Future groundwater extraction scenarios for an aquifer in a semiarid environment: case study of Guadalupe Valley Aquifer, Baja California, Northwest Mexico
Semiarid northwestern Mexico presents a growing water demand produced by agricultural and domestic requirements during the last two decades. The community of Guadalupe Valley and the city of Ensenada rely on groundwater pumping from the local aquifer as its sole source of water supply. This dependen...
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Published in | Environmental monitoring and assessment Vol. 186; no. 11; pp. 7961 - 7985 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
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Springer-Verlag
01.11.2014
Springer International Publishing Springer Nature B.V |
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ISSN | 0167-6369 1573-2959 1573-2959 |
DOI | 10.1007/s10661-014-3980-6 |
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Abstract | Semiarid northwestern Mexico presents a growing water demand produced by agricultural and domestic requirements during the last two decades. The community of Guadalupe Valley and the city of Ensenada rely on groundwater pumping from the local aquifer as its sole source of water supply. This dependency has resulted in an imbalance between groundwater pumpage and natural recharge. A two-dimensional groundwater flow model was applied to the Guadalupe Valley Aquifer, which was calibrated and validated for the period 1984–2005. The model analysis verified that groundwater levels in the region are subject to steep declines due to decades of intensive groundwater exploitation for agricultural and domestic purposes. The calibrated model was used to assess the effects of different water management scenarios for the period 2007–2025. If the base case (status quo) scenario continues, groundwater levels are in a continuous drawdown trend. Some wells would run dry by August 2017, and water demand may not be met without incurring in an overdraft. The optimistic scenario implies the achievement of the mean groundwater recharge and discharge. Groundwater level depletion could be stopped and restored. The sustainable scenario implies the reduction of current extraction (up to about 50 %), when groundwater level depletion could be stopped. A reduction in current extraction mitigates water stress in the aquifer but cannot solely reverse declining water tables across the region. The combination of reduced current extraction and an implemented alternative solution (such as groundwater artificial recharge), provides the most effective measure to stabilize and reverse declining groundwater levels while meeting water demands in the region. |
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AbstractList | Semiarid northwestern Mexico presents a growing water demand produced by agricultural and domestic requirements during the last two decades. The community of Guadalupe Valley and the city of Ensenada rely on groundwater pumping from the local aquifer as its sole source of water supply. This dependency has resulted in an imbalance between groundwater pumpage and natural recharge. A two-dimensional groundwater flow model was applied to the Guadalupe Valley Aquifer, which was calibrated and validated for the period 1984-2005. The model analysis verified that groundwater levels in the region are subject to steep declines due to decades of intensive groundwater exploitation for agricultural and domestic purposes. The calibrated model was used to assess the effects of different water management scenarios for the period 2007-2025. If the base case (status quo) scenario continues, groundwater levels are in a continuous drawdown trend. Some wells would run dry by August 2017, and water demand may not be met without incurring in an overdraft. The optimistic scenario implies the achievement of the mean groundwater recharge and discharge. Groundwater level depletion could be stopped and restored. The sustainable scenario implies the reduction of current extraction (up to about 50 %), when groundwater level depletion could be stopped. A reduction in current extraction mitigates water