Land Use, Not Stream Order, Controls N2O Concentration and Flux in the Upper Mara River Basin, Kenya

Anthropogenic activities have led to increases in nitrous oxide (N2O) emissions from river systems, but there are large uncertainties in estimates due to lack of data in tropical rivers and rapid increase in human activity. We assessed the effects of land use and river size on N2O flux and concentra...

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Autores principales: Mwanake, Ricky M., Gettel, Gretchen M., Aho, K.S., Namwaya, D.W., Masese, F.O., Butterbach-Bahl, Klaus, Raymond, P.A.
Formato: Journal Article
Lenguaje:Inglés
Publicado: American Geophysical Union 2019
Materias:
Acceso en línea:https://hdl.handle.net/10568/129514
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author Mwanake, Ricky M.
Gettel, Gretchen M.
Aho, K.S.
Namwaya, D.W.
Masese, F.O.
Butterbach-Bahl, Klaus
Raymond, P.A.
author_browse Aho, K.S.
Butterbach-Bahl, Klaus
Gettel, Gretchen M.
Masese, F.O.
Mwanake, Ricky M.
Namwaya, D.W.
Raymond, P.A.
author_facet Mwanake, Ricky M.
Gettel, Gretchen M.
Aho, K.S.
Namwaya, D.W.
Masese, F.O.
Butterbach-Bahl, Klaus
Raymond, P.A.
author_sort Mwanake, Ricky M.
collection Repository of Agricultural Research Outputs (CGSpace)
description Anthropogenic activities have led to increases in nitrous oxide (N2O) emissions from river systems, but there are large uncertainties in estimates due to lack of data in tropical rivers and rapid increase in human activity. We assessed the effects of land use and river size on N2O flux and concentration in 46 stream sites in the Mara River, Kenya, during the transition from the wet (short rains) to dry season, November 2017 to January 2018. Flux estimates were similar to other studies in tropical and temperate systems, but in contrast to other studies, land use was more related to N2O concentration and flux than stream size. Agricultural stream sites had the highest fluxes (26.38 ± 5.37 N2O-N μg·m–2·hr–1) compared to both forest and livestock sites (5.66 ± 1.38 N2O-N μg·m–2·hr–1 and 6.95 ± 2.96 N2O-N μg·m–2·hr–1, respectively). N2O concentrations in forest and agriculture streams were positively correlated to stream carbon dioxide (CO2-C(aq)) but showed a negative correlation with dissolved organic carbon, and the dissolved organic carbon:dissolved inorganic nitrogen ratio. N2O concentration in the livestock sites had a negative relationship with CO2-C(aq) and a higher number of negative fluxes. We concluded that in-stream chemoautotrophic nitrification was likely the main biogeochemical process driving N2O production in agricultural and forest streams, whereas complete denitrification led to the consumption of N2O in the livestock stream sites. These results point to the need to better understand the relative importance of nitrification and denitrification in different habitats in producing N2O and for process-based studies.
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spelling CGSpace1295142025-12-08T09:54:28Z Land Use, Not Stream Order, Controls N2O Concentration and Flux in the Upper Mara River Basin, Kenya Mwanake, Ricky M. Gettel, Gretchen M. Aho, K.S. Namwaya, D.W. Masese, F.O. Butterbach-Bahl, Klaus Raymond, P.A. land use land kenya basin Anthropogenic activities have led to increases in nitrous oxide (N2O) emissions from river systems, but there are large uncertainties in estimates due to lack of data in tropical rivers and rapid increase in human activity. We assessed the effects of land use and river size on N2O flux and concentration in 46 stream sites in the Mara River, Kenya, during the transition from the wet (short rains) to dry season, November 2017 to January 2018. Flux estimates were similar to other studies in tropical and temperate systems, but in contrast to other studies, land use was more related to N2O concentration and flux than stream size. Agricultural stream sites had the highest fluxes (26.38 ± 5.37 N2O-N μg·m–2·hr–1) compared to both forest and livestock sites (5.66 ± 1.38 N2O-N μg·m–2·hr–1 and 6.95 ± 2.96 N2O-N μg·m–2·hr–1, respectively). N2O concentrations in forest and agriculture streams were positively correlated to stream carbon dioxide (CO2-C(aq)) but showed a negative correlation with dissolved organic carbon, and the dissolved organic carbon:dissolved inorganic nitrogen ratio. N2O concentration in the livestock sites had a negative relationship with CO2-C(aq) and a higher number of negative fluxes. We concluded that in-stream chemoautotrophic nitrification was likely the main biogeochemical process driving N2O production in agricultural and forest streams, whereas complete denitrification led to the consumption of N2O in the livestock stream sites. These results point to the need to better understand the relative importance of nitrification and denitrification in different habitats in producing N2O and for process-based studies. 2019-11 2023-03-10T14:37:29Z 2023-03-10T14:37:29Z Journal Article https://hdl.handle.net/10568/129514 en Open Access American Geophysical Union Mwanake, Ricky M.; Gettel, Gretchen M.; Aho, K.S.; Namwaya, D.W.; Masese, F.O.; Butterbach-Bahl, Klaus; Raymond, P.A. 2019. Land Use, Not Stream Order, Controls N2O Concentration and Flux in the Upper Mara River Basin, Kenya. Journal of Geophysical Research: Biogeosciences 124: 3491-3506
spellingShingle land use
land
kenya
basin
Mwanake, Ricky M.
Gettel, Gretchen M.
Aho, K.S.
Namwaya, D.W.
Masese, F.O.
Butterbach-Bahl, Klaus
Raymond, P.A.
Land Use, Not Stream Order, Controls N2O Concentration and Flux in the Upper Mara River Basin, Kenya
title Land Use, Not Stream Order, Controls N2O Concentration and Flux in the Upper Mara River Basin, Kenya
title_full Land Use, Not Stream Order, Controls N2O Concentration and Flux in the Upper Mara River Basin, Kenya
title_fullStr Land Use, Not Stream Order, Controls N2O Concentration and Flux in the Upper Mara River Basin, Kenya
title_full_unstemmed Land Use, Not Stream Order, Controls N2O Concentration and Flux in the Upper Mara River Basin, Kenya
title_short Land Use, Not Stream Order, Controls N2O Concentration and Flux in the Upper Mara River Basin, Kenya
title_sort land use not stream order controls n2o concentration and flux in the upper mara river basin kenya
topic land use
land
kenya
basin
url https://hdl.handle.net/10568/129514
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