Impactul antropic asupra formării fracţiei aminoacide a azotului din sol şi rezervelor sale

New data have been obtained regarding the fractional composition of soil amino acid nitrogen and its reserves (0.45 to 1.15 t/ha) in typical chernozem (in a seven-field-rotation system with fodder crops) compared with humus reserves (0.7 to 2.16 %) and gross nitrogen (14.07 to 43.27 %). The content...

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Main Author: FRUNZE Nina
Format: Article
Language:English
Published: Moldova State Agrarian University 2015-06-01
Series:Stiinta Agricola
Subjects:
Online Access:https://sa.uasm.md/index.php?journal=sa&page=article&op=view&path%5B%5D=108&path%5B%5D=112
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spelling doaj-9c19466f227446f4b5c407e1ce66e0392020-11-25T01:15:26ZengMoldova State Agrarian UniversityStiinta Agricola1857-00032587-32022015-06-0114246Impactul antropic asupra formării fracţiei aminoacide a azotului din sol şi rezervelor saleFRUNZE Nina 0Institutul de Microbiologie şi Biotehnologie al Academiei de Ştiinţe a MoldoveiNew data have been obtained regarding the fractional composition of soil amino acid nitrogen and its reserves (0.45 to 1.15 t/ha) in typical chernozem (in a seven-field-rotation system with fodder crops) compared with humus reserves (0.7 to 2.16 %) and gross nitrogen (14.07 to 43.27 %). The content of hydrolyzed nitrogen forms was determined (43.73 to 74.6 %), as well as the contribution of individual amino acids to the formation of amino acid nitrogen (0.22 to 11.07%). The nitrogen of six amino acids (alanine, aspartic acid, glycine, arginine, glutamic acid and serine) constitutes 67 % from the total nitrogen of amino acids. The rate of nine amino acids (lysine, leucine, proline, threonine, histidine, valine, isoleucine, cystine, and phenylalanine) in the formation of nitrogen reserves ranges up to 30 %. Tyrozine, methionine and a aminobutyric acid have made the least contribution to this process. For comparison, soil samples from a forest strip (natural biocenosis) were also analyzed. The obtained results show the superiority of virgin soil in the formation of amino acids nitrogen (1.6 t/ha), as compared witn arable soils (0,45-1,14 t/ha). Structural changes in the latter ones could be characterized by analogy with the modifications in the structure of microbial communities, which are usually observed in the case of situations that are considered as stressful. https://sa.uasm.md/index.php?journal=sa&page=article&op=view&path%5B%5D=108&path%5B%5D=112crop rotationfodder cropstypical chernozemamino acid nitrogenhumus
collection DOAJ
language English
format Article
sources DOAJ
author FRUNZE Nina
spellingShingle FRUNZE Nina
Impactul antropic asupra formării fracţiei aminoacide a azotului din sol şi rezervelor sale
Stiinta Agricola
crop rotation
fodder crops
typical chernozem
amino acid nitrogen
humus
author_facet FRUNZE Nina
author_sort FRUNZE Nina
title Impactul antropic asupra formării fracţiei aminoacide a azotului din sol şi rezervelor sale
title_short Impactul antropic asupra formării fracţiei aminoacide a azotului din sol şi rezervelor sale
title_full Impactul antropic asupra formării fracţiei aminoacide a azotului din sol şi rezervelor sale
title_fullStr Impactul antropic asupra formării fracţiei aminoacide a azotului din sol şi rezervelor sale
title_full_unstemmed Impactul antropic asupra formării fracţiei aminoacide a azotului din sol şi rezervelor sale
title_sort impactul antropic asupra formării fracţiei aminoacide a azotului din sol şi rezervelor sale
publisher Moldova State Agrarian University
series Stiinta Agricola
issn 1857-0003
2587-3202
publishDate 2015-06-01
description New data have been obtained regarding the fractional composition of soil amino acid nitrogen and its reserves (0.45 to 1.15 t/ha) in typical chernozem (in a seven-field-rotation system with fodder crops) compared with humus reserves (0.7 to 2.16 %) and gross nitrogen (14.07 to 43.27 %). The content of hydrolyzed nitrogen forms was determined (43.73 to 74.6 %), as well as the contribution of individual amino acids to the formation of amino acid nitrogen (0.22 to 11.07%). The nitrogen of six amino acids (alanine, aspartic acid, glycine, arginine, glutamic acid and serine) constitutes 67 % from the total nitrogen of amino acids. The rate of nine amino acids (lysine, leucine, proline, threonine, histidine, valine, isoleucine, cystine, and phenylalanine) in the formation of nitrogen reserves ranges up to 30 %. Tyrozine, methionine and a aminobutyric acid have made the least contribution to this process. For comparison, soil samples from a forest strip (natural biocenosis) were also analyzed. The obtained results show the superiority of virgin soil in the formation of amino acids nitrogen (1.6 t/ha), as compared witn arable soils (0,45-1,14 t/ha). Structural changes in the latter ones could be characterized by analogy with the modifications in the structure of microbial communities, which are usually observed in the case of situations that are considered as stressful.
topic crop rotation
fodder crops
typical chernozem
amino acid nitrogen
humus
url https://sa.uasm.md/index.php?journal=sa&page=article&op=view&path%5B%5D=108&path%5B%5D=112
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