首页> 外文期刊>Water, Air, and Soil Pollution >AMINO ACIDS, TOTAL ORGANIC AND INORGANIC NITROGEN IN FOREST FLOOR SOIL SOLUTION AT LOW AND HIGH NITROGEN INPUT
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AMINO ACIDS, TOTAL ORGANIC AND INORGANIC NITROGEN IN FOREST FLOOR SOIL SOLUTION AT LOW AND HIGH NITROGEN INPUT

机译:低氮输入和高氮输入下森林土壤溶液中氨基酸,总有机和无机氮的含量

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摘要

It is now widely accepted that many plants and mycorrhizal fungi have the ability to take up organic nitrogen (N) in the form of amino acids, although the importance of this uptake in the field is less clear. In the laboratory it has been shown that uptake affinity and uptake kinetics of ammonium and some amino acids are comparable. The relative uptake of either N form from the soil solution would thus be related to the relative concentration in the soil solution accessed by roots. We sampled soil solution from the F- and H-layers under a Spruce stand in a fertilisation experiment in Flakaliden, northern Sweden. Tension lysimeters were installed in plots receiving irrigation (I) or irrigation plus liquid fertilisation (IL). The soil solution samples were analysed for ammonium, nitrate, free amino acids, hydrolysable amino acids, total organic N and total organic C. In I plots the concentrations of both ammonium and free amino acids were very low with no obvious dominance of either form. In IL plots inorganic N concentrations were higher and amino acid concentrations were lower compared to I plots, and thus the inorganic N dominated over amino acids. There was no difference in H-layer ammonium concentration between I and IL plots despite the high N addition rate on the soil surface during nights of sampling. The lower amino acid concentrations in IL plots might be an effect of a decreased proteolytic activity due to the documented shift in mycorrhizal fungi species composition at the site.
机译:现已广泛接受的是,许多植物和菌根真菌都具有吸收氨基酸形式的有机氮(N)的能力,尽管这种吸收在田间的重要性尚不清楚。在实验室中,已经证明铵和某些氨基酸的吸收亲和力和吸收动力学是可比的。因此,从土壤溶液中吸收的任何一种氮形式都与根部进入土壤溶液中的相对浓度有关。在瑞典北部的弗拉卡利登的施肥实验中,我们在云杉林下从F层和H层中取样土壤溶液。张力渗漏计安装在接受灌溉(I)或灌溉加液肥(IL)的地块中。分析了土壤溶液样品中的铵,硝酸盐,游离氨基酸,可水解氨基酸,总有机氮和总有机碳。在I图中,铵和游离氨基酸的浓度都非常低,两种形式均无明显优势。在IL图中,与I图中相比,无机N浓度更高而氨基酸浓度更低,因此无机N占主导地位。尽管在夜间采样时土壤表面氮的添加率很高,但I和IL图之间的H层铵浓度没有差异。 IL曲线图中较低的氨基酸浓度可能是蛋白水解活性降低的结果,这是由于该部位的菌根真菌种类组成发生了变化。

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