dor_id: 4120345

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336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://www.investigacionesgeograficas.unam.mx/index.php/rig/index

351.#.#.b: Investigaciones Geográficas

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

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

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856.4.0.u: http://www.investigacionesgeograficas.unam.mx/index.php/rig/article/view/18364/17436

100.1.#.a: Ortiz Zamora, Dalia Del Carmen

524.#.#.a: Ortiz Zamora, Dalia Del Carmen (2007). Origin and evolution of a new lake in the Chalco plain: implications for land subsidence and flooding hazards to the urban areas of Valle de Chalco (State of Mexico) and Tláhuac (Federal District). Investigaciones Geográficas; Núm. 64. Recuperado de https://repositorio.unam.mx/contenidos/4120345

245.1.0.a: Origin and evolution of a new lake in the Chalco plain: implications for land subsidence and flooding hazards to the urban areas of Valle de Chalco (State of Mexico) and Tláhuac (Federal District)

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

561.1.#.a: Instituto de Geografía, UNAM

264.#.0.c: 2007

264.#.1.c: 2023-09-12

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 4.0 Internacional, https://creativecommons.org/licenses/by-nc/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico dianachg@igg.unam.mx

884.#.#.k: http://www.investigacionesgeograficas.unam.mx/index.php/rig/article/view/18364

001.#.#.#: 073.oai:ojs.pkp.sfu.ca:article/18364

041.#.7.h: spa

520.3.#.a: Groundwater extraction from fourteen wells in the Chalco plain since the 1980´s, the Mixquic-Santa Catarina System (MSCS), located at the southeast of Mexico City, is causing one of the more important environmental changes of the landscape within the Basin of Mexico in the last two decades. In the middle of the plain, where the thickness of the lacustrine sediments is the highest (300 m), land subsidence of 40 cm/year has occurred as a result of the transient aquitard response to pumping in the underlying main aquifer. A new lake is developing in this topographic depression due to the accumulation of surface water; the shape of the lake is being controlled by the distribution and geometry of a basalt layer that is present within the lacustrine sequence at 50 m depth, originated at the Sierra Santa Catarina. The New Chalco Lake surface is located 12 m below the original position of ground surface, covering a total extension of 1 000 ha. Based on the controls and magnitude of the regional land subsidence, it is expected that the lake surface will grow about 1 500 ha by the year 2015, increasing the risk of flooding to the urban areas of Valle de Chalco and Tlahuac. To reduce the danger and risk of land subsidence and flooding, there is necessary to analyze the convenience to increase the amount and efficiency of the hydraulic infrastructure in the future against the option relocate particular urban areas, within a radius of 2.5 to 3 km with center in the well P9 of the MSCS. The creation of a Metropolitan Council would permit to define dynamic and integral strategies for territory planning, and in particular for prevention of disasters, and the adequate equilibrium between the planning of proposed conservation areas and the environmental improvement with the reduction or mitigation of risk.

773.1.#.t: Investigaciones Geográficas; Núm. 64

773.1.#.o: http://www.investigacionesgeograficas.unam.mx/index.php/rig/index

022.#.#.a: ISSN electrónico: 2448-7279; ISSN impreso: 0188-4611

310.#.#.a: Cuatrimestral

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

doi: https://doi.org/10.14350/rig.18364

handle: 0082bd9e3efac5cc

harvesting_date: 2023-08-23 17:00:00.0

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245.1.0.b: Origen y evolución de un nuevo lago en la planicie de Chalco: Implicaciones de peligro por subsidencia e inundación de áreas urbanas en Valle de Chalco (Estado de México) y Tláhuac (Distrito Federal)

last_modified: 2023-08-23 17:00:00

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license_type: by-nc

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Artículo

Origin and evolution of a new lake in the Chalco plain: implications for land subsidence and flooding hazards to the urban areas of Valle de Chalco (State of Mexico) and Tláhuac (Federal District)

Ortiz Zamora, Dalia Del Carmen

Instituto de Geografía, UNAM, publicado en Investigaciones Geográficas, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geografía, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Ortiz Zamora, Dalia Del Carmen (2007). Origin and evolution of a new lake in the Chalco plain: implications for land subsidence and flooding hazards to the urban areas of Valle de Chalco (State of Mexico) and Tláhuac (Federal District). Investigaciones Geográficas; Núm. 64. Recuperado de https://repositorio.unam.mx/contenidos/4120345

Descripción del recurso

Autor(es)
Ortiz Zamora, Dalia Del Carmen
Tipo
Artículo de Investigación
Área del conocimiento
Ciencias Sociales y Económicas
Título
Origin and evolution of a new lake in the Chalco plain: implications for land subsidence and flooding hazards to the urban areas of Valle de Chalco (State of Mexico) and Tláhuac (Federal District)
Fecha
2023-09-12
Resumen
Groundwater extraction from fourteen wells in the Chalco plain since the 1980´s, the Mixquic-Santa Catarina System (MSCS), located at the southeast of Mexico City, is causing one of the more important environmental changes of the landscape within the Basin of Mexico in the last two decades. In the middle of the plain, where the thickness of the lacustrine sediments is the highest (300 m), land subsidence of 40 cm/year has occurred as a result of the transient aquitard response to pumping in the underlying main aquifer. A new lake is developing in this topographic depression due to the accumulation of surface water; the shape of the lake is being controlled by the distribution and geometry of a basalt layer that is present within the lacustrine sequence at 50 m depth, originated at the Sierra Santa Catarina. The New Chalco Lake surface is located 12 m below the original position of ground surface, covering a total extension of 1 000 ha. Based on the controls and magnitude of the regional land subsidence, it is expected that the lake surface will grow about 1 500 ha by the year 2015, increasing the risk of flooding to the urban areas of Valle de Chalco and Tlahuac. To reduce the danger and risk of land subsidence and flooding, there is necessary to analyze the convenience to increase the amount and efficiency of the hydraulic infrastructure in the future against the option relocate particular urban areas, within a radius of 2.5 to 3 km with center in the well P9 of the MSCS. The creation of a Metropolitan Council would permit to define dynamic and integral strategies for territory planning, and in particular for prevention of disasters, and the adequate equilibrium between the planning of proposed conservation areas and the environmental improvement with the reduction or mitigation of risk.
Idioma
spa
ISSN
ISSN electrónico: 2448-7279; ISSN impreso: 0188-4611

Enlaces