Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia
Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Lishtvan, I. I. [verfasserIn] Orlov, A. S. [verfasserIn] Selyanina, S. B. [verfasserIn] Sokolova, T. V. [verfasserIn] Sosnovskaya, N. E. [verfasserIn] Trufanova, M. V. [verfasserIn] Yarygina, O. N. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2018 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Solid fuel chemistry - New York, NY : Allerton Press, 2007, 52(2018), 4 vom: Juli, Seite 211-216 |
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| Übergeordnetes Werk: |
volume:52 ; year:2018 ; number:4 ; month:07 ; pages:211-216 |
| Links: |
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| DOI / URN: |
10.3103/S0361521918040067 |
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| Katalog-ID: |
SPR023481439 |
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| 520 | |a Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the pronounced predominance of the fulvate type of humification was revealed. It was established that special climatic effects are a factor affecting the formation of the group chemical composition of peat. It was demonstrated that, under the conditions of northern territories with consideration for the frost zone of a peat deposit, the conditions of oxidation and the kinetics of humification processes in the organic matter of peat in top and bottom layers can be essentially different; this fact explained the nonmonotonic changes in the characteristics of peat with the depth of occurrence. The effect of the bituminous component on the humification process of organic matter in the course of peat deposition was found; this was primarily due to the inhibition of the formation of polyconjugated structures, which are the main structure factor of humic substances. | ||
| 650 | 4 | |a peat |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a peat marsh ecosystems |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a peat-forming plants |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a peat accumulation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a humus formation |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Orlov, A. S. |e verfasserin |4 aut | |
| 700 | 1 | |a Selyanina, S. B. |e verfasserin |4 aut | |
| 700 | 1 | |a Sokolova, T. V. |e verfasserin |4 aut | |
| 700 | 1 | |a Sosnovskaya, N. E. |e verfasserin |4 aut | |
| 700 | 1 | |a Trufanova, M. V. |e verfasserin |4 aut | |
| 700 | 1 | |a Yarygina, O. N. |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Solid fuel chemistry |d New York, NY : Allerton Press, 2007 |g 52(2018), 4 vom: Juli, Seite 211-216 |w (DE-627)530281953 |w (DE-600)2317138-8 |x 1934-8029 |7 nnns |
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10.3103/S0361521918040067 doi (DE-627)SPR023481439 (SPR)S0361521918040067-e DE-627 ger DE-627 rakwb eng 660 ASE Lishtvan, I. I. verfasserin aut Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the pronounced predominance of the fulvate type of humification was revealed. It was established that special climatic effects are a factor affecting the formation of the group chemical composition of peat. It was demonstrated that, under the conditions of northern territories with consideration for the frost zone of a peat deposit, the conditions of oxidation and the kinetics of humification processes in the organic matter of peat in top and bottom layers can be essentially different; this fact explained the nonmonotonic changes in the characteristics of peat with the depth of occurrence. The effect of the bituminous component on the humification process of organic matter in the course of peat deposition was found; this was primarily due to the inhibition of the formation of polyconjugated structures, which are the main structure factor of humic substances. peat (dpeaa)DE-He213 peat marsh ecosystems (dpeaa)DE-He213 peat-forming plants (dpeaa)DE-He213 peat accumulation (dpeaa)DE-He213 humus formation (dpeaa)DE-He213 Orlov, A. S. verfasserin aut Selyanina, S. B. verfasserin aut Sokolova, T. V. verfasserin aut Sosnovskaya, N. E. verfasserin aut Trufanova, M. V. verfasserin aut Yarygina, O. N. verfasserin aut Enthalten in Solid fuel chemistry New York, NY : Allerton Press, 2007 52(2018), 4 vom: Juli, Seite 211-216 (DE-627)530281953 (DE-600)2317138-8 1934-8029 nnns volume:52 year:2018 number:4 month:07 pages:211-216 https://dx.doi.org/10.3103/S0361521918040067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 52 2018 4 07 211-216 |
| spelling |
10.3103/S0361521918040067 doi (DE-627)SPR023481439 (SPR)S0361521918040067-e DE-627 ger DE-627 rakwb eng 660 ASE Lishtvan, I. I. verfasserin aut Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the pronounced predominance of the fulvate type of humification was revealed. It was established that special climatic effects are a factor affecting the formation of the group chemical composition of peat. It was demonstrated that, under the conditions of northern territories with consideration for the frost zone of a peat deposit, the conditions of oxidation and the kinetics of humification processes in the organic matter of peat in top and bottom layers can be essentially different; this fact explained the nonmonotonic changes in the characteristics of peat with the depth of occurrence. The effect of the bituminous component on the humification process of organic matter in the course of peat deposition was found; this was primarily due to the inhibition of the formation of polyconjugated structures, which are the main structure factor of humic substances. peat (dpeaa)DE-He213 peat marsh ecosystems (dpeaa)DE-He213 peat-forming plants (dpeaa)DE-He213 peat accumulation (dpeaa)DE-He213 humus formation (dpeaa)DE-He213 Orlov, A. S. verfasserin aut Selyanina, S. B. verfasserin aut Sokolova, T. V. verfasserin aut Sosnovskaya, N. E. verfasserin aut Trufanova, M. V. verfasserin aut Yarygina, O. N. verfasserin aut Enthalten in Solid fuel chemistry New York, NY : Allerton Press, 2007 52(2018), 4 vom: Juli, Seite 211-216 (DE-627)530281953 (DE-600)2317138-8 1934-8029 nnns volume:52 year:2018 number:4 month:07 pages:211-216 https://dx.doi.org/10.3103/S0361521918040067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 52 2018 4 07 211-216 |
