The pool of pedogenic carbon in the soils of different types and durations of use as croplands in the forest-steppe of the Central Russian Upland
Based on studying five agrochronoseries, including recent forest (dark) gray soils and soils plowed for 100, 150, and 200–240 and more years in the forest-steppe zone of the Central Russian Upland, the dynamics of the pedogenic carbon pool, including the C org and C carb , are considered. In the 2-m...
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| Published in | Eurasian soil science Vol. 46; no. 5; pp. 530 - 540 |
|---|---|
| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
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Dordrecht
SP MAIK Nauka/Interperiodica
01.05.2013
Springer Springer Nature B.V |
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| Abstract | Based on studying five agrochronoseries, including recent forest (dark) gray soils and soils plowed for 100, 150, and 200–240 and more years in the forest-steppe zone of the Central Russian Upland, the dynamics of the pedogenic carbon pool, including the C
org
and C
carb
, are considered. In the 2-m-thick layer of the agrogenic soils studied, the pedogenic carbon pool was shown to increase by 15–30% (up to 50%) mainly due to the changes in the C
carb
content. The insignificant (by ∼10%) growth of the C
org
content was found in the soils that were plowed for more than 200–250 years. As the hydrothermal regime changed when passing from the forest to croplands, the C
carb
reserves increased due to the ascending of carbonates from the parent rock through the capillary pores, probably, in colloid solution-suspensions. This process proceeded without exchange with the soil CO
2
, since the
14
C age and the content of the newly formed carbonates became higher. These carbonates may be called pedogenic-lithogenic agrocarbonates, since they appear in soils as a result of the (agro-) pedogenesis. In this case, their additional source is the lithogenic carbonates, which bring in the “old” carbon. The process of carbonates ascending could be referred to the rapid soil-forming ones with their implementation time being close to ≤50 years. |
|---|---|
| AbstractList | Based on studying five agrochronoseries, including recent forest (dark) gray soils and soils plowed for 100, 150, and 200–240 and more years in the forest-steppe zone of the Central Russian Upland, the dynamics of the pedogenic carbon pool, including the C
org
and C
carb
, are considered. In the 2-m-thick layer of the agrogenic soils studied, the pedogenic carbon pool was shown to increase by 15–30% (up to 50%) mainly due to the changes in the C
carb
content. The insignificant (by ∼10%) growth of the C
org
content was found in the soils that were plowed for more than 200–250 years. As the hydrothermal regime changed when passing from the forest to croplands, the C
carb
reserves increased due to the ascending of carbonates from the parent rock through the capillary pores, probably, in colloid solution-suspensions. This process proceeded without exchange with the soil CO
2
, since the
14
C age and the content of the newly formed carbonates became higher. These carbonates may be called pedogenic-lithogenic agrocarbonates, since they appear in soils as a result of the (agro-) pedogenesis. In this case, their additional source is the lithogenic carbonates, which bring in the “old” carbon. The process of carbonates ascending could be referred to the rapid soil-forming ones with their implementation time being close to ≤50 years. Based on studying five agrochronoseries, including recent forest (dark) gray soils and soils plowed for 100, 150, and 200--240 and more years in the forest-steppe zone of the Central Russian Upland, the dynamics of the pedogenic carbon pool, including the [C.sub.org] and [C.sub.carb], are considered. In the 2-m-thick layer of the agrogenic soils studied, the pedogenic carbon pool was shown to increase by 15--30% (up to 50%) mainly due to the changes in the [C.sub.carb] content. The insignificant (by ~10%) growth of the [C.sub.org] content was found in the soils that were plowed for more than 200--250 years. As the hydrothermal regime changed when passing from the forest to croplands, the [C.sub.carb] reserves increased due to the ascending of carbonates from the parent rock through the capillary pores, probably, in colloid solution--suspensions. This process proceeded without exchange with the soil C[O.sub.2], since the [sup.14]C age and the content of the newly formed carbonates became higher. These carbonates may be called pedogenic--lithogenic agrocarbonates, since they appear in soils as a result of the (agro-) pedogenesis. In this case, their additional source is the lithogenic carbonates, which bring in the "old" carbon. The process of carbonates ascending could be referred to the rapid soil-forming ones with their implementation time being close to [less than or equal to]50 years. Keywords: pedogenic carbon, carbonate pool, agrochronoseries, Central Russian forest-steppe, [sup.14]C dating DOI: 10.1134/S1064229313050062 Based on studying five agrochronoseries, including recent forest (dark) gray soils and soils plowed for 100, 150, and 200-240 and more years in the forest-steppe zone of the Central Russian Upland, the dynamics of the pedogenic carbon pool, including the C sub(org) and C sub(carb), are considered. In the 2-m-thick layer of the agrogenic soils studied, the pedogenic carbon pool was shown to increase by 15-30% (up to 50%) mainly due to the changes in the C sub(carb) content. The insignificant (by 10%) growth of the C sub(org) content was found in the soils that were plowed for more than 200-250 years. As the hydrothermal regime changed when passing from the forest to croplands, the C sub(carb) reserves increased due to the ascending of carbonates from the parent rock through the capillary pores, probably, in colloid solution-suspensions. This process proceeded without exchange with the soil CO sub(2), since the super(14)C age and the content of the newly formed carbonates became higher. These carbonates may be called pedogenic-lithogenic agrocarbonates, since they appear in soils as a result of the (agro-) pedogenesis. In this case, their additional source is the lithogenic carbonates, which bring in the "old" carbon. The process of carbonates ascending could be referred to the rapid soil-forming ones with their implementation time being close to less than or equal to 50 years. Based on studying five agrochronoseries, including recent forest (dark) gray soils and soils plowed for 100, 150, and 200-240 and more years in the forest-steppe zone of the Central Russian Upland, the dynamics of the pedogenic carbon pool, including the C^sub org^ and C^sub carb^, are considered. In the 2-m-thick layer of the agrogenic soils studied, the pedogenic carbon pool was shown to increase by 15-30% (up to 50%) mainly due to the changes in the C^sub carb^ content. The insignificant (by 10%) growth of the C^sub org^ content was found in the soils that were plowed for more than 200-250 years. As the hydrothermal regime changed when passing from the forest to croplands, the C^sub carb^ reserves increased due to the ascending of carbonates from the parent rock through the capillary pores, probably, in colloid solution-suspensions. This process proceeded without exchange with the soil CO2, since the ^sup 14^C age and the content of the newly formed carbonates became higher. These carbonates may be called pedogenic-lithogenic agrocarbonates, since they appear in soils as a result of the (agro-) pedogenesis. In this case, their additional source is the lithogenic carbonates, which bring in the "old" carbon. The process of carbonates ascending could be referred to the rapid soil-forming ones with their implementation time being close to <=50 years.