First assessment on the air CO2 dynamic in the show caves of tropical karst, Vietnam

In this study, air, water, and host rock in show caves in a Vietnam’s karst region was monitored and analyzed to identify the ventilation regime and track the cave air CO2 sources. In general, the studied caves are well ventilated. In dynamic – multiple entrance caves, air ventilation is described w...

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Main Authors: Duc A. Trinh, Quan H. Trinh, Angel Fernández-Cortés, David Mattey, Javier G. Guinea
Format: Article
Language:English
Published: University of South Florida Libraries 2018-01-01
Series:International Journal of Speleology
Subjects:
Online Access:http://scholarcommons.usf.edu/ijs/vol47/iss1/8/
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author Duc A. Trinh
Quan H. Trinh
Angel Fernández-Cortés
David Mattey
Javier G. Guinea
author_facet Duc A. Trinh
Quan H. Trinh
Angel Fernández-Cortés
David Mattey
Javier G. Guinea
author_sort Duc A. Trinh
collection DOAJ
description In this study, air, water, and host rock in show caves in a Vietnam’s karst region was monitored and analyzed to identify the ventilation regime and track the cave air CO2 sources. In general, the studied caves are well ventilated. In dynamic – multiple entrance caves, air ventilation is described with the use of U shape model. In static – single entrance cave, air circulation is explained by cold air trap model. Both ventilation models suggest that air is more circulated in winter than in summer. Seasonally, the cave air CO2 increases from early spring to summer. Value in the deepest part of the single-entrance cave is approximately 1,000 ppmv and 8,000 ppmv in early spring and summer, respectively. In multiple-entrance and wet caves, CO2 level is fairly constant all over the show section, increasing from 500 ppmv in early spring to 2,000 ppmv in summer. Data of microclimate, CO2 content, and particularly δ13C show that cave air, particularly in single entrance cave, has higher CO2 concentration during summer due to a stagnation of cave air circulation and an elevated CO2 input from soil and epikarst. The cave air CO2 increase is also observed after intense rainfalls. A factor that increase cave air CO2 in show caves during the festive days could probably be huma n exhaling but the extent of human factor in these studied cave systems should be further investigated. Cave waters including cave pools and streams mediate CO2 level in wet caves. Above all, the atmospheric fraction of CO2 is always dominant (>60%) in all cave sections.
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spelling doaj.art-d73ce2e7d995421b80fee30c6d675ee92022-12-21T19:15:44ZengUniversity of South Florida LibrariesInternational Journal of Speleology0392-66721827-806X2018-01-014719311210.5038/1827-806X.47.1.2141First assessment on the air CO2 dynamic in the show caves of tropical karst, VietnamDuc A. Trinh0Quan H. Trinh1Angel Fernández-Cortés2David Mattey3Javier G. Guinea4Vietnam Atomic Energy InstituteInstitute of Chemistry, Vietnam Academy of Science and TechnologyUniversidad de AlmeríaRoyal Holloway University of LondonMuseo Nacional Ciencias Naturales (MNCN)In this study, air, water, and host rock in show caves in a Vietnam’s karst region was monitored and analyzed to identify the ventilation regime and track the cave air CO2 sources. In general, the studied caves are well ventilated. In dynamic – multiple entrance caves, air ventilation is described with the use of U shape model. In static – single entrance cave, air circulation is explained by cold air trap model. Both ventilation models suggest that air is more circulated in winter than in summer. Seasonally, the cave air CO2 increases from early spring to summer. Value in the deepest part of the single-entrance cave is approximately 1,000 ppmv and 8,000 ppmv in early spring and summer, respectively. In multiple-entrance and wet caves, CO2 level is fairly constant all over the show section, increasing from 500 ppmv in early spring to 2,000 ppmv in summer. Data of microclimate, CO2 content, and particularly δ13C show that cave air, particularly in single entrance cave, has higher CO2 concentration during summer due to a stagnation of cave air circulation and an elevated CO2 input from soil and epikarst. The cave air CO2 increase is also observed after intense rainfalls. A factor that increase cave air CO2 in show caves during the festive days could probably be huma n exhaling but the extent of human factor in these studied cave systems should be further investigated. Cave waters including cave pools and streams mediate CO2 level in wet caves. Above all, the atmospheric fraction of CO2 is always dominant (>60%) in all cave sections.http://scholarcommons.usf.edu/ijs/vol47/iss1/8/Phong Nha – Ke Bangmicroclimatecave air ventilationsoil air CO 2human exhaling
spellingShingle Duc A. Trinh
Quan H. Trinh
Angel Fernández-Cortés
David Mattey
Javier G. Guinea
First assessment on the air CO2 dynamic in the show caves of tropical karst, Vietnam
International Journal of Speleology
Phong Nha – Ke Bang
microclimate
cave air ventilation
soil air CO 2
human exhaling
title First assessment on the air CO2 dynamic in the show caves of tropical karst, Vietnam
title_full First assessment on the air CO2 dynamic in the show caves of tropical karst, Vietnam
title_fullStr First assessment on the air CO2 dynamic in the show caves of tropical karst, Vietnam
title_full_unstemmed First assessment on the air CO2 dynamic in the show caves of tropical karst, Vietnam
title_short First assessment on the air CO2 dynamic in the show caves of tropical karst, Vietnam
title_sort first assessment on the air co2 dynamic in the show caves of tropical karst vietnam
topic Phong Nha – Ke Bang
microclimate
cave air ventilation
soil air CO 2
human exhaling
url http://scholarcommons.usf.edu/ijs/vol47/iss1/8/
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