Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes
The stability of soil aggregates depends on the organic matter, and the soil use and management can affect the soil organic matter (SOM) content. Therefore, it is necessary to know the relationship between aggregate stability and the content of SOM in different types of soil use at two different alt...
- Autores:
-
Valenzuela Balcázar, Ibonne Geaneth
Visconti Moreno, Efrain Francisco
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 2019
- Institución:
- Universidad Francisco de Paula Santander
- Repositorio:
- Repositorio Digital UFPS
- Idioma:
- eng
- OAI Identifier:
- oai:repositorio.ufps.edu.co:ufps/495
- Acceso en línea:
- http://repositorio.ufps.edu.co/handle/ufps/495
- Palabra clave:
- Soil degradation
Soil structure
Organic matter
Agriculture
Degradación del suelo
Estructura del suelo
Materia orgánica
Agricultura
- Rights
- openAccess
- License
- https://creativecommons.org/licenses/by-nc-nd/4.0/
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dc.title.eng.fl_str_mv |
Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes |
dc.title.spa.fl_str_mv |
Impacto del uso del suelo sobre la estabilidad de agregados y su relación con el carbono orgánico en dos pisos altitudinales en Los Andes de Colombia |
title |
Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes |
spellingShingle |
Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes Soil degradation Soil structure Organic matter Agriculture Degradación del suelo Estructura del suelo Materia orgánica Agricultura |
title_short |
Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes |
title_full |
Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes |
title_fullStr |
Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes |
title_full_unstemmed |
Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes |
title_sort |
Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes |
dc.creator.fl_str_mv |
Valenzuela Balcázar, Ibonne Geaneth Visconti Moreno, Efrain Francisco |
dc.contributor.author.none.fl_str_mv |
Valenzuela Balcázar, Ibonne Geaneth Visconti Moreno, Efrain Francisco |
dc.subject.proposal.eng.fl_str_mv |
Soil degradation Soil structure Organic matter Agriculture |
topic |
Soil degradation Soil structure Organic matter Agriculture Degradación del suelo Estructura del suelo Materia orgánica Agricultura |
dc.subject.proposal.spa.fl_str_mv |
Degradación del suelo Estructura del suelo Materia orgánica Agricultura |
description |
The stability of soil aggregates depends on the organic matter, and the soil use and management can affect the soil organic matter (SOM) content. Therefore, it is necessary to know the relationship between aggregate stability and the content of SOM in different types of soil use at two different altitudes of the Colombian Andes. This study examined the conditions of soil aggregate stability expressed as a distribution of the size classes of stable aggregates (SA) and of the mean weighted diameter of the stable aggregates (MWD). To correlate these characteristics with the soil organic carbon (OC), we measured the particulate organic matter pool (POC), the OC associated with the mineral organic matter pool (HOC), the total organic carbon content (TOC), and the humification rate (HR). Soils were sampled at two altitudes: 1) Humic Dystrudepts in a cold tropical climate (CC) with three plots: tropical mountain rainforest, pastures, and crops; 2) Fluvaquentic Dystrudepts in a warm tropical climate (WC) with three plots: tropical rainforest, an association of oil palm and pastures, and irrigated rice. Soils were sampled at three depths: 0-5, 5-10 and 10-20 cm. The physical properties, mineral particle size distribution, and bulk density were measured. The content of SA with size>2.36 mm was higher in the CC soil (51.48%) than in the WC soil (9.23%). The SA with size 1.18-2.36 mm was also higher in the CC soil (7.78%) than in the WC soil (0.62%). The SA with size 0.60-1.18 mm resulted indifferent. The SA with size between 0.30 and 0.60 mm were higher in the WC soil (13.95%) than in the CC soil (4.67%). The SA<0.30 mm was higher in the WC soil (72.56%) than in the CC soil (32.15%). It was observed that MWD and the SA>2.36 mm increased linearly with a higher POC, but decreased linearly with a higher HR. For the SA<0.30 mm, a linear decrease was observed at a higher POC, while it increased at a higher HR. |
publishDate |
2019 |
dc.date.issued.none.fl_str_mv |
2019-09-01 |
dc.date.accessioned.none.fl_str_mv |
2021-10-29T21:45:12Z |
dc.date.available.none.fl_str_mv |
2021-10-29T21:45:12Z |
dc.type.spa.fl_str_mv |