stress in the aquifer but cannot solely reverse declining water tables across the region. The combination of reduced current extraction and an implemented alternative solution (such as groundwater artificial recharge), provides the most effective measure to stabilize and reverse declining groundwater levels while meeting water demands in the region.Semiarid northwestern Mexico presents a growing water demand produced by agricultural and domestic requirements during the last two decades. The community of Guadalupe Valley and the city of Ensenada rely on groundwater pumping from the local aquifer as its sole source of water supply. This dependency has resulted in an imbalance between groundwater pumpage and natural recharge. A two-dimensional groundwater flow model was applied to the Guadalupe Valley Aquifer, which was calibrated and validated for the period 1984-2005. The model analysis verified that groundwater levels in the region are subject to steep declines due to decades of intensive groundwater exploitation for agricultural and domestic purposes. The calibrated model was used to assess the effects of different water management scenarios for the period 2007-2025. If the base case (status quo) scenario continues, groundwater levels are in a continuous drawdown trend. Some wells would run dry by August 2017, and water demand may not be met without incurring in an overdraft. The optimistic scenario implies the achievement of the mean groundwater recharge and discharge. Groundwater level depletion could be stopped and restored. The sustainable scenario implies the reduction of current extraction (up to about 50 %), when groundwater level depletion could be stopped. A reduction in current extraction mitigates water stress in the aquifer but cannot solely reverse declining water tables across the region. The combination of reduced current extraction and an implemented alternative solution (such as groundwater artificial recharge), provides the most effective measure to stabilize and reverse declining groundwater levels while meeting water demands in the region. Semiarid northwestern Mexico presents a growing water demand produced by agricultural and domestic requirements during the last two decades. The community of Guadalupe Valley and the city of Ensenada rely on groundwater pumping from the local aquifer as its sole source of water supply. This dependency has resulted in an imbalance between groundwater pumpage and natural recharge. A two-dimensional groundwater flow model was applied to the Guadalupe Valley Aquifer, which was calibrated and validated for the period 1984–2005. The model analysis verified that groundwater levels in the region are subject to steep declines due to decades of intensive groundwater exploitation for agricultural and domestic purposes. The calibrated model was used to assess the effects of different water management scenarios for the period 2007–2025. If the base case (status quo) scenario continues, groundwater levels are in a continuous drawdown trend. Some wells would run dry by August 2017, and water demand may not be met without incurring in an overdraft. The optimistic scenario implies the achievement of the mean groundwater recharge and discharge. Groundwater level depletion could be stopped and restored. The sustainable scenario implies the reduction of current extraction (up to about 50 %), when groundwater level depletion could be stopped. A reduction in current extraction mitigates water stress in the aquifer but cannot solely reverse declining water tables across the region. The combination of reduced current extraction and an implemented alternative solution (such as groundwater artificial recharge), provides the most effective measure to stabilize and reverse declining groundwater levels while meeting water demands in the region. Semiarid northwestern Mexico presents a growing water demand produced by agricultural and domestic requirements during the last two decades. The community of Guadalupe Valley and the city of Ensenada rely on groundwater pumping from the local aquifer as its sole source of water supply. This dependency has resulted in an imbalance between groundwater