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Ship emissions of SO_(2) and NO_(2): DOAS measurements from airborne platforms

机译:SO_(2)和NO_(2)的船舶排放:机载平台的DOAS测量

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A unique methodology to measure gas fluxes of SO_(2) and NO_(2) from ships using optical remote sensing is described and demonstrated in a feasibility study. The measurement system is based on Differential Optical Absorption Spectroscopy using reflected skylight from the water surface as light source. A grating spectrometer records spectra around 311 nm and 440 nm, respectively, with the telescope pointed downward at a 30 deg angle from the horizon. The mass column values of SO_(2) and NO_(2) are retrieved from each spectrum and integrated across the plume. A simple geometric approximation is used to calculate the optical path. To obtain the total emission in kg h~(-1) the resulting total mass across the plume is multiplied with the apparent wind, i.e. a dilution factor corresponding to the vector between the wind and the ship speed. The system was tested in two feasibility studies in the Baltic Sea and Kattegat, from a CASA-212 airplane in 2008 and in the North Sea outside Rotterdam from a Dauphin helicopter in an EU campaign in 2009. In the Baltic Sea the average SO_(2) emission out of 22 ships was (54 +- 13) kg h~(-1), and the average NO_(2) emission was (33 +- 8) k gh~(-1), out of 13 ships. In the North Sea the average SO_(2) emission out of 21 ships was (42 +- 11) kg h~(-1), NO_(2) was not measured here. The detection limit of the system made it possible to detect SO_(2) in the ship plumes in 60percent of the measurements when the described method was used. A comparison exercise was carried out by conducting airborne optical measurements on a passenger ferry in parallel with onboard measurements. The comparison shows agreement of (-30 +- 14) percent and (-41 +- 11) percent, respectively, for two days, with equal measurement precision of about 20 percent. This gives an idea of the measurement uncertainty caused by errors in the simple geometric approximation for the optical light path neglecting scattering of the light in ocean waves and direct and multiple scattering in the exhaust plume under various conditions. A tentative error budget indicates uncertainties within 30-45percent but for a reliable error analysis the optical light path needs to be modelled. A ship emission model, FMI-STEAM, has been compared to the optical measurements showing an 18percent overestimation and a correlation coefficient (R~(2)) of 0.6. It is shown that a combination of the optical method with modelled power consumption can estimate the sulphur fuel content within 40percent, which would be sufficient to detect the difference between ships running at 1percent and at 0.1percent, limits applicable within the IMO regulated areas.
机译:描述了一种使用光学遥感技术测量船舶SO_(2)和NO_(2)气体通量的独特方法,并在可行性研究中得到了证明。该测量系统基于差分光学吸收光谱法,使用来自水表面的反射天光作为光源。光栅光谱仪分别记录大约311 nm和440 nm的光谱,望远镜指向与水平线成30度角的向下。从每个光谱中检索SO_(2)和NO_(2)的质量列值,并在羽流中积分。使用简单的几何近似来计算光程。为了获得总排放量(kg h〜(-1)),将整个羽流的总质量乘以视在风,即与风和船速之间的向量相对应的稀释因子。该系统在波罗的海和卡特加特海域进行了两次可行性研究,分别于2008年从CASA-212飞机和北海在鹿特丹郊外,在2009年的一次欧盟战役中由Dauphin直升机进行了测试。在波罗的海,平均SO_(2 )22艘船中的排放量是(54 +-13)kg h〜(-1),13艘船中的平均NO_(2)排放量是(33 +-8)k gh〜(-1)。在北海,21艘船的平均SO_(2)排放量为(42±11)kg h〜(-1),此处未测量NO_(2)。当使用上述方法时,系统的检测极限使得有可能在60%的测量值中检测出船羽中的SO_(2)。通过在客运渡轮上进行机载光学测量并与机载测量并行进行比较。比较显示两天的一致性为(-30 +-14)%和(-41 + -11)%,相等的测量精度约为20%。这给出了由光的简单几何近似中的误差引起的测量不确定性的概念,该误差近似于光波在各种条件下忽略了海浪中的光散射以及排气羽流中的直接和多次散射。暂定的误差预算表示不确定性在30%至45%之内,但要进行可靠的误差分析,必须对光路进行建模。船舶排放模型FMI-STEAM已与光学测量结果进行了比较,光学测量结果显示高估了18%,相关系数(R〜(2))为0.6。结果表明,将光学方法与模拟功耗相结合,可以估算出40%以内的硫燃料含量,这足以检测出IMO管制区域内适用的限值(分别为1%和0.1%)之间的差异。

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