Geochemical and isotopic multi-tracing (δ18O, δ2H, δ13C, Δ14C) of groundwater flow dynamics and mixing patterns in the volcanoclastic aquifer of the semiarid San Juan del Río Basin in central Mexico

Hernández-Pérez, Eliseo; Levresse, Gilles; Carrera-Hernández, J. J.; Inguaggiato, Claudio; Vega-González, Marina; Corbo-Camargo, Fernando; Carreón‐Freyre, Dora; Billarent-Cedillo, Andrea; Contreras, Francisco Javier Sancén; Hernández, Cynthia Paola Ramírez

doi:10.1007/s10040-022-02536-y

Cited by 5 publications

(3 citation statements)

References 50 publications

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“…A unique pattern of high-value TDS was found in the southeastern section ranging from 301 to 450 ppm and 450 to 600 ppm, influenced by connate water traps. TDS results with similar values of 9.4 to 796 ppm as the study location were found in the Mexican volcanoclastic aquifer (Hernández-Pérez et al, 2022). Different TDS values with a larger range of 302 to 1,583 ppm (Morales-Casique, 2012), 149 to 1,693 ppm (Bellia et al, 2015), 287 to 1,814 ppm (Furi et al, 2012), 546 to 2,412 ppm (Parisi et al, 2011), 166 to 4,723 ppm (Afsin et al, 2014), and 118 to 5,342 ppm (Minnisale et al, 1997, are found in Popocatépetl volcano, Mexico, Mt Etna Italy, Fantale Volcano, Ethiopia, Mt Vulture, Italy, Hasandagi Volcano, Turkey, and Amiata Volcano, Italy respectively.…”

Section: Resultssupporting

confidence: 81%

“…A different pattern is also found in Italy's Cimono Volcano from the dominant upstream facies Ca ӓ Na > K > Mg to Ca ӓ Na > Mg > K at the foot of the volcano with the same value at HCO 3 > > Cl > SO 4 (Piscopo et al, 2018). Other different results were also found in the upstream Mexican volcanoclastic aquifer, dominated by Ca-Na-HCO 3 >, hence the richer the valley, the more prosperous the Cl-NO-SO 4 and Na/K-HCO 3 -Cl-SO 4 (Hernández-Pérez et al, 2022). Different facies patterns are also found in Hasandagi Volcano, Turkey, with upstreamdownstream sequences Na-Ca-Mg-HCO 3 > Ca-Mg-HCO 3 > Ca-Na-HCO 3 -Cl (Afsin et al, 2014).…”

Section: Hydrogeochemical Facies Analysis Using the Kurlov Classifica...mentioning

confidence: 83%

“…A different pattern of fingerprint diagrams is found in the Mt Fuji Japan volcanic aquifer, which predominantly has Ca and HCO 3 from the volcano's upper-middle and the foot slopes of Mg SO 4 , Na+K, and Cl values (Ono et al, 2019). The volcanoclastic aquifer of the semiarid San Juan del Río Basin was found in central Mexico with dominant ions in the form of Na+K and HCO 3 +CO 3 (Hernández-Pérez et al, 2022). Different results were also found in volcanic-sedimentary aquifers in central Italy with dominant ion diagrams of Na and HCO 3 +CO 3 (Vivona et al, 2007).…”

Section: Hydrogeochemical Analysis Using the Fingerprint Diagrammentioning

confidence: 96%

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Groundwater Chemistry Characterization in the South and Southeast Merapi Volcano, Indonesia

