In the area north of Lake Kivu, in the western part of the African Rift, deep fractures allow the uptake of gas, especially carbon dioxide. The Nyiragongo territory is located in the western part of the African Rift Valley. The deep fractures allow gases, especially carbon dioxide (CO2), to rise. CO2 is a heavier-than-air gas, asphyxiating, irritating to the eyes, nose and throat, and deadly at concentrations above 15%. The variation of CO2 in the different stations allows us to study the behaviour of the Nyiragongo volcano although in our stations we have not reached the lethal concentration of CO2. The volcanic activity of Nyiragongo is therefore closely monitored by the inhabitants, and any news of increased activity agitates the inhabitants of the region, especially those living in the Nyiragongo territory. Here we report a short carbon dioxide monitoring time series for five stations (BUGARURA I, II, III, IV and MUNIGI stations). The various variations in CO2 give us information about the activity of the Nyiragongo Volcano in the crater. The active volcanoes of the Virunga chain expose the Nyiragongo region to numerous natural hazards such as lava flows, gas plumes, dissolved gases in Lake Kivu and risks related to epidemiological diseases and armed conflicts.
Published in | International Journal of Natural Resource Ecology and Management (Volume 6, Issue 2) |
DOI | 10.11648/j.ijnrem.20210602.12 |
Page(s) | 38-41 |
Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
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Copyright © The Author(s), 2021. Published by Science Publishing Group |
Monitoring, Carbon Dioxide, Crack, Volcano
[1] | AMARAL A. F. S., RODRIGUES A. S. (2011). Volcanogenic Contaminants: Chronic Exposure; Reference Module in Earth Systems and Environmental Sciences. Encyclopedia of Environmental Health, 681-689. |
[2] | BALAGIZI C. M., YALIRE M. M., CIRABA H. M., KAJEJE V. B., MINANI A. S., KINJA A. B., KASEREKA M. M. (2016). Soil temperature and CO2 degassing, SO2 fluxes and field observations before and after the February 29, 2016 new vent inside Nyiragongo crater. Bull. Of Volcanol., 78: 64. |
[3] | BAXTER P. J., BAUBRON J. C., COUNTINHO R. (1999). Health hazards and disaster potential of ground gas emissions at Furnas volcano, Sao Miguel, Azores. J. Volcanol. Geoth. Res. 92: 95-106. |
[4] | BAXTER P. J. (2011). Volcanoes and Human Health. Reference Module in Earth Systems and Environmental Sciences. |
[5] | BEAUBIEN S. E., CIOTOLI G., LOMBARDI S. (2003). Carbon dioxide and radon gas hazard in the Alban Hills area (central Italy). J VolcanolGeotherm Res; 123 (1), 63-80. doi: 10.1016/S0377-0273(03)00028-3. |
[6] | BLONGR. J. (1984). Volcanic hazards. A sourcebook on the effects of eruptions. Academic Press. 424p. |
[7] | CANTRELL L., Young M. (2009). Fatal fall into a volcanic fumarole. Wilderness Environ Med. 20 (1), 77-79, doi: 10.1580/08-WEME-CR-199.1. |
[8] | GRANIERI, D.; CARAPEZZA, M. L.; BARBERI, F.; RANALDI, M.; RICCI, T.; TARCHINI, L. (2014). Atmospheric dispersion of natural carbon dioxide emissions on Vulcano Island, Italy. |
[9] | HANSELL A., OPPENHEIMER C. (2004). Health hazards from volcanic gases: a systematic literature review. Arch Environ Health 2004; 59 (No. 12): 628–39. |
[10] | HATHAWAY G. L., PROCTOR N. H., HUGHES J. P., FISCHMAN M. L. (1991). Proctor and Hughes' chemical hazards of the workplace, 3rd edn, Van Nostraud Reinhold, New York. |
[11] | LOCKWOOD J. P., HAZLETT R. W. (2010). Volcanoes: global perspectives, Wiley-Blackwell. |
[12] | LANGFORD N. J. (2005). Carbon dioxide poisoning. Toxicological Reviews, 24, 229-235. |
[13] | BUREAUDE LA CHEFFERIE DE BUKUMU. (2016). Tableau synoptique général de la population Congolaise, du Territoire de Nyiragongo. |
[14] | MAYENGO NZITA N. ET NSONI ZENO J. (2010). Maîtriser la Chimie 2, édition Loyola, p 37-200. |
[15] | M. M. KASEREKA, M. M. YALIRE, A. S. MINANI, C. V. SAMBA, A. K. BISUSA, E. K. KAMATE, N. MASHAGIRO, M. SYAUSWA, J. K. KAVUKE. (2017). Risks associate with mazuku in the Goma area, Democratic Republic of the Congo (east africa rift). |
APA Style
Faustin Safari Habari, Marcel Bahati Rusimbuka, Arsène Tumaini Sadiki, Mathieu Mapendano Yalire, Charles Muhigirwa Balagizi. (2021). Monitoring of CO2 in the Nyiragongo Volcano Cracks on Bugarura and Munigi Sites from January 2019 to January 2020. International Journal of Natural Resource Ecology and Management, 6(2), 38-41. https://doi.org/10.11648/j.ijnrem.20210602.12
ACS Style
