*Yuya Kobayashi1, Nobuyuki Takegawa1
(1.Graduate School of Science, Tokyo Metropolitan University)
![](https://confit-sfs.atlas.jp/customer/jpgu2021/web/OSPA.png)
Keywords:Sea salt aerosols, Online measurement, Quantification of each sodium salts
Sea salt aerosols are abundant in the marine boundary layer and have large influences on the Earth’s radiative budget. Significant conversion of sodium chloride (NaCl) to sodium sulfate (Na2SO4) or sodium nitrate (NaNO3) can take place via the reactions with sulfuric acid (H2SO4) or nitric acid (HNO3) in polluted air exported from urban areas to coastal regions. In situ, continuous measurements of NaCl, Na2SO4, and NaNO3 aerosols are needed to understand the chemical transformation of sea salt particles with air mass aging. However, there is no established method for quantifying these aerosol compounds with high time resolution. We have developed a new online particle mass spectrometer (refractory aerosol thermal desorption mass spectrometer; rTDMS) to quantify non-refractory and refractory sulfate aerosols. The combination of a graphite particle collector and a carbon dioxide (CO2) laser enables high desorption temperature (radiation temperature > 1200 K). The evolved gas molecules are detected by using a quadrupole mass spectrometer. The purpose of this study is to develop a new method for quantifying the mass concentrations of NaCl, Na2SO4, and NaNO3 aerosols by optimizing the laser desorption scheme of the rTDMS. Laboratory experiments were performed to test the instrument sensitivities to these aerosol compounds. The temporal evolution of ion signals at m/z 23 (Na+), 30 (NO+), 36 (HCl+), and 48 (SO+) during the laser desorption were monitored. Preliminary data indicate that ion signals originating from NaNO3, NaCl, and Na2SO4 particles were clearly identified by three sequential peaks associated with an increase in the radiation temperature. The limit of detection, linearity of the instrument response, and potential artifacts under real world conditions are discussed.