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Controls on greenhouse gas concentrations in polymictic headwater lakes in Ireland

机译:爱尔兰多生源头湖泊中温室气体浓度的控制

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摘要

Freshwater lakes are known to release carbon dioxide (CO_2) and methane (CH_4) to the atmosphere; however, the importance of lakes in global nitrous oxide (N_2O) budgets is not yet known. Further, despite the abundance of small lakes on the landscape, neither emissions of these gases nor their drivers are well described. Dissolved concentrations of CO_2, CH_4 and N_2O greenhouse gases were related to water chemistry, hydrology and catchment characteristics in order to identify factors controlling gas concentrations for 121 small Irish headwater lakes (median area: 2.0 ha) in relatively undisturbed catchments; lake-atmosphere gas fluxes were also calculated. The majority of lakes were supersaturated (relative to the atmosphere) with CO_2 and N_2O while CH_4 was above saturation in all lakes. Dissolved gas concentrations were correlated with land cover (rock, forest and grassland), deuterium excess (an indicator of hydrologic character) and lake organic carbon concentrations, although dissolved CO_2 exhibited few significant relationships. Principal components analysis indicated that higher levels of CH_4 and N_2O supersaturation were exhibited under different conditions. Methane supersaturation was highest in low elevation catchments with an evaporative hydrologic character and high organic carbon concentrations. In contrast, lakes characteristic of N_2O supersaturation were low in carbon and located in more rapidly flushed higher elevation catchments. Estimated fluxes of CO_2, CH_4 and N_2O to the atmosphere averaged 14, 0.36 and 1.3 ×10~(-3) mmol m~(-2) d~(-1), respectively.
机译:已知淡水湖泊会向大气中释放二氧化碳(CO_2)和甲烷(CH_4)。但是,湖泊在全球一氧化二氮(N_2O)预算中的重要性尚不清楚。此外,尽管景观中有许多小湖泊,但对这些气体的排放及其驱动因素都没有很好的描述。 CO_2,CH_4和N_2O温室气体的溶解浓度与水化学,水文学和流域特征有关,以便确定控制相对不受干扰的流域的121个爱尔兰小上游水域湖泊(中位面积:2.0公顷)的气体浓度的因素;还计算了湖泊-大气的气体通量。在所有湖泊中,大多数湖泊都被CO_2和N_2O过饱和(相对于大气),而CH_4则高于饱和度。溶解气体浓度与土地覆盖(岩石,森林和草地),氘过量(水文特征指标)和湖泊有机碳浓度相关,尽管溶解CO_2表现出很少的显着关系。主成分分析表明,在不同条件下,CH_4和N_2O的过饱和度较高。在低海拔流域,具有蒸发水文特征和高有机碳浓度的甲烷过饱和度最高。相反,具有N_2O过饱和特征的湖泊碳含量低,并且位于冲刷得更快的高海拔流域。估计的CO_2,CH_4和N_2O向大气的通量分别为14、0.36和1.3×10〜(-3)mmol m〜(-2)d〜(-1)。

著录项

  • 来源
    《Science of the total environment》 |2011年第1期|p.217-225|共9页
  • 作者单位

    Environmental and Resource Studies, Trent University, 1600 West Bank Drive, Peterborough, ON, Canada K9J 7B8,Water Science and Engineering Laboratory, University of Wisconsin, 660 North Park St. Madison, Wl 53706, USA;

    Environmental and Resource Studies, Trent University, 1600 West Bank Drive, Peterborough, ON, Canada K9J 7B8;

    Center for Limnology, University of Wisconsin, 680 North Park St., Madison, Wl 53706, USA;

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

    carbon dioxide; catchments; emissions; methane; nitrous oxide; surface waters;

    机译:二氧化碳;集水区;排放;甲烷;一氧化二氮;地表水;

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