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3. | | BALMELLI, G.; SIMETO, S.; TORRES, D.; CASTILLO, A.; ALTIER, N.; MAC GREGOR, J.; PEVERELLI, A.; DIEZ, J. Control genético de la resistencia y del escape a Teratosphaeria nubilosaen Eucalyptus globulus en Uruguay. [Presentación oral]. In: Congreso IUFRO, Pucón, Chile, 22-23 de Noviembre. Eucaliptos genéticamente mejorados para aumentar la competitividad del sector forestal en América Latina. Pucón: IUFRO, 2012.Biblioteca(s): INIA Tacuarembó. |
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4. | | BALMELLI, G.; SIMETO, S.; TORRES, D.; CASTILLO, A.; ALTIER, N.; PÉREZ, G.; MAC GREGOR, J.; PEVERELLI, A.; DIEZ, J.J. Mejoramiento genético en eucalyptus globulus y eucalyptus maidenii por resistencia a Teratosphaeria nubilosa. In: BALMELLI, G.; SIMETO, S.; MARTÍNEZ, G.; GÓMEZ, D. (Eds.). V Jornada técnica de protección forestal. Avances de investigación en plagas y enfermedades forestales Montevideo (UY): INIA, 2013. p. 55-65 (INIA Serie Técnica; 209)Biblioteca(s): INIA Tacuarembó. |
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5. | | BALMELLI, G.; SIMETO, S.; TORRES, D.; CASTILLO, A.; PÉREZ, G.; MAC GREGOR, J.; PEVERELLI, A.; ALTIER, N.; DIEZ, J. Mejoramiento genético en Eucalyptus globulus y Eucalyptus maidenii por resistencia a Teratosphaeria nubilosa. ln: INIA TACUAREMBÓ. PROGRAMA NACIONAL DE INVESTIGACIÓN EN PRODUCCIÓN FORESTAL. V Jornada de Protección Forestal, 14 y 15 de noviembre, Tacuarembó. Tacuarembó (Uruguay): INIA, 2012. p. 14 (INIA Serie Actividades de Difusión; 703)Biblioteca(s): INIA Tacuarembó. |
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6. | | BALMELLI, G.; SIMETO, S.; TORRES, D.; CASTILLO, A.; PÉREZ, G.; MAC GREGOR, J.; PEVERELLI, A.; ALTIER, N.; DIEZ, J. Mejoramiento Genético en Eucalyptus globulus y Eucalyptus maidenii por resistencia a Teratosphaeria nubilosa. [Presentación oral]. In: Jornada de Protección Forestal, 5., INIA Tacuarembó, 14 y 15 de Noviembre. Tacuarembó: INIA, 2012.Biblioteca(s): INIA Tacuarembó. |
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Registro completo
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Biblioteca (s) : |
INIA La Estanzuela. |
Fecha actual : |
18/12/2020 |
Actualizado : |
21/05/2021 |
Tipo de producción científica : |
Artículos en Revistas Indexadas Internacionales |
Circulación / Nivel : |
Internacional - -- |
Autor : |
LOICK, N.; DIXON, E.; MATTHEWS, G.P.; MÜLLER, CH.; CIGANDA, V.; LÓPEZ-AIZPÚN, M.; REPULLO, M.A.; CARDENAS, L.M. |
Afiliación : |
NADINE LOICK, Rothamsted Research, North Wyke, Okehampton, Devon EX20 2SB, UK; ELIZABETH DIXON, Rothamsted Research, North Wyke, Okehampton, Devon EX20 2SB, UK.; G. PETER MATTHEWS, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, Devon PL4 8AA, UK.; CHRISTOPH MÜLLER, Institute of Plant Ecology, Justus Liebig University Giessen, 35392 Giessen, German.; VERONICA SOLANGE CIGANDA BRASCA, INIA (Instituto Nacional de Investigación Agropecuaria), Uruguay; MARIA LÓPEZ-AIZPÚN, LICA, Department of Chemistry, University of Navarre, Irunlarrea, 1-31008 Pamplona, Spain.; MIGUEL A. REPULLO, IFAPA, Area of Agriculture and Environment Centre Alameda del Obispo, Av. Menéndez Pidal s/n, Apdo 3092, 14080 Córdoba, Spain; LAURA M. CARDENAS, Rothamsted Research, North Wyke, Okehampton, Devon EX20 2SB, UK. |
Título : |
Application of a triple 15N tracing technique to elucidate N transformations in a UK grassland soil. |
Fecha de publicación : |
2021 |
Fuente / Imprenta : |
Geoderma, 1 March 2021, Volume 385, Article number 114844. Doi: https://doi.org/10.1016/j.geoderma.2020.114844 |
DOI : |
10.1016/j.geoderma.2020.114844 |
Idioma : |
Inglés |
Notas : |
Article history: Received 14 August 2020/ Revised 11 November 2020/ Accepted 13 November 2020/ Available online 2 December 2020. |
Contenido : |
Abstract: To identify the production and consumption pathways and temporal dynamics of N2O emitted from soil, this study uses 15N-labelled substrate-N to quantify the underlying gross N transformation rates using the Ntrace analysis tool and link them to N-emissions. In three experiments twelve soil cores each were incubated in a lab incubation system to measure gaseous emissions, while parallel incubations under the same conditions were set up for destructive soil sampling at 7 time points. Using the triple labelling technique (applying NH4NO3 with either the NH4+-N or the NO3?-N, or both being 15N labelled), this study investigated the effects of 55, 70 and 85% water filled pore space (deemed to promote nitrification, both nitrification and denitrification, and denitrification, respectively) in a clay soil on gaseous N emissions and investigates the source and processes leading to N2O emissions. To assess the utilisation of applied NO3? vs. nitrified NO3? from applied NH4+, the 15N tracing tool Ntrace was used to quantify the rates of immobilisation of NO3? and NH4+, oxidation of NH4+, mineralisation of organic N and subsequent nitrification by the analysis of the 15N in the soil. Gross transformation rates were calculated, indicating the relative importance of added NO3? and NO3? derived from nitrified added NH4+. Results show an important contribution of heterotrophic nitrification (organic N oxidation to NO3?) which was highest