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Free amino acids in Arctic salt marsh coastal sites and plant nitrogen acquisition.

机译:北极盐沼沿海地区的游离氨基酸和植物氮素的获取。

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The importance of free amino acids as a source of plant nitrogen was examined in an Arctic coastal salt-marsh. Concentrations of inorganic nitrogen in salt-marsh soils were low relative to those reported for most temperate soils, whereas soluble organic nitrogen concentrations of salt-marsh soils were relatively high; the median ratio of free amino acid nitrogen as a proportion of ammonium nitrogen was 0.36 and amino acid concentrations exceeded those of ammonium in 24% of samples. Growth of the salt-marsh grass Puccinellia phryganodes on glycine in a continuous flow hydroponic medium was similar to growth on ammonium ions at an equivalent concentration of nitrogen. Furthermore, in short-term excised root uptake experiments, rates of glycine uptake were equal to rates of ammonium and nitrate uptake combined when roots were provided with all three nitrogen substrates at equal concentrations. Amino acid uptake relative to ammonium uptake was favoured at high temperatures, high salinity and low pH. Free amino acids turned over rapidly in the soil, with half-lives in the soil solution ranging from 8–23 h for glycine, compared with ranges of 6–15 h and 6–16 h for ammonium and nitrate ions, respectively. Plant incorporation of 15N tracer injected into soil cores was 56, 83, and 68% of incorporation by soil microorganisms for glycine, ammonium and nitrate ions, respectively. The simultaneous incorporation of 13C and 15N into plant roots following injection of 13C15N-glycine into soil cores indicated that at least a portion of this amino acid was absorbed intact. In a model of the dynamics of nitrogen movement in an Arctic salt-marsh grazed and grubbed by geese, the direct uptake of organic nitrogen by plant roots was required to obtain rates of mineralization consistent with empirical estimates. Overall, these results indicate that free amino acids are likely a substantial contribution to plant nitrogen nutrition in Arctic coastal marshes.
机译:在北极沿海盐沼中研究了游离氨基酸作为植物氮源的重要性。相对于大多数温带土壤而言,盐沼土壤中的无机氮浓度较低,而盐沼土壤中的可溶性有机氮浓度较高。在24%的样品中,游离氨基酸氮与铵态氮的中位数比率为0.36,氨基酸浓度超过铵态。在连续流动的水培介质中,盐沼草 Puccinellia phryganodes 在甘氨酸上的生长类似于在氮浓度相同的铵离子上的生长。此外,在短期切除的根吸收实验中,当以相同浓度的所有三种氮素为根提供根时,甘氨酸的吸收率等于铵和硝酸盐的吸收率之和。在高温,高盐度和低pH值下,氨基酸吸收相对于铵吸收更为有利。游离氨基酸在土壤中的迁移迅速,甘氨酸在土壤溶液中的半衰期为8–23 h,而铵离子和硝酸根离子的半衰期分别为6–15 h和6–16 h。注入土壤核心的 15 N示踪剂的植物掺入量分别为土壤微生物中甘氨酸,铵离子和硝酸根离子掺入量的56%,83%和68%。将 13 C 15 N-甘氨酸注入植物根后,同时将 13 C和 15 N掺入植物根中。土壤核心表明该氨基酸的至少一部分被完整吸收。在一个由鹅吃草和g食的北极盐沼中氮运动的动力学模型中,需要植物根部直接吸收有机氮才能获得与经验估计一致的矿化速率。总体而言,这些结果表明,游离氨基酸可能对北极沿岸沼泽地的植物氮素营养有重要贡献。

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