Hostname: page-component-77c89778f8-rkxrd Total loading time: 0 Render date: 2024-07-16T21:54:03.404Z Has data issue: false hasContentIssue false

The proteins of different types of peat soils

Published online by Cambridge University Press:  27 March 2009

W. L. Davies
Affiliation:
(Faculty of Agriculture and Horticulture, University of Reading.)

Extract

The study has comprised a detailed analysis of twelve samples of soil, ten of which were samples of typical peat soils, the other two being samples of normal soils. The degree of humification of the organic matter of the samples varied, that in the wet peats being high and low in the dry peats.

Extracts of the soil were obtained by the use of boiling hydrogen peroxide, 20 per cent, hydrochloric acid and 2·5 per cent, caustic potash.

Hydrogen peroxide extracted roughly 70–80 per cent, of the soil nitrogen, 60–70 per cent, of this soluble nitrogen appearing as ammonia through the oxidising effects of the reagent. The nitrogen compounds of wet peats were more easily oxidisable to ammonia.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1928

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

André, (1902). Compt. rend. 135, 1353.Google Scholar
Bottomley, (1917). Proc. Soy. Soc. B, 90, 39.Google Scholar
Geblach, and Densoh, (1913). Bied. Zentr. 42, 21.Google Scholar
Jodidi, (1910). J. Amer. Chem. Soc. 32, 396.CrossRefGoogle Scholar
Schreiner, and Shoring, (1910). J. Biol. Chem. 8, 381.CrossRefGoogle Scholar
Waltees, (1915). J. Ind. Eng. Chem. 7, 860.CrossRefGoogle Scholar
Valmari, (1914). Bied. Zentr. 43, 217.Google Scholar