Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/70
Title: Spatial variability of the rate of organic carbon mineralization in a sewage-impacted mangrove forest, Mikindani, Kenya
Authors: Kamau, J.
Ngila, J.
Kirui, B.
Mwangi, S.
Mitto, C.
Wanjeri, V.
Okumu, S.
Keywords: Carbon dioxide production
Fe(II) production
Fe(III) reduction
Sewage
Sulfate reduction
Tudor creek
Environment
Soil Science & Conservation
Environmental Physics
general
Environment
Issue Date: 2015
Publisher: Springer Berlin Heidelberg
Series/Report no.: Journal of Soils and Sediments;
Abstract: Extensive amounts of untreated sewage are discharged in creeks lined by mangrove forests. This is a common occurrence in peri-urban coastal areas of the developing world. There is much evidence to suggest that mangroves filter discharged wastewater and prevent coastal pollution.The Mikindani mangrove system, Kenya has been exposed to sewage for more than a decade. The study seeks to investigate the ability of the Mikindani mangrove system to deal with the sewage carbon load.The ability of the mangrove system to phytoremediate sewage was investigated using anaerobic incubation experiments of sediments collected at several locations along the length of the creek at the study site. Carbon dioxide production was used as a proxy to measure the rate of organic matter degradation. The carbon dioxide production for the 0–1-cm sediment segment at site MKR 1 (the sewage input site) increased twofold after 8 days, implying that the natural system does not get enough time to stabilize since it is dosed continuously every tidal cycle. In situ CO2 efflux at site MKR 3 (~6 km from the sewage input site) was about three times the ∑CO2 production obtained after incubation for 8 days (anaerobic), which indicates that the easily degradable sediment organic carbon pool had degraded by about 67 % after 8 days. This suggests that this is sufficient time for the Rhizophora
URI: http://hdl.handle.net/123456789/70
ISSN: 1614-748
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