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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Moldova State Agrarian University
2015-06-01
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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.
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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 |
work_keys_str_mv |
AT frunzenina impactulantropicasupraformariifractieiaminoacideaazotuluidinsolsirezervelorsale |
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1725153305741492224 |