Artículo de revista |
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http://purl.org/coar/resource_type/c_2df8fbb1 |
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http://purl.org/coar/version/c_970fb48d4fbd8a85 |
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http://purl.org/coar/resource_type/c_6501 |
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http://repositorio.ufps.edu.co/handle/ufps/495 |
dc.identifier.doi.none.fl_str_mv |
10.15446/agron.colomb.v37n3.77601 |
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http://repositorio.ufps.edu.co/handle/ufps/495 |
identifier_str_mv |
10.15446/agron.colomb.v37n3.77601 |
dc.language.iso.spa.fl_str_mv |
eng |
language |
eng |
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Agronomía Colombiana ISSN: 2357-3732, 2019 vol:37 fasc: 3 págs: 263 - 273, DOI:10.15446/agron.colomb.v37n3.77601 |
dc.relation.citationedition.spa.fl_str_mv |
Vol. 37 No. 3 (2019) |
dc.relation.citationendpage.spa.fl_str_mv |
273 |
dc.relation.citationissue.spa.fl_str_mv |
3 (2019) |
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263 |
dc.relation.citationvolume.spa.fl_str_mv |
37 |
dc.relation.cites.none.fl_str_mv |
E. F. Visconti-Moreno and I. G. Valenzuela-Balcázar, “Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes”, Agron. Colomb., vol. 37, no. 3, pp. 263-273, Sep. 2019. |
dc.relation.ispartofjournal.spa.fl_str_mv |
Agronomía Colombiana |
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Atribución-NoComercial-CompartirIgual 4.0 Internacional (CC BY-NC-SA 4.0) |
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11 páginas |
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Agronomía Colombiana |
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Colombia |
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https://revistas.unal.edu.co/index.php/agrocol/article/view/77601 |
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Universidad Francisco de Paula Santander |
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Valenzuela Balcázar, Ibonne Geaneth711399b4f369d258e83eb7a2d3e12953600Visconti Moreno, Efrain Franciscoaee2e3476a13e1bde781d8d32a59cb846002021-10-29T21:45:12Z2021-10-29T21:45:12Z2019-09-01http://repositorio.ufps.edu.co/handle/ufps/49510.15446/agron.colomb.v37n3.77601The stability of soil aggregates depends on the organic matter, and the soil use and management can affect the soil organic matter (SOM) content. Therefore, it is necessary to know the relationship between aggregate stability and the content of SOM in different types of soil use at two different altitudes of the Colombian Andes. This study examined the conditions of soil aggregate stability expressed as a distribution of the size classes of stable aggregates (SA) and of the mean weighted diameter of the stable aggregates (MWD). To correlate these characteristics with the soil organic carbon (OC), we measured the particulate organic matter pool (POC), the OC associated with the mineral organic matter pool (HOC), the total organic carbon content (TOC), and the humification rate (HR). Soils were sampled at two altitudes: 1) Humic Dystrudepts in a cold tropical climate (CC) with three plots: tropical mountain rainforest, pastures, and crops; 2) Fluvaquentic Dystrudepts in a warm tropical climate (WC) with three plots: tropical rainforest, an association of oil palm and pastures, and irrigated rice. Soils were sampled at three depths: 0-5, 5-10 and 10-20 cm. The physical properties, mineral particle size distribution, and bulk density were measured. The content of SA with size>2.36 mm was higher in the CC soil (51.48%) than in the WC soil (9.23%). The SA with size 1.18-2.36 mm was also higher in the CC soil (7.78%) than in the WC soil (0.62%). The SA with size 0.60-1.18 mm resulted indifferent. The SA with size between 0.30 and 0.60 mm were higher in the WC soil (13.95%) than in the CC soil (4.67%). The SA<0.30 mm was higher in the WC soil (72.56%) than in the CC soil (32.15%). It was observed that MWD and the SA>2.36 mm increased linearly with a higher POC, but decreased linearly with a higher HR. For the SA<0.30 mm, a linear decrease was observed at a higher POC, while it increased at a higher HR.La estabilidad de agregados del suelo depende de la materia orgánica y el uso y manejo del suelo puede afectar el contenido de materia orgánica (MOS) del mismo. Por lo tanto, es necesario conocer la relación entre la estabilidad de agregados y el contenido de MOS en diferentes tipos de uso del suelo a diferentes altitudes en Los Andes de Colombia. El presente estudio examinó las condiciones de