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XXIX.—On the Variations of the Amount of Carbonic Acid in the Ground-Air (Grund-Luft of Pettenkofer)
Published online by Cambridge University Press: 06 July 2012
Extract
The chemical examination of ground-air, i.e., the air which is contained in the pores of the soil, was first made by Boussingault and Levy in 1853. Their results, however, attracted little attention till Pettenkofer, in 1857, pointed out that the determination of the amount of carbonic acid in the air of a given soil might be used as a means of estimating the organic decomposition going on there. In 1871 he first published his results, and since that time the subject has been worked at by many investigators both from the agricultural and hygienic point of view, including in the latter class Fleck at Dresden, Eodor at Buda-Pesth, Hesse in Saxony, and Nicholls in America. As researches of this nature have not attracted much attention in this country, a short account of the modus operandi may be interesting as a preliminary.
- Type
- Research Article
- Information
- Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 37 , Issue 3 , 1895 , pp. 695 - 706
- Copyright
- Copyright © Royal Society of Edinburgh 1895
References
page 695 note * Annales de Chemie et de Physique, 1853.
page 695 note † Fig. A shows the apparatus and arrangement of sunk tube.
page 696 note * Before connecting the absorption apparatus, the air is directly aspirated from the iron tube to clear it of its contained air.