Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-17T14:50:53.227Z Has data issue: false hasContentIssue false

Influence of growing various crops in five fixed cropping sequences on the changes in phosphorus and potassium content of soil

Published online by Cambridge University Press:  27 March 2009

K. N. Sharma
Affiliation:
Department of Agronomy, Punjab Agricultural University, Ludhiana 141 004, India
D. S. Rana
Affiliation:
Department of Agronomy, Punjab Agricultural University, Ludhiana 141 004, India
A. L. Bhandari
Affiliation:
Department of Agronomy, Punjab Agricultural University, Ludhiana 141 004, India

Summary

The results on the influence of growing various crops in five fixed annual sequences on the changes in available and total phosphorus and potassium content of a Tolewal sandy loam (Typic Ustipsamment) are reported. The available phosphorus content showed an increase in each of the five crop rotations after completion of two cycles. The maximum increase was observed in groundnut-based cropping sequences whereas the increase under the other three rotations was more or less of the same order. A slight decrease in the available P content during the 3rd year was observed after the harvest of bajra in a bajra fodder–potato–wheat sequence which was replenished after the harvest of potato and wheat. Total P content of the soil also showed an increase in all five rotations after completion of two cycles. A decrease in total P content of the soil was also observed after the bajra harvest. Balance sheet of P indicated net gain of P in all five crop rotations and the maximum gain of 62 kg P/ha was observed in the maize–wheat–moong rotation. Theavailable K status of the soil showed an increase in each of the five cropping sequences after completion of two cycles. The available K status after harvest of various crops in the rotation could not fully explain the dynamics of K availability. The total soil K content indicated a negative K balance in each of the five crop rotations after completion of three cycles and the maximum negative balance occurred in a maize–wheat–moong sequence. The negative K balance was related to the amount of fertilizer K added and that removed by the crops. The results suggested the need for modifying the existing K fertilizer recommendations to compensate gradual loss of native K soil fertility.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1987

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

Bower, C. A., Rbitsmeier, R. F. & Fireman, N. (1952). Exchangeable cation analysis of saline and alkali soils. Soil Science 73, 251261.CrossRefGoogle Scholar
Jackson, M. L. (1967). Soil Chemical Analysis. New Delhi: Asia Publishing House.Google Scholar
Sachdeva, P. D. (1973). Genesis, geochemistry and clay minerology of soil series of Punjab Agricultural University farm, Ludhiana. M.Sc. thesis, Punjab Agricultural University, Ludhiana, India.Google Scholar
Sharma, K. N., Singh, B. & Rana, D. S. (1986). The use of soil solution K value for assessing the K status of soil during a rotation of crops. Journal of Agricultural Science, Cambridge 107, 223225.CrossRefGoogle Scholar
Watanabe, F. S. & Olsen, S. R. (1966). Test of an ascorbic acid method for determining phosphorus in water and NaHC03 extracts from soil. Proceedings of the Soil Science Society of America 29, 677678.CrossRefGoogle Scholar