A spatial assessment of stream-flow characteristics and hydrologic alterations, post dam construction in the Manyame catchment, Zimbabwe

Authors

  • Tongayi Mwedzi Chinhoyi University of Technology, P Bag 7724, Off Harare/ Chirundu Road, Chinhoyi, Zimbabwe
  • Loreen Katiyo Chinhoyi University of Technology, P Bag 7724, Off Harare/ Chirundu Road, Chinhoyi, Zimbabwe
  • Francis T Mugabe Chinhoyi University of Technology, P Bag 7724, Off Harare/ Chirundu Road, Chinhoyi, Zimbabwe
  • Taurai Bere Chinhoyi University of Technology, P Bag 7724, Off Harare/ Chirundu Road, Chinhoyi, Zimbabwe
  • Courage Bangira
  • Tinotenda Mangadze Chinhoyi University of Technology, P Bag 7724, Off Harare/ Chirundu Road, Chinhoyi, Zimbabwe
  • Olga L Kupika Chinhoyi University of Technology, P Bag 7724, Off Harare/ Chirundu Road, Chinhoyi, Zimbabwe

DOI:

https://doi.org/10.4314/wsa.v42i2.03

Keywords:

damming, range of variability approach, stream-flow characteristics

Abstract

The global hydrologic regime has been intensively altered through activities such as dam construction, water abstraction, and inter-basin transfers. This paper uses the Range of Variability Approach (RVA) and daily stream flow records from nine gauging stations to characterize stream-flow post dam construction in the Manyame catchment, Zimbabwe. We identify which variables continue to be altered, upstream and at different distances downstream, to distinguish sections with the highest potential for ecological disruption and to understand how hydrological alterations dissipate downstream of dams. Our results indicate that different sections of the same river have different stream-flow characteristics post dam construction. The most adverse effects of dams were on downstream stretches of the river which were characterized by low flows, extreme low flows and an increased number of zero-flow days. These differences reflect the operation rules of the Manyame catchment dams. While the change in stream-flow characteristics is apparent in the 0–10 km range, it is slightly felt in the 11–20 km range and totally disappears at distances >20 km downstream of dams. These changes in stream characteristics, and that damming is only restricted to the upper third of the catchment, make the hydrologic fragmentations in the catchment minor. However, the continued hydrologic alterations post dam construction raise important concerns about the interactions of hydrology with other factors like sediment deposition upstream of dams and climate change. We recommend that catchment managers target enhancing the natural flow variability of the river instead of meeting target flows.

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Published

2016-04-29

Issue

Section

Research paper

How to Cite

Tongayi Mwedzi (2016) “A spatial assessment of stream-flow characteristics and hydrologic alterations, post dam construction in the Manyame catchment, Zimbabwe”, Water SA, 42(2 April). doi:10.4314/wsa.v42i2.03.