Geochemical and isotopic multi-tracing (delta O-18, delta H-2, delta C-13, Delta C-14) of groundwater flow dynamics and mixing patterns in the volcanoclastic aquifer of the semiarid San Juan del Rio Basin in central Mexico


Por: Hernandez-Perez, Eliseo, Levresse, Gilles, Carrera-Hernandez, Jaime, Inguaggiato, Claudio, Vega-Gonzalez, Marina, Corbo-Camargo, Fernando, Celia Carreon-Freyre, Dora, Billarent-Cedillo, Andrea, Sancen Contreras, Francisco Javier, Ramirez Hernandez, Cynthia Paola

Publicada: 1 nov 2022
Resumen:
Water supply in semiarid areas in Mexico depends on water extraction from compartmentalized aquifers where large drawdown rates can be observed due to increasing demand from urban, industrial and agricultural users. Understanding the behavior of these aquifers is a necessity in order to improve the estimation of water balances. Accordingly, this study assembles both geochemical and isotopic data to identify the source of recharge to the San Juan del Rio graben aquifer and to determine its dynamics. The geological model developed with the aforementioned data reveals a complex system composed of a heterogeneous multilayered compartmentalized aquifer. The San Juan del Rio basin is composed of (1) the Amealco perched aquifer, (2) a shallow granular aquifer, and (3) a fractured aquifer. Hydrogeochemical and isotopic data (delta H-2, delta O-18, delta C-13 and correct carbon activity (Delta C-14)) allow for identification of three end-member sources: (1) local meteoric recharge, (2) old groundwater contained in the siliciclastic shallow aquifer, and (3) regional/local hydrothermal recharge. The contribution of both meteoric and regional hydrogeothermal flow to the different aquifer compartments is determined through a principal component analysis of the hydrogeochemical data. With the aforementioned analysis it was found that the dominant contribution source for all aquifer compartments is meteoric water (up to 60% with a median of 50%), while the regional hydrothermal groundwater contribution represents 15%, even for the shallow aquifer.

Filiaciones:
Hernandez-Perez, Eliseo:
 Univ Nacl Autonoma Mexico, Posgrad Ciencias Tierra, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Mexico

Levresse, Gilles:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Mexico

Carrera-Hernandez, Jaime:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Mexico

Inguaggiato, Claudio:
 Ctr Invest Cient & Educ Super Ensenada CICESE, Dept Geol, Carretera Ensenada Tijuana, Ensenada 3918, Baja California, Mexico

Vega-Gonzalez, Marina:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Mexico

Corbo-Camargo, Fernando:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Mexico

Celia Carreon-Freyre, Dora:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Mexico

Billarent-Cedillo, Andrea:
 Univ Nacl Autonoma Mexico, Posgrad Ciencias Tierra, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Mexico

Sancen Contreras, Francisco Javier:
 Com Tecn Aguas Subterreneas Acuifero San Juan del, Queretaro, Mexico

Ramirez Hernandez, Cynthia Paola:
 Com Tecn Aguas Subterreneas Acuifero San Juan del, Queretaro, Mexico
ISSN: 14312174
Editorial
SPRINGER, 233 SPRING ST, NEW YORK, NY 10013 USA, Estados Unidos America
Tipo de documento: Article
Volumen: 30 Número: 7
Páginas: 2073-2095
WOS Id: 000857684400001

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