Environmental Research Institute, Shandong University, Jinan 250100, China; Collaborative Innovation Center of Climate Change, Jiangsu Province, China.
Environmental Research Institute, Shandong University, Jinan 250100, China.
Environ Pollut. 2017 Feb;221:418-426. doi: 10.1016/j.envpol.2016.12.004. Epub 2016 Dec 8.
Atmospheric black carbon (BC) is an important pollutant for both air quality and Earth's energy balance. Estimates of BC climate forcing remain highly uncertain, e.g., due to the mixing with non-absorbing components. Non-absorbing aerosols create a coating on BC and may thereby act as a lens which may enhance the light absorption. However, this absorption enhancement is poorly constrained. To this end a two-step solvent dissolution protocol was employed to remove both organic and inorganic coatings, and then investigate their effects on BC light absorption. Samples were collected at a severely polluted urban area, Jinan, in the North China Plain (NCP) during February 2014. The BC mass absorption cross-section (MAC) was measured for the aerosol samples before and after the solvent-decoating treatment, and the enhancement of MAC (E) from the coating effect was defined as the ratio. A distinct diurnal pattern for the enhancement was observed, with E 1.3 ± 0.3 (1 S.D.) in the morning, increasing to 2.2 ± 1.0 in the afternoon, after that dropping to 1.5 ± 0.8 in the evening-night. The BC absorption enhancement primarily was associated with urban-scale photochemical production of nitrate and sulfate aerosols. In addition to that, regional-scale haze plume with increasing sulfate levels strengthened the absorption enhancement. These observations offer direct evidence for an increased absorption enhancement of BC due to severe air pollution in China.
大气黑碳(BC)是空气质量和地球能量平衡的重要污染物。BC 气候强迫的估计仍然存在很大的不确定性,例如,由于与非吸收性成分混合。非吸收性气溶胶在 BC 上形成涂层,并且可以充当透镜,从而可能增强光吸收。然而,这种吸收增强受到限制。为此,采用两步溶剂溶解法去除有机和无机涂层,然后研究它们对 BC 光吸收的影响。在 2014 年 2 月,于中国华北平原(NCP)的严重污染城市济南收集了样品。在进行溶剂脱涂层处理前后,测量了气溶胶样品的 BC 质量吸收截面(MAC),并将涂层效应引起的 MAC 增强(E)定义为比值。观察到增强的明显的日变化模式,清晨的 E 为 1.3 ± 0.3(1 S.D.),下午增加到 2.2 ± 1.0,然后晚上-夜间下降到 1.5 ± 0.8。BC 吸收增强主要与城市尺度的硝酸盐和硫酸盐气溶胶的光化学产生有关。此外,硫酸盐水平升高的区域性霾羽流增强了吸收增强。这些观察结果为中国严重空气污染导致的 BC 吸收增强提供了直接证据。