The rates of organic matter renewal in gray forest soils and chernozems
The rates of soil carbon renewal were determined by the method of natural 13 C abundance in a chernozem under a 40-year-long monoculture of corn and in a gray forest soil after application of corn residues. The mean rate of soil carbon renewal in the chernozem reached 1271–1498 years, whereas in the...
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| Veröffentlicht in: | Eurasian soil science 2008-12, Vol.41 (13), p.1378-1386 |
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| container_title | Eurasian soil science |
| container_volume | 41 |
| creator | Larionova, A. A. Zolotareva, B. N. Yevdokimov, I. V. Sapronov, D. V. Kuzyakov, Ya. V. Buegger, F. |
| description | The rates of soil carbon renewal were determined by the method of natural
13
C abundance in a chernozem under a 40-year-long monoculture of corn and in a gray forest soil after application of corn residues. The mean rate of soil carbon renewal in the chernozem reached 1271–1498 years, whereas in the gray forest soil it depended on the amount of carbon introduced with corn residues and varied from 19 to 63 years. The rate of organic carbon renewal in the chernozem decreased from 697 years in the upper horizon to 2742 years in the layer of 40–60 cm. The mean residence time of organic carbon generally increased with a decrease in the size of particle-size fractions. |
| doi_str_mv | 10.1134/S106422930813005X |
| format | Article |
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C abundance in a chernozem under a 40-year-long monoculture of corn and in a gray forest soil after application of corn residues. The mean rate of soil carbon renewal in the chernozem reached 1271–1498 years, whereas in the gray forest soil it depended on the amount of carbon introduced with corn residues and varied from 19 to 63 years. The rate of organic carbon renewal in the chernozem decreased from 697 years in the upper horizon to 2742 years in the layer of 40–60 cm. The mean residence time of organic carbon generally increased with a decrease in the size of particle-size fractions.</description><identifier>ISSN: 1064-2293</identifier><identifier>EISSN: 1556-195X</identifier><identifier>DOI: 10.1134/S106422930813005X</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Carbon ; Carbon content ; Corn ; Earth and Environmental Science ; Earth Sciences ; Forest soils ; Geochemistry ; Geotechnical Engineering & Applied Earth Sciences ; Monoculture ; Organic carbon ; Organic matter ; Soil Chemistry ; Soils ; Terrestrial ecosystems</subject><ispartof>Eurasian soil science, 2008-12, Vol.41 (13), p.1378-1386</ispartof><rights>Pleiades Publishing, Ltd. 2008</rights><rights>COPYRIGHT 2008 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c354t-9f983289712057d040606c686f621788beda9dd659ae74dc94025f49ddd217583</citedby><cites>FETCH-LOGICAL-c354t-9f983289712057d040606c686f621788beda9dd659ae74dc94025f49ddd217583</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S106422930813005X$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S106422930813005X$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Larionova, A. A.</creatorcontrib><creatorcontrib>Zolotareva, B. N.</creatorcontrib><creatorcontrib>Yevdokimov, I. V.</creatorcontrib><creatorcontrib>Sapronov, D. V.</creatorcontrib><creatorcontrib>Kuzyakov, Ya. V.</creatorcontrib><creatorcontrib>Buegger, F.</creatorcontrib><title>The rates of organic matter renewal in gray forest soils and chernozems</title><title>Eurasian soil science</title><addtitle>Eurasian Soil Sc</addtitle><description>The rates of soil carbon renewal were determined by the method of natural
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C abundance in a chernozem under a 40-year-long monoculture of corn and in a gray forest soil after application of corn residues. The mean rate of soil carbon renewal in the chernozem reached 1271–1498 years, whereas in the gray forest soil it depended on the amount of carbon introduced with corn residues and varied from 19 to 63 years. The rate of organic carbon renewal in the chernozem decreased from 697 years in the upper horizon to 2742 years in the layer of 40–60 cm. 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C abundance in a chernozem under a 40-year-long monoculture of corn and in a gray forest soil after application of corn residues. The mean rate of soil carbon renewal in the chernozem reached 1271–1498 years, whereas in the gray forest soil it depended on the amount of carbon introduced with corn residues and varied from 19 to 63 years. The rate of organic carbon renewal in the chernozem decreased from 697 years in the upper horizon to 2742 years in the layer of 40–60 cm. The mean residence time of organic carbon generally increased with a decrease in the size of particle-size fractions.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S106422930813005X</doi><tpages>9</tpages></addata></record> |
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| source | SpringerNature Journals |
| subjects | Carbon Carbon content Corn Earth and Environmental Science Earth Sciences Forest soils Geochemistry Geotechnical Engineering & Applied Earth Sciences Monoculture Organic carbon Organic matter Soil Chemistry Soils Terrestrial ecosystems |
| title | The rates of organic matter renewal in gray forest soils and chernozems |
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