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| 10. |  | SANTOS, P. L. dos; MARTINS, J. S.; VALENTE, M. A.; OLIVEIRA JUNIOR, R. C. de. Capacidade de troca de cations da fração argila em Latossolo amarelo de textura média e muito argilosa. In: CONGRESSO LATINO AMERICANO DE CIÊNCIA DO SOLO, 13.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 1.; SIMPÓSIO BRASILEIRO SOBRE MICROBIOLOGIA DO SOLO, 4.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 6.; REUNIÃO BRASILEIRA DE MANEJO E CONSERVAÇÃO DO SOLO E DA ÁGUA, 11., 1996, Aguas de Lindoia. Solo suelo 96. Aguas de Lindoia: SBCS/SLCS, 1996. 1 CD-ROM.| Biblioteca(s): Embrapa Amazônia Oriental; Embrapa Solos. |
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| 20. | | SANTOS, P. L. dos; OLIVEIRA JUNIOR, R. C. de; RODRIGUES, T. E. Mapa de reconhecimento dos solos do Planalto de Santarém, Estado do Pará. [Belém, PA]: Embrapa Amazônia Oriental, 2002. 1 mapa color. Escala 1:200.000. Parte de: RODRIGUES, T. E.; SANTOS, P. L. dos; OLIVEIRA JUNIOR, R. C. de; VALENTE, M. A.; SILVA, J. M. L. da; CARDOSO JÚNIOR, E. Q. Caracterização dos solos da área do planalto de Belterra, município de Santarém, Estado do Pará. Belém,...| Biblioteca(s): Embrapa Amazônia Oriental. |
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Registro Completo
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Biblioteca(s): |
Embrapa Meio-Norte. |
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Data corrente: |
02/07/2020 |
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Data da última atualização: |
10/12/2020 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 2 |
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Autoria: |
RITTL, T. F.; CANISARES, L.; SAGRILO, E.; BAHL, K. B.; DANNENMANN, M.; CERRI, C. E. P. |
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Afiliação: |
Tatiana F. Rittl, USP-ESALQ, Piracicaba, SP.; Luiza Canisares, USP-ESALQ, Piracicaba, SP.; EDVALDO SAGRILO, CPAMN; Klaus Butterbach Bahl, Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research, Atmospheric Environmental Research (IMK-IFU), Garmisch-Parten-kirchen 82467 (Germany); Michael Dannenmann, Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research, Atmospheric Environmental Research (IMK-IFU), Garmisch-Parten-kirchen 82467 (Germany); Carlos E. P. Cerri, USP-ESALQ, Piracicaba, SP. |
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Título: |
Temperature sensitivity of soil organic matter decomposition varies with biocharapplication and soil type. |
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Ano de publicação: |
2020 |
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Fonte/Imprenta: |
Pedosphere, v. 30, n. 3, p. 336-342, 2020. |
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ISSN: |
1002-0160 |
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DOI: |
10.1016/S1002-0160(20)60013-3 |
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Idioma: |
Inglês |
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Conteúdo: |
Biochar application has the potential to improve soil fertility and increase soil carbon stock, especially in tropical regions. Information on the temperaturesensitivity of carbon dioxide (CO2) evolution from biochar-amended soils at very high temperatures, as observed for tropical surface soils, is limited buturgently needed for the development of region-specific biochar management targeted to optimize biochar effects on soil functions. Here, we investigated thetemperature sensitivity of soil respiration to the addition of different rates ofMiscanthusbiochar (0, 6.25, 12.5, and 25 Mg ha−1) in two types of soils withcontrasting textures. Biochar-amended soil treatments and their controls were incubated at constant temperatures of 20, 30, and 40◦C. Overall, our resultsshow that: i) considering data from all treatments and temperatures, the addition of biochar decreased soil CO2emissions when compared to untreated soils;ii) CO2emissions from biochar-amended soils had a higher temperature sensitivity than those from biochar-free soils; iii) the temperature sensitivity of soilrespiration in sandy soils was higher than that in clay soils; and iv) for clay soils, relative increases in soil CO2emissions from biochar-amended soils werehigher when the temperature increased from 30 to 40◦C, while for sandy soils, the highest temperature responses of soil respiration were observed whenincreasing the temperature from 20 to 30◦C. Together, these findings suggest a significantly reduced potential to increase soil organic carbon stocks whenMiscanthusbiochar is applied