estabilidad de agregados del suelo expresados como una distribución por tamaño de las clases de agregados estables (AE) y el diámetro medio ponderado (DMP) de agregados estables. Para relacionar estas características con el contenido de carbono orgánico del suelo (CO), se midieron la materia orgánica particulada (COP), el CO asociado con la materia orgánica mineral (COM), el contenido total de carbono orgánico (COT) y el índice de humificación (IH). Se realizaron muestreos de dos suelos de pisos altitudinales diferentes: 1) Un Humic Dystrudepts en clima frío (CF) con tres lotes: bosque natural, pastura y cultivos; 2) Un Fluvaquentic Dystrudepts en clima cálido (CC) con tres lotes: bosque natural, palma de aceite asociada con pastura y arroz con riego. Se muestreó el suelo a tres profundidades: 0 a 5, 5 a 10, y 10 a 20 cm. Se midieron las propiedades físicas, distribución por tamaño de la partícula mineral y densidad aparente. El contenido de AE con tamaño >2.36 mm fue mayor en el suelo de clima frío (51.48%) que en el de clima cálido (9.23%). Los AE de tamaño 1.18 a 2.36 mm fueron también mayores en clima frío (7.78%) que en clima cálido (0.62%). Los AE de tamaño 0.60 a 1.18 mm resultaron indiferentes. Los AE de tamaño entre 0.30 y 0.60 mm presentaron un contenido más alto en el suelo de clima cálido (13.95%) en comparación al de clima frío (4.67%). Los AE<0.30 mm fueron mayores en clima cálido (72.56%) con respecto al clima frío (32.15%). Se observó que el DMP y los AE>2.36 mm aumentaron linealmente con el contenido de COP más alto, pero disminuyeron linealmente con un IH más alto. Para los AE<0.30 mm se observa una disminución lineal a mayor COP, mientras que este aumenta a un IH más alto.11 páginasapplication/pdfengAgronomía ColombianaColombiaAgronomía Colombiana ISSN: 2357-3732, 2019 vol:37 fasc: 3 págs: 263 - 273, DOI:10.15446/agron.colomb.v37n3.77601Vol. 37 No. 3 (2019)2733 (2019)26337E. F. Visconti-Moreno and I. G. Valenzuela-Balcázar, “Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian Andes”, Agron. Colomb., vol. 37, no. 3, pp. 263-273, Sep. 2019.Agronomía ColombianaThis work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.Agronomia Colombiana by Centro Editorial of Facultad de Ciencias Agrarias, Universidad Nacional de Colombia is licensed under a Creative Commons Reconocimiento-NoComercial-CompartirIgual 4.0 Internacional License.https://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessAtribución-NoComercial-CompartirIgual 4.0 Internacional (CC BY-NC-SA 4.0)http://purl.org/coar/access_right/c_abf2https://revistas.unal.edu.co/index.php/agrocol/article/view/77601Impact of soil use on aggregate stability and its relationship with soil organic carbon at two different altitudes in the Colombian AndesImpacto del uso del suelo sobre la estabilidad de agregados y su relación con el carbono orgánico en dos pisos altitudinales en Los Andes de ColombiaArtículo de revistahttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1Textinfo:eu-repo/semantics/articlehttp://purl.org/redcol/resource_type/ARTinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/version/c_970fb48d4fbd8a85Soil degradationSoil structureOrganic matterAgricultureDegradación del sueloEstructura del sueloMateria orgánicaAgriculturaAn, S., A. Mentler, H. Mayer, and W. Blum. 2010. Soil aggregation, aggregate stability, organic carbon and nitrogen in different soil aggregate fractions under forest and shrub vegetation on the Loess Plateau, China. Catena 81, 226-233. Doi: 10.1016/j. catena.2010.04.002Briedis, C., J. Moraes-Sá, E. Caires, J. Navarro, T. Massao-Inagaki, A. Boer, C. Quadros-Neto, A. Oliveira-Ferreira, L. Canalli, and J. Burkner-Dos Santos. 2012. Soil organic matter pools and carbon-protection mechanisms in aggregate classes influenced by surface liming in a no-till system. Geoderma 170, 80-88. Doi: 10.1016/j.geoderma.2011.10.011Bronick, C. and R. Lal. 2005. Soil structure and management: a review. Geoderma 124, 3-22. Doi: 10.1016/j.geoderma.2004.03.005FAO, Food and Agriculture Organization of the United Nations. 2006. Guidelines for soil description. FAO, Rome.Figueiredo, C, D. Siqueira-Resck, and M. Carbone-Carneiro. 2010 Labile and stable fractions of soil organic matter under management systems and native Cerrado. Rev. Bras. Cienc. Solo 34, 907-916. Doi: 10.1590/S0100-06832010000300032IGAC, Instituto Geográfico Agustín Codazzi. 2006a. Estudio general de suelos y zonificación de tierras del departamento Norte de Santander. Instituto Geográfico Agustín Codazzi, Bogota.IGAC, Instituto Geográfico Agustín Codazzi. 