Effects of microbial activity on the hydrochemistry and sedimentology of Lake Logipi, Kenya View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1993-09

AUTHORS

Sabine Castanier, Marie-Claire Bernet-Rollande, André Maurin, Jean-Pierre Perthuisot

ABSTRACT

Lake Logipi is a saline soda and alkaline lake which marks the northern termination of the Suguta River drainage system. It also receives waters from streams, possible seepage from Lake Turkana, and hot springs. Present hydrochemistry and sedimentology is controlled by numerous factors including seasonal variations, composition of incoming waters, water depth and, above all, bacterial activity. Given the scarcity of Ca2+ and Mg2+ in the lake waters, bacterial activity seems to intensify the alkalinization of the waters which inhibits the deposition of organic matter and leads to the genesis of a poorly organic, zeolitic mud that reaches 1.5 m in tickness in the deepest part of the lake. This black layer may be overlaid with thin crusts of trona and halite which prograde over the basin from its southern bank when the lake is drying out and which are dissolved in the lake waters during the rainy season. More... »

PAGES

99-112

References to SciGraph publications

  • 1969-04. Inorganic bedded cherts from the Magadi area, Kenya in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1981-07. Distribution of different anaerobic bacteria in arabian sea sediments in MARINE BIOLOGY
  • Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1007/bf00018793

    DOI

    http://dx.doi.org/10.1007/bf00018793

    DIMENSIONS

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