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长期施肥对砂姜黑土无机磷形态的影响
引用本文:王道中,郭熙盛,刘枫,何传龙. 长期施肥对砂姜黑土无机磷形态的影响[J]. 植物营养与肥料学报, 2009, 15(3): 601-606
作者姓名:王道中  郭熙盛  刘枫  何传龙
作者单位:1.安徽省农业科学院土壤与肥料研究所,安徽合肥230031;
摘    要:采用顾益初、蒋柏藩的无机磷分级方法,研究了长期施肥下砂姜黑土无机磷组分含量变化、生物有效性及其与土壤有效磷的关系。结果表明,长期耗竭状况下Ca2-P和Ca8-P的植物营养效率最高,其次为Al-P和Fe-P,O-P和Ca10-P也表现出了一定的有效性;Fe-P和Al-P对植物的营养贡献率最高,虽然Ca2-P和Ca8-P活性最高,但由于含量低,对磷素养分的贡献率较低,土壤磷素极度耗竭下,Ca2-P的植物营养贡献率甚至低于Ca10-P和O-P。砂姜黑土对磷的固定严重,土壤中积累的磷主要向Al-P、Fe-P和有效性更低的Ca10-P和O-P转化,Ca2-P、Ca8-P的增量较少。相关分析和通径分析表明,无机磷组分对有效磷的贡献为:Al-P>Ca8-P>Ca2-P>Fe-P>O-P>Ca10-P;建立了Olsen-P与无机磷组分间的回归方程:Y = 3.8751 +0.4674X1 +0.4470X2+ 0.3769X3-0.1166X4-0.07838 X 5 (Y代表有效磷含量,X1、、X2、X3 、X4 、X5分别代表Ca2-P、Ca8-P、Al-P、Fe-P和Ca10-P含量;P<0.01,R2=0.9989)。

关 键 词:长期施肥   砂姜黑土   无机磷形态
收稿时间:2008-04-29

Effects of long-term fertilization on inorganic phosphorus fractions in lime concretion black soil
WANG Dao-zhong,GUO Xi-sheng,LIU Feng,HE Chuan-long. Effects of long-term fertilization on inorganic phosphorus fractions in lime concretion black soil[J]. Plant Nutrition and Fertilizer Science, 2009, 15(3): 601-606
Authors:WANG Dao-zhong  GUO Xi-sheng  LIU Feng  HE Chuan-long
Affiliation:1.Soil and Fertilizer Institute,Anhui Academy of Agricultural Sciences,Hefei 230031,China;
Abstract:The effects of long-term fertilization on inorganic phosphorus fractions and their availability in Shajiang black soil were studied using the fraction classification developed by Gu Yi-chu and Jiang Bo-fan. The results show that nutrition efficiency of Ca2-P and Ca8-P is higher than that of Al-P and Fe-P respectively, and Ca10-P and O-P have some availability when soil phosphorus is depleted. The contribution rates of Al-P and Fe-P for plant are the highest, while those of Ca2-P and Ca8-P are low although the two fractions have high availability. To some extent, the contribution rate of Ca2-P is even lower than that of Ca10-P and O-P when soil phosphorus is extremely depleted. The accumulated phosphorus is mainly transformed into the fractions of Al-P, Fe-P, O-P and Ca10-P, while the transformation to Ca2-P and Ca8-P are little. The results of correlation and path analyses indicate that soil available P is significantly correlated to Ca2-P, Ca8-P, Fe-P, Al-P, O-P and Ca10-P. The contribution of the different inorganic phosphorus fractions to soil available P is Al-P>Ca8-P>Ca2-P>Fe-P>O-P>Ca10-P.
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