Hostname: page-component-78c5997874-4rdpn Total loading time: 0 Render date: 2024-11-20T03:36:46.364Z Has data issue: false hasContentIssue false

Soil changes in ley-arable experiments

Published online by Cambridge University Press:  27 March 2009

A. J. Low
Affiliation:
Imperial Chemical Industries, Ltd., Jealott's Hill Research Station, Bracknell, Berks
F. J. Piper
Affiliation:
Imperial Chemical Industries, Ltd., Jealott's Hill Research Station, Bracknell, Berks
P. Roberts
Affiliation:
Imperial Chemical Industries, Ltd., Jealott's Hill Research Station, Bracknell, Berks

Extract

The effects of four five-course and six four-course rotations on some physical and chemical properties of a sandy loam overlying London Clay are reported.

Periods under ley increased the water stability of the air-dry soil aggregates, the resistance of moist soil aggregates to simulated raindrops, the rate of drainage under 60 cm. of water tension as measured in the laboratory, decreased the draw-bar pull during ploughing and the force required to crush air-dry aggregates. These effects increased with the number of years under grass.

After 2 years of arable cultivation the effect of a 3-year ley on water-stable aggregation was still apparent whereas the effect of a 2-year ley had largely disappeared, and those of a 1-year ley had completely disappeared.

A 2-year ley in a five-course ley-arable rotation was sufficient to maintain the total soil nitrogen at about 0·16%. With one year of ley in a four-course rotation a slow decline in nitrogen was found when the initial level was about 0·21%.

The rate of CO2 formation in soils of the arable break was proportional to the number of years they had been under ley; the longer the period the greater the volume of CO2 produced.

Evidence is presented that fertilizer nitrogen is used most efficiently by cereals growing in soil in good physical condition. This is usually best following a period under grass.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1963

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

Dobben, W. H. van (1950). Versl. Inst. landb. Onderz. Wageningen, p. 87.Google Scholar
Hood, A. E. M. & Procter, J. (1961). J. Agric. Sci. 57, 241.CrossRefGoogle Scholar
Lewis, A. H., Procter, J. & Hood, A. E. M. (1960). J. Agric. Sci. 54, 310.CrossRefGoogle Scholar
Low, A. J. (1954). J. Soil Sci. 5, 57.CrossRefGoogle Scholar
Low, A. J. (1955). J. Soil Sci. 6, 179.CrossRefGoogle Scholar
Low, A. J. (1956). Detailed soil maps for Experimental Farms. VIth Int. Congr, Soil Sci. Vol. A, p. 247.Google Scholar
Low, A. J. (1957). Outlook on Agriculture, 1, 165.Google Scholar