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Moravian Karst, Czech International Journal of Speleology 46 (3) 345-358 Tampa, FL (USA) September 2017 Available online at scholarcommons.usf.edu/ijs International Journal of Speleology Off icial Journal of Union Internationale de Spéléologie The impact of door opening on CO2 levels: A case study from the Balcarka Cave (Moravian Karst, Czech Republic) Marek Lang1*, Jiří Faimon1,2, and Sandra Kejíková1 1Department of Geological Sciences, Faculty of Sciences, Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic 2Department of Geology, Faculty of Science, Palacký University Olomouc, 17. listopadu 1192/12, 771 46 Olomouc, Czech Republic Abstract: The impact of door opening on cave carbon dioxide (CO2) levels was studied in the Entrance Chamber and the Gallery Chamber of the Balcarka Cave (Moravian Karst, Czech Republic). The effect of door opening differed with cave ventilation modes. Under upward airflow mode, the cave door opening led to the increase of output advective CO2 fluxes from the cave and to the decrease of CO2 levels. This effect was evident especially in the Entrance Chamber near the cave entrance and then suppressed in the Gallery Chamber situated deeper in the cave. Under the downward airflow mode, the cave door opening changed airflow paths and main CO2 sources/fluxes. This resulted in the increase of CO2 level in the Entrance Chamber while the levels in the Gallery Chamber decrease. Modeling indicates that the increase could -2 -1 be result of input advective CO2 fluxes from epikarst (up to 5.9 × 10 mol s ). To reduce the impact on cave microclimate, a careful control of the visiting regime without overlapping of individual doors’ openings is recommended. Keywords: cave chamber, CO2 levels, cave ventilation, door opening, advective CO2 flux Received 6 December 2016; Revised 29 April 2017; Accepted 29 April 2017 Citation: Lang M., Faimon J. and Kejíková S., 2017. The impact of door opening on CO2 levels: A case study from the Balcarka Cave (Moravian Karst, Czech Republic). International Journal of Speleology, 46 (3), 345-358. Tampa, FL (USA) ISSN 0392-6672 https://doi.org/10.5038/1827-806X.46.3.2100 LIST OF SYMBOLS PCO2 carbon dioxide partial pressure [dimensionless] (C) PCO2 carbon dioxide partial pressure in cave A total diffusion area [m2] atmosphere [dimensionless] -3 (H) cCO2 carbon dioxide concentration [mol m ] PCO2 hypothetical PCO2 reconstructed from cave cEK carbon dioxide concentration in soils/epikarst dripwater chemistry [dimensionless] -3 (W) [mol m ] PCO2 carbon dioxide partial pressure in water cGal carbon dioxide concentration in Gallery [dimensionless] Chamber [mol m-3] t time [s] Δc difference in carbon dioxide concentrations T temperature [°C] -3 [mol m ] Tcave temperature in cave atmosphere [°C] 2 -1 D carbon dioxide diffusion coefficient [m s ] Texterior temperature in external atmosphere [°C] j total carbon dioxide flux [mol s-1] DT temperature difference [°C] -1 -1 jadv input advective carbon dioxide flux [mol s ] v linear airflow rate [m s ] 3 jdeg input carbon dioxide flux derived from one V cave total volume [m ] liter of dripwater by degassing [mol s-1] EK jdif total input diffusive carbon dioxide flux from ABBREVIATIONS soils/epikarst [mol s-1] EK jadv input advective carbon dioxide flux from C1-UAF campaign 1; upward airflow soils/epikarst [mol s-1] C2-DAF campaign 2; downward airflow Gal jadv input advective carbon dioxide flux from C3-DAF campaign 3; downward airflow Gallery Chamber [mol s-1] C4-DAF campaign 4; downward airflow DL overburden thickness [m] CC Chimney Chamber P barometric pressure [Pa] CD connecting door 3 -1 Q volumetric airflow rate [m s ] CO2 carbon dioxide R the universal gas constant [J kg-1 K-1] DAF mode downward airflow ventilation mode *[email protected] The author’s rights are protected under a Creative Commons Attribution- NonCommercial 4.0 International (CC BY-NC 4.0) license. 346 Lang et al. DMC-DAF detailed monitoring campaign; opening during visiting hours, which could contribute downward airflow to changes in the cave ventilation and consequently in EC Entrance Chamber CO2 levels. The goal of this work was to verify in detail GC Gallery Chamber the impact of cave door opening on (i) cave ventilation UAF mode upward airflow ventilation mode and (ii) cave CO2 levels based on a case study in the Balcarka Cave (Moravian Karst). INTRODUCTION METHODS Carbon dioxide (CO2) is an important component of the global carbon cycle (e.g., Schlesinger & Andrews, Site of study 2000) and plays important role in many karst The Balcarka Cave is situated in the northern part of processes such as limestone dissolution (e.g., Stumm the Moravian Karst near the Ostrov u Macochy village & Morgan, 1996), calcite speleothem formation (e.g., (Faimon et al., 2012a; Lang et al., 2015a, b). The position Dreybrodt, 1999; Banner et al., 2007; Frisia et al., and sketch map of the cave are illustrated in Fig. 1A. 2011), or speleothem corrosion (e.g., Sarbu & Lascu, Mean annual precipitation in the study area