Use this URL to cite or link to this record in EThOS:
Title: The climate controls and process of groundwater recharge in a semi-arid tropical environment : evidence from the Makutapora Basin, Tanzania
Author: Seddon, David
ISNI:       0000 0004 7970 7112
Awarding Body: UCL (University College London)
Current Institution: University College London (University of London)
Date of Award: 2019
Availability of Full Text:
Access from EThOS:
Full text unavailable from EThOS. Please try the link below.
Access from Institution:
Groundwater is a vital source of freshwater in semi-arid sub-Saharan Africa. Climate change, to which this region is particularly vulnerable, and increasing water demand are expected to increase the strategic importance of groundwater. The responses of groundwater systems to these forcings remain unclear. Here, in the intensively monitored and pumped groundwater system in the Makutapora Basin of central Tanzania, an analogue for semi-arid tropical areas underlain by weathered and fractured crystalline rock aquifers, I: (1) assess the relationship between precipitation intensity and groundwater recharge, (2) delineate the predominant recharge processes, and (3) project the impacts of climate change and increasing groundwater abstraction on future groundwater resources. Analysis of one of the longest known groundwater-level records in tropical Africa using a modified water-table fluctuation method, incorporating a numerical flow model to account for transience in response to pumping, shows more intensive precipitation disproportionately generates groundwater recharge. This bias is corroborated by a comparison of the stable-isotope composition of groundwater and precipitation as a function of intensity. Recharge is shown to occur via leakage from ephemeral streambeds through the formation and decay of groundwater 'mounds'. Stable-isotope tracers and hydrometric evidence of streambed inundation confirm the predominance of focused recharge pathways. Projections of groundwater resources, using a fully integrated MIKE SHE/MIKE 11 model, indicate that changes to recharge due to climate change will be small in the context of likely increases in groundwater abstraction. However, the bias of disproportionate groundwater recharge production from intensive precipitation, together with new insight regarding the processes and controls of recharge in this semi-arid environment, suggest that climate change may not only enhance groundwater recharge but also enable strategies (e.g. Managed Aquifer Recharge) to artificially enhance the sustainability of groundwater withdrawals since these events and processes are predictable.
Supervisor: Not available Sponsor: Not available
Qualification Name: Thesis (Ph.D.) Qualification Level: Doctoral
EThOS ID:  DOI: Not available