2006b. Métodos analíticos de laboratorio de suelos. Instituto Geográfico Agustín Codazzi, Bogota.Loss, A., E. Dos Santos, D. Schmitz, M. Da Veiga, C. Kurtz, and J. Comin. 2017. Atributos físicos do solo em cultivo de cebola sob sistemas de plantio direto e preparo convencional. Rev. Colomb. Cienc. Hort. 11(1), 105-113. Doi: 10.17584/ rcch.2017v11i1.6144Lozano, Z., S. Cabrera, J. Peña, and M. Adams. 1997. Efecto de los sistemas de labranza sobre dos inceptisoles de los llanos occidentales de Venezuela. II. Propiedades físicas de los suelos. Revista Venesuelos, 5, 25-33.Lozano, Z., R. Hernández, and A. Ojeda. 2005. Manual de métodos para la evaluación de la calidad física, química y biológica de los suelos. Universidad Central de Venezuela, Maracay, Venezuela.Martínez, E., J. Fuentes, and E. Acevedo. 2008. Carbono orgánico y propiedades del suelo. J. Soil Sci. Plant Nutr. 8(1), 68-96.Moraes-Sa, J. and R. Lal. 2009. Stratification ratio of soil organic matter pools as an indicator of carbon sequestration in a tillage chronosequence on a Brazilian Oxisol. Soil Tillage Res. 133, 65-74. Doi: 10.1016/j.still.2008.09.003Mujuru, L., A. Mureva, E. Velthorst, and M. Hoosbeek. 2013. Land use and management effects on soil organic matter fractions in Rhodic Ferralsols and Haplic Arenosols in Bindura and Shamva districts of Zimbabwe. Geoderma 209-210, 262-272. Doi: 10.1016/j.geoderma.2013.06.025Nascente, A., Y. Li, and C. Costa-Crusciol. 2015. Soil aggregation, organic carbon concentration, and soil bulk density as affected by cover crop species in a no-tillage system. Rev. Bras. Ciênc. Solo 39, 871-879. Doi: 10.1590/01000683rbcs20140388Oades, J. 1984. Soil organic matter and structural stability: mechanisms and implications for management. Plant Soil 76, 319-337. Doi: 10.1007/BF02205590Oliveira-Marques, J., F. Luizão, W. Teixeira, M. Sarrazin, S. Filgueira-Ferreira, T. Beldini, and E. Araújo-Marques. 2015 Distribution of organic carbon in different soil fractions in ecosystems of central Amazonia. Rev. Bras. Cienc. Solo 39, 232-242. Doi: 10.1590/01000683rbcs20150142Pinto, Y., J. Álvarez, and F. Forero. 2016. Efecto de la labranza en la estabilidad estructural y resistencia a la penetración en un inceptisol sembrado con arracacha (Arracacia xanthorrhiza Bancroft) en Boyacá. Rev. Col. Cienc. Hort. 10(1), 99-112. Doi: 10.17584/rcch.2016v10i1.5049Pla, I. 1983. Metodología para la caracterización física con fines de diagnóstico de problemas de manejo y conservación de suelos en condiciones tropicales. Rev. Fac. Agron. Alcance 32, 5-91.Pla, I. 2010. Medición y evaluación de propiedades físicas de los suelos: dificultades y errores más frecuentes. I - Propiedades mecánicas. Suelos Ecuatoriales 40(2), 75-93.Pulido, M., D. Lobo, and Z. Lozano. 2009. Asociación entre indicadores de estabilidad estructural y la materia orgánica en suelos agrícolas de Venezuela. Agrociencia 43, 221-230.Sena, K., K. Maltoni, G. Amorim-Faria, and A. Rodrigues-Cassiolato. 2017. Organic carbon and physical properties in sandy soil after conversion from degraded pasture to Eucalyptus in the Brazilian Cerrado. Rev. Bras. Cienc. Solo 41, e0150505. Doi: 10.1590/18069657rbcs20150505Six, J., H. Bossuyt, S. Degryze, and K. Denef. 2004. A history of research on the link between (micro)aggregates, soil biota, and soil organic matter dynamics. Soil Till. Res. 79, 7-31 Doi: 10.1016/j.still.2004.03.008Tivet, F., J. Moraes-Sa, R. Lal, C. Briedis, P. Borszowskei, J. BurknerDos Santos, A. Farias, G. Eurich, D. Hartman, M. Nadolny, S. Bouzinac, and L. Seguy. 2013. Aggregate C depletion by plowing and its restoration by diverse biomass-C inputs under no-till in sub-tropical and tropical regions of Brazil. Soil Till. Res. 126, 203-218 Doi: 10.1016/j.still.2012.09.004ORIGINALImpact of soil use on aggregate stability and its relationship with soil organic carbon.pdfImpact of soil use on aggregate stability and its relationship with soil organic carbon.pdfapplication/pdf638789https://repositorio.ufps.edu.co/bitstream/ufps/495/1/Impact%20of%20soil%20use%20on%20aggregate%20stability%20and%20its%20relationship%20with%20soil%20organic%20carbon.pdf39fd5e834194d60069b97f636f23ece1MD51open accessLICENSElicense.txtlicense.txttext/plain; charset=utf-814828https://repositorio.ufps.edu.co/bitstream/ufps/495/2/license.txt2f9959eaf5b71fae44bbf9ec84150c7aMD52open accessTEXTImpact of soil use on aggregate stability and its relationship with soil organic carbon.pdf.txtImpact of soil use on aggregate stability and its relationship with soil organic carbon.pdf.txtExtracted 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 incorporada en las Obras Colectivas.

