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Impact of long-term phosphorous fertilization on Olsen-P and grain yields in maize-wheat cropping sequence

机译:长期磷肥对玉米-小麦种植顺序中Olsen-P和籽粒产量的影响

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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.
机译:由于印度西北部玉米-小麦种植系统中磷(P)的回收效率普遍较低,农民在过去几十年中过度使用了磷肥,以改善作物生长并提高利润。这种做法导致相当一部分耕地在土壤中具有“非常高”(> 50.0 kg P ha(-1))的Olsen-P值。这项研究旨在找到玉米(Zea mays L.)和小麦(Triticum aestivum L.)的临界Olsen-P浓度,以有效利用积累的磷和最佳P速率来维持该地区土壤中的临界Olsen-P。通过使用一项长期(11年)和2次短期(3年)试验。在高Olsen-P土壤上进行的长期研究表明,目前推荐的两种作物施肥量为26 kg ha(-1),因此磷积累量增加。如果不施用磷,土壤中的Olsen-P值将以3.0 kg P ha(-1)年(-1)的速度下降。为了维持玉米和小麦的产量,从不同的统计模型(线性平稳,二次平稳和指数)获得的Olsen-P的临界浓度范围为玉米的36.7至50.0 kg P ha(-1)和39.4-57.1 kg P ha(- 1)对于小麦,使用Cate和Nelson分裂方法,两种作物的小麦均重38 kg P ha(-1)。与上述统计和图形方法相比,使用Mitscherlich方程确定“有效” P和Olsen-P要求以获得更高的产量是一种更好的方法。 Mitscherlich方程估算了为达到土壤中所需的Olsen-P水平而施用的P量。

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