to tropical soils at high surface temperatures, which could be counteracted by the soil- and weather-specific timing of biocharapplication. MenosBiochar application has the potential to improve soil fertility and increase soil carbon stock, especially in tropical regions. Information on the temperaturesensitivity of carbon dioxide (CO2) evolution from biochar-amended soils at very high temperatures, as observed for tropical surface soils, is limited buturgently needed for the development of region-specific biochar management targeted to optimize biochar effects on soil functions. Here, we investigated thetemperature sensitivity of soil respiration to the addition of different rates ofMiscanthusbiochar (0, 6.25, 12.5, and 25 Mg ha−1) in two types of soils withcontrasting textures. Biochar-amended soil treatments and their controls were incubated at constant temperatures of 20, 30, and 40◦C. Overall, our resultsshow that: i) considering data from all treatments and temperatures, the addition of biochar decreased soil CO2emissions when compared to untreated soils;ii) CO2emissions from biochar-amended soils had a higher temperature sensitivity than those from biochar-free soils; iii) the temperature sensitivity of soilrespiration in sandy soils was higher than that in clay soils; and iv) for clay soils, relative increases in soil CO2emissions from biochar-amended soils werehigher when the temperature increased from 30 to 40◦C, while for sandy soils, the highest temperature responses of soil respiration were observed whenincreasing the temperature from 20 to 30◦C. Together, these findings suggest a... Mostrar Tudo |
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Thesagro: |
Dióxido de Carbono; Efeito Estufa; Solo Arenoso; Solo Argiloso; Solo Tropical. |
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Thesaurus NAL: |
Carbon dioxide; Clay soils; Greenhouse gas emissions; Miscanthus; Sandy soils; Tropical soils. |
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Categoria do assunto: |
X Pesquisa, Tecnologia e Engenharia |
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Marc: |
LEADER 02703naa a2200337 a 4500
001 2123590
005 2020-12-10
008 2020 bl uuuu u00u1 u #d
022 $a1002-0160
024 7 $a10.1016/S1002-0160(20)60013-3$2DOI
100 1 $aRITTL, T. F.
245 $aTemperature sensitivity of soil organic matter decomposition varies with biocharapplication and soil type.$h[electronic resource]
260 $c2020
520 $aBiochar application has the potential to improve soil fertility and increase soil carbon stock, especially in tropical regions. Information on the temperaturesensitivity of carbon dioxide (CO2) evolution from biochar-amended soils at very high temperatures, as observed for tropical surface soils, is limited buturgently needed for the development of region-specific biochar management targeted to optimize biochar effects on soil functions. Here, we investigated thetemperature sensitivity of soil respiration to the addition of different rates ofMiscanthusbiochar (0, 6.25, 12.5, and 25 Mg ha−1) in two types of soils withcontrasting textures. Biochar-amended soil treatments and their controls were incubated at constant temperatures of 20, 30, and 40◦C. Overall, our resultsshow that: i) considering data from all treatments and temperatures, the addition of biochar decreased soil CO2emissions when compared to untreated soils;ii) CO2emissions from biochar-amended soils had a higher temperature sensitivity than those from biochar-free soils; iii) the temperature sensitivity of soilrespiration in sandy soils was higher than that in clay soils; and iv) for clay soils, relative increases in soil CO2emissions from biochar-amended soils werehigher when the temperature increased from 30 to 40◦C, while for sandy soils, the highest temperature responses of soil respiration were observed whenincreasing the temperature from 20 to 30◦C. Together, these findings suggest a significantly reduced potential to increase soil organic carbon stocks whenMiscanthusbiochar is applied to tropical soils at high surface temperatures, which could be counteracted by the soil- and weather-specific timing of biocharapplication.
650 $aCarbon dioxide
650 $aClay soils
650 $aGreenhouse gas emissions
650 $aMiscanthus
650 $aSandy soils
650 $aTropical soils
650 $aDióxido de Carbono
650 $aEfeito Estufa
650 $aSolo Arenoso
650 $aSolo Argiloso
650 $aSolo Tropical
700 1 $aCANISARES, L.
700 1 $aSAGRILO, E.
700 1 $aBAHL, K. B.
700 1 $aDANNENMANN, M.
700 1 $aCERRI, C. E. P.
773 $tPedosphere$gv. 30, n. 3, p. 336-342, 2020.
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