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Identification of free amino acids in peat by gas chromatography and mass spectrometry
Author(s) -
KUNNAS A.V.,
ERONEN M.
Publication year - 1994
Publication title -
european journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 1351-0754
DOI - 10.1111/j.1365-2389.1994.tb00523.x
Subject(s) - amino acid , valine , chemistry , alanine , phenylalanine , isoleucine , glycine , proline , leucine , chromatography , mass spectrometry , aromatic amino acids , methionine , biochemistry
Summary The qualitative and quantitative composition of free amino acids in a typical Finnish peat bog at various depths down to 5.3 m below the surface was studied using capillary gas chromatography and mass spectrometry. Sixteen amino acids were identified at each depth: α‐alanine, β‐alanine, glycine, valine, leucine, proline, isoleucine, serine, threonine, glutamic acid, aspartic acid, phenylalanine, tyrosine, γ‐aminobutyric acid, ornithine and lysine. Their amounts decreased markedly at a depth of 40–100 cm. The total amount of amino acids varied between 0.6 and 5.6 g kg −1 dry matter (i.e. 0.06–0.56%) depending on the depth. The proportion of neutral amino acids was greatest at all depths studied, except at the surface layer where it ranged between 41 and 72% by mass. The acidic amino acids decreased with depth from 56 to 23% of the total. The proportion of aromatic amino acids was very small, 3.2–5.5% by mass. In samples from aerobic conditions, where the microbial production of free amino acids was the greatest, α‐ala, gly, glu and asp were most abundant. In peat from anaerobic conditions, where the microbiological activity was low, the proportion of the most chemically stable amino acid was exceptionally high. This may have been because glycine was a degradation product of other amino acids or peptides. Peat type and degree of decomposition had a strong influence on the total amount of free amino acids and their qualitative composition.