| dc.creator |
Nkotagu, Hudson H. |
|
| dc.date |
2016-09-21T13:25:03Z |
|
| dc.date |
2016-09-21T13:25:03Z |
|
| dc.date |
2005 |
|
| dc.date.accessioned |
2018-03-27T08:57:36Z |
|
| dc.date.available |
2018-03-27T08:57:36Z |
|
| dc.identifier |
Nkotagu, H.H., 2005. Paleolimnological investigations of anthropogenic change in Lake Tanganyika: VIII. Hydrological evaluation of two contrasting watersheds of the Lake Tanganyika catchment. Journal of Paleolimnology, 34(1), pp.107-123. |
|
| dc.identifier |
http://hdl.handle.net/20.500.11810/3936 |
|
| dc.identifier |
10.1007/s10933-005-2421-5 |
|
| dc.identifier.uri |
http://hdl.handle.net/20.500.11810/3936 |
|
| dc.description |
This study was conducted to delineate the impact of human activities on stream flow and water chemistry as
well as other factors that influence the chemical character of both surface and groundwater in two contrasting
watersheds of the Lake Tanganyika catchment. The study sites the Mwamgongo and Mitumba streams along
the northern Tanzanian coastline of the lake are representative of disturbed and undisturbed watersheds,
respectively, but are quite similar in other characteristics of slope, bedrock geology and size. Separation of
stream flow components was undertaken using classical hydrograph analysis along with chemical methods
using both Cl and 18O data. All the data show that groundwater accounts for the predominant source of total
stream flow in both the Mwamgongo and Mitumba watersheds (65 and 70% respectively). The streams have
an average d18O of about 3.0% and less than 10 mg/l for Cl. The basin recession constants of 9.4 · 10 3 d 1
and 9.6 · 10 3 d 1 for Mwamgongo and Mitumba, respectively, indicate existence of both fissured and
fractured aquifer systems. The chemical data exhibit low values of all determined ions. This supported the
hypothesis that natural processes influence the water chemical character of the study area. An Mg–HCO3 type
of water dominates in the two watersheds. Despite their similar size and bedrock character the Mwamgongo
watershed has an order of magnitude in sediment transport than the Mitumba one. The data show that the
disturbed watershed discharges less groundwater and more sediments, and has a poorer water quality than the
forested Mitumba watershed, which lies within the Gombe National Park. The data show that soil erosion
processes are more active at Mwamgongo, and that both the surface runoff component of the total stream flow
and increased dissolved salt load is greater in the deforested Mwamgongo watershed than in the Mitumba
watershed. The chloride and d18O data complemented each other in delineating the amounts of groundwater
in the total stream flow as the results using both data differed insignificantly. It may be concluded that the
undisturbed watershed has a higher retention of good quality water and traps more sediments than the
disturbed one. In addition, the groundwater component plays a dominant role in the total annual stream flow
at each watershed. |
|
| dc.language |
en |
|
| dc.publisher |
Springer |
|
| dc.subject |
Baseflow |
|
| dc.subject |
Hydrograph |
|
| dc.subject |
Stable isotopes |
|
| dc.subject |
Surface runoff |
|
| dc.subject |
Types of water |
|
| dc.subject |
Watersheds |
|
| dc.title |
Paleolimnological Investigations of Anthropogenic Change in Lake Tanganyika: VIII. Hydrological Evaluation of Two Contrasting Watersheds of the Lake Tanganyika Catchment |
|
| dc.type |
Journal Article, Peer Reviewed |
|