Hostname: page-component-586b7cd67f-tf8b9 Total loading time: 0 Render date: 2024-11-25T19:53:47.587Z Has data issue: false hasContentIssue false

Differential effect of pasture species on the pH and cation exchange capacity of a subsequently cultivated soil

Published online by Cambridge University Press:  27 March 2009

A. J. Rixon
Affiliation:
Division of Plant Industry, C.S.I.R.O., Biverina Laboratory, Charlotte Street, Deniliquin, New South Wales, Australia

Summary

Higher pH values had been established under grass than under clover pastures during a prior pasture phase. The differential effect of pasture species on the pH of the subsequently cultivated soil was reduced in time, but continued to be significant after 4 years.

There was greater cation exchange capacity and lower percentage base saturation after clovers than after grasses. The cation exchange capacity of the inorganic fraction of the soil was not affected by the type of pasture and did not change with time. The difference in cation exchange capacity for the cultivated soil was, therefore, due to the difference in the cation exchange capacity of organic matter residual from the clover and grass pastures.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1970

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

Chandler, R. F. (1939). Cation exchange properties of certain forest soils in the Adirondack Section. J. agric. Res. 59, 491505.Google Scholar
Churchward, H. M. (1958). The soils and land use of the Denimein District, N.S.W. Soils Ld Use Ser. No. 27 G.S.I.R.O. Aust.Google Scholar
Coile, T. S. (1936). Soil samplers. Soil Sci. 42, 139–42.CrossRefGoogle Scholar
David, D. J. (1960). The determination of exchangeable sodium, potassium, calcium and magnesium in soils by atomic absorption spectrophotometry. Analyst, Lond. 85, 495503.CrossRefGoogle Scholar
Dormaar, J. F. & Lutwick, L. E. (1966). A biosequence of soils of the rough fescue prairie-poplar transition in south western Alberta. Can. J. Earth Sci. 3, 457–71.CrossRefGoogle Scholar
Greenland, D. J. (1965). Interaction between clays and organic compounds in soils. Part II. Absorption of soil organic compounds and its effect on soil properties. Soils Fertil. 28, 531–32.Google Scholar
Jackson, M. L. (1958). Soil Chemical Analysis. Englewood-Cliffs, New Jersey: Prentice-Hall, Inc.Google Scholar
Jenkinson, D. S. (1966). The turnover of organic matter in soil. In The Use of Isotopes in Soil Organic Matter Studies, Special supplement to J. appl. Radiat. Isotopes. London: Pergamon Press.Google Scholar
Jenkinson, D. S. (1968). Chemical tests for potentially available nitrogen in soil. J. Sci. Fd Agric. 19, 160–8.CrossRefGoogle ScholarPubMed
Piper, C. S. (1942). Soil and Plant Analysis, p. 200. Univ. of Adelaide.Google Scholar
Rixon, A. J. (1966). Soil fertility changes in a red-brown earth under irrigated pastures. 1. Changes in organic carbon, carbon/nitrogen ratio, cation exchange capacity and pH. Aust. J. agric. Res. 17, 303–16.CrossRefGoogle Scholar
Rixon, A. J. (1969). The influence of annual and porennial irrigated pastures on soil fertility as shown by the yield and quality of a subsequent wheat crop. Aust. J. agric. Res. 20, 243–55.CrossRefGoogle Scholar
Williams, C. H. & Donald, C. M. (1957). Changes in organic matter and pH in a podzolic soil as influenced by subterranean clover and superphosphate. Aust. J. agric. Res. 8, 179–89.CrossRefGoogle Scholar
Williams, C. H. & Lipsett, J. (1961). Fertility changes in soils cultivated for wheat in southern New South Wales. Aust. J. agric. Res. 12, 612–29.CrossRefGoogle Scholar
Zinke, P. J. (1962). The pattern of individual forest trees on soil properties. Ecology 43, 130–33.CrossRefGoogle Scholar