Hostname: page-component-848d4c4894-r5zm4 Total loading time: 0 Render date: 2024-06-22T18:20:58.141Z Has data issue: false hasContentIssue false

Availability of magnesium to ryegrass from soils during intensive cropping in the glasshouse

Published online by Cambridge University Press:  27 March 2009

A. H. Sinclair
Affiliation:
The Macaulay Institute for Soil Research, Aberdeen, Scotland, AB9 2QJ

Summary

Ten Scottish soils were cropped in a glasshouse with three sowings of perennial ryegrass (Lolium perenne, cv. Dutch Barenza) without added magnesium. After 25 cuts (185 weeks) growth was poor in some soils, but soil Mg was not limiting growth in others.

Uptake of Mg and the Mg concentration in the ryegrass correlated well over the entire cropping period with the equilibrium Mg-concentration ratio Mg/(Ca, Mg) = CR0, determined from the Mg quantity/intensity isotherms measured before cropping in 0·01 m chloride solutions. A CR0 value of 0·16 was required in the early stages of cropping to give 0·2 % Mg in grass dry matter.

Seven soils released 12–37 mg non-exchangeable Mg/kg, between one-fifth and one-third of the total Mg uptake. These reserves probably came from vermiculite minerals, but the release was too slow to maintain Mg concentrations of 0·2 % in the ryegrass.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1981

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

Alston, A. M. (1972). Availability of magnesium in soils. Journal of Agricultural Science, Cambridge 79, 197204.CrossRefGoogle Scholar
Baker, D. E. (1972). Soil chemistry of magnesium. In Magnesium in the Environment – Soils, Crops, Animals and Man (ed. Jones, J. B. Jr, Blount, M. C. and Wilkinson, S. R.), pp. 139, Reynolds, Georgia, U.S.A.: Taylor County Printing Company.Google Scholar
Bolton, J. (1973). Total cations in the size-fractions of some British and Malayan soils and their release to H+ – resins. Journal of the Science of Food and Agriculture 24, 727738.CrossRefGoogle Scholar
Bolton, J. (1974). Release of magnesium from soil. Rothamsted Report for 1973, Part 1, p. 60.Google Scholar
Bolton, J. & Penny, A. (1968). The effects of potassium and magnesium fertilizers on yield and composition of successive crops of ryegrass, clover, sugar beet, potatoes, kale and barley on sandy soil at Woburn. Journal of Agricultural Science, Cambridge 70, 303311.CrossRefGoogle Scholar
Christenson, D. R. & Doll, E. C. (1978). Magnesium uptake from exchangeable and non-exchangeable souroes in soils as measured by intensive cropping. Soil Science 126, 166168.CrossRefGoogle Scholar
Jackson, M. L. (1958). Exchangeable metallic cation determinations for soils. In Soil Chemical Analysis, chapter 5, pp. 82110, London: Constable and Company Ltd.Google Scholar
Kemp, A. (1960). Hypomagnesaemia in milking cows: the response of serum magnesium to alterations in herbage composition resulting from potash and nitrogen dressings on pasture. Netherlands Journal of Agricultural Science 8, 281304.CrossRefGoogle Scholar
McNaught, K. J. (1970). Diagnosis of mineral deficiencies in grass–legume pastures by plant analysis. Proceedings of the llth International Grassland Congress, pp. 334338.Google Scholar
Metson, A. J. (1974). Magnesium in New Zealand soils. I. Some factors governing the availability of soil magnesium: a review. New Zealand Journal of Experimental Agriculture 2, 277319.CrossRefGoogle Scholar
Reith, J. W. S. (1967). Effects of soil magnesium levels and of magnesium dressings on crop yield and composition. In Soil Potassium and Magnesium, Technical Bulletin no. 14, pp. 97109. Ministry of Agriculture, Fisheries and Food, London: H.M.S.O.Google Scholar
Rice, H. B. & Kamprath, E. J. (1968). Availability of exchangeable and non-exchangeable Mg in sandy coastal plain soils. Proceedings of the Soil Science Society of America 32, 386388.CrossRefGoogle Scholar
Salmon, R. C. (1963). Magnesium relationships in soils and plants. Journal of the Science of Food and Agriculture 14, 605610.CrossRefGoogle Scholar
Salmon, R. C. (1964 a). Cation exchange reactions. Journal of Soil Science 15, 273283.CrossRefGoogle Scholar
Salmon, R. C. (1964 b). Cation-activity ratios in equilibrium soil solutions and the availability of magnesium. Soil Science 98, 213221.CrossRefGoogle Scholar
Salmon, R. C. & Arnold, P. W. (1963). The uptake of magnesium under exhaustive cropping. Journal of Agricultural Science, Cambridge 61, 421425.CrossRefGoogle Scholar
Sarkar, B. C. R. & Chauhan, U. P. S. (1967). A new method for determining micro quantities of calcium in biological materials. Analytical Biochemistry 20, 155166.CrossRefGoogle ScholarPubMed
Sinclair, A. H. (1979). Availability of potassium to ryegrass from Scottish soils. I. Effects of intensive cropping on potassium parameters. Journal of Soil Science 30, 757773.CrossRefGoogle Scholar
Sinclair, A. H. (1980). Desorption of cations from Scottish soils by electro-ultrafiltration. Journal of the Science of Food and Agriculture 31, 532540.CrossRefGoogle Scholar