pumpage and natural recharge. A two-dimensional groundwater flow model was applied to the Guadalupe Valley Aquifer, which was calibrated and validated for the period 1984–2005. The model analysis verified that groundwater levels in the region are subject to steep declines due to decades of intensive groundwater exploitation for agricultural and domestic purposes. The calibrated model was used to assess the effects of different water management scenarios for the period 2007–2025. If the base case (status quo) scenario continues, groundwater levels are in a continuous drawdown trend. Some wells would run dry by August 2017, and water demand may not be met without incurring in an overdraft. The optimistic scenario implies the achievement of the mean groundwater recharge and discharge. Groundwater level depletion could be stopped and restored. The sustainable scenario implies the reduction of current extraction (up to about 50 %), when groundwater level depletion could be stopped. A reduction in current extraction mitigates water stress in the aquifer but cannot solely reverse declining water tables across the region. The combination of reduced current extraction and an implemented alternative solution (such as groundwater artificial recharge), provides the most effective measure to stabilize and reverse declining groundwater levels while meeting water demands in the region. Semiarid northwestern Mexico presents a growing water demand produced by agricultural and domestic requirements during the last two decades. The community of Guadalupe Valley and the city of Ensenada rely on groundwater pumping from the local aquifer as its sole source of water supply. This dependency has resulted in an imbalance between groundwater pumpage and natural recharge. A two-dimensional groundwater flow model was applied to the Guadalupe Valley Aquifer, which was calibrated and validated for the period 1984-2005. The model analysis verified that groundwater levels in the region are subject to steep declines due to decades of intensive groundwater exploitation for agricultural and domestic purposes. The calibrated model was used to assess the effects of different water management scenarios for the period 2007-2025. If the base case (status quo) scenario continues, groundwater levels are in a continuous drawdown trend. Some wells would run dry by August 2017, and water demand may not be met without incurring in an overdraft. The optimistic scenario implies the achievement of the mean groundwater recharge and discharge. Groundwater level depletion could be stopped and restored. The sustainable scenario implies the reduction of current extraction (up to about 50 %), when groundwater level depletion could be stopped. A reduction in current extraction mitigates water stress in the aquifer but cannot solely reverse declining water tables across the region. The combination of reduced current extraction and an implemented alternative solution (such as groundwater artificial recharge), provides the most effective measure to stabilize and reverse declining groundwater levels while meeting water demands in the region. [PUBLICATION ABSTRACT] |
Author | Kretzschmar, Thomas Herrera-Oliva, Claudia Soledad Campos-Gaytan, Jose Ruben |
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BackLink | https://www.ncbi.nlm.nih.gov/pubmed/25086715$$D View this record in MEDLINE/PubMed |
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CitedBy_id | crossref_primary_10_1016_j_asej_2021_02_023 crossref_primary_10_5004_dwt_2020_25877 crossref_primary_10_1016_j_envint_2022_107130 crossref_primary_10_1016_j_agwat_2015_10_029 crossref_primary_10_1016_j_ejrh_2025_102189 crossref_primary_10_1080_10807039_2017_1300858 crossref_primary_10_3390_hydrology11020016 crossref_primary_10_1016_j_ejrh_2019_100653 crossref_primary_10_1007_s11269_022_03310_1 crossref_primary_10_3390_w11081586 crossref_primary_10_1016_j_gsd_2022_100758 crossref_primary_10_1061_JWRMD5_WRENG_5985 crossref_primary_10_1016_j_egyr_2022_11_191 crossref_primary_10_1007_s12665_015_4959_5 crossref_primary_10_1016_j_scitotenv_2020_136715 |
Cites_doi | 10.1029/JZ068i016p04795 10.5194/hessd-3-707-2006 10.1016/S0022-1694(00)00331-0 |
