Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration
Understanding biogeochemical cycles and especially carbon budgets is clue to validate global change models in the present and near future. As a consequence, sinks and sources of carbon in the world are being studied. One of those sinks is the non-well known behavior of the planet vegetation which in...
- Autores:
-
Moreno-Ramírez, H. A. (Hernán Alonso)
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 2008
- Institución:
- Universidad EIA .
- Repositorio:
- Repositorio EIA .
- Idioma:
- eng
- OAI Identifier:
- oai:repository.eia.edu.co:11190/602
- Acceso en línea:
- https://repository.eia.edu.co/handle/11190/602
- Palabra clave:
- REI00082
RECURSOS NATURALES: AGUA, MINERALES, BIODIVERSIDAD
NATURAL RESOURCES: WATER, MINERALS, BIODIVERSITY
CICLO DEL CARBONO
CARBON CYCLE
CARBON SEQUESTRATION
EVAPOTRANSPIRATION
NET EXCHANGE OF CO2
EDDY COVARIANCE
LATENT HEAT FLUX
FIJACIÓN DE CARBONO
EVAPOTRANSPIRACIÓN
INTERCAMBIO NETO DE CO2
EDDY COVARIANZA
FLUJO DE CALOR LATENTE
- Rights
- openAccess
- License
- Derechos Reservados - Universidad EIA, 2020
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REIA2 |
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|
| dc.title.spa.fl_str_mv |
Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration |
| title |
Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration |
| spellingShingle |
Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration REI00082 RECURSOS NATURALES: AGUA, MINERALES, BIODIVERSIDAD NATURAL RESOURCES: WATER, MINERALS, BIODIVERSITY CICLO DEL CARBONO CARBON CYCLE CARBON SEQUESTRATION EVAPOTRANSPIRATION NET EXCHANGE OF CO2 EDDY COVARIANCE LATENT HEAT FLUX FIJACIÓN DE CARBONO EVAPOTRANSPIRACIÓN INTERCAMBIO NETO DE CO2 EDDY COVARIANZA FLUJO DE CALOR LATENTE |
| title_short |
Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration |
| title_full |
Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration |
| title_fullStr |
Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration |
| title_full_unstemmed |
Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration |
| title_sort |
Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration |
| dc.creator.fl_str_mv |
Moreno-Ramírez, H. A. (Hernán Alonso) |
| dc.contributor.author.spa.fl_str_mv |
Moreno-Ramírez, H. A. (Hernán Alonso) |
| dc.subject.lcsh.spa.fl_str_mv |
REI00082 |
| topic |
REI00082 RECURSOS NATURALES: AGUA, MINERALES, BIODIVERSIDAD NATURAL RESOURCES: WATER, MINERALS, BIODIVERSITY CICLO DEL CARBONO CARBON CYCLE CARBON SEQUESTRATION EVAPOTRANSPIRATION NET EXCHANGE OF CO2 EDDY COVARIANCE LATENT HEAT FLUX FIJACIÓN DE CARBONO EVAPOTRANSPIRACIÓN INTERCAMBIO NETO DE CO2 EDDY COVARIANZA FLUJO DE CALOR LATENTE |
| dc.subject.eia.spa.fl_str_mv |
RECURSOS NATURALES: AGUA, MINERALES, BIODIVERSIDAD NATURAL RESOURCES: WATER, MINERALS, BIODIVERSITY |
| dc.subject.eurovoc.spa.fl_str_mv |
CICLO DEL CARBONO CARBON CYCLE |
| dc.subject.keywords.spa.fl_str_mv |
CARBON SEQUESTRATION EVAPOTRANSPIRATION NET EXCHANGE OF CO2 EDDY COVARIANCE LATENT HEAT FLUX FIJACIÓN DE CARBONO EVAPOTRANSPIRACIÓN INTERCAMBIO NETO DE CO2 EDDY COVARIANZA FLUJO DE CALOR LATENTE |
| description |
Understanding biogeochemical cycles and especially carbon budgets is clue to validate global change models in the present and near future. As a consequence, sinks and sources of carbon in the world are being studied. One of those sinks is the non-well known behavior of the planet vegetation which involves the processes of photosynthesis and respiration. Carbon sequestration rates are highly related to the transpiration through a molecular diffusion process occurring at the stomatal level which can be recorded by an eddy covariance micrometeorological station. This paper explores annual and diurnal cycles of latent heat (LE) and CO2 net (FC) fluxes over 6 different ecosystems. Based on the physics of the transpiration process, different time-scale analysis are performed, finding a near-linear relation between LE and CO2 net fluxes, which is stronger at the more vegetated areas. The North American monsoon season increases carbon up taking and LE-CO2 flux relation preserves at different time scales analysis (hours to days to months). |
| publishDate |
2008 |
| dc.date.created.spa.fl_str_mv |
2008-07 |
| dc.date.submitted.spa.fl_str_mv |
2008-01-14 |
| dc.date.accepted.spa.fl_str_mv |
2008-06-15 |
| dc.date.accessioned.spa.fl_str_mv |
2014-05-09T20:58:23Z |
| dc.date.available.spa.fl_str_mv |
2014-05-09T20:58:23Z |
| dc.date.issued.spa.fl_str_mv |
2014-05-09 |
| dc.type.spa.fl_str_mv |
Artículo de revista |
| dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
| dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 |
| dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/article |
| dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
| dc.type.content.spa.fl_str_mv |
Text |
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https://purl.org/redcol/resource_type/ART |
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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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publishedVersion |
| dc.identifier.issn.spa.fl_str_mv |
ISSN 17941237 |
| dc.identifier.uri.spa.fl_str_mv |
https://repository.eia.edu.co/handle/11190/602 |
| dc.identifier.bibliographiccitation.spa.fl_str_mv |
Moreno, H. A.. Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration, Revista EIA, 9, 53-68. doi: http://repository.eia.edu.co/handle/11190/602 |
| identifier_str_mv |
ISSN 17941237 Moreno, H. A.. Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration, Revista EIA, 9, 53-68. doi: http://repository.eia.edu.co/handle/11190/602 |
| url |
https://repository.eia.edu.co/handle/11190/602 |
| dc.language.iso.spa.fl_str_mv |
eng |
| language |
eng |
| dc.relation.references.spa.fl_str_mv |
Ameriflux network: http://cdiac.esd.ornl.gov/programs/ ameriflux/data_system/aamer.html Brack, C., 2002. Pollution mitigation and carbon sequestration by an urban forest. Environmental Pollution 116 S195-S200. Cowan, I. R., 1977. Stomatal behavior and environment. Adv. Bot. Res. 4, 117-228. |
| dc.rights.spa.fl_str_mv |
Derechos Reservados - Universidad EIA, 2020 |
| dc.rights.uri.spa.fl_str_mv |
https://creativecommons.org/licenses/by-nc/4.0/ |
| dc.rights.accessrights.spa.fl_str_mv |
info:eu-repo/semantics/openAccess |
| dc.rights.creativecommons.spa.fl_str_mv |
Atribución-NoComercial |
| dc.rights.coar.spa.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
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Derechos Reservados - Universidad EIA, 2020 https://creativecommons.org/licenses/by-nc/4.0/ Atribución-NoComercial http://purl.org/coar/access_right/c_abf2 |
| eu_rights_str_mv |
openAccess |
| dc.format.extent.spa.fl_str_mv |
16 p. |
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application/pdf |
| dc.publisher.department.spa.fl_str_mv |
Civil, Ambiental Geológica e Industrial |
| dc.publisher.editor.spa.fl_str_mv |
Escuela de Ingeniería de Antioquia EIA |
| institution |
Universidad EIA . |
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Moreno-Ramírez, H. A. (Hernán Alonso)7c6b0d34565200aa16e9910f918d5b99-1pfhemo@eia.edu.co.2014-05-09T20:58:23Z2014-05-09T20:58:23Z2008-072014-05-092008-01-142008-06-15ISSN 17941237https://repository.eia.edu.co/handle/11190/602Moreno, H. A.. Annual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestration, Revista EIA, 9, 53-68. doi: http://repository.eia.edu.co/handle/11190/602Understanding biogeochemical cycles and especially carbon budgets is clue to validate global change models in the present and near future. As a consequence, sinks and sources of carbon in the world are being studied. One of those sinks is the non-well known behavior of the planet vegetation which involves the processes of photosynthesis and respiration. Carbon sequestration rates are highly related to the transpiration through a molecular diffusion process occurring at the stomatal level which can be recorded by an eddy covariance micrometeorological station. This paper explores annual and diurnal cycles of latent heat (LE) and CO2 net (FC) fluxes over 6 different ecosystems. Based on the physics of the transpiration process, different time-scale analysis are performed, finding a near-linear relation between LE and CO2 net fluxes, which is stronger at the more vegetated areas. The North American monsoon season increases carbon up taking and LE-CO2 flux relation preserves at different time scales analysis (hours to days to months).El conocimiento de los ciclos biogeoquímicos y, en especial, de los balances de carbono es clave para la validación de los modelos de cambio global para el presente y el futuro cercano. Como consecuencia, en el mundo se estudian las fuentes y los sumideros de carbono. Uno de esos sumideros es la vegetación del planeta, que involucra los procesos de respiración y fotosíntesis y cuyo comportamiento se empieza a estudiar. Las tasas de captura del carbono están muy ligadas a la transpiración mediante un proceso de difusión molecular en los estomas, que puede registrarse por un sistema micrometeorológico de eddy covarianza. Este artículo explora los ciclos anuales y diurnos de los flujos netos de CO2 y calor latente de seis ecosistemas