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Temporal variation in pools of amino acids, inorganic and microbial N in a temperate grassland soil

机译:温带草原土壤中氨基酸,无机氮和微生物氮库的时间变化

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Plants can take up intact amino acids, even in competition with soil microbes, yet we lack detailed information on which amino acids dominate the soil and whether amino acid composition varies seasonally. This study tested the hypotheses that 1) the pool of amino acid N is generally larger than inorganic N; 2) temporal changes in the concentration of amino acid N is related to changes in the size of the microbial N pool; and 3) amino acid N is dominated by simple, neutral amino acids during warm months, whereas during cold months the amino acid N is dominated by more complex aromatic and basic amino acids. Approximately every month for two years we collected soil from a temperate, sub-alpine grassland in the Snowy Mountains of Australia. We quantified exchangeable pools of amino acids, nitrate and ammonium in 1 M KCl extracts. Microbial N was quantified by chloroform fumigation. Averaged across the 21 monthly samples, nitrate was 13% of the quantified pool of soluble non-protein N, ammonium was 34% and amino acid N was 53%. These data are consistent with our hypothesis that the pool of amino acid N is larger than inorganic N. There was substantial variation between months in concentrations of amino acids and inorganic N, but no clear temporal pattern. Microbial N did not vary between months, and thus changes in amino acid N were unrelated to microbial N. Principal components analysis indicated multivariate groupings of the different pools of N that were broadly indicative of function and/or biosynthetic relationships. Thus PCA identified a grouping of aromatic amino acids (Phe and Try) with amino acids derived from oxaloacetate (Asp, Ala, Val, Leu, Ile), and a second group comprising microbial N, nitrate and glycine. The pool of exchangeable amino acid N was dominated by Arg (26% of amino N) Val (20%) Gln (18%), Try (8%) and Asn (8%). Contrary to our hypothesis, the composition of the amino acid pool did not vary in a consistent way between months, and there was no evidence simple amino acids were relatively more abundant in warm months and complex amino acids in cool months.
机译:即使与土壤微生物竞争,植物也可以吸收完整的氨基酸,但是我们缺乏有关哪些氨基酸在土壤中占主导地位以及氨基酸组成是否随季节变化的详细信息。这项研究检验了以下假设:1)氨基酸N的库通常大于无机N。 2)氨基酸N浓度的时间变化与微生物N库大小的变化有关; 3)在温暖的月份,氨基酸N以简单的中性氨基酸为主,而在寒冷的月份,氨基酸N以较复杂的芳香族和碱性氨基酸为主。在大约两年的时间里,我们每个月大约从澳大利亚雪山的温带亚高山草原上收集土壤。我们量化了1 M KCl提取物中氨基酸,硝酸盐和铵盐的可交换池。通过氯仿熏蒸对微生物氮进行定量。在21个月度样品中取平均值,硝酸盐为可溶性非蛋白N定量池的13%,铵为34%,氨基酸N为53%。这些数据与我们的假设一致,即氨基酸N的池大于无机N。氨基酸和无机N的浓度在数月之间存在很大差异,但没有明确的时间模式。微生物氮在数月之间没有变化,因此氨基酸N的变化与微生物N无关。主成分分析表明,不同氮素库的多元分组广泛地表明了功能和/或生物合成关系。因此,PCA将芳香族氨基酸(Phe和Try)与衍生自草酰乙酸的氨基酸(Asp,Ala,Val,Leu,Ile)组成一组,第二组包括微生物N,硝酸盐和甘氨酸。可交换氨基酸N的集合由Arg(占氨基N的26%)Val(20%)Gln(18%),Try(8%)和Asn(8%)主导。与我们的假设相反,氨基酸库的组成在几个月之间没有一致的变化,并且没有证据表明在温暖的月份中简单氨基酸相对较多,而在凉爽的月份中复杂氨基酸相对较多。

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