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Efficiency of Phosphatases in Mobilization of Native Phosphorus Fractions Under Different Vegetation

机译:磷素在不同植被下调动天然磷组分的效率

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摘要

The efficiency of acid and alkaline phosphatase toward hydrolysis of different P fractions was studied under fallow, rhizosphere and non-rhizosphere soils of crops, trees and grasses from Aridisol, and forest rhizosphere and non-rhizosphere soils of Inceptisol. Native P of soil was fractioned into four different pools: water-soluble inorganic phosphorus (Pi) and organic phosphorus (Po), NaHC03 (0.5 M)-extractable Pi and Po, NaOH (0.1 M)-extractable Pi and Po, HC1 (1.0 M)-extractable Pi and Po and residual P after digestion to H202:H2S04 (1:4). The decrease in different Po fractions due to the action of both acid and alkaline phosphatase showed 41.3-86.7 % of water-soluble fraction, 50-84.1 % of NaHC03 fraction, 14.6-25.9 % of NaOH fraction and 8.0-19.2 % of HC1 fraction was hydrolyzed under different vegetation. The rate of organic phosphorus hydrolysis by acid and alkaline phosphatase was initially rapid followed by a gradual declining rate, which was constant after 8 h onwards for acid phosphatase and after 9 h onward till 24 h for alkaline phosphatase. At initial stage (<4 h), the rate of hydrolysis by acid phosphatase was almost doubled than alkaline phosphatase. The result indicates that acid phosphatase was 8.8-13.8 % more efficient as compared to the alkaline phosphatase toward hydrolysis of different soil P fractions, while the residual P fractions were hydrolyzed 17.3 % more by alkaline phosphatase than acid phosphatase. Among the different P fractions, the residual P was most resistantand water soluble and NaHC03-P was most susceptible to phosphatase enzymes.
机译:研究了在Aridisol作物,树木和草类的休耕土壤,根际土壤和非根际土壤以及Inceptisol的森林根际土壤和非根际土壤中,酸性和碱性磷酸酶对不同P组分的水解效率。土壤的天然P被分为四个不同的库:水溶性无机磷(Pi)和有机磷(Po),NaHC03(0.5 M)可萃取的Pi和Po,NaOH(0.1 M)可萃取的Pi和Po,HC1(消化至H2O2:H2SO4(1:4)后可提取1.0 M)的Pi和Po,以及残留的P.由于酸性和碱性磷酸酶的作用,不同Po组分的减少表明,水溶性组分占41.3-86.7%,NaHCO 3组分占50-84.1%,NaOH组分占14.6-25.9%,HCl组分占8.0-19.2%。在不同的植被下被水解最初由酸和碱性磷酸酶水解的有机磷的速率很快,然后逐渐下降,对于酸性磷酸酶而言,此速率在8小时后保持恒定,而对于碱性磷酸酶而言,此速率在9小时后至24小时之后均保持恒定。在初始阶段(<4小时),酸性磷酸酶的水解速率几乎是碱性磷酸酶的两倍。结果表明,与碱性磷酸酶相比,酸性磷酸酶对不同土壤P组分的水解效率高8.8-13.8%,而碱性磷酸酶比酸性磷酸酶水解残留的P组分的效率高17.3%。在不同的P部分中,残留的P具有最高的抵抗力和水溶性,而NaHCO 3 -P对磷酸酶最敏感。

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