[ HYDROGEOCHIMIE DES SOURCES SALINES DE BISHUSHA / Nord-Kivu-RDC ]
Volume 17, Issue 1, July 2016, Pages 4–12
Bosco Muhindo Musubao1 and Guy SHUNGU LAMA2
1 Department de Géologie, Université de Goma, Goma, Nord Kivu, RD Congo
2 Faculty of Sciences, Department of Geology, University of Goma, RD Congo
Original language: French
Copyright © 2016 ISSR Journals. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
The Bishusha salt sources are numerous. But as part of our research, we looked at four: Mariba 1, Mariba 2, Kazihiro and Makera. They contain various salts belonging either facies
Author Keywords: Hydrogeochemistry, saline, Bishusha, evaporite, dissolution, hardness.
Volume 17, Issue 1, July 2016, Pages 4–12
Bosco Muhindo Musubao1 and Guy SHUNGU LAMA2
1 Department de Géologie, Université de Goma, Goma, Nord Kivu, RD Congo
2 Faculty of Sciences, Department of Geology, University of Goma, RD Congo
Original language: French
Copyright © 2016 ISSR Journals. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Abstract
The Bishusha salt sources are numerous. But as part of our research, we looked at four: Mariba 1, Mariba 2, Kazihiro and Makera. They contain various salts belonging either facies
Author Keywords: Hydrogeochemistry, saline, Bishusha, evaporite, dissolution, hardness.
Abstract: (french)
Les sources salines de Bishusha sont nombreuses. Mais, dans le cadre de nos recherches, nous nous sommes intéressés à quatre : Mariba 1, Mariba 2, Kazihiro et Makera. Elles renferment différents sels appartenant soit au faciès « chloruré et sulfaté calcique et magnésien » soit à celui « chloruré sodique et potassique et magnésien ». Leur origine est profonde et est liée au lessivage et à la dissolution de l’encaissant évaporitique enfoui sous les formations quartzitiques, schisteuses, argileuses, laviques et pyroclastiques. Leurs eaux sont potables et consommables sans dangers excepté celles de Mariba 1.
Author Keywords: Hydrogéochimie, salin, Bishusha, évaporite, dissolution, dureté.
How to Cite this Article
Bosco Muhindo Musubao and Guy SHUNGU LAMA, “HYDROGEOCHEMISTRY OF SALT SOURCES OF Bishusha / North Kivu, DRC,” International Journal of Innovation and Applied Studies, vol. 17, no. 1, pp. 4–12, July 2016.
