Hostname: page-component-848d4c4894-mwx4w Total loading time: 0 Render date: 2024-06-30T01:21:08.688Z Has data issue: false hasContentIssue false

Effects of Irrigation Interval, Urea and Gypsum on N, P and K Uptake by Forage Sorghum on Highly Saline–Sodic Clay

Published online by Cambridge University Press:  03 October 2008

E. A. Abdel Magid
Affiliation:
Department of Biochemistry and Soil Science, Faculty of Agriculture, Shambat, Sudan
M. A. Mustafa
Affiliation:
Department of Biochemistry and Soil Science, Faculty of Agriculture, Shambat, Sudan
I. Ayed
Affiliation:
Department of Biochemistry and Soil Science, Faculty of Agriculture, Shambat, Sudan

Summary

The effects of three irrigation intervals (7, 10 and 15 days), four nitrogen levels (0N, 1N, 2N and 3N where 1N = 43.8 kg N/ha), and 0 or 11.9 tons/ha gypsum on leaf N, P and K uptake by forage sorghum grown on a highly saline–sodic clay soil were investigated in two successive seasons. The two seasons' data consistently showed that both leaf-N and leaf-K increased significantly with increasing N-rate and by splitting the same quantity of irrigation water into more frequent irrigations. Gypsum had no consistent effect. The responses of both leaf-N and leaf-K to nitrogen rates were significantly linear and a linear response of dry matter yield to leaf-N was also observed. P uptake was improved by more frequent irrigations in the first cutting of 1978, but was not otherwise affected by treatments.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1982

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

Begg, J. E. & Turner, N. C. (1976). Crop water deficits. Advances in Agronomy 28:161172.CrossRefGoogle Scholar
Chapman, H. D. & Pratt, P. F. (1961). Methods of Analysis for Soils, Plants and Waters. Riverside: University of California.Google Scholar
El Mahi, Y. E. & Mustafa, M. A. (1980). The effects of electrolyte concentration and sodium adsorption ratio on phosphate retention by soils. Soil Science 130:321324.CrossRefGoogle Scholar
Fadl, O. A. A. & Ali, M. A. (1977). Irrigation of a saline–sodic site in the Sudan Gezira. I. Water movement. Tropical Agriculture, Trinidad 54:157165.Google Scholar
Frota, T. N. E. & Tucker, T. C. (1978). Salt and water stress influences nitrogen metabolism in red kidney beans. Soil Science Society of America Journal 42:743746.CrossRefGoogle Scholar
Greene, H. & Snow, O. W. (1939). Soil improvement in Sudan Gezira. Journal of Agricultural Science, Cambridge 29:134.CrossRefGoogle Scholar
Hamid, K. S. & Mustafa, M. A. (1975). Dispersion as an index of relative hydraulic conductivity in salt-affected soils of the Sudan. Geoderma 14:107114.CrossRefGoogle Scholar
Hassan, N. A. K., Drew, T. V., Knudsen, D. & Olson, A. (1970). Influence of soil salinity on production of dry matter and uptake and distribution of nutrients in barley and corn: II Corn (Zea mays L.). Agronomy Journal 62:4648.CrossRefGoogle Scholar
Musa, M. M. (1968). Nitrogenous fertilizer transformations in the Sudan Gezira soil. Plant and Soil 28:413421.CrossRefGoogle Scholar
Mustafa, M. A. (1973). Appraisal of the water quality of the Blue and the White Niles for irrigation use. African Soils 18:113123.Google Scholar
Mustafa, M. A. & AbdelMagid, E. A. (submitted). Inter-relationships of irrigation frequency, urea nitrogen and gypsum on forage sorghum growth on a saline sodic clay soil. Agronomy Journal.Google Scholar
Mustafa, M. A. & AbdelMagid, E. A. (in press). The effects of irrigation interval, urea-N and gypsum on salt redistribution in a highly saline–sodic montmorillonitic clay soil under forage sorghum. Soil Science.Google Scholar
Olson, T. C. (1971). Yield and water use by different populations of dryland corn, grain sorghum and forage sorghum in the West corn belt. Agronomy Journal 63:104106.CrossRefGoogle Scholar