EGU2020-7483
https://doi.org/10.5194/egusphere-egu2020-7483
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Borehole-based study of CO2-rich air transport in the vadose zone of a Mediterranean karst system (Malaga, southern Spain)

Lucía Ojeda1, José Benavente2,3, Iñaki Vadillo1, Cristina Liñán1,4, and Enrique P. Sanchez-Cañete5,6
Lucía Ojeda et al.
  • 1Group of Hydrogeology, Faculty of Science, University of Málaga, 29071, Málaga, Spain (luciaor@uma.es)
  • 2Department of Geodynamics, University of Granada, 18071, Granada, Spain
  • 3Water Institute, University of Granada, 18071, Granada, Spain
  • 4Research Institute, Nerja Cave Foundation, Maro road s/n, 29787, Nerja, Málaga, Spain
  • 5Department of Applied Physics, University of Granada, 18071, Granada, Spain
  • 6Centro Andaluz de Medio Ambiente (IISTA-CEAMA), Granada, Spain

The characterization of CO2 transport, and other C compounds (CH4, DIC, organic matter, etc.), in the vadose zone of a karst aquifer is key in order to quantify sources and sinks of carbon. In karst environments, most of the studies are focused on the dynamics of CO2 in caves, but only a few studies are related to field measurements of the CO2 content in boreholes, which provides direct insights about the vadose zone. Located at the east of the Nerja Cave (Malaga, Andalusia), one of the most important tourist caves in Spain, the vadose zone was accessed by 9 boreholes drilled into the vadose zone of a Triassic carbonate aquifer, with depths ranging between 15 and 30 m. The karst network in the study area is characterized by a great vertical heterogeneity, with significant cavities and voids at specific intervals. Groundwater levels at different altitudes are a consequence of this heterogeneity. Similarly, CO2 distribution and transport are clearly determined by the complex karst network.

Our study aims to identify significant horizontal gradients of CO2 in the karst vadose air, both spatial and temporally. We present monthly measurements of CO2 concentration, relative humidity, air temperature and 222Rn inside boreholes. In addition, we present CO2 results from an 18 hours-atmospheric air injection test. Linking them to the geophysical knowledge of voids in the study area, the results allow us to identify lateral fluxes of CO2-rich air in the vadose zone and how these fluxes are favoured by the incidence of the main karst discontinuity orientations. We observe different ventilation patterns:  in spring the vadose air seems to be stored in specific orientations, while in summer there is a lower convective ventilation. The results contribute to explain the temporal variations of the chemical composition of recharge water in karst systems, as well as to support studies on the global carbon budget.

How to cite: Ojeda, L., Benavente, J., Vadillo, I., Liñán, C., and P. Sanchez-Cañete, E.: Borehole-based study of CO2-rich air transport in the vadose zone of a Mediterranean karst system (Malaga, southern Spain), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7483, https://doi.org/10.5194/egusphere-egu2020-7483, 2020