2008
DOI: 10.5038/1827-806x.37.2.2
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Carbon dioxide concentration in air within the Nerja Cave (Malaga, Andalusia, Spain)

Abstract: the CO 2 concentration of the air in the interior and exterior of the Nerja Cave was studied and its relation with the air temperature and visitor number. The average annual CO 2 concentration outside of the cave is 320 ppmv, whilst inside, the mean concentration increases to 525 ppmv during autumn and winter, and in the order of 750 ppmv during spring and summer. The temporal variation of CO 2 content in the air of the cave is strongly influenced by its degree of natural ventilation which is, in turn, determi… Show more

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Cited by 42 publications
(22 citation statements)
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“…The analysis of the data in Table 2 shows that the CO 2 rates were impacted by the human presence, as observed in other studies related to show cave management (e.g. Liñán, Vadillo, & Carrasco, 2008). However, considering the principle of stabilization of the variable after the impact, in Santana cave the CO 2 was not considered the critical atmospheric factor to the cave management.…”
Section: Resultsmentioning
confidence: 74%
“…The analysis of the data in Table 2 shows that the CO 2 rates were impacted by the human presence, as observed in other studies related to show cave management (e.g. Liñán, Vadillo, & Carrasco, 2008). However, considering the principle of stabilization of the variable after the impact, in Santana cave the CO 2 was not considered the critical atmospheric factor to the cave management.…”
Section: Resultsmentioning
confidence: 74%
“…This phenomenon was documented by many studies, e.g., Merenne-Schoumaker (1975), Faimon et al (2006), Liñán et al (2008), Milanolo & Gabrovšek (2009), Šebela et al (2013Šebela et al ( ), or Lang et al (2015. It is generally believed that anthropogenic CO 2 contributes to total cave CO 2 level by the net positive flux derived from visitor exhaling.…”
Section: Introductionmentioning
confidence: 96%
“…Estes mesmos processos possibilitam o acúmulo de CO 2 , quer pelo carreamento de matéria orgânica nos rios -a qual posteriormente entra em decomposição -, quer pelo transporte por águas meteóricas do CO 2 originado no solo acima da caverna (BUECHER, 1999;CARRASCO et al, 2002;LIÑÁN et al, 2008).…”
Section: Caracterização Do Espeleoclimaunclassified