dor_id: 4132258

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

561.#.#.u: https://www.geofisica.unam.mx/

650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

590.#.#.c: Open Journal Systems (OJS)

270.#.#.d: MX

270.1.#.d: México

590.#.#.b: Concentrador

883.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

883.#.#.1: https://www.publicaciones.unam.mx/

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/454/468

100.1.#.a: Pérez Quezadas, Juan; Cortés Silva, Alejandra; Inguaggiato, Salvatore; Salas Ortega, María Del Rocío; Cervantes Pérez, Juan; Heilweil, Victor Michael

524.#.#.a: Pérez Quezadas, Juan, et al. (2015). Meteoric isotopic gradient on the windward side of the Sierra Madre Oriental area, Veracruz - Mexico. Geofísica Internacional; Vol. 54 Núm. 3: Julio 1, 2015; 267-276. Recuperado de https://repositorio.unam.mx/contenidos/4132258

245.1.0.a: Meteoric isotopic gradient on the windward side of the Sierra Madre Oriental area, Veracruz - Mexico

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2015

264.#.1.c: 2015-07-01

653.#.#.a: Isótopos estables; gradiente isotópico; Veracruz México; composición isotópica; precipitación; Stable isotopes; isotopic gradient; Veracruz; México; isotopic composition; precipitation

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/454

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/454

041.#.7.h: spa

520.3.#.a: The isotopic composition (δ18O, δD‰) of precipitation in the windward side of the Sierra Madre Oriental on the eastern flank of the Mexican Volcanic Belt was characterized along a 90 km transect from sea level up to an altitude of 4220 meters. Rain samples were collected during the rainy season (May through October) from 2007 through 2012. The Local Meteoric Water Line (LMWL), determined with linear regression of isotope results, is δD = 7.44 δ18O + 7.3, R2 = 0.99. This line departs from the Global Meteoric Water Line (GMWL) for precipitation at altitudes greater than 3000 masl due to deuterium enrichment processes. The results obtained in this research were compared with isotopic data of the Global Network of Isotopes Precipitation (GNIP) data base from the port of Veracruz. The altitude (Z) gradient of δ18O was also determined by the linear regression of precipitation data, resulting in the relation δ18O = -2.1Z - 5.56, R2 = 0.86, where Z is altitude in kilometers.This implies a δ18O vertical gradient of -0.21 ‰/ 100 m, which falls within the normal range described in the literature for tropical areas. Finally, the isotopic record of meteoric waters during the years of observation shows anomalous enrichment in δ18O and δD at an altitude of about 1400 m, probably influenced by the local topography and/or an isotope effect related to tropical storms typical of this latitude. This characterization will increase the understanding of important hydrological processes and will provide a foundation for future hydrological research.doi: https://doi.org/10.1016/j.gi.2015.04.021

773.1.#.t: Geofísica Internacional; Vol. 54 Núm. 3: Julio 1, 2015; 267-276

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 267-276

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.1016/j.gi.2015.04.021

handle: 71ad063609b6dec1

harvesting_date: 2023-06-20 16:00:00.0

856.#.0.q: application/pdf

file_creation_date: 2017-04-07 17:15:26.0

file_modification_date: 2022-07-05 21:20:01.0

file_creator: Pérez Quezadas J.

file_name: a52e7101f21274205c294d032991186e006a422dfd84ea663ef0e264aadf3acd.pdf

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245.1.0.b: Meteoric isotopic gradient on the windward side of the Sierra Madre Oriental area, Veracruz - Mexico

last_modified: 2023-06-20 16:00:00

license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

license_type: by-nc-sa

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