#John dalton's atomic theory series#

The papers contained Dalton’s independent statement of Charles’s law (see Joseph Louis Gay-Lussac): “all elastic fluids expand the same quantity by heat.” He also clarified what he had pointed out in Meteorological Observations-that the air is not a vast chemical solvent as Antoine-Laurent Lavoisier and his followers had thought, but a mechanical system, where the pressure exerted by each gas in a mixture is independent of the pressure exerted by the other gases, and where the total pressure is the sum of the pressures of each gas.Įngraving of John Dalton by William Henry Worthington after a painting by William Allen, 1823.

#John dalton's atomic theory series#

Theories of Atomism and the Law of Partial Pressuresĭalton arrived at his view of atomism by way of meteorology, in which he was seriously interested for a long period: he kept daily weather records from 1787 until his death, his first book was Meteorological Observations (1793), and he read a series of papers on meteorological topics before the Literary and Philosophical Society between 17. The first paper he delivered before the society was on color blindness, which afflicted him and is sometimes still called Daltonism. There he joined the Manchester Literary and Philosophical Society, which provided him with a stimulating intellectual environment and laboratory facilities. After teaching for 10 years at a Quaker boarding school in Kendal, he moved on to a teaching position in the burgeoning city of Manchester. Early Lifeĭalton (1766–1844) was born into a modest Quaker family in Cumberland, England, and for most of his life-beginning in his village school at the age of 12-earned his living as a teacher and public lecturer. He also developed methods to calculate atomic weights and structures and formulated the law of partial pressures. Science History InstituteĪlthough a schoolteacher, a meteorologist, and an expert on color blindness, John Dalton is best known for his pioneering theory of atomism.

Plate 5: Elements from John Dalton’s A New System of Chemical Philosophy, 1810.