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Keywords | Extraction scenarios Dry conditions Guadalupe Valley Groundwater Semiarid environment Baja California |
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Reporte técnico. 8 pp. Badan, A., Kretzschmar, T., Espejel, I., Cavazos, T., D’Acosta, H., Vargas, P., et al. (2005). Hacia un plan de manejo del agua en Valle de Guadalupe, Baja California. Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias (INIFAP). Memorias del II Seminario Internacional de Vitivinicultura. August 3–4, 2005. Ensenada, BC, México. 70 pp. FetterCWApplied hydrogeology19943New YorkMacmillan College Publishing Company, Inc. SARH (1977). Informe final del estudio geohidrológico del Valle de Guadalupe, Estado de Baja California Norte. Beltrán, L. (2001). Balance Geohidrológico del acuífero BC-07 Valle de Guadalupe, Municipio de Ensenada, B.C., CONAGUA. Gerencia Regional en la Península de Baja California. Subgerencia Regional Técnica. 19 pp. IzbickiJARadykJMichelRLWater movement through a thick unsaturated zone underlying an intermittent stream in the western Mojave Desert, southern California, USAJournal of Hydrology200023819421710.1016/S0022-1694(00)00331-01:CAS:528:DC%2BD3cXptFSgurk%3D Anderson, M.P., & Woessner, W.W. (1992). Applied groundwater modeling, simulation of flow and advective transport. Academic Press. 381 pp. Beltrán, L. (1998a). Actualización Hidrogeológica del acuífero del Valle de Guadalupe, Municipio de Ensenada, Baja California. Ensenada, México. CONAGUA. Gerencia Regional de la Península de Baja California. Subgerencia Técnica Regional. 24 pp. Campos-GaytanJRKretzschmarTNumerical understanding of regional scale water table behavior in the Guadalupe Valley aquifer, Baja California, MexicoHydrology and Earth System Sciences Discussions20063370773010.5194/hessd-3-707-2006 McDonald, M.G., & Harbaugh, A.W. (1988). A modular three-dimensional finite-difference ground-water flow model. US Department of the Interior and US Geological Survey. US Geological Survey, Techniques of Water Resources Investigations, Book 6. CONAGUA (2003). Nivelación de brocales de la red de monitoreo piezométrico del Acuífero 0207 del Valle de Guadalupe, Ensenada, B.C., Geomática Integral y Servicios De Baja California S. C. Contrato No. SGT-GRPBC-BC-03-008-CE-I3. 107 pp. KrásnýJDistribución espacial de los parámetros hidráulicos en diversos medios hidrogeológicosBoletín Geológico y Minero2003114171182 Campos-Gaytan, J.R. (2002). Actualización del modelo geohidrológico del acuífero del Valle de Ojos Negros, Baja California. CICESE. Master Thesis. 151 pp. Cavazos Pérez, T., & Arriaga Ramírez, S. (2009). Plan estatal de acción climática de Baja California: Escenarios de cambio climático a escala regional. 2009 SIMPOSIO SOBRE CAMBIO CLIMÁTICO. División de Oceanología, CICESE. Geos, 29(1). http://www.ugm.org.mx/publicaciones/geos/pdf/geos09-1/sesiones_especiales/SE24.pdf. Accessed 22 Dec 2011. AndradeMActualización geohidrológica del Valle de Guadalupe, Municipio de Ensenada, Baja California1992EnsenadaSecretaria de Asentamientos Humanos y Obras Publicas de Ensenada (SAHOPE) and CESPE69 pp CONAGUA (2010). Estadísticas del Agua en México, Edición 2010. Edited by: SEMARNAT. 249 pp. http://www.siagua.org/archivos_adjuntos/documentos/estadisticas_mexico.pdf. Accessed 07 May 2012. VillanuevaMIglesiasAPozos y acuíferos; Técnicas de evaluación mediante ensayos de bombeo1984MadridInstituto Geológico y Minero de España. Talleres Gráficos IBERGESA Wagoner, J. L., & McKague, L. H. (1984) Variation of physical properties of alluvium in an arid basin, Lawrence Livermore National Laboratory. UCRL-90672, PREPRINT, paper submittal to Journal of Sedimentary Petrology. 18 pp. Hernández-Rosas, M.T., & Mejía-Vázquez, R. (2003). Relación de aguas superficiales y subterráneas del acuífero BC-07, Valle de Guadalupe, Municipio de Ensenada, Baja California. XII Congreso Nacional de Hidráulica. CONAGUA. Gerencia de Aguas Subterráneas. Subgerencia Regional Técnica. Jefatura de Aguas Subterráneas. Ensenada, Baja California. 