b.	Distribuir copias o fonogramas de las Obras, exhibirlas públicamente, ejecutarlas públicamente y/o ponerlas a disposición pública, incluyéndolas como incorporadas en Obras Colectivas, según corresponda.

c.	Distribuir copias de las Obras Derivadas que se generen, exhibirlas públicamente, ejecutarlas públicamente y/o ponerlas a disposición pública.
Los derechos mencionados anteriormente pueden ser ejercidos en todos los medios y formatos, actualmente conocidos o que se inventen en el futuro. Los derechos antes mencionados incluyen el derecho a realizar dichas modificaciones en la medida que sean técnicamente necesarias para ejercer los derechos en otro medio o formatos, pero de otra manera usted no está autorizado para realizar obras derivadas. Todos los derechos no otorgados expresamente por el Licenciante quedan por este medio reservados, incluyendo pero sin limitarse a aquellos que se mencionan en las secciones 4(d) y 4(e).

4. Restricciones.
La licencia otorgada en la anterior Sección 3 está expresamente sujeta y limitada por las siguientes restricciones:

a.	Usted puede distribuir, exhibir públicamente, ejecutar públicamente, o poner a disposición pública la Obra sólo bajo las condiciones de esta Licencia, y Usted debe incluir una copia de esta licencia o del Identificador Universal de Recursos de la misma con cada copia de la Obra que distribuya, exhiba públicamente, ejecute públicamente o ponga a disposición pública. No es posible ofrecer o imponer ninguna condición sobre la Obra que altere o limite las condiciones de esta Licencia o el ejercicio de los derechos de los destinatarios otorgados en este documento. No es posible sublicenciar la Obra. Usted debe mantener intactos todos los avisos que hagan referencia a esta Licencia y a la cláusula de limitación de garantías. Usted no puede distribuir, exhibir públicamente, ejecutar públicamente, o poner a disposición pública la Obra con alguna medida tecnológica que controle el acceso o la utilización de ella de una forma que sea inconsistente con las condiciones de esta Licencia. Lo anterior se aplica a la Obra incorporada a una Obra Colectiva, pero esto no exige que la Obra Colectiva aparte de la obra misma quede sujeta a las condiciones de esta Licencia. Si Usted crea una Obra Colectiva, previo aviso de cualquier Licenciante debe, en la medida de lo posible, eliminar de la Obra Colectiva cualquier referencia a dicho Licenciante o al Autor Original, según lo solicitado por el Licenciante y conforme lo exige la cláusula 4(c).