is about 1997; Dublyandsky & Dublyansky, 1998; Tarhule- 700 mm; mean annual temperature of the external Lips & Ford, 1998; Faimon et al., 2006). The difference atmosphere is about 10°C (Pracný et al., 2016a). between the CO2 partial pressures in (1) soil/upper The cave has been formed in the Upper Devonian (H) (C) epikarst, PCO2, and (2) cave atmosphere, PCO2, limestones of the Macocha Formation. It consists represents the driving force for these processes (White, of a two-level complex of relatively narrow corridors 1988; Ford & Williams, 2007). Some studies showed (total length of about 350 m) and the chambers. The (H) that hypothetical PCO2 values could be reconstructed cave is known for rich speleothem decoration of all from cave dripwater hydrogeochemistry (Faimon et al., types: stalactites/stalagmites, flowstones, curtains, 2012c; Peyraube et al., 2013; Milanolo & Gabrovšek, and thick-walled soda straws. The height distance 2015; Pracný et al., 2016a, b). Generally, enhanced between both cave levels is about 20 m. The thickness (H) PCO2 (Fairchild et al., 2000; Faimon et al., 2012c) of cave rock overburden is about 20-50 m (Fig. 1B). is responsible for limestone dissolution and cave The cave has three entrances equipped by steel doors: (C) development (Baldini et al., 2006). The lower PCO2 the main entrance #1 is at 459.3 m above sea level controls dripwater degassing and calcite precipitation (a.s.l.), the old cave exit #3 at 457.5 m a.s.l., and the (speleothem growth) (Holland et al., 1964). new cave exit #4 at 446.9 m a.s.l. (Fig. 1B). Additional It is well known that the environment of show doors, the door #2 and the connecting door (CD) caves is significantly influenced by (1) human activity separate the input cave portal from the Entrance derived from the works required for ensuring the Chamber and the Chimney Chamber, respectively access of cave visitors, and by (2) presence of visitors (Fig. 1). Note that only doors #1 (entrance into the inside the cave. The anthropogenic impact in show cave), #2 (input to the Entrance Chamber) and #4 caves was documented by many studies focused on (exit from the cave) are used during visitor tours, (i) temperature (e.g., Pulido-Bosch et al., 1997; de doors #3 and CD were opened only for the purpose Freitas & Schmekal, 2006; Šebela & Turk, 2014), (ii) of the experimental monitoring. In addition to the CO2 concentrations (Faimon et al., 2006; Liñán et al., known entrances, some hidden/unknown openings 2008; Milanolo & Gabrovšek, 2009; Šebela et al., 2013; undoubtedly exist in the cave. All the entrances/ Lang et al., 2015a), and (iii) both the components openings in distinct altitudes are responsible for the above (e.g., Hoyos et al., 1998; Sánchez-Moral et al., dynamic behavior of cave air circulation. A theoretical 1999; de Freitas, 2010). In addition, there were some background on cave air circulation was given by attempts to summarize the principles of optimum cave Cigna (1968) and Wigley & Brown (1971). Several management and cave environment conservation (e.g., studies on artificial systems (e.g., Richon et al., Fernández et al., 1986; Calaforra et al., 2003; Lario & 2005) can also be useful for the better understanding Soler, 2010; Lobo, 2015; Lang et al., 2017). In addition natural systems. The cave airflows principally depend to former “standard” phenomena, so-called “parasitic on (1) cave geometry and (2) the pressure difference phenomena” may also be recognized in caves. This resulting from contrasting air densities (de Freitas et term was adopted from electrical engineering. It al., 1982; Kowalczk & Froelich, 2010). Since density represents various adverse phenomena that distort is primarily a function of temperature, cave airflows time series of basic variables. In cave environment, are mostly related to the temperature difference such phenomena could be associated especially between external and cave atmospheres, ΔT = Texterior – with temporary anthropogenic interventions into Tcave (where Texterior is external air temperature and Tcave the cave microclimate. As an example, Lang et al. is cave air temperature [°C]) (Baker & Genty, 1998; (2015b) recently presented the study of the visitor Bourges et al., 2001; Spötl et al., 2005; Faimon et movement in low-profile passages that affect cave al., 2012a; Faimon & Lang, 2013). Based on sign of ventilation and disturb or even make inverse the the temperature difference, two ventilation regimes CO2 level evolution. Another similar phenomenon are distinguished. When ΔT < 0, upward airflows is linked to door opening. The caves made available occur and cave is in the upward airflow ventilation to tourists are often equipped with doors to protect mode (UAF mode). If ΔT > 0, the cave airflow direction cave microclimate. However, the high attendance in is opposite; this corresponds to the downward show caves is associated with the frequent cave door airflow ventilation mode (DAF mode) (see Faimon et International Journal of Speleology, 46 (3), 345-358.
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