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10.3103/S0361521918040067 doi (DE-627)SPR023481439 (SPR)S0361521918040067-e DE-627 ger DE-627 rakwb eng 660 ASE Lishtvan, I. I. verfasserin aut Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the pronounced predominance of the fulvate type of humification was revealed. It was established that special climatic effects are a factor affecting the formation of the group chemical composition of peat. It was demonstrated that, under the conditions of northern territories with consideration for the frost zone of a peat deposit, the conditions of oxidation and the kinetics of humification processes in the organic matter of peat in top and bottom layers can be essentially different; this fact explained the nonmonotonic changes in the characteristics of peat with the depth of occurrence. The effect of the bituminous component on the humification process of organic matter in the course of peat deposition was found; this was primarily due to the inhibition of the formation of polyconjugated structures, which are the main structure factor of humic substances. peat (dpeaa)DE-He213 peat marsh ecosystems (dpeaa)DE-He213 peat-forming plants (dpeaa)DE-He213 peat accumulation (dpeaa)DE-He213 humus formation (dpeaa)DE-He213 Orlov, A. S. verfasserin aut Selyanina, S. B. verfasserin aut Sokolova, T. V. verfasserin aut Sosnovskaya, N. E. verfasserin aut Trufanova, M. V. verfasserin aut Yarygina, O. N. verfasserin aut Enthalten in Solid fuel chemistry New York, NY : Allerton Press, 2007 52(2018), 4 vom: Juli, Seite 211-216 (DE-627)530281953 (DE-600)2317138-8 1934-8029 nnns volume:52 year:2018 number:4 month:07 pages:211-216 https://dx.doi.org/10.3103/S0361521918040067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 52 2018 4 07 211-216 |
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10.3103/S0361521918040067 doi (DE-627)SPR023481439 (SPR)S0361521918040067-e DE-627 ger DE-627 rakwb eng 660 ASE Lishtvan, I. I. verfasserin aut Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the pronounced predominance of the fulvate type of humification was revealed. It was established that special climatic effects are a factor affecting the formation of the group chemical composition of peat. It was demonstrated that, under the conditions of northern territories with consideration for the frost zone of a peat deposit, the conditions of oxidation and the kinetics of humification processes in the organic matter of peat in top and bottom layers can be essentially different; this fact explained the nonmonotonic changes in the characteristics of peat with the depth of occurrence. The effect of the bituminous component on the humification process of organic matter in the course of peat deposition was found; this was primarily due to the inhibition of the formation of polyconjugated structures, which are the main structure factor of humic substances. peat (dpeaa)DE-He213 peat marsh ecosystems (dpeaa)DE-He213 peat-forming plants (dpeaa)DE-He213 peat accumulation (dpeaa)DE-He213 humus formation (dpeaa)DE-He213 Orlov, A. S. verfasserin aut Selyanina, S. B. verfasserin aut Sokolova, T. V. verfasserin aut Sosnovskaya, N. E. verfasserin aut Trufanova, M. V. verfasserin aut Yarygina, O. N. verfasserin aut Enthalten in Solid fuel chemistry New York, NY : Allerton Press, 2007 52(2018), 4 vom: Juli, Seite 211-216 (DE-627)530281953 (DE-600)2317138-8 1934-8029 nnns volume:52 year:2018 number:4 month:07 pages:211-216 https://dx.doi.org/10.3103/S0361521918040067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 52 2018 4 07 211-216 |
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10.3103/S0361521918040067 doi (DE-627)SPR023481439 (SPR)S0361521918040067-e DE-627 ger DE-627 rakwb eng 660 ASE Lishtvan, I. I. verfasserin aut Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the pronounced predominance of the fulvate type of humification was revealed. It was established that special climatic effects are a factor affecting the formation of the group chemical composition of peat. It was demonstrated that, under the conditions of northern territories with consideration for the frost zone of a peat deposit, the conditions of oxidation and the kinetics of humification processes in the organic matter of peat in top and bottom layers can be essentially different; this fact explained the nonmonotonic changes in the characteristics of peat with the depth of occurrence. The effect of the bituminous component on the humification process of organic matter in the course of peat deposition was found; this was primarily due to the inhibition of the formation of polyconjugated structures, which are the main structure factor of humic substances. peat (dpeaa)DE-He213 peat marsh ecosystems (dpeaa)DE-He213 peat-forming plants (dpeaa)DE-He213 peat accumulation (dpeaa)DE-He213 humus formation (dpeaa)DE-He213 Orlov, A. S. verfasserin aut Selyanina, S. B. verfasserin aut Sokolova, T. V. verfasserin aut Sosnovskaya, N. E. verfasserin aut Trufanova, M. V. verfasserin aut Yarygina, O. N. verfasserin aut Enthalten in Solid fuel chemistry New York, NY : Allerton Press, 2007 52(2018), 4 vom: Juli, Seite 211-216 (DE-627)530281953 (DE-600)2317138-8 1934-8029 nnns volume:52 year:2018 number:4 month:07 pages:211-216 https://dx.doi.org/10.3103/S0361521918040067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 52 2018 4 07 211-216 |
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Enthalten in Solid fuel chemistry 52(2018), 4 vom: Juli, Seite 211-216 volume:52 year:2018 number:4 month:07 pages:211-216 |
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Enthalten in Solid fuel chemistry 52(2018), 4 vom: Juli, Seite 211-216 volume:52 year:2018 number:4 month:07 pages:211-216 |
