IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT

The aim of the work was to study the direction and intensity of mineralization and immobilization processes in different layers of gray forest soil at fallow fields, extensively and intensively used agrosoils. The research included laboratory analysis, microbiological studies, and statistical processing. For the fallow plots, the layers chosen for study were Hd – turf (010 cm), He – humus-eluvial (11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (116156 cm), Pi – bedrock with occasional insertions of illuvial soil (157191 cm); for the agrosoils of the stationary experiments: He – humus-eluvial (0-10 and 11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (11656 cm). We found that humus mineralization differed in some layers of the gray forest soil under these management regimes. At fallows, the intensity of humus mineralization tended to decrease with depth, and it was interrupted in the Ih and Ip layers. In the intensively used agrosoil, humus mineralization was more active in Hi- and Ih- layers. Comparatively, the activity of humus mineralization smoothly decreased in the profile of the extensively used agrosoil from the uppermost layer to the lower by 97.2%. The mineralization coefficient of Nitrogen compounds gradually decreased in the fallow ground and extensively used agrosoil, unlike the intensively managed agrosoil, in which the intensity of mineralization-immobilization of nitrogen compounds increased in the He and Hi layers. It was shown that the fallow ground had the more efficient system to transfer substrates and mineral ions down the profile to the lower layers. The difference in biologic activity between the upper and lower layers was maximum in the fallow ground, intermediate in the intensively used agrosoil and minimum in the extensive agrosoil. Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Malynovska I. M. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch ; Russisch ; Ukrainisch

Erschienen:	2019

Schlagwörter:	soil horizons index of pedotrophy nitrogen mineralization coefficient humus mineralization activity fallow ground agrosoil

Übergeordnetes Werk:	In: Biotechnologia Acta - National Academy of Sciences of Ukraine, Palladin Institute of Biochemistry, 2016, 12(2019), 6, Seite 65-70
Übergeordnetes Werk:	volume:12 ; year:2019 ; number:6 ; pages:65-70

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.15407/biotech12.06.065

Katalog-ID:	DOAJ018009212

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allfields	10.15407/biotech12.06.065 doi (DE-627)DOAJ018009212 (DE-599)DOAJ047a07cfb8494b91b6af08d9fae074f7 DE-627 ger DE-627 rakwb eng rus ukr TP248.13-248.65 Malynovska I. M. verfasserin aut IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The aim of the work was to study the direction and intensity of mineralization and immobilization processes in different layers of gray forest soil at fallow fields, extensively and intensively used agrosoils. The research included laboratory analysis, microbiological studies, and statistical processing. For the fallow plots, the layers chosen for study were Hd – turf (010 cm), He – humus-eluvial (11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (116156 cm), Pi – bedrock with occasional insertions of illuvial soil (157191 cm); for the agrosoils of the stationary experiments: He – humus-eluvial (0-10 and 11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (11656 cm). We found that humus mineralization differed in some layers of the gray forest soil under these management regimes. At fallows, the intensity of humus mineralization tended to decrease with depth, and it was interrupted in the Ih and Ip layers. In the intensively used agrosoil, humus mineralization was more active in Hi- and Ih- layers. Comparatively, the activity of humus mineralization smoothly decreased in the profile of the extensively used agrosoil from the uppermost layer to the lower by 97.2%. The mineralization coefficient of Nitrogen compounds gradually decreased in the fallow ground and extensively used agrosoil, unlike the intensively managed agrosoil, in which the intensity of mineralization-immobilization of nitrogen compounds increased in the He and Hi layers. It was shown that the fallow ground had the more efficient system to transfer substrates and mineral ions down the profile to the lower layers. The difference in biologic activity between the upper and lower layers was maximum in the fallow ground, intermediate in the intensively used agrosoil and minimum in the extensive agrosoil. soil horizons index of pedotrophy nitrogen mineralization coefficient humus mineralization activity fallow ground agrosoil Biotechnology In Biotechnologia Acta National Academy of Sciences of Ukraine, Palladin Institute of Biochemistry, 2016 12(2019), 6, Seite 65-70 (DE-627)863737730 (DE-600)2863118-3 2410776X nnns volume:12 year:2019 number:6 pages:65-70 https://doi.org/10.15407/biotech12.06.065 kostenfrei https://doaj.org/article/047a07cfb8494b91b6af08d9fae074f7 kostenfrei http://biotechnology.kiev.ua/images/storage/6_2019/malinovska_6_2019.pdf kostenfrei https://doaj.org/toc/2410-7751 Journal toc kostenfrei https://doaj.org/toc/2410-776X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 12 2019 6 65-70
