1989年春季加拿大高北极对流层低层化学的观测

B.N Kieser , J.W Bottenheim , T Sideris , H Niki
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引用次数: 33

摘要

还进行了空中臭氧测量、粒子计数测量和气象观测。对罐和过滤器样品的分析提供了C2 - C4碳氢化合物和离子种类(Cl−,Br−,NO3−,SO42−,Na+, K+和NH4+)的数据。这些数据,连同对臭氧的观测,提供了对北极春季近地面臭氧消耗的进一步了解。观察到臭氧、乙烷、丙烷、i-丁烷、正丁烷和乙炔的浓度呈正相关。此外,有迹象表明臭氧浓度与可过滤溴之间呈负相关关系。对臭氧和碳氢化合物浓度之间关系的分析提供了证据,表明氯原子可能是所观察到的碳氢化合物耗竭的原因,而不是臭氧耗竭的原因。后者更容易用与溴原子的反应来解释。
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Spring 1989 observations of lower tropospheric chemistry in the Canadian high arctic

In the spring of 1989, airborne observations were made of C2−C4 hydrocarbons, ozone, and aerosols in the tropospheric boundary layer over a 96,000 km2 area in the vicinity of Alert, NWT, Canada (82.5° N, 61.5° W). Samples were collected in stainless steel canisters and on filters. Aerial ozone measurements, particle counting measurements, and meteorological observations were also made.

Analysis of the canister and filter samples has provided data on C2−C4 hydrocarbons and ionic species (Cl, Br, NO3, SO42−, Na+, K+, and NH4+). These data, together with observations of ozone, have provided further insight into the near-ground level ozone depletion during the Arctic spring. A positive correlation between the concentrations of ozone, ethane, propane, i-butane, n-butane, and acetylene was observed. In addition, there is an indication of a negative correlation between ozone concentrations and filterable bromine. An analysis of the relationship between the concentrations of ozone and hydrocarbons has provided evidence that chlorine atoms may be responsible for the observed depletion of hydrocarbons, but not ozone. The latter is more readily explained by reaction with bromine atoms.

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