Faustin Safari Habari; Marcel Bahati Rusimbuka; Arsène Tumaini Sadiki; Mathieu Mapendano Yalire; Charles Muhigirwa Balagizi. Monitoring of CO2 in the Nyiragongo Volcano Cracks on Bugarura and Munigi Sites from January 2019 to January 2020. Int. J. Nat. Resour. Ecol. Manag. 2021, 6(2), 38-41. doi: 10.11648/j.ijnrem.20210602.12
AMA Style
Faustin Safari Habari, Marcel Bahati Rusimbuka, Arsène Tumaini Sadiki, Mathieu Mapendano Yalire, Charles Muhigirwa Balagizi. Monitoring of CO2 in the Nyiragongo Volcano Cracks on Bugarura and Munigi Sites from January 2019 to January 2020. Int J Nat Resour Ecol Manag. 2021;6(2):38-41. doi: 10.11648/j.ijnrem.20210602.12
@article{10.11648/j.ijnrem.20210602.12, author = {Faustin Safari Habari and Marcel Bahati Rusimbuka and Arsène Tumaini Sadiki and Mathieu Mapendano Yalire and Charles Muhigirwa Balagizi}, title = {Monitoring of CO2 in the Nyiragongo Volcano Cracks on Bugarura and Munigi Sites from January 2019 to January 2020}, journal = {International Journal of Natural Resource Ecology and Management}, volume = {6}, number = {2}, pages = {38-41}, doi = {10.11648/j.ijnrem.20210602.12}, url = {https://doi.org/10.11648/j.ijnrem.20210602.12}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijnrem.20210602.12}, abstract = {In the area north of Lake Kivu, in the western part of the African Rift, deep fractures allow the uptake of gas, especially carbon dioxide. The Nyiragongo territory is located in the western part of the African Rift Valley. The deep fractures allow gases, especially carbon dioxide (CO2), to rise. CO2 is a heavier-than-air gas, asphyxiating, irritating to the eyes, nose and throat, and deadly at concentrations above 15%. The variation of CO2 in the different stations allows us to study the behaviour of the Nyiragongo volcano although in our stations we have not reached the lethal concentration of CO2. The volcanic activity of Nyiragongo is therefore closely monitored by the inhabitants, and any news of increased activity agitates the inhabitants of the region, especially those living in the Nyiragongo territory. Here we report a short carbon dioxide monitoring time series for five stations (BUGARURA I, II, III, IV and MUNIGI stations). The various variations in CO2 give us information about the activity of the Nyiragongo Volcano in the crater. The active volcanoes of the Virunga chain expose the Nyiragongo region to numerous natural hazards such as lava flows, gas plumes, dissolved gases in Lake Kivu and risks related to epidemiological diseases and armed conflicts.}, year = {2021} }
TY - JOUR T1 - Monitoring of CO2 in the Nyiragongo Volcano Cracks on Bugarura and Munigi Sites from January 2019 to January 2020 AU - Faustin Safari Habari AU - Marcel Bahati Rusimbuka AU - Arsène Tumaini Sadiki AU - Mathieu Mapendano Yalire AU - Charles Muhigirwa Balagizi Y1 - 2021/05/20 PY - 2021 N1 - https://doi.org/10.11648/j.ijnrem.20210602.12 DO - 10.11648/j.ijnrem.20210602.12 T2 - International Journal of Natural Resource Ecology and Management JF - International Journal of Natural Resource Ecology and Management JO - International Journal of Natural Resource Ecology and Management SP - 38 EP - 41 PB - Science Publishing Group SN - 2575-3061 UR - https://doi.org/10.11648/j.ijnrem.20210602.12 AB - In the area north of Lake Kivu, in the western part of the African Rift, deep fractures allow the uptake of gas, especially carbon dioxide. The Nyiragongo territory is located in the western part of the African Rift Valley. The deep fractures allow gases, especially carbon dioxide (CO2), to rise. CO2 is a heavier-than-air gas, asphyxiating, irritating to the eyes, nose and throat, and deadly at concentrations above 15%. The variation of CO2 in the different stations allows us to study the behaviour of the Nyiragongo volcano although in our stations we have not reached the lethal concentration of CO2. The volcanic activity of Nyiragongo is therefore closely monitored by the inhabitants, and any news of increased activity agitates the inhabitants of the region, especially those living in the Nyiragongo territory. Here we report a short carbon dioxide monitoring time series for five stations (BUGARURA I, II, III, IV and MUNIGI stations). The various variations in CO2 give us information about the activity of the Nyiragongo Volcano in the crater. The active volcanoes of the Virunga chain expose the Nyiragongo region to numerous natural hazards such as lava flows, gas plumes, dissolved gases in Lake Kivu and risks related to epidemiological diseases and armed conflicts. VL - 6 IS - 2 ER -