critiques/pecquet/?do=pg&let=0028&cln=22 (Consulté le 08/12/2025) |