13 pp. Trescott, P.C., G.F., Pinder, & S.O. Larson (1976). Finite-difference model for aquifer simulation in two dimensions with results of numerical experiments. Techniques of Water-Resources Investigations of the United States Geological Survey. United States Government Printing Office, Washington. 7. C1:2–3. 116 pp. Escolero-Fuentes, O.A., & Hernández-Rosas, M.T. (1992). Manejo conjunto en el Valle de Guadalupe, B.C., como una estrategia apropiada para el uso eficiente del agua en zonas áridas. Comisión Internacional de riesgo y drenaje. Tercera Conferencia Panamericana de Riesgo y Drenaje: Modernización de los distritos de riego. Mazatlán, Sinaloa. November, 1992. 12 pp. Martínez Austria, P.F., & Patiño Gómez, C. (2001). Cambio climático y recursos hídricos. Ciencia y Desarrollo. Consejo Nacional de Ciencia y Tecnología. México. March, 2011. 237(250): 34–41. (SARH) Secretaría de Agricultura y Recursos Hidráulicos (1982). Dictamen geohidrológico del Valle de Guadalupe. 20 pp. SARH (1967). Inventario de aprovechamientos superficiales y subterráneos para riego. Baja California Norte. Tomo único. Jefatura de irrigación y control de ríos. Dirección de pequeña irrigación. Campos-Gaytan, J.R. (2008). Simulación del flujo de agua subterránea en el Acuífero del Valle de Guadalupe, Baja California, Baja California, México. Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE). PHD Thesis. 220 pp. Salgado Transito, J.A. (2010) El uso de tecnologías de la información en el desarrollo de un plan de manejo sustentable del Acuífero del Valle de Guadalupe, BC. Colegio de Postgraduados (COLPOS) Institución de Enseñanza e Investigación en Ciencias Agrícolas. PhD Thesis. 209 pp. Beltrán, L. (1998b). Balance de los recursos hidráulicos subterráneos, Acuífero BC-07, Guadalupe, Municipio de Ensenada, Baja California. Ensenada, México. CONAGUA. Gerencia Regional de la Península de Baja California. Subgerencia Técnica Regional. Aguas subterráneas. 17 pp. RA Freeze (3980_CR19) 1979 M Andrade (3980_CR3) 1997 J Krásný (3980_CR23) 2003; 114 JR Campos-Gaytan (3980_CR10) 2006; 3 3980_CR21 3980_CR20 JA Izbicki (3980_CR22) 2000; 238 J Tóth (3980_CR32) 1963; 68 3980_CR27 3980_CR26 3980_CR29 3980_CR28 3980_CR25 3980_CR24 3980_CR30 3980_CR31 CW Fetter (3980_CR17) 1994 M Andrade (3980_CR2) 1992 3980_CR16 3980_CR15 3980_CR18 3980_CR12 3980_CR11 3980_CR33 3980_CR9 3980_CR14 3980_CR8 3980_CR13 3980_CR35 3980_CR7 3980_CR6 3980_CR5 3980_CR4 M Villanueva (3980_CR34) 1984 3980_CR1 |
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Academic Press. 381 pp. – reference: McDonald, M.G., & Harbaugh, A.W. (1988). A modular three-dimensional finite-difference ground-water flow model. US Department of the Interior and US Geological Survey. US Geological Survey, Techniques of Water Resources Investigations, Book 6. – reference: (SEMARNAT) Secretaria de Medio Ambiente y Recursos Naturales (2001). Diario Oficial. Acuerdo por el que se establece y da a conocer al público en general la denominación única de los acuíferos reconocidos en el territorio de los Estados Unidos Mexicanos, por la CONAGUA, y la homologación de los nombres de los acuíferos que fueron utilizados para la emisión de los títulos de concesión, asignación o permisos otorgados por este órgano desconcentrado. Miércoles 5 de diciembre de 2001 (Segunda Sección). – reference: Escolero-Fuentes, O.A., & Hernández-Rosas, M.T. (1992). Manejo conjunto en el Valle de Guadalupe, B.C., como una estrategia apropiada para el uso eficiente del agua en zonas áridas. Comisión Internacional de riesgo y drenaje. Tercera Conferencia Panamericana de Riesgo y Drenaje: Modernización de los distritos de riego. Mazatlán, Sinaloa. November, 1992. 12 pp. – reference: Campos-Gaytan, J.R. (2008). Simulación del flujo de agua subterránea en el Acuífero del Valle de Guadalupe, Baja California, Baja California, México. Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE). PHD Thesis. 220 pp. – reference: Beltrán, L. (1998a). Actualización Hidrogeológica del acuífero del Valle de Guadalupe, Municipio de Ensenada, Baja California. Ensenada, México. CONAGUA. Gerencia Regional de la Península de Baja California. Subgerencia Técnica Regional. 