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Solid fuel chemistry |
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Lishtvan, I. I. @@aut@@ Orlov, A. S. @@aut@@ Selyanina, S. B. @@aut@@ Sokolova, T. V. @@aut@@ Sosnovskaya, N. E. @@aut@@ Trufanova, M. V. @@aut@@ Yarygina, O. N. @@aut@@ |
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| author |
Lishtvan, I. I. |
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Lishtvan, I. I. ddc 660 misc peat misc peat marsh ecosystems misc peat-forming plants misc peat accumulation misc humus formation Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia |
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660 ASE Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia peat (dpeaa)DE-He213 peat marsh ecosystems (dpeaa)DE-He213 peat-forming plants (dpeaa)DE-He213 peat accumulation (dpeaa)DE-He213 humus formation (dpeaa)DE-He213 |
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ddc 660 misc peat misc peat marsh ecosystems misc peat-forming plants misc peat accumulation misc humus formation |
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ddc 660 misc peat misc peat marsh ecosystems misc peat-forming plants misc peat accumulation misc humus formation |
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Solid fuel chemistry |
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Solid fuel chemistry |
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Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia |
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Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia |
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Lishtvan, I. I. |
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Solid fuel chemistry |
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Lishtvan, I. I. Orlov, A. S. Selyanina, S. B. Sokolova, T. V. Sosnovskaya, N. E. Trufanova, M. V. Yarygina, O. N. |
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verfasserin |
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formation of the organic matter of high-moor peat under conditions of the european north of russia |
| title_auth |
Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia |
| abstract |
Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the pronounced predominance of the fulvate type of humification was revealed. It was established that special climatic effects are a factor affecting the formation of the group chemical composition of peat. It was demonstrated that, under the conditions of northern territories with consideration for the frost zone of a peat deposit, the conditions of oxidation and the kinetics of humification processes in the organic matter of peat in top and bottom layers can be essentially different; this fact explained the nonmonotonic changes in the characteristics of peat with the depth of occurrence. The effect of the bituminous component on the humification process of organic matter in the course of peat deposition was found; this was primarily due to the inhibition of the formation of polyconjugated structures, which are the main structure factor of humic substances. |
| abstractGer |
Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the pronounced predominance of the fulvate type of humification was revealed. It was established that special climatic effects are a factor affecting the formation of the group chemical composition of peat. It was demonstrated that, under the conditions of northern territories with consideration for the frost zone of a peat deposit, the conditions of oxidation and the kinetics of humification processes in the organic matter of peat in top and bottom layers can be essentially different; this fact explained the nonmonotonic changes in the characteristics of peat with the depth of occurrence. The effect of the bituminous component on the humification process of organic matter in the course of peat deposition was found; this was primarily due to the inhibition of the formation of polyconjugated structures, which are the main structure factor of humic substances. |
| abstract_unstemmed |
Abstract The key role of oxidation processes in the humification of peat-forming plant components was experimentally confirmed. A number of characteristic properties of the transformation of organic matter under conditions of the North, in particular, a decrease in the depth of humification and the pronounced predominance of the fulvate type of humification was revealed. It was established that special climatic effects are a factor affecting the formation of the group chemical composition of peat. It was demonstrated that, under the conditions of northern territories with consideration for the frost zone of a peat deposit, the conditions of oxidation and the kinetics of humification processes in the organic matter of peat in top and bottom layers can be essentially different; this fact explained the nonmonotonic changes in the characteristics of peat with the depth of occurrence. The effect of the bituminous component on the humification process of organic matter in the course of peat deposition was found; this was primarily due to the inhibition of the formation of polyconjugated structures, which are the main structure factor of humic substances. |
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Formation of the Organic Matter of High-Moor Peat under Conditions of the European North of Russia |
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https://dx.doi.org/10.3103/S0361521918040067 |
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Orlov, A. S. Selyanina, S. B. Sokolova, T. V. Sosnovskaya, N. E. Trufanova, M. V. Yarygina, O. N. |
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Orlov, A. S. Selyanina, S. B. Sokolova, T. V. Sosnovskaya, N. E. Trufanova, M. V. Yarygina, O. N. |
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10.3103/S0361521918040067 |
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2024-07-03T19:12:17.699Z |
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| score |
7.3992643 |