spelling	10.15407/biotech12.06.065 doi (DE-627)DOAJ018009212 (DE-599)DOAJ047a07cfb8494b91b6af08d9fae074f7 DE-627 ger DE-627 rakwb eng rus ukr TP248.13-248.65 Malynovska I. M. verfasserin aut IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The aim of the work was to study the direction and intensity of mineralization and immobilization processes in different layers of gray forest soil at fallow fields, extensively and intensively used agrosoils. The research included laboratory analysis, microbiological studies, and statistical processing. For the fallow plots, the layers chosen for study were Hd – turf (010 cm), He – humus-eluvial (11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (116156 cm), Pi – bedrock with occasional insertions of illuvial soil (157191 cm); for the agrosoils of the stationary experiments: He – humus-eluvial (0-10 and 11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (11656 cm). We found that humus mineralization differed in some layers of the gray forest soil under these management regimes. At fallows, the intensity of humus mineralization tended to decrease with depth, and it was interrupted in the Ih and Ip layers. In the intensively used agrosoil, humus mineralization was more active in Hi- and Ih- layers. Comparatively, the activity of humus mineralization smoothly decreased in the profile of the extensively used agrosoil from the uppermost layer to the lower by 97.2%. The mineralization coefficient of Nitrogen compounds gradually decreased in the fallow ground and extensively used agrosoil, unlike the intensively managed agrosoil, in which the intensity of mineralization-immobilization of nitrogen compounds increased in the He and Hi layers. It was shown that the fallow ground had the more efficient system to transfer substrates and mineral ions down the profile to the lower layers. The difference in biologic activity between the upper and lower layers was maximum in the fallow ground, intermediate in the intensively used agrosoil and minimum in the extensive agrosoil. soil horizons index of pedotrophy nitrogen mineralization coefficient humus mineralization activity fallow ground agrosoil Biotechnology In Biotechnologia Acta National Academy of Sciences of Ukraine, Palladin Institute of Biochemistry, 2016 12(2019), 6, Seite 65-70 (DE-627)863737730 (DE-600)2863118-3 2410776X nnns volume:12 year:2019 number:6 pages:65-70 https://doi.org/10.15407/biotech12.06.065 kostenfrei https://doaj.org/article/047a07cfb8494b91b6af08d9fae074f7 kostenfrei http://biotechnology.kiev.ua/images/storage/6_2019/malinovska_6_2019.pdf kostenfrei https://doaj.org/toc/2410-7751 Journal toc kostenfrei https://doaj.org/toc/2410-776X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 12 2019 6 65-70
allfields_unstemmed	10.15407/biotech12.06.065 doi (DE-627)DOAJ018009212 (DE-599)DOAJ047a07cfb8494b91b6af08d9fae074f7 DE-627 ger DE-627 rakwb eng rus ukr TP248.13-248.65 Malynovska I. M. verfasserin aut IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The aim of the work was to study the direction and intensity of mineralization and immobilization processes in different layers of gray forest soil at fallow fields, extensively and intensively used agrosoils. The research included laboratory analysis, microbiological studies, and statistical processing. For the fallow plots, the layers chosen for study were Hd – turf (010 cm), He – humus-eluvial (11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (116156 cm), Pi – bedrock with occasional insertions of illuvial soil (157191 cm); for the agrosoils of the stationary experiments: He – humus-eluvial (0-10 and 11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (11656 cm). We found that humus mineralization differed in some layers of the gray forest soil under these management regimes. At fallows, the intensity of humus mineralization tended to decrease with depth, and it was interrupted in the Ih and Ip layers. In the intensively used agrosoil, humus mineralization was more active in Hi- and Ih- layers. Comparatively, the activity of humus mineralization smoothly decreased in the profile of the extensively used agrosoil from the uppermost layer to the lower by 97.2%. The mineralization coefficient of Nitrogen compounds gradually decreased in the fallow ground and extensively used agrosoil, unlike the intensively managed agrosoil, in which the intensity of mineralization-immobilization of nitrogen compounds increased in the He and Hi layers. It was shown that the fallow ground had the more efficient system to transfer substrates and mineral ions down the profile to the lower layers. The difference in biologic activity between the upper and lower layers was maximum in the fallow ground, intermediate in the intensively used agrosoil and minimum in the extensive agrosoil. soil horizons index of pedotrophy nitrogen mineralization coefficient humus mineralization activity fallow ground agrosoil Biotechnology In Biotechnologia Acta National Academy of Sciences of Ukraine, Palladin Institute of Biochemistry, 2016 12(2019), 6, Seite 65-70 (DE-627)863737730 (DE-600)2863118-3 2410776X nnns volume:12 year:2019 number:6 pages:65-70 https://doi.org/10.15407/biotech12.06.065 kostenfrei https://doaj.org/article/047a07cfb8494b91b6af08d9fae074f7 kostenfrei http://biotechnology.kiev.ua/images/storage/6_2019/malinovska_6_2019.pdf kostenfrei https://doaj.org/toc/2410-7751 Journal toc kostenfrei https://doaj.org/toc/2410-776X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 12 2019 6 65-70
