Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, Colombia

The increase and stabilization of soil organic carbon (SOC) represent a feasible alternative for mitigating greenhouse effect. But, SOC is severely affected by changes in soil use, and there is uncertainty about which types of soil use favor carbon sequestration. In addition, climate influences SOC...

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Tipo de recurso:
http://purl.org/coar/resource_type/c_7093
Fecha de publicación:
2018
Institución:
Universidad Pedagógica y Tecnológica de Colombia
Repositorio:
RiUPTC: Repositorio Institucional UPTC
Idioma:
spa
OAI Identifier:
oai:repositorio.uptc.edu.co:001/16790
Acceso en línea:
https://revistas.uptc.edu.co/index.php/ciencias_horticolas/article/view/7349
https://repositorio.uptc.edu.co/handle/001/16790
Palabra clave:
Carbon sequestration
soil management
organic matter
temperature
land.
S622-627
Secuestro de carbono
manejo de suelo
materia orgánica
temperatura
tierra.
S622-627
Rights
License
https://creativecommons.org/licenses/by-nc/4.0/
id REPOUPTC2_e2715f0eb702f00c6083dc0e7140eca8
oai_identifier_str oai:repositorio.uptc.edu.co:001/16790
network_acronym_str REPOUPTC2
network_name_str RiUPTC: Repositorio Institucional UPTC
repository_id_str
dc.title.en-US.fl_str_mv Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, Colombia
dc.title.es-ES.fl_str_mv Influencia del clima, uso del suelo y profundidad sobre el contenido de carbono orgánico en dos pisos altitudinales andinos del departamento Norte de Santander, Colombia
title Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, Colombia
spellingShingle Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, Colombia
Carbon sequestration
soil management
organic matter
temperature
land.
S622-627
Secuestro de carbono
manejo de suelo
materia orgánica
temperatura
tierra.
S622-627
title_short Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, Colombia
title_full Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, Colombia
title_fullStr Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, Colombia
title_full_unstemmed Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, Colombia
title_sort Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, Colombia
dc.subject.en-US.fl_str_mv Carbon sequestration
soil management
organic matter
temperature
land.
S622-627
topic Carbon sequestration
soil management
organic matter
temperature
land.
S622-627
Secuestro de carbono
manejo de suelo
materia orgánica
temperatura
tierra.
S622-627
dc.subject.es-ES.fl_str_mv Secuestro de carbono
manejo de suelo
materia orgánica
temperatura
tierra.
S622-627
description The increase and stabilization of soil organic carbon (SOC) represent a feasible alternative for mitigating greenhouse effect. But, SOC is severely affected by changes in soil use, and there is uncertainty about which types of soil use favor carbon sequestration. In addition, climate influences SOC dynamics; therefore, the effect generated by the use and management of soils is different in cold climates and warm climates. In order to understand how climate, soil use and soil depth influence SOC dynamics at two Andean sites in Norte de Santander, Colombia, the soil physical (sands, silts, clays, and bulk density) and chemical (pH, E.C., C.E.C. and S.B) properties were studied. Also, the total organic carbon (TOC), light fraction (LF), humic fraction (HF), microbiol biomass (MB) and organic carbon were measured. These evaluations were performed in two climates (cold and warm), with three soil uses per climate and three soil depths (0 to 5 cm, 5 to 10 cm and 10 to 20 cm). The amount of organic carbon was statistically higher in the cold climate soils for all compartments (TOC, OC of MB, OC of LF and OC of HF). The Forest and Pasture were more favorable for SOC storage in the cold climates, and the intensive crops presented a lower content of TOC, OC of MB and OC of LF. The humification rate and OC of HF were higher in the soils with intensive crops as the soil use in the warm climate.
