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 | Acceso al texto completo restringido a Biblioteca INIA Tacuarembó. Por información adicional contacte bibliotb@tb.inia.org.uy. |
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Registro completo
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Biblioteca (s) : |
INIA Tacuarembó; INIA Treinta y Tres. |
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Fecha : |
23/11/2021 |
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Actualizado : |
18/08/2022 |
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Tipo de producción científica : |
Libros |
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Autor : |
MEUS, L. D.; SILVA, M. R. DA; RIBAS, G. G.; ZANON, A. J.; ROSSATO, I. G.; PEREIRA, V. F.; PILECCO, I. B.; RIBEIRO, B. SAN MARTIN ROLIM; SOUZA, P. M. DE; NASCIMENTO, M. DE F. DO.; POERSCH, A. H.; DUARTE JUNIOR, A. J.; QUINTERO, C. E.; CARRACELAS, G.; CARMONA, L. DE C.; STRECK, N. A. |
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Afiliación : |
LORENZO DALCIN MEUS, Universidade Federal de Santa Maria (UFSM).; MICHEL ROCHA DA SILVA; GIOVANA GHISLENI RIBAS; ALENCAR JUNIOR ZANON; IORAN GUEDES ROSSATO; VLADISON FOGLIATO PEREIRA; ISABELA BULEGON PILECCO; BRUNA SAN MARTIN ROLIM RIBEIRO; PABLO MAZZUCO DE SOUZA; MOISES DE FREITAS DO NASCIMENTO; ABDERSON HAAS POERSCH; ARY JOSÉ DUARTE JUNIOR; CÉSAR EUGENIO QUINTERO; JULIO GONZALO CARRACELAS GARRIDO, INIA (Instituto Nacional de Investigación Agropecuaria), Uruguay; LUCIANO DE CAMPOS CARMONA; NEREU AUGUSTO STRECK. |
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Título : |
Ecofisiología del arroz buscando altos rendimientos. [Ecophysiology of rice for reaching high yield]. |
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Fecha de publicación : |
2020 |
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Fuente / Imprenta : |
Santa Maria, RS (Brasil): FieldCrops, 2020. 312 p. |
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ISBN : |
978-65-992356-4-1 |
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Idioma : |
Español |
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Contenido : |
Lograr altos rendimientos y rentabilidad en el cultivo del arroz, conocer la ecofisiología de los cultivares actualmente sembrados, el sistema de producción y las particularidades de cada zona de producción, será la línea divisoria entre una cosecha exitosa y una cosecha insatisfactoria. En este sentido, a través de la cooperación y unión de universidades e instituciones públicas de investigación y extensión rural en Brasil, Argentina, Uruguay, Colombia y Estados Unidos, se buscó resumir claramente los conceptos y prácticas de ecofisiología y manejo del arroz, combinados con agricultura digital (4.0) y la infinidad de posibilidades que abren. |
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Palabras claves : |
ARROZ; CULTIVO; ECOFISIOLOGÍA DEL CULTIVO. |
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Asunto categoría : |
F01 Cultivo |
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Marc : |
LEADER 01642nam a2200337 a 4500
001 1062545
005 2022-08-18
008 2020 bl uuuu u00u1 u #d
020 $a978-65-992356-4-1
100 1 $aMEUS, L. D.
245 $aEcofisiología del arroz buscando altos rendimientos. [Ecophysiology of rice for reaching high yield].
260 $aSanta Maria, RS (Brasil): FieldCrops, 2020. 312 p.$c2020
520 $aLograr altos rendimientos y rentabilidad en el cultivo del arroz, conocer la ecofisiología de los cultivares actualmente sembrados, el sistema de producción y las particularidades de cada zona de producción, será la línea divisoria entre una cosecha exitosa y una cosecha insatisfactoria. En este sentido, a través de la cooperación y unión de universidades e instituciones públicas de investigación y extensión rural en Brasil, Argentina, Uruguay, Colombia y Estados Unidos, se buscó resumir claramente los conceptos y prácticas de ecofisiología y manejo del arroz, combinados con agricultura digital (4.0) y la infinidad de posibilidades que abren.
