4.6 Article

Understanding the processes in a historically relevant thermal and mineral spring water by using mixing and inverse geochemical models

期刊

ENVIRONMENTAL GEOCHEMISTRY AND HEALTH
卷 44, 期 7, 页码 2301-2323

出版社

SPRINGER
DOI: 10.1007/s10653-021-01166-9

关键词

Thermal water; Mineral water; Geochemical models; Water-rock interaction; Mixing; Sustainable water use

资金

  1. Program of Support for Research and Technological Innovation Projects - Programa de apoyo a proyectos de investigacion e inovacion tecnologica (PAPIIT) of the Nacional Autonomous University of Mexico (UNAM) [IN106421]
  2. International Atomic Energy Agency by means of IAEA Research [23189]
  3. Secretaria de Educacion, Ciencia, Tecnologiae Innovacion del Gobierno de la Ciudad de Mexico (SECTEI) [SECTEI/198/2019]

向作者/读者索取更多资源

The thermal mineral water of Penon de los Banos spa in Mexico City has a rich history and is famous for its therapeutic effects. However, heavy groundwater extraction and urban water extractions have led to a drop in water table and changes in chemical composition, affecting the sustainability and therapeutic properties of the spa. Establishing a monitoring program and reducing nearby water extractions are crucial for preserving the thermal water's properties.
The thermal mineral water of Penon de los Banos spa (Mexico City) has been used for over 500 years starting in pre-Hispanic times and is famous for the treatment of various pathologies. It has a temperature of 45 degrees C, which is rich in HCO3,- and its main trace elements are B, Li and Fe, which confers healing effects. Concerns about the sustainability of this important spa have motivated this study to understand the thermal system, possible hydraulic and hydrochemical changes over time and its implications. Stable water isotope data indicate that the thermal water sources originate from local precipitation at Sierra de las Cruces with a recharge elevation of approximately 2770 m above sea level. The recharged water percolates through volcanic and carbonate rock formations and ascends via fault structure conduits, where it eventually is extracted 25 km downstream in Penon de los Banos. During the gravity-driven deep circulation of up to 4.9 km, the groundwater is heated up to 136-160 degrees C. A comparison of past and current water levels and water chemical analyses indicates a water table drop and few variations in the chemical composition, confirming the presence of anthropic impact on water quality. Due to the heavy groundwater extractions in Mexico City, the spring water flow has ceased, and water must be pumped now from a 203-m deep well. In addition, the concentration of bicarbonate, sodium and chloride has been reduced by half since the onset of groundwater development. The therapeutic effects of this thermal mineral water are at risk due to the alteration of the chemical signature. However, new and different therapeutical uses may prevent a future deterioration or closure of this historically important thermal spa. It is crucial to establish a monitoring program of the thermal mineral water and reducing or minimizing nearby urban extractions which tap the regional flow component to preserve the properties of the thermal water.

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