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首页> 外文期刊>Lakes & Reservoirs >Diffusive emissions of methane and nitrous oxide from a cascade of tropical hydropower reservoirs in Kenya
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Diffusive emissions of methane and nitrous oxide from a cascade of tropical hydropower reservoirs in Kenya

机译:肯尼亚一系列热带水库的甲烷和一氧化二氮的扩散排放

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摘要

The present study investigated diffusive emissions of methane (CH_4) and nitrousoxide (N_2O) to the atmosphere from three relatively small (3–120 km~2) reservoirs(Masinga, Kamburu and Gitaru) on the Tana River (Kenya). Sampling was conductedbiweekly in 2011, 2012 and 2013, at sampling sites upstream and downstream ofthese reservoirs while five sampling campaigns were carried out in 2011, 2012 and2013 for different sites within each of the reservoirs. The dissolved CH_4 (range:19–2101 nmol/L) and N_2O (range: 6.2–11.5 nmol/L) concentrations in the surfacewaters were generally very low in the three reservoirs, compared with other reservoirsglobally. The lower diffusive emissions of CH4 (20–216 μmol/m~2 day~(−1)) andN_2O (1.0–1.6 μmol/m~2 day~(−1)) from these reservoirs, compared with other tropicalreservoirs, are probably related to their age (30–40 years), and lower vegetation biomass(savannah) originally present and submerged during their commissioning. Thereservoirs with longer water residence times were characterized by higher diffusiveCH4 fluxes (216 ± 666 μmol/m~2 day~(−1)) and slightly lower N_2O fluxes (1.0 ± 1.5 μmol/m~2 day~(−1)). The relative contribution of turbine fluxes of CH_4 and N_2O, comparedto diffusive fluxes, was also highly variable among the three dams, being lower inMasinga Reservoir and higher in Gitaru Reservoir.
机译:本研究调查了塔纳河上三个相对较小(3–120 km〜2)的水库 r n(Masinga,Kamburu和Gitaru)向大气中的甲烷(CH_4)和一氧化二氮 n n氧化物(N_2O)的扩散排放。河(肯尼亚)。 n n每两周分别在2011、2012和2013年对这些水库的上游和下游进行采样,而2011、2012和2013年针对每个水库中的不同地点进行了五次采样活动。与其他水库相比,三个水库中地表水中水的溶解CH_4(范围: r n19–2101 nmol / L)和N_2O(范围:6.2-11.5 nmol / L)的浓度通常非常低 r n全局。与其他水库相比,这些储层中的CH4(20–216μmol/ m〜2天〜(-1))和 r nN_2O(1.0–1.6μmol/ m〜2天〜(-1))的扩散排放较低热带 r n水库可能与它们的年龄(30–40岁)有关,并且在调试期间最初存在并淹没的较低植被生物量 r n(热带稀树草原)。具有较长水停留时间的 r n储层的特征是较高的扩散 r nCH4通量(216±666μmol/ m〜2天〜(-1))和略低的N_2O通量(1.0±1.5μmol/ r nm〜2天〜(-1))。 CH_4和N_2O的透平通量相对于扩散通量的相对贡献在三个大坝中也变化很大,在Masinga水库中较低,而在Gitaru水库中较高。

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  • 来源
    《Lakes & Reservoirs 》 |2019年第2期| 127-135| 共9页
  • 作者单位

    Department of Earth and Environmental Sciences, Katholieke Universiteit Leuven, Leuven, Belgium Kenya Marine and Fisheries Research Institute, Mombasa, Kenya;

    Department of Earth and Environmental Sciences, Katholieke Universiteit Leuven, Leuven, Belgium;

    School of Agriculture and Environmental Sciences, Department of Environmental Sciences, Pwani University, Kilifi, Kenya;

    Unite d’Oceanographie Chimique, Universite de Liege, Liege, Belgium;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    African (tropical) reservoirs; greenhouse gases; Methane emissions; nitrous oxide emissions;

    机译:非洲(热带)水库;温室气体;甲烷排放;氧化亚氧化物排放量;

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