Measurements to determine the mixing state of black carbon emitted from the 2017–2018 California wildfires and urban Los Angeles

oleh: J. Ko, T. Krasowsky, T. Krasowsky, G. Ban-Weiss

Format: Article
Diterbitkan: Copernicus Publications 2020-12-01

Deskripsi

<p>The effects of atmospheric black carbon (BC) on climate and public health have been well established, but large uncertainties remain regarding the extent of the impacts of BC at different temporal and spatial scales. These uncertainties are largely due to the heterogeneous nature of BC in terms of its spatiotemporal distribution, mixing state, and coating composition. Here, we seek to further understand the size and mixing state of BC emitted from various sources and aged over different timescales using field measurements in the Los Angeles region. We measured refractory black carbon (rBC) with a single-particle soot photometer (SP2) on Catalina Island, California (<span class="inline-formula">∼70</span> km southwest of downtown Los Angeles) during three different time periods. During the first campaign (September 2017), westerly winds were dominant and measured air masses were representative of well-aged background over the Pacific Ocean. In the second and third campaigns (December 2017 and November 2018, respectively), atypical Santa Ana wind conditions allowed us to measure biomass burning rBC (BC<span class="inline-formula"><sub>bb</sub></span>) from air masses dominated by large biomass burning events in California and fossil fuel rBC (BC<span class="inline-formula"><sub>ff</sub></span>) from the Los Angeles Basin. We observed that the emissions source type heavily influenced both the size distribution of the rBC cores and the rBC mixing state. BC<span class="inline-formula"><sub>bb</sub></span> had thicker coatings and larger core diameters than BB<span class="inline-formula"><sub>ff</sub></span>. We observed a mean coating thickness (CT<span class="inline-formula"><sub>BC</sub></span>) of <span class="inline-formula">∼40</span>–70 nm and a count mean diameter (CMD) of <span class="inline-formula">∼120</span> nm for BC<span class="inline-formula"><sub>bb</sub></span>. For BC<span class="inline-formula"><sub>ff</sub></span>, we observed a CT<span class="inline-formula"><sub>BC</sub></span> of <span class="inline-formula">∼5</span>–15 nm and a CMD of <span class="inline-formula">∼100</span> nm. Our observations also provided evidence that aging led to an increased CT<span class="inline-formula"><sub>BC</sub></span> for both BC<span class="inline-formula"><sub>bb</sub></span> and BC<span class="inline-formula"><sub>ff</sub></span>. Aging timescales <span class="inline-formula">&lt;</span> <span class="inline-formula">∼1</span> d were insufficient to thickly coat freshly emitted BC<span class="inline-formula"><sub>ff</sub></span>. However, CT<span class="inline-formula"><sub>BC</sub></span> for aged BC<span class="inline-formula"><sub>ff</sub></span> within aged background plumes was <span class="inline-formula">∼35</span> nm thicker than CT<span class="inline-formula"><sub>BC</sub></span> for fresh BC<span class="inline-formula"><sub>ff</sub></span>. Likewise, we found that CT<span class="inline-formula"><sub>BC</sub></span> for aged BC<span class="inline-formula"><sub>bb</sub></span> was <span class="inline-formula">∼18</span> nm thicker than CT<span class="inline-formula"><sub>BC</sub></span> for fresh BC<span class="inline-formula"><sub>bb</sub></span>. The results presented in this study highlight the wide variability in the BC mixing state and provide additional evidence that the emissions source type and aging influence rBC microphysical properties.</p>