TY - GEN
T1 - A Geohydrological Mapping of the Modder River Catchment of the Upper Orange River System of Southern Africa
AU - Alowo, Rebecca
N1 - Publisher Copyright:
© The Author(s), under exclusive license to Springer Nature Switzerland AG 2025.
PY - 2025
Y1 - 2025
N2 - The Modder River basin is part of the Upper Orange River drainage, which encompasses South Africa and Lesotho. The Orange River basin is a cross-border catchment that spans over Lesotho, Namibia, South Africa, and Botswana. The geohydrological mapping of the Modder River Catchment encompasses the identification and classification of rock types, aquifer types, precipitation patterns, river networks, groundwater recharge mechanisms, stratigraphy, and a digital elevation model (DEM). The mapping process utilized a total of 51 monitoring boreholes, both privately owned and government-operated, that were already in place. The western portion of the catchment exhibits efficient drainage because of its interconnected river system, receiving an average annual precipitation of 400–600 mm. In contrast, the eastern sector of the catchment experiences inadequate drainage and receives lower precipitation levels ranging from 300–400 mm. The primary types of aquifers are fractured aquifers and intergranular and fractured aquifers, which have yields ranging from 0.5 to 2.0 L. The annual replenishment of groundwater varies from 0.1 to 12 mm in the western half of the basin, and from 12 to 34 mm in the eastern section. To ensure water security for the residents of major urban areas in the Modder River Catchment, such as Bloemfontein, Thaba Nchu, and Botsabello, it is essential to accurately map and characterize the hydrological and geohydrological features of significant aquifers in the catchment area.
AB - The Modder River basin is part of the Upper Orange River drainage, which encompasses South Africa and Lesotho. The Orange River basin is a cross-border catchment that spans over Lesotho, Namibia, South Africa, and Botswana. The geohydrological mapping of the Modder River Catchment encompasses the identification and classification of rock types, aquifer types, precipitation patterns, river networks, groundwater recharge mechanisms, stratigraphy, and a digital elevation model (DEM). The mapping process utilized a total of 51 monitoring boreholes, both privately owned and government-operated, that were already in place. The western portion of the catchment exhibits efficient drainage because of its interconnected river system, receiving an average annual precipitation of 400–600 mm. In contrast, the eastern sector of the catchment experiences inadequate drainage and receives lower precipitation levels ranging from 300–400 mm. The primary types of aquifers are fractured aquifers and intergranular and fractured aquifers, which have yields ranging from 0.5 to 2.0 L. The annual replenishment of groundwater varies from 0.1 to 12 mm in the western half of the basin, and from 12 to 34 mm in the eastern section. To ensure water security for the residents of major urban areas in the Modder River Catchment, such as Bloemfontein, Thaba Nchu, and Botsabello, it is essential to accurately map and characterize the hydrological and geohydrological features of significant aquifers in the catchment area.
KW - Aquifer types
KW - Catchment
KW - Fracture
KW - Modder River
KW - Recharge
UR - https://www.scopus.com/pages/publications/105028257314
U2 - 10.1007/978-3-031-86777-4_78
DO - 10.1007/978-3-031-86777-4_78
M3 - Conference contribution
AN - SCOPUS:105028257314
SN - 9783031867767
T3 - Advances in Science, Technology and Innovation
SP - 405
EP - 410
BT - Dynamic Evolution of Atmospheric, Ecological, and Hydrological Systems in Circum-Mediterranean Regions - Proceedings of the 3rd MedGU 2023 Volume 1
A2 - Zhang, Zhihua
A2 - Chenchouni, Haroun
A2 - Sarikaya, Mehmet Akif
A2 - Ciner, Attila
A2 - Knight, Jasper
A2 - Gentilucci, Matteo
A2 - Ali, Imran
PB - Springer Nature
T2 - 3rd International conference on Mediterranean Geosciences Union, MedGU 2023
Y2 - 26 November 2023 through 30 November 2023
ER -