The present study is the first appraisal of regional hydrogeochemical programme for environmental assessment of the mineralized Lom Basin in East Cameroon. Fifty-two streamwater samples were collected and analysed for major cations (Ca2+, Mg2+, Na+, K+) and major anions (HCO3–, F–, Cl–, NO2–, NO3–, Br–, PO43–, SO42–). Calcium and HCO3– were the dominant ions. The chemical facies for the surface water were CaHCO3 and NaHCO3 types indicating a fresh water source. Major ion geochemistry demonstrated the potential to discriminate between natural and anthropogenic origins. Calcium ion, Mg2+, Na+, K+and HCO3– had similar distribution trends reflecting weathering from the parent rocks. Sulphate distribution correlated with the occurrence of sulphide minerals associated with hydrothermal gold mineralization in the area while the distribution patterns of NO3–and Cl– reflected pollution from domestic activities within the municipality. Overall, the chemistry of stream water in the Lom Basin is mainly controlled by silicate weathering with only minor anthropogenic influence. This study forms an analogue for hydrogeochemical mapping in other mineralized terrains in Cameroon.
Published in | Hydrology (Volume 5, Issue 2) |
DOI | 10.11648/j.hyd.20170502.11 |
Page(s) | 15-31 |
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), 2017. Published by Science Publishing Group |
Hydrogeochemical Survey, Major Ions, Provenance, Lom Basin, Cameroon
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APA Style
Mumbfu Ernestine Mimba, Takeshi Ohba, Salomon César Nguemhe Fils, Mengnjo Jude Wirmvem, Edith Etakah Bate Tibang, et al. (2017). Regional Hydrogeochemical Mapping for Environmental Studies in the Mineralized Lom Basin, East Cameroon: A Pre-industrial Mining Survey. Hydrology, 5(2), 15-31. https://doi.org/10.11648/j.hyd.20170502.11
ACS Style
Mumbfu Ernestine Mimba; Takeshi Ohba; Salomon César Nguemhe Fils; Mengnjo Jude Wirmvem; Edith Etakah Bate Tibang, et al. Regional Hydrogeochemical Mapping for Environmental Studies in the Mineralized Lom Basin, East Cameroon: A Pre-industrial Mining Survey. Hydrology. 2017, 5(2), 15-31. doi: 10.11648/j.hyd.20170502.11
AMA Style
Mumbfu Ernestine Mimba, Takeshi Ohba, Salomon César Nguemhe Fils, Mengnjo Jude Wirmvem, Edith Etakah Bate Tibang, et al. Regional Hydrogeochemical Mapping for Environmental Studies in the Mineralized Lom Basin, East Cameroon: A Pre-industrial Mining Survey. Hydrology. 2017;5(2):15-31. doi: 10.11648/j.hyd.20170502.11
@article{10.11648/j.hyd.20170502.11, author = {Mumbfu Ernestine Mimba and Takeshi Ohba and Salomon César Nguemhe Fils and Mengnjo Jude Wirmvem and Edith Etakah Bate Tibang and Melvin Tamta Nforba and Festus Togwa Aka}, title = {Regional Hydrogeochemical Mapping for Environmental Studies in the Mineralized Lom Basin, East Cameroon: A Pre-industrial Mining Survey}, journal = {Hydrology}, volume = {5}, number = {2}, pages = {15-31}, doi = {10.11648/j.hyd.20170502.11}, url = {https://doi.org/10.11648/j.hyd.20170502.11}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.hyd.20170502.11}, abstract = {The present study is the first appraisal of regional hydrogeochemical programme for environmental assessment of the mineralized Lom Basin in East Cameroon. Fifty-two streamwater samples were collected and analysed for major cations (Ca2+, Mg2+, Na+, K+) and major anions (HCO3–, F–, Cl–, NO2–, NO3–, Br–, PO43–, SO42–). Calcium and HCO3– were the dominant ions. The chemical facies for the surface water were CaHCO3 and NaHCO3 types indicating a fresh water source. Major ion geochemistry demonstrated the potential to discriminate between natural and anthropogenic origins. Calcium ion, Mg2+, Na+, K+and HCO3– had similar distribution trends reflecting weathering from the parent rocks. Sulphate distribution correlated with the occurrence of sulphide minerals associated with hydrothermal gold mineralization in the area while the distribution patterns of NO3–and Cl– reflected pollution from domestic activities within the municipality. Overall, the chemistry of stream water in the Lom Basin is mainly controlled by silicate weathering with only minor anthropogenic influence. This study forms an analogue for hydrogeochemical mapping in other mineralized terrains in Cameroon.}, year = {2017} }
TY - JOUR T1 - Regional Hydrogeochemical Mapping for Environmental Studies in the Mineralized Lom Basin, East Cameroon: A Pre-industrial Mining Survey AU - Mumbfu Ernestine Mimba AU - Takeshi Ohba AU - Salomon César Nguemhe Fils AU - Mengnjo Jude Wirmvem AU - Edith Etakah Bate Tibang AU - Melvin Tamta Nforba AU - Festus Togwa Aka Y1 - 2017/06/26 PY - 2017 N1 - https://doi.org/10.11648/j.hyd.20170502.11 DO - 10.11648/j.hyd.20170502.11 T2 - Hydrology JF - Hydrology JO - Hydrology SP - 15 EP - 31 PB - Science Publishing Group SN - 2330-7617 UR - https://doi.org/10.11648/j.hyd.20170502.11 AB - The present study is the first appraisal of regional hydrogeochemical programme for environmental assessment of the mineralized Lom Basin in East Cameroon. Fifty-two streamwater samples were collected and analysed for major cations (Ca2+, Mg2+, Na+, K+) and major anions (HCO3–, F–, Cl–, NO2–, NO3–, Br–, PO43–, SO42–). Calcium and HCO3– were the dominant ions. The chemical facies for the surface water were CaHCO3 and NaHCO3 types indicating a fresh water source. Major ion geochemistry demonstrated the potential to discriminate between natural and anthropogenic origins. Calcium ion, Mg2+, Na+, K+and HCO3– had similar distribution trends reflecting weathering from the parent rocks. Sulphate distribution correlated with the occurrence of sulphide minerals associated with hydrothermal gold mineralization in the area while the distribution patterns of NO3–and Cl– reflected pollution from domestic activities within the municipality. Overall, the chemistry of stream water in the Lom Basin is mainly controlled by silicate weathering with only minor anthropogenic influence. This study forms an analogue for hydrogeochemical mapping in other mineralized terrains in Cameroon. VL - 5 IS - 2 ER -