24 pp. – reference: SARH (1977). Informe final del estudio geohidrológico del Valle de Guadalupe, Estado de Baja California Norte. – reference: AndradeMActualización geohidrológica del Valle de Guadalupe, Municipio de Ensenada, Baja California1997EnsenadaGrupo Agroindustrial del Valle de Guadalupe60 pp – reference: Campos-GaytanJRKretzschmarTNumerical understanding of regional scale water table behavior in the Guadalupe Valley aquifer, Baja California, MexicoHydrology and Earth System Sciences Discussions20063370773010.5194/hessd-3-707-2006 – reference: KrásnýJDistribución espacial de los parámetros hidráulicos en diversos medios hidrogeológicosBoletín Geológico y Minero2003114171182 – reference: Martínez Austria, P.F., & Patiño Gómez, C. (2001). Cambio climático y recursos hídricos. Ciencia y Desarrollo. Consejo Nacional de Ciencia y Tecnología. México. March, 2011. 237(250): 34–41. – reference: Trescott, P.C., G.F., Pinder, & S.O. Larson (1976). Finite-difference model for aquifer simulation in two dimensions with results of numerical experiments. Techniques of Water-Resources Investigations of the United States Geological Survey. United States Government Printing Office, Washington. 7. C1:2–3. 116 pp. – reference: VillanuevaMIglesiasAPozos y acuíferos; Técnicas de evaluación mediante ensayos de bombeo1984MadridInstituto Geológico y Minero de España. Talleres Gráficos IBERGESA – reference: FreezeRACherryJAGroundwater1979Englewood CliffsPrentice Hall – reference: SARH (1967). Inventario de aprovechamientos superficiales y subterráneos para riego. Baja California Norte. Tomo único. Jefatura de irrigación y control de ríos. Dirección de pequeña irrigación. – reference: Plata Caudillo JA. 2010. Aislamiento y evaluación in vitro del efecto de Trichoderma SPP nativas sobre hongos patógenos de la madera de vid aislados en la región vitivinícola de Ensenada, Baja California. Master Thesis. CICESE. 96 pp. – reference: (INEGI) Instituto Nacional de Estadística, Geografía e Informática (1976). Carta geológica Francisco Zarco (I11D82). – reference: IzbickiJARadykJMichelRLWater movement through a thick unsaturated zone underlying an intermittent stream in the western Mojave Desert, southern California, USAJournal of Hydrology200023819421710.1016/S0022-1694(00)00331-01:CAS:528:DC%2BD3cXptFSgurk%3D – reference: Hernández-Rosas, M.T., & Mejía-Vázquez, R. (2003). Relación de aguas superficiales y subterráneas del acuífero BC-07, Valle de Guadalupe, Municipio de Ensenada, Baja California. XII Congreso Nacional de Hidráulica. CONAGUA. Gerencia de Aguas Subterráneas. Subgerencia Regional Técnica. Jefatura de Aguas Subterráneas. Ensenada, Baja California. 13 pp. – reference: TóthJA theoretical analysis of groundwater flow in small drainage basinsJournal of Geophysical Research196368164795481210.1029/JZ068i016p04795 – reference: FetterCWApplied hydrogeology19943New YorkMacmillan College Publishing Company, Inc. – reference: AndradeMActualización geohidrológica del Valle de Guadalupe, Municipio de Ensenada, Baja California1992EnsenadaSecretaria de Asentamientos Humanos y Obras Publicas de Ensenada (SAHOPE) and CESPE69 pp – reference: (SARH) Secretaría de Agricultura y Recursos Hidráulicos (1982). Dictamen geohidrológico del Valle de Guadalupe. 20 pp. – reference: Figueroa Nuñez, A. (2013). Conducción de agua tratada de El Sauzal hasta el Valle de Guadalupe. Universidad Autónoma de Baja California. Facultad de Ingeniería, Arquitectura y Diseño. Master Thesis. 133 pp. – reference: CONAGUA (2003). Nivelación de brocales de la red de monitoreo piezométrico del Acuífero 0207 del Valle de Guadalupe, Ensenada, B.C., Geomática Integral y Servicios De Baja California S. C. Contrato No. SGT-GRPBC-BC-03-008-CE-I3. 107 pp. – reference: Salgado Transito, J.A. (2010) El uso de tecnologías de la información en el desarrollo de un plan de manejo sustentable del Acuífero del Valle de Guadalupe, BC. Colegio de Postgraduados (COLPOS) Institución de Enseñanza e Investigación en Ciencias Agrícolas. PhD Thesis. 209 pp. – reference: Beltrán, L. (2001). Balance Geohidrológico del acuífero BC-07 Valle de Guadalupe, Municipio de Ensenada, B.C., CONAGUA. Gerencia Regional en la Península de Baja California. Subgerencia Regional Técnica. 