b.	Usted no puede ejercer ninguno de los derechos que le han sido otorgados en la Sección 3 precedente de modo que estén principalmente destinados o directamente dirigidos a conseguir un provecho comercial o una compensación monetaria privada. El intercambio de la Obra por otras obras protegidas por derechos de autor, ya sea a través de un sistema para compartir archivos digitales (digital file-sharing) o de cualquier otra manera no será considerado como estar destinado principalmente o dirigido directamente a conseguir un provecho comercial o una compensación monetaria privada, siempre que no se realice un pago mediante una compensación monetaria en relación con el intercambio de obras protegidas por el derecho de autor.

c.	Si usted distribuye, exhibe públicamente, ejecuta públicamente o ejecuta públicamente en forma digital la Obra o cualquier Obra Derivada u Obra Colectiva, Usted debe mantener intacta toda la información de derecho de autor de la Obra y proporcionar, de forma razonable según el medio o manera que Usted esté utilizando: (i) el nombre del Autor Original si está provisto (o seudónimo, si fuere aplicable), y/o (ii) el nombre de la parte o las partes que el Autor Original y/o el Licenciante hubieren designado para la atribución (v.g., un instituto patrocinador, editorial, publicación) en la información de los derechos de autor del Licenciante, términos de servicios o de otras formas razonables; el título de la Obra si está provisto; en la medida de lo razonablemente factible y, si está provisto, el Identificador Uniforme de Recursos (Uniform Resource Identifier) que el Licenciante especifica para ser asociado con la Obra, salvo que tal URI no se refiera a la nota sobre los derechos de autor o a la información sobre el licenciamiento de la Obra; y en el caso de una Obra Derivada, atribuir el crédito identificando el uso de la Obra en la Obra Derivada (v.g., "Traducción Francesa de la Obra del Autor Original," o "Guión Cinematográfico basado en la Obra original del Autor Original"). Tal crédito puede ser implementado de cualquier forma razonable; en el caso, sin embargo, de Obras Derivadas u Obras Colectivas, tal crédito aparecerá, como mínimo, donde aparece el crédito de cualquier otro autor comparable y de una manera, al menos, tan destacada como el crédito de otro autor comparable.

