Monitoring network of the northwestern coastal aquifer of the State of Yucatan

Categories / Monitoring systems / Geohidrology

Monitoring network of the northwestern coastal aquifer of the State of Yucatan

Principal Investigator: Dr. Roger Pacheco
Dr. Paulo Salles

Description

The Laboratory of Engineering and Coastal Processes (LIPC) and the National Laboratory of Coastal Resilience (LANRESC) established a monitoring network for the coastal northwestern aquifer of the State of Yucatan. The intention is to monitor aquifer heads, and the position and evolution of the saline interface. Currently, it consists of 9 wells, some of them part of the monitoring network of the National Water Commission (CONAGUA). The list of wells is:

   |     P4         |   Nohuayun          
   |    P5          |   Sisal          
   |    P7a        |     UAY Sisal          
   |   P7b         |     Hunucmá        
   |   P8           |     Granja Crío        
   |   P9           |     Torre de Flujos        
   |   SP           |     Sierra Papacal        
   |   B1           |     Ciénega Chuburná        
   |   B9           |     Chuburná       

The location of those wells is shown in Fig 1. Fig 2 shows the stratigraphy between Sisal and Hunucma towns, obtained from well drilling. Figs 3, 4 and 5 show the drilling work of one of our wells, as well as one of our students realizing a salinity profile and some slug tests respectively. Each monitoring site has a pressure, temperature and electrical conductivity loggers (ONSET HoBo), sampling every 30 minutes (48 daily measurements), allowing the observation of daily and seasonal phenomena and processes affecting the aquifer and saline interface. Pressure loggers are installed 2 meters below the mean water table level and electrical conductivity loggers are installed at different depths depending on the well, and the saline interface depth.

The monitoring started in 2017, with the objective of gathering continuous water data to derive information about the functioning of the aquifer and its interaction with the sea. From our data, we have published one work where we analyze the behavior of the saline interface to tides, for example (Canul-Macario 2020).

One example of our measurements is shown in Fig 6. This figure shows the effects in the aquifer caused by the precipitation caused by the storm Cristobal. We can see, the aquifer responds in different locations. If you want to visualize those and other data. Follow the link below. 
https://filedn.com/lvynRc1IcGgVl9iPpJ80vS7/heads.html

Also, Fig 7 show the variation of salinity in a sensor installed 2 meters bellow the well head. If you wat to check out the behavior of the saline interface, in the following links you could access our interactive plots. The numbers in the brackets are the depth of each sensor.
    B1 [B1_S: 1.5 m, B1_I: 6.5 m]
    https://filedn.com/lvynRc1IcGgVl9iPpJ80vS7/ce_b1.html
    B9 [2 m]
    https://filedn.com/lvynRc1IcGgVl9iPpJ80vS7/ce_b9.html
    P7A [P7A_S: 10 m, P7A_M: 11 m, P7S_F: 12 m]
    https://filedn.com/lvynRc1IcGgVl9iPpJ80vS7/ce_p7a.html 
 
We also perform monthly salinity profiles on some of our monitoring wells. If you are interested in this data, please check the following plots.
    B1
    https://filedn.com/lvynRc1IcGgVl9iPpJ80vS7/profiles_B1.html
    B9
    https://filedn.com/lvynRc1IcGgVl9iPpJ80vS7/profiles_B9.html
    P5
    https://filedn.com/lvynRc1IcGgVl9iPpJ80vS7/profiles_P5.html
    P7A
    https://filedn.com/lvynRc1IcGgVl9iPpJ80vS7/profiles_P7A.html

All this data will be used to obtain better and more realistic models and predictions for the behavior of the aquifer. If you require more information, please do not hesitate in contacting us.

Publications and conference proceedings:
  • Canul-Macario, C., Salles, P., Hernández-Espriú, A.,     Pacheco-Castro, R. (2020). Empirical     relationships of groundwater head–salinity response to variations of sea     level and vertical recharge in coastal confined karst aquifers. Hydrogeol J 28, 1679–1694. https://doi.org/10.1007/s10040-020-02151-9 
  • Medina J. (2020). Caracterización geohidrológica del acuífero     de la Duna costera de Sisal, Yucatán. Universidad Autónoma de Yucatán.     Thesis B. Eng. 
  • Pacheco Castro, R., Salles, P., Canul-Macario, C.,     Paladio-Hernández, A. (Submitted). An open water mechanism of seawater intrusion in the northern     Yucatan aquifer. Hydrogeology Journal. 
  • Pacheco Castro, R., Salles, P., Canul-Macario, C.,     Paladio-Hernández, A. (2018).  Flow reversal in the coastal lagoon “La Carbonera” AGU Fall Meeting     2018.  
  •  Canul-Macario,     C., Salles, P., Hernández-Espriu, J. A., & Gonzalez-Herrera, R.     (2018). Simulación numérica de flujo y transporte de solutos de la porción     noroeste del acuífero cárstico península de Yucatán. In U. Nacional &     Salta (Eds.), El Agua Subterránea: Recurso sin Fronteras: Química, Calidad     y Contaminación del Agua. Volumen I. (First edit, pp. 53–60). Salta,     Argentina. 
 

Acknowledgements:
Catedras CONACYT, project 1146 Observatorio costero para estudios de resiliencia al cambio climático.

Gallery

Image min google earth
Fig 1. Zona de estudio: Región Noroeste del Estado de Yucatán (Imagen de Google Earth)
Image min estratigrafia
Fig 2. Estratigrafía del transecto Hunucmá - Sisal.
Image min image pozo 02
Fig 3. Trabajos de perforación de pozos.
Image min image pozo 05
Fig 4. Perfiles de Salinidad.
Image min pozo 07
Fig 5. Slug test, realizado en algunos pozos.
Image min cristobal
Fig 6. Niveles piezométricos durante la tormenta cristobal.
Image min salinidad b9
Fig 7. Salinidad en el pozo B9.

PDF Files


Guia uso html

Contact the principal investigator