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
@inproceedings{2d026ad44aa24f3b943271fad3ae290d,
title = "Geophysical investigation of the groundwater regimes in the lower Okavango Delta, Northwestern Botswana",
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.",
author = "Shemang, {Elisha M.} and Molwalefhe, {Loago N.} and Harish Kumar and Tej Bakaya and Joel Ntsatsi",
year = "2005",
language = "English",
isbn = "9781622760664",
volume = "1",
pages = "476--487",
booktitle = "18th Symposium on the Application of Geophysics to Engineering and Environmental Problems, SAGEEP 2005: Geophysical Solutions for Today's Challenges",

}

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

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.

UR - http://www.scopus.com/inward/record.url?scp=84867469229&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84867469229&partnerID=8YFLogxK

M3 - Conference contribution

AN - SCOPUS:84867469229

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 -

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