椰子种植中长期肥料和粪肥试验的无机磷组分和磷的可用性

Q4 Agricultural and Biological Sciences
S. Neenu, Ravi Bhat, V. Selvamani, P. Subramanian
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引用次数: 0

摘要

磷是椰子生产所需的主要养分之一。有关土壤中原生磷和施用磷归宿的信息对于更好地管理这种养分至关重要。在卡萨拉戈德 CPCRI 进行的一项长期肥料和人工试验中,研究了椰子种植 43 年后土壤中无机磷组分和可利用磷的变化情况。试验共分为 6 个处理,即有机和无机肥料耕作处理、无机肥料耕作处理、无机肥料和盆叉处理、单独耕作处理、不耕作和不施肥的除草剂施用处理以及对照处理。从椰子盆中提取了两个深度(0-30 厘米和 30-60 厘米)的土壤样本进行分析。通过顺序萃取法将磷分为易溶磷(ES-P)、铝溶磷(AI-P)、铁溶磷(Fe-P)、钙溶磷(Ca-P)和还原溶磷(RS-P)。椰子盆中 0-30 厘米深度的主要磷组分是 Ca-P,其变化趋势如下:Ca-P> Fe-P> RS-P:Ca-P>Fe-P>RS-P>Al-P>ES-P。然而,在 30-60 厘米深度,Fe-P 成为主要部分,其趋势为:Fe-P>Ca-P>RS-P>Al-P>ES-P。长期施用磷肥将促进土壤中 Ca-P 的积累,从而提高土壤中 P 的可利用性。在间隙中,Fe-P 是两个深度的主要组分,其次是 Ca-P 和 RS-P。施肥地块和非施肥地块中磷组分的差异清楚地表明,施肥地块在两个深度都有较高的无机磷组分含量。与其他施肥处理相比,在盆地中施用矿质磷肥和叉肥后,所有无机磷组分的含量都很高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Inorganic phosphorus fractions and phosphorus availability in long term fertilizer cum manurial trials under coconut cultivation
Phosphorus is one of the major nutrients required for coconut production. The information about the fate of native and applied phosphorus in soil is essential for better management of the nutrient. The changes on inorganic P fractions and P availability in soil after 43 years of coconut cultivation were studied from a long term fertilizer cum manurial experiment at CPCRI, Kasaragod. There were 6 treatments viz. tillage with organic and inorganic fertilizer, tillage with inorganic fertilizer, inorganic fertilizers with basin forking, tillage alone, herbicide application without tillage and fertilizer and the control. Soil samples were taken at two depths (0-30 and 30-60 cm) from coconut basin for analysis. Phosphorus was fractionated into Easily Soluble P (ES-P), Aluminium P (AI-P), Iron P (Fe-P), Calcium P (Ca-P) and Reductant Soluble P (RS-P) through sequential extraction. The dominant phosphorus fraction in the coconut basin at 0-30 cm depth was Ca-P and the trend is as follows: Ca-P> Fe-P> RS-P>Al-P>ES-P. However, at 30-60 cm depth, Fe-P became the dominant fraction and the trend is Fe-P>Ca-P>RS-P>Al-P>ES-P. Long-term phosphorus fertilization would facilitate the accumulation of soil Ca-P, and thus improve soil P availability. In the interspaces, Fe-P was the dominating fraction in both the depths followed by Ca-P and RS-P. The difference in P fractions in fertilized and non-fertilized plots clearly showed that the fertilized plots have high content of all the inorganic phosphorus fractions in both the depths. Application of mineral P along with forking in basin showed a high concentration of all the inorganic P fractions compared to other fertilizer applied treatments.
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来源期刊
Journal of Plantation Crops
Journal of Plantation Crops Agricultural and Biological Sciences-Agronomy and Crop Science
CiteScore
0.60
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15
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