d.	Para evitar toda confusión, el Licenciante aclara que, cuando la obra es una composición musical:

i.	Regalías por interpretación y ejecución bajo licencias generales. El Licenciante se reserva el derecho exclusivo de autorizar la ejecución pública o la ejecución pública digital de la obra y de recolectar, sea individualmente o a través de una sociedad de gestión colectiva de derechos de autor y derechos conexos (por ejemplo, SAYCO), las regalías por la ejecución pública o por la ejecución pública digital de la obra (por ejemplo Webcast) licenciada bajo licencias generales, si la interpretación o ejecución de la obra está primordialmente orientada por o dirigida a la obtención de una ventaja comercial o una compensación monetaria privada.

ii.	Regalías por Fonogramas. El Licenciante se reserva el derecho exclusivo de recolectar, individualmente o a través de una sociedad de gestión colectiva de derechos de autor y derechos conexos (por ejemplo, los consagrados por la SAYCO), una agencia de derechos musicales o algún agente designado, las regalías por cualquier fonograma que Usted cree a partir de la obra (“versión cover”) y distribuya, en los términos del régimen de derechos de autor, si la creación o distribución de esa versión cover está primordialmente destinada o dirigida a obtener una ventaja comercial o una compensación monetaria privada.

e.	Gestión de Derechos de Autor sobre Interpretaciones y Ejecuciones Digitales (WebCasting). Para evitar toda confusión, el Licenciante aclara que, cuando la obra sea un fonograma, el Licenciante se reserva el derecho exclusivo de autorizar la ejecución pública digital de la obra (por ejemplo, webcast) y de recolectar, individualmente o a través de una sociedad de gestión colectiva de derechos de autor y derechos conexos (por ejemplo, ACINPRO), las regalías por la ejecución pública digital de la obra (por ejemplo, webcast), sujeta a las disposiciones aplicables del régimen de Derecho de Autor, si esta ejecución pública digital está primordialmente dirigida a obtener una ventaja comercial o una compensación monetaria privada.

5. Representaciones, Garantías y Limitaciones de Responsabilidad.
A MENOS QUE LAS PARTES LO ACORDARAN DE OTRA FORMA POR ESCRITO, EL LICENCIANTE OFRECE LA OBRA (EN EL ESTADO EN EL QUE SE ENCUENTRA) “TAL CUAL”, SIN BRINDAR GARANTÍAS DE CLASE ALGUNA RESPECTO DE LA OBRA, YA SEA EXPRESA, IMPLÍCITA, LEGAL O CUALQUIERA OTRA, INCLUYENDO, SIN LIMITARSE A ELLAS, GARANTÍAS DE TITULARIDAD, COMERCIABILIDAD, ADAPTABILIDAD O ADECUACIÓN A PROPÓSITO DETERMINADO, AUSENCIA DE INFRACCIÓN, DE AUSENCIA DE DEFECTOS LATENTES O DE OTRO TIPO, O LA PRESENCIA O AUSENCIA DE ERRORES, SEAN O NO DESCUBRIBLES (PUEDAN O NO SER ESTOS DESCUBIERTOS). ALGUNAS JURISDICCIONES NO PERMITEN LA EXCLUSIÓN DE GARANTÍAS IMPLÍCITAS, EN CUYO CASO ESTA EXCLUSIÓN PUEDE NO APLICARSE A USTED.