19 pp. – reference: (CONAGUA) Comisión Nacional del Agua (1990). Estudio de actividades piezometría en el Valle de Guadalupe, Municipio de Ensenada, Baja California. Gerencia Regional de la Península de Baja California. Jefatura de proyecto de aguas subterráneas. 34 pp. – reference: CONAGUA (2010). Estadísticas del Agua en México, Edición 2010. Edited by: SEMARNAT. 249 pp. http://www.siagua.org/archivos_adjuntos/documentos/estadisticas_mexico.pdf. Accessed 07 May 2012. – reference: Cavazos Pérez, T., & Arriaga Ramírez, S. (2009). Plan estatal de acción climática de Baja California: Escenarios de cambio climático a escala regional. 2009 SIMPOSIO SOBRE CAMBIO CLIMÁTICO. División de Oceanología, CICESE. Geos, 29(1). http://www.ugm.org.mx/publicaciones/geos/pdf/geos09-1/sesiones_especiales/SE24.pdf. Accessed 22 Dec 2011. – reference: Beltrán, L. (1998b). Balance de los recursos hidráulicos subterráneos, Acuífero BC-07, Guadalupe, Municipio de Ensenada, Baja California. Ensenada, México. CONAGUA. Gerencia Regional de la Península de Baja California. Subgerencia Técnica Regional. Aguas subterráneas. 17 pp. – reference: Campos-Gaytan, J.R. (2002). Actualización del modelo geohidrológico del acuífero del Valle de Ojos Negros, Baja California. CICESE. Master Thesis. 151 pp. – ident: 3980_CR7 – ident: 3980_CR14 – ident: 3980_CR9 – ident: 3980_CR35 – ident: 3980_CR16 – ident: 3980_CR12 – ident: 3980_CR20 – ident: 3980_CR5 – ident: 3980_CR29 – ident: 3980_CR1 – volume-title: Applied hydrogeology year: 1994 ident: 3980_CR17 – ident: 3980_CR24 – ident: 3980_CR26 – volume: 68 start-page: 4795 issue: 16 year: 1963 ident: 3980_CR32 publication-title: Journal of Geophysical Research doi: 10.1029/JZ068i016p04795 – volume: 114 start-page: 171 year: 2003 ident: 3980_CR23 publication-title: Boletín Geológico y Minero – ident: 3980_CR30 – volume-title: Actualización geohidrológica del Valle de Guadalupe, Municipio de Ensenada, Baja California year: 1992 ident: 3980_CR2 – volume: 3 start-page: 707 issue: 3 year: 2006 ident: 3980_CR10 publication-title: Hydrology and Earth System Sciences Discussions doi: 10.5194/hessd-3-707-2006 – ident: 3980_CR13 – ident: 3980_CR6 – ident: 3980_CR8 – ident: 3980_CR15 – ident: 3980_CR11 – ident: 3980_CR4 – ident: 3980_CR28 – volume-title: Actualización geohidrológica del Valle de Guadalupe, Municipio de Ensenada, Baja California year: 1997 ident: 3980_CR3 – ident: 3980_CR25 – volume-title: Groundwater year: 1979 ident: 3980_CR19 – volume: 238 start-page: 194 year: 2000 ident: 3980_CR22 publication-title: Journal of Hydrology doi: 10.1016/S0022-1694(00)00331-0 – ident: 3980_CR27 – ident: 3980_CR21 – ident: 3980_CR31 – ident: 3980_CR33 – ident: 3980_CR18 – volume-title: Pozos y acuíferos; Técnicas de evaluación mediante ensayos de bombeo year: 1984 ident: 3980_CR34 |
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SubjectTerms | Agriculture - statistics & numerical data Aquifers Arid zones Artificial recharge Atmospheric Protection/Air Quality Control/Air Pollution California Case studies Cities - statistics & numerical data Climate Conservation of Natural Resources Demand Depletion Drawdown Earth and Environmental Science Ecology Ecotoxicology Environment Environmental Management Environmental Monitoring Extraction Forecasting Groundwater Groundwater - chemistry Groundwater depletion Groundwater discharge groundwater extraction Groundwater flow Groundwater levels Groundwater recharge Hydrologic cycle Hydrologic modeling Mexico Models, Theoretical Monitoring/Environmental Analysis Natural recharge Natural resource management Overdraft Precipitation Pumpage Reduction Semiarid environments semiarid zones Simulation Studies Surface water Valleys Water demand Water management Water Resources - statistics & numerical data Water stress Water supply Water Supply - statistics & numerical data Water table wells |
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Title | Future groundwater extraction scenarios for an aquifer in a semiarid environment: case study of Guadalupe Valley Aquifer, Baja California, Northwest Mexico |
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