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Assessment of bioavailable organic phosphorus in tropical forest soils by organic acid extraction and phosphatase hydrolysis

机译:通过有机酸萃取和磷酸酶水解评估热带森林土壤中可生物利用的有机磷

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摘要

Soil organic phosphorus contributes to the nutrition of tropical trees, but is not accounted for in standard soil phosphorus tests. Plants and microbes can release organic anions to solubilize organic phosphorus from soil surfaces, and synthesize phosphatases to release inorganic phosphate from the solubilized compounds. We developed a procedure to estimate bioavailable organic phosphorus in tropical forest soils by simulating the secretion processes of organic acids and phosphatases. Five lowland tropical forest soils with contrasting properties (pH 4.4–6.1, total P 86–429 mg P kg− 1) were extracted with 2 mM citric acid (i.e., 10 μmol g− 1, approximating rhizosphere concentrations) adjusted to soil pH in a 4:1 solution to soil ratio for 1 h. Three phosphatase enzymes were then added to the soil extract to determine the forms of hydrolysable organic phosphorus. Total phosphorus extracted by the procedure ranged between 3.22 and 8.06 mg P kg− 1 (mean 5.55 ± 0.42 mg P kg− 1), of which on average three quarters was unreactive phosphorus (i.e., organic phosphorus plus inorganic polyphosphate). Of the enzyme-hydrolysable unreactive phosphorus, 28% was simple phosphomonoesters hydrolyzed by phosphomonoesterase from bovine intestinal mucosa, a further 18% was phosphodiesters hydrolyzed by a combination of nuclease from Penicillium citrinum and phosphomonoesterase, and the remaining 51% was hydrolyzed by a broad-spectrum phytase from wheat. We conclude that soil organic phosphorus can be solubilized and hydrolyzed by a combination of organic acids and phosphatase enzymes in lowland tropical forest soils, indicating that this pathway could make a significant contribution to biological phosphorus acquisition in tropical forests. Furthermore, we have developed a method that can be used to assess the bioavailability of this soil organic phosphorus.
机译:土壤有机磷有助于热带树木的营养,但在标准土壤磷测试中并未考虑。植物和微生物可以释放有机阴离子以溶解土壤表面的有机磷,并合成磷酸酶以释放溶解的化合物中的无机磷酸盐。我们通过模拟有机酸和磷酸酶的分泌过程,开发了一种估算热带森林土壤中可生物利用的有机磷的程序。用2 mM柠檬酸(即10μmolg −1)提取五种具有相反特性的低地热带森林土壤(pH值4.4-6.1,总P 86-429 mg P kg −1 ,近似根际浓度),以溶液与土壤的比例为4:1调整至土壤pH值1小时。然后将三种磷酸酶添加到土壤提取物中,以确定可水解有机磷的形式。该程序提取的总磷含量在3.22至8.06 mg P P kg −1 之间(平均5.55±0.42 mg P P kg kg −1 ),其中平均四分之三没有反应磷(即有机磷加无机多磷酸盐)。酶可水解的非反应性磷中,有28%是由牛肠粘膜中的磷酸单酯酶水解的简单磷酸单酯,另外18%是由柠檬酸青霉菌的核酸酶和磷酸单酯酶的组合水解的磷酸二酯,其余的51%是由广谱水解的。小麦的光谱植酸酶。我们得出的结论是,有机酸和磷酸酶的组合可以使低地热带森林土壤中的有机磷溶解和水解,这表明该途径可以为热带森林生物磷的吸收做出重要贡献。此外,我们开发了一种可用于评估这种土壤有机磷的生物利用度的方法。

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