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Monitoring of CO2 in the Nyiragongo Volcano Cracks on Bugarura and Munigi Sites from January 2019 to January 2020

Received: 16 April 2021     Accepted: 5 May 2021     Published: 20 May 2021
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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.

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.

Copyright

Copyright © The Author(s), 2021. Published by Science Publishing Group

Keywords

Monitoring, Carbon Dioxide, Crack, Volcano

References
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[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).
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    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

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    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

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    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

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  • @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}
    }
    

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  • 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  - 

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Author Information
  • Geochemistry an d Environment Department, Goma Volcano Observatory, Goma, Democratic Republic of Congo

  • Geochemistry an d Environment Department, Goma Volcano Observatory, Goma, Democratic Republic of Congo

  • Seismological Department, Goma Volcano Observatory, Goma, Democratic Republic of Congo

  • Geochemistry an d Environment Department, Goma Volcano Observatory, Goma, Democratic Republic of Congo

  • Geochemistry an d Environment Department, Goma Volcano Observatory, Goma, Democratic Republic of Congo

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