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首页> 外文期刊>Journal of great lakes research >Nitrogen dry deposition to Lake Superior and Lake Michigan
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Nitrogen dry deposition to Lake Superior and Lake Michigan

机译:氮气干沉降到苏必利尔湖和密歇根湖

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Nitrate (NO3-) levels in Lake Superior have increased from historic levels of about 5 mu M to its current concentration of about 25 mu M. The atmosphere makes a substantial contribution to the nitrogen budgets for Lake Superior and Lake Michigan. This study provides a more well-defined estimate of nitrogen dry deposition rates derived from the measurement of over-water concentrations, and in situ meteorological measurements, which were input into the Resistance Model. We obtained a nitrogen dry deposition rate of [(3.41 +/- 2.26) x 10(7) kg N/yr; (5.90 +/- 3.91) kg N/ha/yr] over Lake Michigan, and [(1.54 +/- 1.06) x 10(7) kg N/yr; (1.87 +/- 1.27) kg N/ha/yr] over Lake Superior. Nitric acid (HNO3), which originates from the combustion of fossil fuels, contributes 84% of the total nitrogen dry deposition to Lake Michigan; and 66% to Lake Superior. Ammonia (NH3), which originates from agricultural activities and gasoline combustion, is the second highest contributor of nitrogen dry deposition to both lakes: contributing 13% to Lake Michigan and 32% to Lake Superior. The nitrogen dry deposition is approximately 68% of the nitrogen wet deposition over lake Superior, and approximately 80% of wet deposition over Lake Michigan. The over-water dry deposition velocity of HNO3 and NH3 were also evaluated. We obtained morning deposition velocities of 0.099 cm/s for NH3 and 0.095 cm/s for HNO3; and afternoon values of 0.137 cm/s for NH3 and 0.132 cm/s for HNO3. Another key finding is that the atmospheric concentrations of nitrogen compounds near Lake Michigan and Lake Superior have decreased since 2003. (C) 2018 Published by Elsevier B.V. on behalf of International Association for Great Lakes Research.
机译:苏必利尔湖的硝酸盐(NO3-)水平已从约5微米的历史水平增加到目前的约25微米。目前,大气对苏必利尔湖和密歇根湖的氮预算做出了重大贡献。这项研究提供了一个更明确的氮干沉降速率估算值,该估算值是通过将超水浓度测量值和原位气象测量值输入阻力模型得出的。我们得到的氮干沉积速率为[(3.41 +/- 2.26)x 10(7)kg N / yr; (5.90 +/- 3.91)千克牛顿/公顷/年]和[(1.54 +/- 1.06)x 10(7)千克牛顿/年; (1.87 +/- 1.27)千克N / ha /年]。源自化石燃料燃烧的硝酸(HNO3)占密歇根湖总氮干沉降的84%。 66%的人是苏必利尔湖。氨(NH3)来自农业活动和汽油燃烧,是两个湖泊的第二大氮干沉降贡献者:密歇根湖占13%,苏必利尔湖占32%。氮干沉降约占苏必利尔湖上氮湿沉降的68%,密歇根湖约占80%。还评估了HNO3和NH3的水上干沉降速度。 NH3的早晨沉积速度为0.099 cm / s,HNO3的早晨沉积速度为0.095 cm / s。 NH3的午后值为0.137 cm / s,HNO3的下午值为0.132 cm / s。另一个重要发现是,自2003年以来,密歇根湖和苏必利尔湖附近的氮化合物的大气浓度有所下降。(C)2018年由Elsevier B.V.代表国际大湖研究协会发布。

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