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 language | English |
|---|---|
| Title of host publication | 18th Symposium on the Application of Geophysics to Engineering and Environmental Problems, SAGEEP 2005: Geophysical Solutions for Today's Challenges |
| Pages | 476-487 |
| Number of pages | 12 |
| Volume | 1 |
| Publication status | Published - 2005 |
| Event | 18th 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 2005 → Apr 7 2005 |
Other
| Other | 18th Symposium on the Application of Geophysics to Engineering and Environmental Problems: Geophysical Solutions for Today's Challenges, SAGEEP 2005 |
|---|---|
| Country | United States |
| City | Atlanta, GA |
| Period | 4/3/05 → 4/7/05 |
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All Science Journal Classification (ASJC) codes
- Geophysics
- Geotechnical Engineering and Engineering Geology
- Environmental Engineering
Cite this
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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 proceeding › Conference contribution
TY - GEN
T1 - Geophysical investigation of the groundwater regimes in the lower Okavango Delta, Northwestern Botswana
AU - Shemang, Elisha M.
AU - Molwalefhe, Loago N.
AU - Kumar, Harish
AU - Bakaya, Tej
AU - Ntsatsi, Joel
PY - 2005
Y1 - 2005
N2 - 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.
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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M3 - Conference contribution
SN - 9781622760664
VL - 1
SP - 476
EP - 487
BT - 18th Symposium on the Application of Geophysics to Engineering and Environmental Problems, SAGEEP 2005: Geophysical Solutions for Today's Challenges
ER -