allfieldsGer	10.15407/biotech12.06.065 doi (DE-627)DOAJ018009212 (DE-599)DOAJ047a07cfb8494b91b6af08d9fae074f7 DE-627 ger DE-627 rakwb eng rus ukr TP248.13-248.65 Malynovska I. M. verfasserin aut IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The aim of the work was to study the direction and intensity of mineralization and immobilization processes in different layers of gray forest soil at fallow fields, extensively and intensively used agrosoils. The research included laboratory analysis, microbiological studies, and statistical processing. For the fallow plots, the layers chosen for study were Hd – turf (010 cm), He – humus-eluvial (11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (116156 cm), Pi – bedrock with occasional insertions of illuvial soil (157191 cm); for the agrosoils of the stationary experiments: He – humus-eluvial (0-10 and 11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (11656 cm). We found that humus mineralization differed in some layers of the gray forest soil under these management regimes. At fallows, the intensity of humus mineralization tended to decrease with depth, and it was interrupted in the Ih and Ip layers. In the intensively used agrosoil, humus mineralization was more active in Hi- and Ih- layers. Comparatively, the activity of humus mineralization smoothly decreased in the profile of the extensively used agrosoil from the uppermost layer to the lower by 97.2%. The mineralization coefficient of Nitrogen compounds gradually decreased in the fallow ground and extensively used agrosoil, unlike the intensively managed agrosoil, in which the intensity of mineralization-immobilization of nitrogen compounds increased in the He and Hi layers. It was shown that the fallow ground had the more efficient system to transfer substrates and mineral ions down the profile to the lower layers. The difference in biologic activity between the upper and lower layers was maximum in the fallow ground, intermediate in the intensively used agrosoil and minimum in the extensive agrosoil. soil horizons index of pedotrophy nitrogen mineralization coefficient humus mineralization activity fallow ground agrosoil Biotechnology In Biotechnologia Acta National Academy of Sciences of Ukraine, Palladin Institute of Biochemistry, 2016 12(2019), 6, Seite 65-70 (DE-627)863737730 (DE-600)2863118-3 2410776X nnns volume:12 year:2019 number:6 pages:65-70 https://doi.org/10.15407/biotech12.06.065 kostenfrei https://doaj.org/article/047a07cfb8494b91b6af08d9fae074f7 kostenfrei http://biotechnology.kiev.ua/images/storage/6_2019/malinovska_6_2019.pdf kostenfrei https://doaj.org/toc/2410-7751 Journal toc kostenfrei https://doaj.org/toc/2410-776X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 12 2019 6 65-70
allfieldsSound	10.15407/biotech12.06.065 doi (DE-627)DOAJ018009212 (DE-599)DOAJ047a07cfb8494b91b6af08d9fae074f7 DE-627 ger DE-627 rakwb eng rus ukr TP248.13-248.65 Malynovska I. M. verfasserin aut IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The aim of the work was to study the direction and intensity of mineralization and immobilization processes in different layers of gray forest soil at fallow fields, extensively and intensively used agrosoils. The research included laboratory analysis, microbiological studies, and statistical processing. For the fallow plots, the layers chosen for study were Hd – turf (010 cm), He – humus-eluvial (11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (116156 cm), Pi – bedrock with occasional insertions of illuvial soil (157191 cm); for the agrosoils of the stationary experiments: He – humus-eluvial (0-10 and 11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (11656 cm). We found that humus mineralization differed in some layers of the gray forest soil under these management regimes. At fallows, the intensity of humus mineralization tended to decrease with depth, and it was interrupted in the Ih and Ip layers. In the intensively used agrosoil, humus mineralization was more active in Hi- and Ih- layers. Comparatively, the activity of humus mineralization smoothly decreased in the profile of the extensively used agrosoil from the uppermost layer to the lower by 97.2%. The mineralization coefficient of Nitrogen compounds gradually decreased in the fallow ground and extensively used agrosoil, unlike the intensively managed agrosoil, in which the intensity of mineralization-immobilization of nitrogen compounds increased in the He and Hi layers. It was shown that the fallow ground had the more efficient system to transfer substrates and mineral ions down the profile to the lower layers. The difference in biologic activity between the upper and lower