6. Limitación de responsabilidad.
A MENOS QUE LO EXIJA EXPRESAMENTE LA LEY APLICABLE, EL LICENCIANTE NO SERÁ RESPONSABLE ANTE USTED POR DAÑO ALGUNO, SEA POR RESPONSABILIDAD EXTRACONTRACTUAL, PRECONTRACTUAL O CONTRACTUAL, OBJETIVA O SUBJETIVA, SE TRATE DE DAÑOS MORALES O PATRIMONIALES, DIRECTOS O INDIRECTOS, PREVISTOS O IMPREVISTOS PRODUCIDOS POR EL USO DE ESTA LICENCIA O DE LA OBRA, AUN CUANDO EL LICENCIANTE HAYA SIDO ADVERTIDO DE LA POSIBILIDAD DE DICHOS DAÑOS. ALGUNAS LEYES NO PERMITEN LA EXCLUSIÓN DE CIERTA RESPONSABILIDAD, EN CUYO CASO ESTA EXCLUSIÓN PUEDE NO APLICARSE A USTED.

7. Término.

a.	Esta Licencia y los derechos otorgados en virtud de ella terminarán automáticamente si Usted infringe alguna condición establecida en ella. Sin embargo, los individuos o entidades que han recibido Obras Derivadas o Colectivas de Usted de conformidad con esta Licencia, no verán terminadas sus licencias, siempre que estos individuos o entidades sigan cumpliendo íntegramente las condiciones de estas licencias. Las Secciones 1, 2, 5, 6, 7, y 8 subsistirán a cualquier terminación de esta Licencia.

b.	Sujeta a las condiciones y términos anteriores, la licencia otorgada aquí es perpetua (durante el período de vigencia de los derechos de autor de la obra). No obstante lo anterior, el Licenciante se reserva el derecho a publicar y/o estrenar la Obra bajo condiciones de licencia diferentes o a dejar de distribuirla en los términos de esta Licencia en cualquier momento; en el entendido, sin embargo, que esa elección no servirá para revocar esta licencia o que deba ser otorgada , bajo los términos de esta licencia), y esta licencia continuará en pleno vigor y efecto a menos que sea terminada como se expresa atrás. La Licencia revocada continuará siendo plenamente vigente y efectiva si no se le da término en las condiciones indicadas anteriormente.

8. Varios.

a.	Cada vez que Usted distribuya o ponga a disposición pública la Obra o una Obra Colectiva, el Licenciante ofrecerá al destinatario una licencia en los mismos términos y condiciones que la licencia otorgada a Usted bajo esta Licencia.

b.	Si alguna disposición de esta Licencia resulta invalidada o no exigible, según la legislación vigente, esto no afectará ni la validez ni la aplicabilidad del resto de condiciones de esta Licencia y, sin acción adicional por parte de los sujetos de este acuerdo, aquélla se entenderá reformada lo mínimo necesario para hacer que dicha disposición sea válida y exigible.

c.	Ningún término o disposición de esta Licencia se estimará renunciada y ninguna violación de ella será consentida a menos que esa renuncia o consentimiento sea otorgado por escrito y firmado por la parte que renuncie o consienta.

d.	Esta Licencia refleja el acuerdo pleno entre las partes respecto a la Obra aquí licenciada. No hay arreglos, acuerdos o declaraciones respecto a la Obra que no estén especificados en este documento. El Licenciante no se verá limitado por ninguna disposición adicional que pueda surgir en alguna comunicación emanada de Usted. Esta Licencia no puede ser modificada sin el consentimiento mutuo por escrito del Licenciante y Usted.
0000-0002-1173-3133711399b4f369d258e83eb7a2d3e129536000000-0002-7017-313Xaee2e3476a13e1bde781d8d32a59cb84600 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