at the 55% water filled pore space (WFPS), decreasing in its contribution to N-transformation processes with increasing WFPS, while nitrification (NH4+ oxidation to NO3?) was contributing the most at 70% WFPS. The contribution of denitrification increased with increasing WFPS, but only became dominant at 85% WFPS. While denitrification still showed to be most important at high and nitrification at lower WFPS, the actual % WFPS values were not as expected and highlight the fact that WFPS is a contributor, but not the sole/most important parameter determining the type of N-transformation processes taking place. MenosAbstract: To identify the production and consumption pathways and temporal dynamics of N2O emitted from soil, this study uses 15N-labelled substrate-N to quantify the underlying gross N transformation rates using the Ntrace analysis tool and link them to N-emissions. In three experiments twelve soil cores each were incubated in a lab incubation system to measure gaseous emissions, while parallel incubations under the same conditions were set up for destructive soil sampling at 7 time points. Using the triple labelling technique (applying NH4NO3 with either the NH4+-N or the NO3?-N, or both being 15N labelled), this study investigated the effects of 55, 70 and 85% water filled pore space (deemed to promote nitrification, both nitrification and denitrification, and denitrification, respectively) in a clay soil on gaseous N emissions and investigates the source and processes leading to N2O emissions. To assess the utilisation of applied NO3? vs. nitrified NO3? from applied NH4+, the 15N tracing tool Ntrace was used to quantify the rates of immobilisation of NO3? and NH4+, oxidation of NH4+, mineralisation of organic N and subsequent nitrification by the analysis of the 15N in the soil. Gross transformation rates were calculated, indicating the relative importance of added NO3? and NO3? derived from nitrified added NH4+. Results show an important contribution of heterotrophic nitrification (organic N oxidation to NO3?) which was highest at the 55% water filled pore space (WFPS),... Presentar Todo |
Palabras claves : |
DENITRIFICATION; EMISIONES DE N20; HETEROTROPHIC NITRIFICATION; NITRIFICATION; NITROUS OXIDE. |
Thesagro : |
DENITRIFICACION. |
Asunto categoría : |
-- |
Marc : |
LEADER 03134naa a2200301 a 4500 001 1061589 005 2021-05-21 008 2021 bl uuuu u00u1 u #d 024 7 $a10.1016/j.geoderma.2020.114844$2DOI 100 1 $aLOICK, N. 245 $aApplication of a triple 15N tracing technique to elucidate N transformations in a UK grassland soil.$h[electronic resource] 260 $c2021 500 $aArticle history: Received 14 August 2020/ Revised 11 November 2020/ Accepted 13 November 2020/ Available online 2 December 2020. 520 $aAbstract: To identify the production and consumption pathways and temporal dynamics of N2O emitted from soil, this study uses 15N-labelled substrate-N to quantify the underlying gross N transformation rates using the Ntrace analysis tool and link them to N-emissions. In three experiments twelve soil cores each were incubated in a lab incubation system to measure gaseous emissions, while parallel incubations under the same conditions were set up for destructive soil sampling at 7 time points. Using the triple labelling technique (applying NH4NO3 with either the NH4+-N or the NO3?-N, or both being 15N labelled), this study investigated the effects of 55, 70 and 85% water filled pore space (deemed to promote nitrification, both nitrification and denitrification, and denitrification, respectively) in a clay soil on gaseous N emissions and investigates the source and processes leading to N2O emissions. To assess the utilisation of applied NO3? vs. nitrified NO3? from applied NH4+, the 15N tracing tool Ntrace was used to quantify the rates of immobilisation of NO3? and NH4+, oxidation of NH4+, mineralisation of organic N and subsequent nitrification by the analysis of the 15N in the soil. Gross transformation rates were calculated, indicating the relative importance of added NO3? and NO3? derived from nitrified added NH4+. Results show an important contribution of heterotrophic nitrification (organic N oxidation to NO3?) which was highest at the 55% water filled pore space (WFPS), decreasing in its contribution to N-transformation processes with increasing WFPS, while nitrification (NH4+ oxidation to NO3?) was contributing the most at 70% WFPS. The contribution of denitrification increased with increasing WFPS, but only became dominant at 85% WFPS. While denitrification still showed to be most important at high and nitrification at lower WFPS, the actual % WFPS values were not as expected and highlight the fact that WFPS is a contributor, but not the sole/most important parameter determining the type of N-transformation processes taking place. 650 $aDENITRIFICACION 653 $aDENITRIFICATION 653 $aEMISIONES DE N20 653 $aHETEROTROPHIC NITRIFICATION 653 $aNITRIFICATION 653 $aNITROUS OXIDE 700 1 $aDIXON, E. 700 1 $aMATTHEWS, G.P. 700 1 $aMÜLLER, CH. 700 1 $aCIGANDA, V. 700 1 $aLÓPEZ-AIZPÚN, M. 700 1 $aREPULLO, M.A. 700 1 $aCARDENAS, L.M. 773 $tGeoderma, 1 March 2021, Volume 385, Article number 114844. Doi: https://doi.org/10.1016/j.geoderma.2020.114844
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