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爱尔兰多成因源头湖温室气体浓度的控制因素。

Controls on greenhouse gas concentrations in polymictic headwater lakes in Ireland.

机构信息

Environmental and Resource Studies, Trent University, 1600 West Bank Drive, Peterborough, ON, Canada.

出版信息

Sci Total Environ. 2011 Dec 1;410-411:217-25. doi: 10.1016/j.scitotenv.2011.09.045. Epub 2011 Oct 20.

Abstract

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(2)O) 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(2)O 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: 2.0ha) 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(2)O 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(2)O 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(2)O supersaturation were low in carbon and located in more rapidly flushed higher elevation catchments. Estimated fluxes of CO(2), CH(4) and N(2)O to the atmosphere averaged 14, 0.36 and 1.3×10(-3)mmolm(-2)d(-1), respectively.

摘要

淡水湖泊会向大气中释放二氧化碳(CO(2))和甲烷(CH(4));然而,湖泊在全球氧化亚氮(N(2)O)预算中的重要性尚不清楚。此外,尽管景观上有大量的小湖泊,但这些气体的排放及其驱动因素都没有得到很好的描述。为了确定控制 121 个爱尔兰小集水区(中位数面积:2.0ha)中气体浓度的因素,将水中溶解的 CO(2)、CH(4)和 N(2)O 温室气体浓度与水化学、水文学和集水区特征相关联;还计算了湖泊-大气气体通量。大多数湖泊的 CO(2)和 N(2)O 均处于过饱和状态(相对于大气),而所有湖泊的 CH(4)均超过饱和。溶解气体浓度与土地覆盖(岩石、森林和草地)、氘过剩(水文学特征的指标)和湖泊有机碳浓度相关,尽管溶解 CO(2)表现出很少的显著关系。主成分分析表明,在不同条件下,CH(4)和 N(2)O 的过饱和度水平更高。甲烷过饱和度在具有蒸发水文学特征和高有机碳浓度的低海拔集水区中最高。相比之下,具有 N(2)O 过饱和度特征的湖泊的碳含量较低,位于水流更快、海拔更高的集水区。大气中 CO(2)、CH(4)和 N(2)O 的估计通量分别平均为 14、0.36 和 1.3×10(-3)mmolm(-2)d(-1)。

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