layers was maximum in the fallow ground, intermediate in the intensively used agrosoil and minimum in the extensive agrosoil. soil horizons index of pedotrophy nitrogen mineralization coefficient humus mineralization activity fallow ground agrosoil Biotechnology In Biotechnologia Acta National Academy of Sciences of Ukraine, Palladin Institute of Biochemistry, 2016 12(2019), 6, Seite 65-70 (DE-627)863737730 (DE-600)2863118-3 2410776X nnns volume:12 year:2019 number:6 pages:65-70 https://doi.org/10.15407/biotech12.06.065 kostenfrei https://doaj.org/article/047a07cfb8494b91b6af08d9fae074f7 kostenfrei http://biotechnology.kiev.ua/images/storage/6_2019/malinovska_6_2019.pdf kostenfrei https://doaj.org/toc/2410-7751 Journal toc kostenfrei https://doaj.org/toc/2410-776X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 12 2019 6 65-70
language	English Russian Ukrainian
source	In Biotechnologia Acta 12(2019), 6, Seite 65-70 volume:12 year:2019 number:6 pages:65-70
sourceStr	In Biotechnologia Acta 12(2019), 6, Seite 65-70 volume:12 year:2019 number:6 pages:65-70
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	soil horizons index of pedotrophy nitrogen mineralization coefficient humus mineralization activity fallow ground agrosoil Biotechnology
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container_title	Biotechnologia Acta
authorswithroles_txt_mv	Malynovska I. M. @@aut@@
publishDateDaySort_date	2019-01-01T00:00:00Z
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callnumber-first	T - Technology
author	Malynovska I. M.
spellingShingle	Malynovska I. M. misc TP248.13-248.65 misc soil horizons misc index of pedotrophy misc nitrogen mineralization coefficient misc humus mineralization activity misc fallow ground misc agrosoil misc Biotechnology IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT
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topic_title	TP248.13-248.65 IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT soil horizons index of pedotrophy nitrogen mineralization coefficient humus mineralization activity fallow ground agrosoil
topic	misc TP248.13-248.65 misc soil horizons misc index of pedotrophy misc nitrogen mineralization coefficient misc humus mineralization activity misc fallow ground misc agrosoil misc Biotechnology
topic_unstemmed	misc TP248.13-248.65 misc soil horizons misc index of pedotrophy misc nitrogen mineralization coefficient misc humus mineralization activity misc fallow ground misc agrosoil misc Biotechnology
topic_browse	misc TP248.13-248.65 misc soil horizons misc index of pedotrophy misc nitrogen mineralization coefficient misc humus mineralization activity misc fallow ground misc agrosoil misc Biotechnology
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title	IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT
ctrlnum	(DE-627)DOAJ018009212 (DE-599)DOAJ047a07cfb8494b91b6af08d9fae074f7
title_full	IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT
author_sort	Malynovska I. M.
journal	Biotechnologia Acta
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author-letter	Malynovska I. M.
doi_str_mv	10.15407/biotech12.06.065
title_sort	irection and strength of microbiological processes in layers of gray forest soil under different regimes of management
callnumber	TP248.13-248.65
title_auth	IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT
abstract	The aim of the work was to study the direction and intensity of mineralization and immobilization processes in different layers of gray forest soil at fallow fields, extensively and intensively used agrosoils. The research included laboratory analysis, microbiological studies, and statistical processing. For the fallow plots, the layers chosen for study were Hd – turf (010 cm), He – humus-eluvial (11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (116156 cm), Pi – bedrock with occasional insertions of illuvial soil (157191 cm); for the agrosoils of the stationary experiments: He – humus-eluvial (0-10 and 11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (11656 cm). We found that humus mineralization differed in some layers of the gray forest soil under these management regimes. At fallows, the intensity of humus mineralization tended to decrease with depth, and it was interrupted in the Ih and Ip layers. In the intensively used agrosoil, humus mineralization was more active in Hi- and Ih- layers. Comparatively, the activity of humus mineralization smoothly decreased in the profile of the extensively used agrosoil from the uppermost layer to the lower by 97.2%. The mineralization coefficient of Nitrogen compounds gradually decreased in the fallow ground and extensively used agrosoil, unlike the intensively managed agrosoil, in which the intensity of mineralization-immobilization of nitrogen compounds increased in the He and Hi layers. It was shown that the fallow ground had the more efficient system to transfer substrates and mineral ions down the profile to the lower layers. The difference in biologic activity between the upper and lower layers was maximum in the fallow ground, intermediate in the intensively used agrosoil and minimum in the extensive agrosoil.