[PUBLICATION ABSTRACT] Based on studying five agrochronoseries, including recent forest (dark) gray soils and soils plowed for 100, 150, and 200–240 and more years in the forest-steppe zone of the Central Russian Upland, the dynamics of the pedogenic carbon pool, including the Cₒᵣg and Ccₐᵣb, are considered. In the 2-m-thick layer of the agrogenic soils studied, the pedogenic carbon pool was shown to increase by 15–30% (up to 50%) mainly due to the changes in the Ccₐᵣb content. The insignificant (by ∼10%) growth of the Cₒᵣg content was found in the soils that were plowed for more than 200–250 years. As the hydrothermal regime changed when passing from the forest to croplands, the Ccₐᵣb reserves increased due to the ascending of carbonates from the parent rock through the capillary pores, probably, in colloid solution-suspensions. This process proceeded without exchange with the soil CO₂, since the ¹⁴C age and the content of the newly formed carbonates became higher. These carbonates may be called pedogenic-lithogenic agrocarbonates, since they appear in soils as a result of the (agro-) pedogenesis. In this case, their additional source is the lithogenic carbonates, which bring in the “old” carbon. The process of carbonates ascending could be referred to the rapid soil-forming ones with their implementation time being close to ≤50 years. |
| Audience | Academic |
| Author | Shishkov, V. A. Chendev, Yu. G. Myakshina, T. N. Khokhlova, O. S. |
| Author_xml | – sequence: 1 givenname: O. S. surname: Khokhlova fullname: Khokhlova, O. S. email: akhokhlov@mail.ru organization: Institute of Physicochemical and Biological Problems of Soil Science, Russian Academy of Sciences – sequence: 2 givenname: Yu. G. surname: Chendev fullname: Chendev, Yu. G. organization: Belgorod State University – sequence: 3 givenname: T. N. surname: Myakshina fullname: Myakshina, T. N. organization: Institute of Physicochemical and Biological Problems of Soil Science, Russian Academy of Sciences – sequence: 4 givenname: V. A. surname: Shishkov fullname: Shishkov, V. A. organization: Institute of Geography, Russian Academy of Sciences |
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| Cites_doi | 10.1134/S1064229312060063 10.1134/S1064229310130119 10.1134/S1064229311010030 10.1134/S1064229308090032 |
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| References | O. S. Khokhlova, A. V. Rusakov, A. M. Kuznetsova, T. N. Myakshina, and Yu. G. Chendev, “Radiocarbon dating of pedogenic carbonates in the deep horizons of forest-steppe soils,” Eur. Soil Sci. 46. ArinushkinaE VManual on the Chemical Analysis of Soils1970MoscowIzd. Mosk. Gos. Univ. StulinA FThe impact of the long-term fertilization in a continuous corn crop on the yields and nutrient removal with harvested corn from a leached chernozemAgrokhimiya, No. 120072530 ChendevYu GThe Holocene Evolution of Forest-Steppe Soils on the Central Russian Upland2008MoscowGEOS ChendevYu GAleksandrovskiiA LKhokhlovaO SSmirnovaL GNovykhL LDolgikhA VAnthropogenic evolution of dark gray forest-steppe soils in the southern part of the Central Russian UplandEur. Soil Sci.201144111210.1134/S1064229311010030 IonkoO AMel’nikovaM GThe impact of shelterbelts on the carbonate regime of soils in the Kamennaya SteppeChernozems of Russia: Ecological State and Modern Soil Processes2006VoronezhIzd. Voronezhsk. Gos. Univ.8487 KhokhlovaO SKhokhlovA AChichagovaO AKuznetsovaA MOleinikS ATransformation of carbonate pedofeatures in paleosols buried under kurgans in the North Caucasus regionEur. Soil Sci.200841992393610.1134/S1064229308090032 GlazovskayaM APedolithogenesis and Continental Carbon Cycles2009MoscowKnizhn. dom “Limbrokom,” KhokhlovaO SExtended abstract of doctoral dissertation in geography2008 LarionovaA AStulinA FZaninaO GEvdokimovI VKhokhlovaO SByuggerFShloterMKudeyarovV NSavchenkoN ADistribution of stable carbon isotopes in an agrochernozem during the transition from C3 vegetation to a corn monocultureEur. Soil Sci.201245876877810.1134/S1064229312060063 KuznetsovaA MKhokhlovaO SChendevYu GAleksandrovskiiA LEvolution of the carbonate state of agrogenically transformed dark gray forest soils in the central forest-steppeEur. Soil Sci.201043131527153410.1134/S1064229310130119 A M Kuznetsova (9685_CR11) 2010; 43 O S Khokhlova (9685_CR7) 2008; 41 Yu G Chendev (9685_CR10) 2011; 44 M A Glazovskaya (9685_CR2) 2009 Yu G Chendev (9685_CR9) 2008 A A Larionova (9685_CR4) 2012; 45 A F Stulin (9685_CR5) 2007 O S Khokhlova (9685_CR6) 2008 9685_CR8 E V Arinushkina (9685_CR1) 1970 O A Ionko (9685_CR3) 2006 |