653 $aARROZ
653 $aCULTIVO
653 $aECOFISIOLOGÍA DEL CULTIVO
700 1 $aSILVA, M. R. DA
700 1 $aRIBAS, G. G.
700 1 $aZANON, A. J.
700 1 $aROSSATO, I. G.
700 1 $aPEREIRA, V. F.
700 1 $aPILECCO, I. B.
700 1 $aRIBEIRO, B. SAN MARTIN ROLIM
700 1 $aSOUZA, P. M. DE
700 1 $aNASCIMENTO, M. DE F. DO.
700 1 $aPOERSCH, A. H.
700 1 $aDUARTE JUNIOR, A. J.
700 1 $aQUINTERO, C. E.
700 1 $aCARRACELAS, G.
700 1 $aCARMONA, L. DE C.
700 1 $aSTRECK, N. A.
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INIA Tacuarembó (TBO) |
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| Acceso al texto completo restringido a Biblioteca INIA La Estanzuela. Por información adicional contacte bib_le@inia.org.uy. |
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Registro completo
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Biblioteca (s) : |
INIA La Estanzuela. |
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Fecha actual : |
21/02/2014 |
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Actualizado : |
28/10/2019 |
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Tipo de producción científica : |
Artículos en Revistas Indexadas Internacionales |
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Circulación / Nivel : |
A - 2 |
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Autor : |
QUINCKE, A.; WORTMANN, C.S.; MAMO, M.; FRANTI, T.G.; DRIJBER, R.A. |
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Afiliación : |
JUAN ANDRES QUINCKE WALDEN, INIA (Instituto Nacional de Investigación Agropecuaria), Uruguay; C. S. WORTMANN, University of Nebraska at Lincoln.; MARTHA MAMO, University of Nebraska at Lincoln.; THOMAS G FRANTI, University of Nebraska at Lincoln.; RHAE A. DRIJBER, University of Nebraska at Lincoln. |
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Título : |
Occasional tillage of no-till systems: Carbon dioxide flux and changes in total and labile soil organic carbon. |
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Fecha de publicación : |
2007 |
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Fuente / Imprenta : |
Agronomy Journal, July 2007, Volume 99, Issue 4, Pages 1158-1168. |
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DOI : |
10.2134/agronj2006.0317 |
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Idioma : |
Inglés |
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Contenido : |
ABSTRACT: Soil organic carbon (SOC) accumulation occurs mostly in the top 5 cm of soil with continuous no-till (NT) while SOC losses often occur atdeeperdepths.Wehypothesizethatone-timetillageconductedonce in .10 yr to mix the high SOC surface layer with deeper soil will not result in large SOC losses following tillage with a net positive gain in SOCeventually.Twoexperimentsinlong-termNTfieldswereinstalled under rainfed corn (Zea mays L.) or sorghum [Sorghum bicolor (L.) Moench.] rotated with soybean [Glycine max (L.) Merr.] in eastern Nebraska. Tillage treatments were applied in the spring or fall and included: NT, disk, chisel with 10-cm wide twisted shanks, moldboard plow (MP), and mini-moldboard plow (miniMP). A portable infrared gas analyzer was used to monitor CO2 flux immediately following tillage. Effect of tillage on profile distribution of total and labile (particulate and oxidizable) SOC was determined. At 24 to 32 mo following tillage, SOC mass was determined for depths of 0 to 5, 5 to 20, and 20 to 30 cm. Some tillage operations effectively redistributed total and labile SOC with little increase in CO2 flux compared with NT. TotalandlabileSOCconcentrationswerereducedby24to88%inthe 0- to 2.5-cm depth and increased by 13 to 381% for the 5- to 10-cm depth for the various tillage operations. Moldboard plowing caused the greatest redistribution of SOC. On an equivalent soil mass basis, tillage did not cause significant losses of total or labile SOC between tillage and planting of the next crop or by 24 to 32 mo after tillage. Stratification of SOC in long-term NT soil could be reduced most effectively by means of one-time MP tillage without increased loss of labile