Geophysical investigation of the groundwater regimes in the lower Okavango Delta, Northwestern Botswana

Elisha M. Shemang, Loago N. Molwalefhe, Harish Kumar, Tej Bakaya, Joel Ntsatsi

    Research output: Chapter in Book/Report/Conference proceedingConference contribution

    Abstract

    The Okavango Delta in the northwestern part of Botswana is unique and it is the largest inland delta in the world. Instead of flowing into the sea, the annual flood of fresh water from the highlands flows inland, spreading over 15 000km 2 of the arid Kalahari environment and forming several islands and channels that emerge from its waterways. Parts of the Lower Okavango Delta that have been receiving large and frequent flood events have developed extensive fresh water aquifers, while other parts that have been receiving intermittently small floods have limited fresh water aquifers. The present study used aeromagnetic, airborne Electromagnetic (AEM), ground transient electromagnetic (TEM) soundings, drilling and down-hole geophysical logging data to map the distribution and geometry of these fresh water aquifer systems. The results of this study showed that the occurrence of freshwater aquifers in the lower delta are associated with active drainage channels and are bounded below and on their edges by brackish/ saline groundwater. The geometry of these aquifers provides an insight into the long term flooding history of the delta. This can be seen from the Gomoti River, which has had only intermittent flow in recent times, but is one of the largest fresh water aquifers in the lower delta.

    Original languageEnglish
    Title of host publication18th Symposium on the Application of Geophysics to Engineering and Environmental Problems, SAGEEP 2005: Geophysical Solutions for Today's Challenges
    Pages476-487
    Number of pages12
    Volume1
    Publication statusPublished - 2005
    Event18th Symposium on the Application of Geophysics to Engineering and Environmental Problems: Geophysical Solutions for Today's Challenges, SAGEEP 2005 - Atlanta, GA, United States
    Duration: Apr 3 2005Apr 7 2005

    Other

    Other18th Symposium on the Application of Geophysics to Engineering and Environmental Problems: Geophysical Solutions for Today's Challenges, SAGEEP 2005
    CountryUnited States
    CityAtlanta, GA
    Period4/3/054/7/05

    Fingerprint

    Botswana
    aquifers
    fresh water
    ground water
    Aquifers
    Groundwater
    aquifer
    groundwater
    Water
    water
    waterways
    electromagnetism
    geometry
    highlands
    Geometry
    arid environment
    sounding
    drainage
    drilling
    rivers

    All Science Journal Classification (ASJC) codes

    • Geophysics
    • Geotechnical Engineering and Engineering Geology
    • Environmental Engineering

    Cite this

    Shemang, E. M., Molwalefhe, L. N., Kumar, H., Bakaya, T., & Ntsatsi, J. (2005). Geophysical investigation of the groundwater regimes in the lower Okavango Delta, Northwestern Botswana. In 18th Symposium on the Application of Geophysics to Engineering and Environmental Problems, SAGEEP 2005: Geophysical Solutions for Today's Challenges (Vol. 1, pp. 476-487)
    Shemang, Elisha M. ; Molwalefhe, Loago N. ; Kumar, Harish ; Bakaya, Tej ; Ntsatsi, Joel. / Geophysical investigation of the groundwater regimes in the lower Okavango Delta, Northwestern Botswana. 18th Symposium on the Application of Geophysics to Engineering and Environmental Problems, SAGEEP 2005: Geophysical Solutions for Today's Challenges. Vol. 1 2005. pp. 476-487
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    abstract = "The Okavango Delta in the northwestern part of Botswana is unique and it is the largest inland delta in the world. Instead of flowing into the sea, the annual flood of fresh water from the highlands flows inland, spreading over 15 000km 2 of the arid Kalahari environment and forming several islands and channels that emerge from its waterways. Parts of the Lower Okavango Delta that have been receiving large and frequent flood events have developed extensive fresh water aquifers, while other parts that have been receiving intermittently small floods have limited fresh water aquifers. The present study used aeromagnetic, airborne Electromagnetic (AEM), ground transient electromagnetic (TEM) soundings, drilling and down-hole geophysical logging data to map the distribution and geometry of these fresh water aquifer systems. The results of this study showed that the occurrence of freshwater aquifers in the lower delta are associated with active drainage channels and are bounded below and on their edges by brackish/ saline groundwater. The geometry of these aquifers provides an insight into the long term flooding history of the delta. This can be seen from the Gomoti River, which has had only intermittent flow in recent times, but is one of the largest fresh water aquifers in the lower delta.",
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    Shemang, EM, Molwalefhe, LN, Kumar, H, Bakaya, T & Ntsatsi, J 2005, Geophysical investigation of the groundwater regimes in the lower Okavango Delta, Northwestern Botswana. in 18th Symposium on the Application of Geophysics to Engineering and Environmental Problems, SAGEEP 2005: Geophysical Solutions for Today's Challenges. vol. 1, pp. 476-487, 18th Symposium on the Application of Geophysics to Engineering and Environmental Problems: Geophysical Solutions for Today's Challenges, SAGEEP 2005, Atlanta, GA, United States, 4/3/05.

    Geophysical investigation of the groundwater regimes in the lower Okavango Delta, Northwestern Botswana. / Shemang, Elisha M.; Molwalefhe, Loago N.; Kumar, Harish; Bakaya, Tej; Ntsatsi, Joel.

    18th Symposium on the Application of Geophysics to Engineering and Environmental Problems, SAGEEP 2005: Geophysical Solutions for Today's Challenges. Vol. 1 2005. p. 476-487.

    Research output: Chapter in Book/Report/Conference proceedingConference contribution

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    AB - The Okavango Delta in the northwestern part of Botswana is unique and it is the largest inland delta in the world. Instead of flowing into the sea, the annual flood of fresh water from the highlands flows inland, spreading over 15 000km 2 of the arid Kalahari environment and forming several islands and channels that emerge from its waterways. Parts of the Lower Okavango Delta that have been receiving large and frequent flood events have developed extensive fresh water aquifers, while other parts that have been receiving intermittently small floods have limited fresh water aquifers. The present study used aeromagnetic, airborne Electromagnetic (AEM), ground transient electromagnetic (TEM) soundings, drilling and down-hole geophysical logging data to map the distribution and geometry of these fresh water aquifer systems. The results of this study showed that the occurrence of freshwater aquifers in the lower delta are associated with active drainage channels and are bounded below and on their edges by brackish/ saline groundwater. The geometry of these aquifers provides an insight into the long term flooding history of the delta. This can be seen from the Gomoti River, which has had only intermittent flow in recent times, but is one of the largest fresh water aquifers in the lower delta.

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    Shemang EM, Molwalefhe LN, Kumar H, Bakaya T, Ntsatsi J. Geophysical investigation of the groundwater regimes in the lower Okavango Delta, Northwestern Botswana. In 18th Symposium on the Application of Geophysics to Engineering and Environmental Problems, SAGEEP 2005: Geophysical Solutions for Today's Challenges. Vol. 1. 2005. p. 476-487