publishDate 2018
dc.date.accessioned.none.fl_str_mv 2024-07-08T14:42:25Z
dc.date.available.none.fl_str_mv 2024-07-08T14:42:25Z
dc.date.none.fl_str_mv 2018-05-02
dc.type.en-US.fl_str_mv Exploratory
dc.type.es-ES.fl_str_mv Exploratorio
dc.type.none.fl_str_mv info:eu-repo/semantics/article
dc.type.coar.fl_str_mv http://purl.org/coar/resource_type/c_2df8fbb1
dc.type.coarversion.fl_str_mv http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.coar.spa.fl_str_mv http://purl.org/coar/resource_type/c_7093
dc.type.version.spa.fl_str_mv info:eu-repo/semantics/publishedVersion
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status_str publishedVersion
dc.identifier.none.fl_str_mv https://revistas.uptc.edu.co/index.php/ciencias_horticolas/article/view/7349
10.17584/rcch.2018v12i1.7349
dc.identifier.uri.none.fl_str_mv https://repositorio.uptc.edu.co/handle/001/16790
url https://revistas.uptc.edu.co/index.php/ciencias_horticolas/article/view/7349
https://repositorio.uptc.edu.co/handle/001/16790
identifier_str_mv 10.17584/rcch.2018v12i1.7349
dc.language.none.fl_str_mv spa
dc.language.iso.spa.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv https://revistas.uptc.edu.co/index.php/ciencias_horticolas/article/view/7349/pdf
dc.rights.coar.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.rights.uri.spa.fl_str_mv https://creativecommons.org/licenses/by-nc/4.0/
dc.rights.coar.spa.fl_str_mv http://purl.org/coar/access_right/c_abf594
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc/4.0/
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dc.format.none.fl_str_mv application/pdf
dc.publisher.en-US.fl_str_mv Sociedad Colombiana de Ciencias Hortícolas-SCCH and Universidad Pedagógica y Tecnológica de Colombia-UPTC
dc.source.en-US.fl_str_mv Revista Colombiana de Ciencias Hortícolas; Vol. 12 No. 1 (2018); 233-243
dc.source.es-ES.fl_str_mv Revista Colombiana de Ciencias Hortícolas; Vol. 12 Núm. 1 (2018); 233-243
dc.source.fr-FR.fl_str_mv Revista Colombiana de Ciencias Hortícolas; Vol. 12 No 1 (2018); 233-243
dc.source.it-IT.fl_str_mv Revista Colombiana de Ciencias Hortícolas; V. 12 N. 1 (2018); 233-243
dc.source.pt-BR.fl_str_mv Revista Colombiana de Ciencias Hortícolas; v. 12 n. 1 (2018); 233-243
dc.source.none.fl_str_mv 2422-3719
2011-2173
institution Universidad Pedagógica y Tecnológica de Colombia
repository.name.fl_str_mv Repositorio Institucional UPTC
repository.mail.fl_str_mv repositorio.uptc@uptc.edu.co
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spelling 2018-05-022024-07-08T14:42:25Z2024-07-08T14:42:25Zhttps://revistas.uptc.edu.co/index.php/ciencias_horticolas/article/view/734910.17584/rcch.2018v12i1.7349https://repositorio.uptc.edu.co/handle/001/16790The increase and stabilization of soil organic carbon (SOC) represent a feasible alternative for mitigating greenhouse effect. But, SOC is severely affected by changes in soil use, and there is uncertainty about which types of soil use favor carbon sequestration. In addition, climate influences SOC dynamics; therefore, the effect generated by the use and management of soils is different in cold climates and warm climates. In order to understand how climate, soil use and soil depth influence SOC dynamics at two Andean sites in Norte de Santander, Colombia, the soil physical (sands, silts, clays, and bulk density) and chemical (pH, E.C., C.E.C. and S.B) properties were studied. Also, the total organic carbon (TOC), light fraction (LF), humic fraction (HF), microbiol biomass (MB) and organic carbon were measured. These evaluations were performed in two climates (cold and warm), with three soil uses per climate and three soil depths (0 to 5 cm, 5 to 10 cm and 10 to 20 cm). The amount