abstractGer	The aim of the work was to study the direction and intensity of mineralization and immobilization processes in different layers of gray forest soil at fallow fields, extensively and intensively used agrosoils. The research included laboratory analysis, microbiological studies, and statistical processing. For the fallow plots, the layers chosen for study were Hd – turf (010 cm), He – humus-eluvial (11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (116156 cm), Pi – bedrock with occasional insertions of illuvial soil (157191 cm); for the agrosoils of the stationary experiments: He – humus-eluvial (0-10 and 11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (11656 cm). We found that humus mineralization differed in some layers of the gray forest soil under these management regimes. At fallows, the intensity of humus mineralization tended to decrease with depth, and it was interrupted in the Ih and Ip layers. In the intensively used agrosoil, humus mineralization was more active in Hi- and Ih- layers. Comparatively, the activity of humus mineralization smoothly decreased in the profile of the extensively used agrosoil from the uppermost layer to the lower by 97.2%. The mineralization coefficient of Nitrogen compounds gradually decreased in the fallow ground and extensively used agrosoil, unlike the intensively managed agrosoil, in which the intensity of mineralization-immobilization of nitrogen compounds increased in the He and Hi layers. It was shown that the fallow ground had the more efficient system to transfer substrates and mineral ions down the profile to the lower layers. The difference in biologic activity between the upper and lower layers was maximum in the fallow ground, intermediate in the intensively used agrosoil and minimum in the extensive agrosoil.
abstract_unstemmed	The aim of the work was to study the direction and intensity of mineralization and immobilization processes in different layers of gray forest soil at fallow fields, extensively and intensively used agrosoils. The research included laboratory analysis, microbiological studies, and statistical processing. For the fallow plots, the layers chosen for study were Hd – turf (010 cm), He – humus-eluvial (11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (116156 cm), Pi – bedrock with occasional insertions of illuvial soil (157191 cm); for the agrosoils of the stationary experiments: He – humus-eluvial (0-10 and 11–40 cm), Hi – humus-illuvial (4174 cm), Ih – illuvial-humus (75115 cm), Ip – transitional from the illuvial layer to bedrock (11656 cm). We found that humus mineralization differed in some layers of the gray forest soil under these management regimes. At fallows, the intensity of humus mineralization tended to decrease with depth, and it was interrupted in the Ih and Ip layers. In the intensively used agrosoil, humus mineralization was more active in Hi- and Ih- layers. Comparatively, the activity of humus mineralization smoothly decreased in the profile of the extensively used agrosoil from the uppermost layer to the lower by 97.2%. The mineralization coefficient of Nitrogen compounds gradually decreased in the fallow ground and extensively used agrosoil, unlike the intensively managed agrosoil, in which the intensity of mineralization-immobilization of nitrogen compounds increased in the He and Hi layers. It was shown that the fallow ground had the more efficient system to transfer substrates and mineral ions down the profile to the lower layers. The difference in biologic activity between the upper and lower layers was maximum in the fallow ground, intermediate in the intensively used agrosoil and minimum in the extensive agrosoil.
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container_issue	6
title_short	IRECTION AND STRENGTH OF MICROBIOLOGICAL PROCESSES IN LAYERS OF GRAY FOREST SOIL UNDER DIFFERENT REGIMES OF MANAGEMENT
url	https://doi.org/10.15407/biotech12.06.065 https://doaj.org/article/047a07cfb8494b91b6af08d9fae074f7 http://biotechnology.kiev.ua/images/storage/6_2019/malinovska_6_2019.pdf https://doaj.org/toc/2410-7751 https://doaj.org/toc/2410-776X
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