玉米栽培下土壤无机磷和有机磷的变化

H. D. Preez, A. Claassens
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引用次数: 17

摘要

采用Hedley, Stewart和Chauhan(1982)的P分选方法研究了Avalon和Clovelly土壤在耕作条件下的施磷和残磷变化。土壤磷分为6个主要组分,其中部分组分又分为有机磷(Po)和无机磷(Pi)形态:磷由阴离子交换树脂(resin -P)提取;0.5 M NaHCO3-P (NaHCO3-Pi和Po);0.1 M NaOH (NaOH-l- pi和Po);在0.75瓦的0.1 M NaOH (NaOH-l - pi和Po)中超声;1.0 M HCI(HCI- pi);H2SO4消解和H2O2氧化(H2SO4P)。在15年的栽培过程中,土壤磷的总体变化趋势很明显。树脂- p、NaHCO3-Pi、naoh - 1 - pi、naoh - 1 - pi和HCl-Pi在Avalon土壤中降低,而Clovelly土壤中只有NaHCO3-Pi和naoh - 1 - pi降低。假设减少幅度最大的NaOH-l-Pi主要负责补充活性磷库。在阿瓦隆土壤中,Po组分中NaHCO3-Po和naoh -l -Po随时间的增加而减少,且随时间的增加而减少。
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Changes in inorganic and organic Phosphorus in soil under maize (Zea mays) cultivation
The changes in applied and residual phosphorus (P) were examined in Avalon and Clovelly soils under cultivation by using the P fractionation method of Hedley, Stewart and Chauhan (1982). Soil P was separated into six major fractions of which some fractions were subdivided into organic (Po) and inorganic (Pi) P forms: P extracted by an anion exchange resin (Resin-P); 0.5 M NaHCO3-P (NaHCO3-Pi and Po); 0.1 M NaOH (NaOH-l-Pi and Po); ultrasonication in 0.1 M NaOH at 75 watt (NaOH-ll-Pi and Po); 1.0 M HCI(HCI-Pi); and H2SO4 digestion and H2O2 oxidation, (H2SO4P). General trends in soil P were evident over 15 years of cultivation. Resin-P, NaHCO3-Pi, NaOH-l-Pi, NaOH-ll-Pi and HCl-Pi were reduced in the Avalon soil, while only the NaHCO3-Pi and NaOH-ll-Pi decreased in the Clovelly soil. It is hypothesised that NaOH-l-Pi, which showed the largest decrease, was mainly responsible for the replenishment of the labile P pool. In the Po fraction, NaHCO3-Po and NaOH-ll-Po decreased with time in the Avalon soil, in con...
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