SOC. MenosABSTRACT: Soil organic carbon (SOC) accumulation occurs mostly in the top 5 cm of soil with continuous no-till (NT) while SOC losses often occur atdeeperdepths.Wehypothesizethatone-timetillageconductedonce in .10 yr to mix the high SOC surface layer with deeper soil will not result in large SOC losses following tillage with a net positive gain in SOCeventually.Twoexperimentsinlong-termNTfieldswereinstalled under rainfed corn (Zea mays L.) or sorghum [Sorghum bicolor (L.) Moench.] rotated with soybean [Glycine max (L.) Merr.] in eastern Nebraska. Tillage treatments were applied in the spring or fall and included: NT, disk, chisel with 10-cm wide twisted shanks, moldboard plow (MP), and mini-moldboard plow (miniMP). A portable infrared gas analyzer was used to monitor CO2 flux immediately following tillage. Effect of tillage on profile distribution of total and labile (particulate and oxidizable) SOC was determined. At 24 to 32 mo following tillage, SOC mass was determined for depths of 0 to 5, 5 to 20, and 20 to 30 cm. Some tillage operations effectively redistributed total and labile SOC with little increase in CO2 flux compared with NT. TotalandlabileSOCconcentrationswerereducedby24to88%inthe 0- to 2.5-cm depth and increased by 13 to 381% for the 5- to 10-cm depth for the various tillage operations. Moldboard plowing caused the greatest redistribution of SOC. On an equivalent soil mass basis, tillage did not cause significant losses of total or labile SOC between tillage an... Presentar Todo |
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Palabras claves : |
CARBON DIOXIDE; SOIL MICROORGANISMS; SOYBEANS; ZEA MAYS. |
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Asunto categoría : |
-- |
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Marc : |
LEADER 02404naa a2200229 a 4500
001 1049477
005 2019-10-28
008 2007 bl uuuu u00u1 u #d
024 7 $a10.2134/agronj2006.0317$2DOI
100 1 $aQUINCKE, A.
245 $aOccasional tillage of no-till systems$bCarbon dioxide flux and changes in total and labile soil organic carbon.$h[electronic resource]
260 $c2007
520 $aABSTRACT: Soil organic carbon (SOC) accumulation occurs mostly in the top 5 cm of soil with continuous no-till (NT) while SOC losses often occur atdeeperdepths.Wehypothesizethatone-timetillageconductedonce in .10 yr to mix the high SOC surface layer with deeper soil will not result in large SOC losses following tillage with a net positive gain in SOCeventually.Twoexperimentsinlong-termNTfieldswereinstalled under rainfed corn (Zea mays L.) or sorghum [Sorghum bicolor (L.) Moench.] rotated with soybean [Glycine max (L.) Merr.] in eastern Nebraska. Tillage treatments were applied in the spring or fall and included: NT, disk, chisel with 10-cm wide twisted shanks, moldboard plow (MP), and mini-moldboard plow (miniMP). A portable infrared gas analyzer was used to monitor CO2 flux immediately following tillage. Effect of tillage on profile distribution of total and labile (particulate and oxidizable) SOC was determined. At 24 to 32 mo following tillage, SOC mass was determined for depths of 0 to 5, 5 to 20, and 20 to 30 cm. Some tillage operations effectively redistributed total and labile SOC with little increase in CO2 flux compared with NT. TotalandlabileSOCconcentrationswerereducedby24to88%inthe 0- to 2.5-cm depth and increased by 13 to 381% for the 5- to 10-cm depth for the various tillage operations. Moldboard plowing caused the greatest redistribution of SOC. On an equivalent soil mass basis, tillage did not cause significant losses of total or labile SOC between tillage and planting of the next crop or by 24 to 32 mo after tillage. Stratification of SOC in long-term NT soil could be reduced most effectively by means of one-time MP tillage without increased loss of labile SOC.
653 $aCARBON DIOXIDE
653 $aSOIL MICROORGANISMS
653 $aSOYBEANS
653 $aZEA MAYS
700 1 $aWORTMANN, C.S.
700 1 $aMAMO, M.
700 1 $aFRANTI, T.G.
700 1 $aDRIJBER, R.A.
773 $tAgronomy Journal, July 2007, Volume 99, Issue 4, Pages 1158-1168.
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