of organic carbon was statistically higher in the cold climate soils for all compartments (TOC, OC of MB, OC of LF and OC of HF). The Forest and Pasture were more favorable for SOC storage in the cold climates, and the intensive crops presented a lower content of TOC, OC of MB and OC of LF. The humification rate and OC of HF were higher in the soils with intensive crops as the soil use in the warm climate.El incremento y estabilización del carbono orgánico del suelo (COS) representa una alternativa viable para la mitigación del efecto invernadero. Pero el COS es severamente afectado por los cambios del suelo, existiendo controversias sobre cuáles tipos de uso de la tierra favorecen el secuestro de carbono. El clima tiene efecto importante sobre la dinámica del COS, por tanto el efecto generado por el uso y manejo del suelo es distinto en climas fríos y cálidos. Para entender como los factores clima, uso del suelo y profundidad del suelo, afectan la dinámica del COS en dos lugares del departamento de Norte de Santander en Colombia, se evaluaron propiedades físicas (arenas, limos y arcillas, densidad aparente) y propiedades químicas (pH, conductividad eléctrica, capacidad de intercambio catiónico y saturación de bases). Se determinó el contenido de carbono orgánico total (COT), fracción ligera (CO de FL), fracción húmica (CO de FH) y biomasa microbiana (CO de BM). Estas evaluaciones se realizaron en dos climas contrastantes (frío y cálido), tres tipos de uso del suelo (bosque, pasturas y cultivo intensivo) y tres profundidades (0 a 5 cm, 5 a 10 cm y 10 a 20 cm). Se encontró que hay mayor carbono orgánico en todos los compartimientos (COT, CO de BM, CO de FL y CO de FH) del suelo en clima frío. Los usos del suelo en bosque y pastura, son más favorables para el almacenamiento de COS en clima frío, mientras en cultivo intensivo genera menor contenido de COT, CO de FL y CO de BM. El índice de humificación y el CO de FH fueron mayores en cultivo intensivo de clima cálido.application/pdfspaspaSociedad Colombiana de Ciencias Hortícolas-SCCH and Universidad Pedagógica y Tecnológica de Colombia-UPTChttps://revistas.uptc.edu.co/index.php/ciencias_horticolas/article/view/7349/pdfhttps://creativecommons.org/licenses/by-nc/4.0/http://purl.org/coar/access_right/c_abf594http://purl.org/coar/access_right/c_abf2Revista Colombiana de Ciencias Hortícolas; Vol. 12 No. 1 (2018); 233-243Revista Colombiana de Ciencias Hortícolas; Vol. 12 Núm. 1 (2018); 233-243Revista Colombiana de Ciencias Hortícolas; Vol. 12 No 1 (2018); 233-243Revista Colombiana de Ciencias Hortícolas; V. 12 N. 1 (2018); 233-243Revista Colombiana de Ciencias Hortícolas; v. 12 n. 1 (2018); 233-2432422-37192011-2173Carbon sequestrationsoil managementorganic mattertemperatureland.S622-627Secuestro de carbonomanejo de suelomateria orgánicatemperaturatierra.S622-627Influence of climate, soil use and soil depth on soil organic carbon content at two Andean altitudinal sites in Norte de Santander, ColombiaInfluencia del clima, uso del suelo y profundidad sobre el contenido de carbono orgánico en dos pisos altitudinales andinos del departamento Norte de Santander, ColombiaExploratoryExploratorioinfo:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_7093http://purl.org/coar/resource_type/c_2df8fbb1info:eu-repo/semantics/publishedVersionhttp://purl.org/coar/version/c_970fb48d4fbd8a677http://purl.org/coar/version/c_970fb48d4fbd8a85Valenzuela B., Ibonne GeanethVisconti M., Efraín Francisco001/16790oai:repositorio.uptc.edu.co:001/167902025-07-18 11:49:35.785https://creativecommons.org/licenses/by-nc/4.0/metadata.onlyhttps://repositorio.uptc.edu.coRepositorio Institucional UPTCrepositorio.uptc@uptc.edu.co