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Formaldehyde integral content in troposphere of Moscow Region: preliminary results of 6 years of measurements using DOAS technique

机译:莫斯科地区对流层中的甲醛积分含量:使用DOAS技术6年测量的初步结果

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Formaldehyde (HCHO) in the atmosphere is directly emitted by anthropogenic and biogenic sources and, more significantly, produced during oxidation of methane and other volatile organic compounds (VOCs), and so its content is one of observable indicators of air pollution by VOCs. HCHO has a sufficiently large absorption cross-section in the UV spectral region to be detected by the technique of the differential optical absorption spectroscopy (DOAS). Spectral measurements of scattered solar radiation are performed at Zvenigorod Scientific Station (ZSS, 55°41'49"N, 36°46'29"E) located in 38 km west from Moscow Ring Road by MAX-DOAS instrument since 2008. This location of the observational station allows evaluating the background levels of formaldehyde in the troposphere and the levels that are associated with pollution from Moscow. For analysis of the HCHO variability we selected spectra taken in cloud free conditions from October 2009 to April 2016. Version 1.3 of the retrieval algorithm is used. It uses information on the surface albedo and the height of the atmospheric boundary layer inferred from a model. It has optimized interpolation parameter of DOAS processing. Cloud screening algorithm using UV color index (the ratio of 370-nm radiance to 340-nm one) was implemented. The obtained data quantify the Moscow megapolis influence on air quality at Zvenigorod by comparison of HCHO VCD for east and west wind directions. HCHO VCD at East winds in average more than one at West winds for 0.4 ± 0.1 × 10~(16) mol×cm~(-2) at air temperatures from +5 to +35°C, and for 0.8 ± 0.2 × 10~(16) mol×cm~(-2) at temperatures from -20 to +5°C. It may be caused by Moscow emissions of HCHO precursors. Strong dependence of HCHO VCD on air temperature is noticeable in our data for air temperatures from +5 to +35°C. In different wind conditions the gradient of the temperature effect is about 0.86 ± 0.07 × 10~(15) mol×cm~(-2)×°C~(-1) in average. The increase of the formaldehyde content with the increase of the air temperature can be caused by the HCHO formation from non-methane biogenic volatile organic compounds for which more emission is expected at higher temperatures.
机译:大气中的甲醛(HCHO)由人体和生物源直接发出,并且更显着,更显着地在甲烷和其他挥发性有机化合物(VOC)氧化期间产生,因此其含量是VOCS的可观察到的空气污染指标之一。 HCHO在UV光谱区域中具有足够大的吸收横截面,以通过差分光学吸收光谱(DOA)的技术来检测。分散的太阳辐射的光谱测量在Zvenigorod Scientific Station(ZSS,55°41'49“N,36°46'29”e)位于2008年以来Max-Doas仪器以来,位于莫斯科环路路38公里处。这个位置在观察台允许评估对流层中甲醛的背景水平和与莫斯科污染有关的水平。为了分析HCHO可变性,我们从2009年10月到2016年4月的无云条件下所选择的光谱。使用检索算法的1.3版。它使用关于从模型推断的表面反玻璃的信息和大气边界层的高度。它具有DOAS处理的优化插值参数。实现了使用紫外线索引的云筛选算法(将370-nm辐射与340-nm的比率)实现。通过对东方和西风方向的比较,所获得的数据量化Zvenigorod在Zvenigorod对空气质量的影响。在东风的HCHO VCD平均超过一个在西风0.4±0.1×10〜(16)摩尔×cm〜( - 2),空气温度从+ 5到+ + 35°C,并且0.8±0.2×10 〜(16)×cm〜(-2)在-20至+ 5°C的温度下。它可能是由Hcho前体的莫斯科排放引起的。 HCHO VCD对空气温度的强烈依赖性在我们的空气温度从+ 5至+ + 35°C的空间中显着。在不同的风条件下,温度效应的梯度平均为约0.86±0.07×10〜(15)摩尔×cm〜(-2)×°C〜(-1)。随着空气温度的增加,甲醛含量的增加可能是由非甲烷生物挥发性有机化合物的Hcho形成引起的,在较高温度下预期更多排放。

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