diferentes. Se desarrollan diversos análisis de escala temporal, basados en la física de la transpiración, y se halla una relación cuasilineal entre los flujos netos de calor latente y CO2, más fuerte en las áreas con mayor cobertura vegetal. La temporada del monzón norteamericano incrementa la captura de carbono y la relación entre la evapotranspiración y el intercambio de gas carbónico se mantiene en las diferentes escalas temporales analizadas (horas, días, meses).16 p.application/pdfengDerechos Reservados - Universidad EIA, 2020https://creativecommons.org/licenses/by-nc/4.0/El autor de la obra, actuando en nombre propio, hace entrega del ejemplar respectivo y de sus anexos en formato digital o electrónico y autoriza a la ESCUELA DE INGENIERIA DE ANTIOQUIA, para que en los términos establecidos en la Ley 23 de 1982, Ley 44 de 1993, Decisión andina 351 de 1993, Decreto 460 de 1995, y demás normas generales sobre la materia, utilice y use por cualquier medio conocido o por conocer, los derechos patrimoniales de reproducción, comunicación pública, transformación y distribución de la obra objeto del presente documento. PARÁGRAFO: La presente autorización se hace extensiva no sólo a las dependencias y derechos de uso sobre la obra en formato o soporte material, sino también para formato virtual, electrónico, digital, y en red, internet, extranet, intranet, etc., y en general en cualquier formato conocido o por conocer. EL AUTOR, manifiesta que la obra objeto de la presente autorización es original y la realiza sin violar o usurpar derechos de autor de terceros, por lo tanto la obra es de exclusiva autoría y tiene la titularidad sobre la misma. PARÁGRAFO: En caso de presentarse cualquier reclamación o acción por parte de un tercero en cuanto a los derechos de autor sobre la obra en cuestión, EL AUTOR, asumirá toda la responsabilidad, y saldrá en defensa de los derechos aquí autorizados; para todos los efectos la ESCUELA DE INGENIERÍA DE ANTIOQUIA actúa como un tercero de buena fe.info:eu-repo/semantics/openAccessAtribución-NoComercialhttp://purl.org/coar/access_right/c_abf2REI00082RECURSOS NATURALES: AGUA, MINERALES, BIODIVERSIDADNATURAL RESOURCES: WATER, MINERALS, BIODIVERSITYCICLO DEL CARBONOCARBON CYCLECARBON SEQUESTRATIONEVAPOTRANSPIRATIONNET EXCHANGE OF CO2EDDY COVARIANCELATENT HEAT FLUXFIJACIÓN DE CARBONOEVAPOTRANSPIRACIÓNINTERCAMBIO NETO DE CO2EDDY COVARIANZAFLUJO DE CALOR LATENTEAnnual and diurnal cycles of the inverse relation between plant transpiration and carbon sequestrationArtículo de revistahttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionTexthttps://purl.org/redcol/resource_type/ARThttp://purl.org/coar/version/c_970fb48d4fbd8a85Civil, Ambiental Geológica e IndustrialEscuela de Ingeniería de Antioquia EIAAmeriflux network: http://cdiac.esd.ornl.gov/programs/ ameriflux/data_system/aamer.htmlBrack, C., 2002. Pollution mitigation and carbon sequestration by an urban forest. Environmental Pollution 116 S195-S200.Cowan, I. R., 1977. Stomatal behavior and environment. Adv. Bot. Res. 4, 117-228.PublicationTHUMBNAILREI00082.pdf.jpgREI00082.pdf.jpgGenerated Thumbnailimage/jpeg11753https://repository.eia.edu.co/bitstreams/30c7e8bc-02b2-4fbd-bb0f-80466733882a/download210c6339daf9706435fad67f4e012afdMD57ORIGINALREI00082.pdfREI00082.pdfapplication/pdf1551050https://repository.eia.edu.co/bitstreams/46307879-1250-4fe8-809c-795491fdabb4/download906a5bcdc8f1b4171afa788303efa4b9MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81494https://repository.eia.edu.co/bitstreams/6d0cbc2c-e530-4bba-b855-af59ca1dcbcf/download66874b0b9366b748c60895d2fb6339f8MD52CC-LICENSElicense_urllicense_urltext/plain; charset=utf-849https://repository.eia.edu.co/bitstreams/00d0e0c9-25e5-4171-b2aa-e15a08169df8/download4afdbb8c545fd630ea7db775da747b2fMD53license_textlicense_texttext/html; charset=utf-821310https://repository.eia.edu.co/bitstreams/291d2809-53db-4570-8659-0bc54b5292f4/download10a9da7597c333616da297895d0393ecMD54license_rdflicense_rdfapplication/rdf+xml; charset=utf-823253https://repository.eia.edu.co/bitstreams/3879ef4c-da2a-4782-b7a8-8bcaebf1bf49/downloadcd76e7886171c964e259dcf5e912e299MD55TEXTREI00082.pdf.txtREI00082.pdf.txtExtracted texttext/plain28555https://repository.eia.edu.co/bitstreams/49e59682-f32b-4f3d-a014-132c35a40611/download431e493331dc61ca721a51a68057f998MD5611190/602oai:repository.eia.edu.co:11190/6022023-07-25 17:20:33.268https://creativecommons.org/licenses/by-nc/4.0/Derechos Reservados - Universidad EIA, 2020open.accesshttps://repository.eia.edu.coRepositorio Institucional Universidad EIAbdigital@metabiblioteca.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 |