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Impact of long-term phosphorous fertilization on Olsen-P and grain yields in maize–wheat cropping sequence
Due to generally low phosphorus (P) recovery efficiency in maize–wheat cropping systems in northwest India, farmers have over-applied P fertilizers over many decades to improve crop growth and increase profitability. This practice caused a considerable part of cultivated land to have ‘very high’ (&g...
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Published in: | Nutrient cycling in agroecosystems 2016-11, Vol.106 (2), p.157-168 |
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Main Authors: | , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Due to generally low phosphorus (P) recovery efficiency in maize–wheat cropping systems in northwest India, farmers have over-applied P fertilizers over many decades to improve crop growth and increase profitability. This practice caused a considerable part of cultivated land to have ‘very high’ (>50.0 kg P ha
−1
) Olsen-P values in soil. This study was aimed at finding critical concentrations of Olsen-P for maize (
Zea mays
L.) and wheat (
Triticum aestivum
L.) sequence for effective utilization of buildup P and optimal P rates for maintaining critical Olsen-P in soil in this region by utilizing one long-term (11 years) and 2 short-term (3 years) trials. Long-term studies in high Olsen-P soils showed increased P buildup with present recommended fertilizer P application rates of 26 kg ha
−1
to both crops. With no P application, Olsen-P values in soils decline at rate of 3.0 kg P ha
−1
year
−1
. For sustaining maize and wheat yields, critical concentrations of Olsen-P obtained from different statistical models (linear plateau, quadratic plateau and exponential) range from 36.7 to 50.0 kg P ha
−1
for maize and 39.4–57.1 kg P ha
−1
for wheat and 38 kg P ha
−1
for both crops using Cate and Nelson split method. The use of Mitscherlich equation for determining the ‘effective’ P and Olsen-P requirement for getting higher yields was found to be a better method compared to above-mentioned statistical and graphical methods. Mitscherlich equation estimates the amount of P applied to achieve the desired Olsen-P levels in soil. |
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ISSN: | 1385-1314 1573-0867 |
DOI: | 10.1007/s10705-016-9796-8 |