Hendrayana

Harijoko

Riyanto

et al. 2022

IJG

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Merapi Volcano, which differs from volcanoes in other climates due to its location on the Indonesian Maritime Continent influenced by ENSO, ICTZ, and Moonsons, plays an essential role as a source of groundwater for the surrounding population. Some problems associated with groundwater in Mount Merapi are high utilization compared to other volcanoes worldwide, changes in land use, pollution, and its lowering table. Therefore, this study aims to compare the hydrogeological characteristics and aquifer systems of the southern and southeastern parts of Merapi Volcano. The hydrogeological characteristics were obtained from geological mapping, surface and subsurface, as well as rock XRF tests. Meanwhile, the hydrogeochemical characterization was determined through chemical data using the Trilinear Piper, Kurlov, Fingerprint, Composition, and Harker Diagram methods. The results of the Trilinear Piper, Kurlov, Fingerprint, and Composition Diagram methods show that Mount Merapi has 3, 7, 4, and 2 types of patterns different from other volcanoes in the world. On the other hand, the Harker diagram has the same pattern of Mg-Ca and Mg-Na as several other volcanoes. In conclusion, the hydrostratigraphy in the southern part of the volcano, consists of aquifuge, aquiclude, and aquifer, while in the southeast, there are aquitards of volcanic sandstone and tuff.

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Section: Resultssupporting

confidence: 81%

Section: Hydrogeochemical Facies Analysis Using the Kurlov Classifica...mentioning

confidence: 83%

Section: Hydrogeochemical Analysis Using the Fingerprint Diagrammentioning

confidence: 96%

See 1 more Smart Citation

Groundwater Chemistry Characterization in the South and Southeast Merapi Volcano, Indonesia

Hendrayana

Harijoko

Riyanto

et al. 2022

IJG

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Evaluation des processus de recharge d’un système aquifère peu profond et profond (vallée du Maggiore, nord-ouest de l’Italie): approche hydrogéochimique et isotopique

Cocca,

Lasagna,

Marchina

et al. 2023

Hydrogeol J

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The Maggiore Valley well field plays a fundamental role in supplying drinking water to a large territory of the Piedmont Region (northwestern Italy) and has been intensively exploited since the early twentieth century. This water resource is hosted in a deep, multilayered aquifer system. The main purpose of this study was to characterize the recharge processes of the deep aquifer through hydrochemical and isotopic assessments, as well as the water quality in the recharge and drainage areas. For this purpose, 128 physical–chemical analyses (major ions) and 50 isotopic analyses (δ18O and δ2H) were carried out on samples collected in shallow and deep aquifer complexes in two sampling campaigns in 2021. From the results, a hydrogeological conceptual model of recharge processes was developed. The chemical data confirm the presence of bicarbonate–calcium facies in most samples of the shallow and deep aquifer complexes. Clear hydrochemical differences were observed among the investigated sectors. The recharge areas were identified as (1) far zones, namely the shallow aquifer complex of the Cuneo Plain, and (2) the shallow and deep aquifer complexes with groundwater mixing in the riverside sector of Po Plain in the Turin area. The mixing of waters from the Cuneo Plain and Turin Plain was verified in the well field area. The isotopic values of the artesian well water also confirmed contributions from the Turin and Cuneo Alps. This study clarified the recharge processes, thereby defining potential pollutant pathways, and the results provide additional support for groundwater resource management and protection.

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Identification of recharge processes and mixing patterns by using CFC's and isotopic multi-tracing (δ18O, δ2H) of groundwater in a stratified volcanoclastic aquifer of the semiarid Amazcala Basin in Central Mexico

Hernández-Pérez,

Levresse,

Carrera-Hernandez

et al. 2023

Applied Geochemistry

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Geochemical and isotopic multi-tracing (δ18O, δ2H, δ13C, Δ14C) of groundwater flow dynamics and mixing patterns in the volcanoclastic aquifer of the semiarid San Juan del Río Basin in central Mexico

Cited by 5 publications

References 50 publications

Groundwater Chemistry Characterization in the South and Southeast Merapi Volcano, Indonesia

Groundwater Chemistry Characterization in the South and Southeast Merapi Volcano, Indonesia

Evaluation des processus de recharge d’un système aquifère peu profond et profond (vallée du Maggiore, nord-ouest de l’Italie): approche hydrogéochimique et isotopique

Identification of recharge processes and mixing patterns by using CFC's and isotopic multi-tracing (δ18O, δ2H) of groundwater in a stratified volcanoclastic aquifer of the semiarid Amazcala Basin in Central Mexico

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