长期定位施肥对潮土磷素形态和有效性的影响

Effect of Long-term Fertilization on Phosphorus Fraction and Availability in Fluvo-Aquic Soil

  • 摘要: 研究长期定位施肥对潮土各形态磷含量变化及磷有效性的影响,为潮土合理施用磷肥提供理论依据。长期定位施肥试验开始于1990年,设CK(不施肥)、N2(单施尿素)、N2P(不施钾肥)、N2K(不施磷肥)、N1PK(低量氮肥和磷钾肥)、N2PK(平衡施肥)、N3PK(中高量施肥)、N4PK(高量氮肥和磷钾肥)、N2PKM(化肥和有机肥)、N2PKS(化肥和玉米秸秆还田)10个处理;采用Tiessen-Moir磷素分级法测定各施肥处理土壤不同形态磷含量,用常规方法测定有效磷、全磷含量,分析不同形态磷含量间的相关性。结果表明:经过28年定位施肥处理,N2PKM处理土壤各形态磷含量为盐酸态磷(HCl-P)> 残留态磷(Residual-P)> 氢氧化钠无机磷(NaOH-Pi)> 氢氧化钠有机磷(NaOH-Po)> 碳酸氢钠无机磷(NaHCO3-Pi)> 水溶性磷(Resin-Pi)> 碳酸氢钠有机磷(NaHCO3-Po)。在各施肥处理间,N2P、N1PK、N2PK、N3PK、N4PK、N2PKM、N2PKS处理土壤Resin-Pi、NaHCO3-Pi和NaOH-Pi含量显著高于CK、N2、N2K处理,而处理间NaHCO3-Po、NaOH-Po、HCl-P和Residual-P含量差异不显著。除NaOH-Po外,其它形态磷含量与供试土壤有效磷、全磷含量呈极显著相关,其中Resin-Pi对有效磷贡献最大,说明Resin-Pi是最有效的磷源。供试土壤条件下,合理配施化肥有机肥,可以激发磷素后效,使积累磷素向有效态转化,施用有机肥料能显著提高土壤中各磷组分含量,其中有机无机配施处理(N2PKM)提高程度高于单施化肥(N2PK),施用秸秆处理的各磷组分含量同样显著高于不施肥和化肥处理,且施用有机肥和秸秆处理(N2PKS)的中活性和中等活性磷均与土壤速效磷、全磷呈显著正相关,可在潮土上施用有机肥或秸秆处理,从而保持高比例的土壤有效磷库。

     

    Abstract: The changes of various fractions of phosphorus (P) separated with Tiessen-Moir method and its availability under long-term fertilization were investigated, in order to provide a theoretical basis for the reasonable application of P fertilizers in the Fluvo-aquic soil. Different fertilization treatments included no fertilization (control, CK), single application of urea (N2), no potassium (K) fertilizer (N2P); no P fertilizer (N2K), low amount of nitrogen (N) fertilizer combined with P and K fertilizers (N1PK), balanced fertilization (N2PK), medium or high amount of fertilizers (N3PK), high amount of N fertilizer combined with P and K fertilizers (N4PK), chemical combined with organic fertilizers (N2PKM), chemical fertilizers combined with corn straw returning (N2PKS). The correlation between soil P and available P and total P were analyzed. After 28 years of different fertilization treatments, the P fraction contents in the N2PKM treatment were decreased in the order of hydrochloric acid extractable P (HCl-P) > residual P (Residual-P) > sodium hydroxide extractable inorganic P (NaOH-Pi) > sodium hydroxide extractable organic P (NaOH-Po) > sodium bicarbonate extractable inorganic P (NaHCO3-Pi) > Water-soluble P (Resin-Pi)> sodium bicarbonate extractable organic P (NaHCO3-Po). Compared with CK, N2, and N2K treatments, N2P, N1PK, N2PK, N3PK, N4PK, N2PKM and N2PKS treatments significantly increased the contents of Resin-Pi, NaHCO3-Pi and NaOH-Pi, while the contents of NaHCO3-Po, NaOH- Po, HCl-P and Residual-P were not significant among different treatments. Except for NaOH-Po, the correlations among the contents of the other P fractions, available P and total P in the soil were significant. The contribution of Resin-Pi to available P was the most, indicating that Resin-Pi was the most effective source of P. The application of organic fertilizers significantly increased the contents of various P fractions in the soil, especially in the N2PKM compared with N2PK treatments. The contents of various P fractions in the N2PKS treatment were also significantly higher than those in the chemical fertilizer application treatments. The contents of soil medium and medium active P were significantly correlated with those of available P and total P in the organic fertilizer and straw treatments(N2PKS). Organic fertilizer or straw could be applied to fluvo-aquic soil to maintain a high percentage of soil available P pool.

     

/

返回文章
返回