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Leys and soil organic matter:III. The accumulation of macro-organic matter in the soil under different swards

Published online by Cambridge University Press:  27 March 2009

E. A. Garwood ,
C. R. Clement  and
T. E. Williams
E. A. Garwood
Affiliation:
The Grassland Research Institute, Hurley, Berkshire
C. R. Clement
Affiliation:
The Grassland Research Institute, Hurley, Berkshire
T. E. Williams
Affiliation:
The Grassland Research Institute, Hurley, Berkshire
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Summary

Macro-organic matter (roots and partially decomposed plant debris retained on a 0·25 mm mesh sieve) was measured in soils under various swards. Under a grazed perennial ryegrass/white clover sward, sown on arable land, macro-organic matter in the top 15 cm of soil rose steadily in the first 8 years to 15·8 t/ha, but subsequently declined. Under arable cropping there was great variation with crop and season. Under grass, most of the macro-organic matter accumulated in the top 2 cm of soil, particularly during the first 3 or 4 years. More macro-organic matter was found under perennial ryegrass/white clover than under cocksfoot/white clover swards.

After 3 years under grass macro-organic matter accounted for 10% of the total soil carbon, and represented about half the increase in soil carbon.

Half, or less, of the nitrogen which accumulated in soil under grass was in the macroorganic matter fraction. The differences between swards which received no N fertilizer and those which received 940 kg/ha over 3 years was small, 16–40 kg N/ha respectively for cut and frequently grazed swards. The ratio of C:N in macro-organic matter under different swards averaged 22:1.

Type
Research Article
Information
The Journal of Agricultural Science , Volume 78 , Issue 2 , April 1972 , pp. 333 - 341
Copyright
Copyright © Cambridge University Press 1972

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