ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    ISSN: 1573-5117
    Keywords: water pollution ; Lake Tanganyika ; Burundi
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Sources of pollution at the north end of Lake Tanganyika are concentrated around Bujumbura, Burundi. The impact of River Ntahangwa on the water quality of this part of Lake Tanganyika was compared with that of an unpolluted river, the Mugere. A shallow bay, not influenced by a river, was used as a reference station. Chemical analyses were carried out at four week intervals during nearly a year. Samples were taken at different distances from the shore and at different depths. River impact was detected up to 100 m from both river mouths. Even at 50 m from the mouth of the polluted River Ntahangwa, no important decrease of dissolved oxygen was detected. Chlorophyll-a maxima were found 100 m from the Ntahangwa mouth, but this was also the case 100 m from shore in the unpolluted bay. Lake water at 60 m depth was saturated with oxygen during the dry season, as it used to be in 1956. The rivers studied descent initially within the lake due to greater sediment load and lower water temperature. Nevertheless, it appears that these rivers mix completely in the lake within 100–300 m from the river mouths. The direct effects from organic pollution of the Ntahangwa on the lake seem to be rather negligible. Appropriate anti-erosion measures should reduce massive sediment discharge into the lake.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 407 (1999), S. 65-73 
    ISSN: 1573-5117
    Keywords: Lake Tanganyika ; Burundi ; hydrodynamics ; sedimentation ; Rusizi River
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The inflow of River Rusizi to Lake Tanganyika has been assumed not to mix with the lake epilimnion as it would sink as an interflow or an underflow, because of its higher density due to sediment load, lower temperature and higher salinity. Nevertheless, efforts made to trace the Rusizi flow into the lake have failed. Ten sampling surveys were carried out from March 1994 to July 1995. Each consisted of 22 samples, at different distances off the Rusizi estuary and at different depths. Eighteen physical and chemical variables were studied at each site. The Rusizi water was always denser (800 – 1400 g m-3) than the lake water. The relative importance of temperature, suspended solids and salinity varied seasonally. A descent of the Rusizi inflow was observed. Close to the river estuary, river and lake waters mixed and Rusizi sediments settled. Complete mixing occurred within 800 m off- shore. The Rusizi inflow merged with the epilimnion rather than the hypolimnion. Horizontal spread by shorebound currents seemed to be more important than offshore spread.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...