| References_xml | – reference: LarionovaA AStulinA FZaninaO GEvdokimovI VKhokhlovaO SByuggerFShloterMKudeyarovV NSavchenkoN ADistribution of stable carbon isotopes in an agrochernozem during the transition from C3 vegetation to a corn monocultureEur. Soil Sci.201245876877810.1134/S1064229312060063 – reference: StulinA FThe impact of the long-term fertilization in a continuous corn crop on the yields and nutrient removal with harvested corn from a leached chernozemAgrokhimiya, No. 120072530 – reference: GlazovskayaM APedolithogenesis and Continental Carbon Cycles2009MoscowKnizhn. dom “Limbrokom,” – reference: KhokhlovaO SExtended abstract of doctoral dissertation in geography2008 – reference: ChendevYu GThe Holocene Evolution of Forest-Steppe Soils on the Central Russian Upland2008MoscowGEOS – reference: ChendevYu GAleksandrovskiiA LKhokhlovaO SSmirnovaL GNovykhL LDolgikhA VAnthropogenic evolution of dark gray forest-steppe soils in the southern part of the Central Russian UplandEur. Soil Sci.201144111210.1134/S1064229311010030 – reference: KhokhlovaO SKhokhlovA AChichagovaO AKuznetsovaA MOleinikS ATransformation of carbonate pedofeatures in paleosols buried under kurgans in the North Caucasus regionEur. Soil Sci.200841992393610.1134/S1064229308090032 – reference: IonkoO AMel’nikovaM GThe impact of shelterbelts on the carbonate regime of soils in the Kamennaya SteppeChernozems of Russia: Ecological State and Modern Soil Processes2006VoronezhIzd. Voronezhsk. Gos. Univ.8487 – reference: KuznetsovaA MKhokhlovaO SChendevYu GAleksandrovskiiA LEvolution of the carbonate state of agrogenically transformed dark gray forest soils in the central forest-steppeEur. Soil Sci.201043131527153410.1134/S1064229310130119 – reference: ArinushkinaE VManual on the Chemical Analysis of Soils1970MoscowIzd. Mosk. Gos. Univ. – reference: O. S. Khokhlova, A. V. Rusakov, A. M. Kuznetsova, T. N. Myakshina, and Yu. G. Chendev, “Radiocarbon dating of pedogenic carbonates in the deep horizons of forest-steppe soils,” Eur. Soil Sci. 46. – volume-title: Manual on the Chemical Analysis of Soils year: 1970 ident: 9685_CR1 – volume: 45 start-page: 768 issue: 8 year: 2012 ident: 9685_CR4 publication-title: Eur. Soil Sci. doi: 10.1134/S1064229312060063 – volume: 43 start-page: 1527 issue: 13 year: 2010 ident: 9685_CR11 publication-title: Eur. Soil Sci. doi: 10.1134/S1064229310130119 – ident: 9685_CR8 – volume: 44 start-page: 1 issue: 1 year: 2011 ident: 9685_CR10 publication-title: Eur. Soil Sci. doi: 10.1134/S1064229311010030 – start-page: 84 volume-title: Chernozems of Russia: Ecological State and Modern Soil Processes year: 2006 ident: 9685_CR3 – volume-title: Extended abstract of doctoral dissertation in geography year: 2008 ident: 9685_CR6 – volume: 41 start-page: 923 issue: 9 year: 2008 ident: 9685_CR7 publication-title: Eur. Soil Sci. doi: 10.1134/S1064229308090032 – volume-title: Pedolithogenesis and Continental Carbon Cycles year: 2009 ident: 9685_CR2 – start-page: 25 volume-title: Agrokhimiya, No. 1 year: 2007 ident: 9685_CR5 – volume-title: The Holocene Evolution of Forest-Steppe Soils on the Central Russian Upland year: 2008 ident: 9685_CR9 |
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| SubjectTerms | Agricultural land Carbon Carbon content Carbon dating Carbon dioxide carbon sinks Carbonates Earth and Environmental Science Earth Sciences Forest soils Forests Geotechnical Engineering & Applied Earth Sciences Grasslands plowing soil Soil Chemistry Soil formation Soil sciences Soils Steppes |
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| Title | The pool of pedogenic carbon in the soils of different types and durations of use as croplands in the forest-steppe of the Central Russian Upland |
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