Seasonal ventilation patterns in Cueva Larga (Sierra de los Filabres, Almería, SE Spain))
DOI:
https://doi.org/10.55407/geogaceta104506Keywords:
cave monitoring, cave ventilation, radon, methaneAbstract
Speleothems are useful archives for paleoclimate reconstructions. However, environmental monitoring of cave atmosphere is necessary to understand underground ventilation dynamics, ensuring accurate interpretation of geochemical results obtained from stalagmites. This study focuses on the environmental monitoring of Cueva Larga (Sierra de los Filabres, Almería). Both the external (rainfall and temperature) and the in cave atmosphere (temperature, relative humidity, CO2, CH4 and 222Rn contents) were monitored over a one year period. The cave was highly ventilated over the monitoring period, as shown by relatively low levels of 222Rn (~ 160 Bq/m3) and CO2 (~ 490 ppm). However, we observed that intervals of less ventilation occur (222Rn up to 300 Bq/m3), coinciding with high relative humidity conditions. This is due to the low convective air circulation and the partial saturation of fractures in the cave ceiling, resulting in decreased exchange of gases with the exterior.
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Copyright (c) 2024 Elvira Ruiz Caballero, Fernando Gázquez, Ángel Fernández-Cortés, José María Calaforra

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