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:氮气通过微生物生物量对旱地土壤施氮氮吸收的贡献,不同的物理化学性质。

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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N,在浅色和溶胶,腐殖和溶剂,棕色的低地土壤(Flyvisol),深红色土壤和沙丘升温中,研究了N通过微生物生物量对植物N吸收的贡献。在3个日期修正案中,15周播种和培养旱稻。播种后每3周拍摄土壤和植物样品。结果表明:(1)土壤微生物生物量N的数量有序:深红色土壤>腐殖质和溶溶胶>棕色低地土壤>浅色和溶胶>沙丘雷科尔。在种植期间,所有土壤中的微生物生物量N几乎是恒定的; (2)植物N吐痰是有序:棕色低地土壤>腐殖质和溶胶>深红色土壤>浅色和溶胶>沙丘雷科尔。在标题阶段,所有土壤中的植物都是最大的,这表明生殖阶段中的N吸收很高; (3)在0-3的情况下,所有土壤中的植物N富度均接近微生物生物量N.然而,在6-15处,它接近土壤总体N的近。假设由植物占用的N主要来自营养生长阶段(0-6)中通过微生物生物量产生的N,主要来自生殖阶段中的微生物生物量N除了有机N外(6-15曾是); (4)除了深红色土壤外,植物N吸收与营养生长阶段的微生物生物量N紧密相关(r = 0.995,n = 4),显示微生物生物量N是植物的n的主要来源这个阶段。

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