Surface water origin and attenuation of meteoric water input signal in the transboundary Lake Malawi basin : isotopic and hydrochemical evidence
Banda, Limbikani C. and Kalin, Robert M. and Phoenix, Vernon and Shuaibu, Abdulrahman (2025) Surface water origin and attenuation of meteoric water input signal in the transboundary Lake Malawi basin : isotopic and hydrochemical evidence. Science of the Total Environment, 1003. 180626. ISSN 1879-1026 (https://doi.org/10.1016/j.scitotenv.2025.180626)
Preview |
Text.
Filename: Banda-etal-STE-2025-Surface-water-origin-and-attenuation-of-meteoric-water-input-signal.pdf
Final Published Version License:
Download (15MB)| Preview |
Abstract
Understanding surface water origins and flow dynamics is essential for water quality protection and sustainable transboundary water governance. This study provides the first basin-wide isotopic (δ18O, δ2H) and hydrochemical characterisation of surface waters across the Lake Malawi basin, establishing a comprehensive baseline to support Integrated Water Resources Management (IWRM) amid growing climatic and developmental pressures. Seasonal hydrological regimes were identified: wet season surface flows dominated by tropical storm precipitation with minimal evaporation effect, and dry season flows sustained by isotopically distinct groundwater and spring discharges. Lakes exhibit strong evaporative enrichment (LEL slope: 5.5 ± 0.5; mean d-excess: −3.1 ‰), indicating kinetic fractionation. River and reservoir isotopic responses vary seasonally and spatially, with distinct transitions where mature plateau rivers meet escarpment headwaters. These rejuvenated rivers become progressively enriched across the rift valley lakeshore plains. While riverine δ18O and δ2H signatures fluctuate seasonally, lake and lagoon waters retain enriched signatures year-round due to longer residence times and internal mixing. Elevated total dissolved salts and corresponding isotopic enrichment suggest mixing with groundwater (influenced by water–rock interactions), and meteoric water inputs. The study underscores evaporation, groundwater, and meteoric water inputs as key drivers of surface water hydrochemistry, offering a robust framework for adaptive and evidence-based water resource management in tropical rift settings.
ORCID iDs
Banda, Limbikani C., Kalin, Robert M.
ORCID: https://orcid.org/0000-0003-3768-3848, Phoenix, Vernon
ORCID: https://orcid.org/0000-0002-8682-5200 and Shuaibu, Abdulrahman
ORCID: https://orcid.org/0000-0003-1679-0572;
-
-
Item type: Article ID code: 94408 Dates: DateEvent10 November 2025Published9 October 2025Published Online24 September 2025AcceptedSubjects: Geography. Anthropology. Recreation > Physical geography > Hydrology. Water Department: Faculty of Engineering > Civil and Environmental Engineering Depositing user: Pure Administrator Date deposited: 10 Oct 2025 07:14 Last modified: 08 Feb 2026 01:43 URI: https://strathprints.strath.ac.uk/id/eprint/94408
Tools
Tools






