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首页> 外文期刊>日本土壤肥料学雑誌 >The contribution of nitrogen through microbial biomass to plant nitrogen uptake in upland soils with different physiochemical properties.
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The contribution of nitrogen through microbial biomass to plant nitrogen uptake in upland soils with different physiochemical properties.

机译:氮通过微生物生物量对具有不同理化特性的旱地土壤植物氮吸收的贡献。

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摘要

The contribution of N through microbial biomass to plant N uptake was investigated in a light-coloured Andosol, Humic Andosol, brown lowland soil (Fluvisol), dark red soil and a sand-dune Regosol by labelling microbial biomass N with 15N. At 3 weeksafter amendment, upland rice was sown and cultivated in 15 weeks. Soil and plant samples were taken at every 3 weeks after sowing (WAS). The results showed: (1) soil microbial biomass N amounts were in the order: dark red soil > Humic Andosol > brown lowland soil > light-coloured Andosol > sand-dune Regosol. Microbial biomass N in all soils was almost constant during the cropping period; (2) plant N uptake was in the order: brown lowland soil > Humic Andosol > dark red soil > light-coloured Andosol > sand-dune Regosol. Plant N uptake in all soils was greatest in the heading stage, suggesting that the N uptake is high in the reproductive stage; (3) At 0-3 WAS, the 15N abundance of plant N uptake in all soils was close to that of the microbial biomass N. At 6-15 WAS, however, it was close to that of soil total N. It is assumed that the N taken up by the plant is mainly derived from the N produced through the microbial biomass in the vegetative growth stage (0-6 WAS), and mainly from organic N except for the microbial biomass N in the reproductive stage (6-15 WAS); and (4) except for the dark red soil, plant N uptake was closely correlated with microbial biomass N at the vegetative growth stage (R=0.995, n = 4), showing that microbial biomass N is a major source of N for plants at this stage.
机译:通过用15N标记微生物生物量氮,在浅色的Andosol,腐殖质Andosol,棕色低地土壤(Fluvisol),深红色土壤和沙丘Regosol中研究了N通过微生物生物量对植物N吸收的贡献。改良后3周,播种并培育了15周的旱稻。播种后每3周采集一次土壤和植物样本(WAS)。结果表明:(1)土壤微生物量氮的含量顺序为:暗红色土壤>腐殖质安多索尔>棕色低地土壤>浅色安多索尔>沙丘雷哥索尔。在耕作期间,所有土壤中的微生物生物量氮几乎恒定。 (2)植物氮素吸收的顺序为:棕色低地土壤>腐殖质Andosol>深红色土壤>浅色Andosol>沙丘Regosol。在抽穗期,所有土壤中植物的氮素吸收量最大,这表明在生育期氮素吸收量较高。 (3)在0-3 WAS时,所有土壤中15 N的植物氮吸收量接近微生物生物量N。但是在6-15 WAS时,它接近于土壤总氮。植物吸收的氮主要来自营养生长阶段(0-6 WAS)通过微生物量生产的氮,主要来自有机氮(生殖阶段(6-15)除外) WAS); (4)除深红色土壤外,营养生长阶段植物的氮吸收与微生物量氮密切相关(R = 0.995,n = 4),表明微生物量氮是植物生长时氮的主要来源。这个阶段。

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