TY - JOUR
T1 - Acoustic levitation with polarising optical microscopy (AL-POM)
T2 - water uptake in a nanostructured atmospheric aerosol proxy
AU - Milsom, Adam
AU - Squires, Adam M.
AU - Brasnett, Christopher
AU - Sharratt, William N.
AU - Seddon, Annela M.
AU - Pfrang, Christian
N1 - Publisher Copyright:
© 2023 RSC.
PY - 2023/9/26
Y1 - 2023/9/26
N2 - Laboratory studies on levitated particles of atmospheric aerosol proxies have provided significant contributions to our understanding of aerosol processes. We present an experimental method combining acoustic levitation with polarising optical microscopy (AL-POM) to probe optically birefringent particles, such as the nanostructured surfactant atmospheric aerosol proxy studied here. Birefringent particles were subjected to a step increase in humidity. A decrease in birefringence was measured over time as a result of a nanostructure change, confirmed by complementary synchrotron X-ray scattering. A multi-layer water uptake model was created and fitted to the experimental data, revealing a water diffusion coefficient increase by ca. 5-6 orders of magnitude upon phase transition. This has implications for the timescale of water uptake in surfactant-containing aerosols and their atmospheric lifetimes. This experimental setup has strong potential to be used in conjunction with other levitation methods and in different contexts concerning birefringent materials such as crystallisation.
AB - Laboratory studies on levitated particles of atmospheric aerosol proxies have provided significant contributions to our understanding of aerosol processes. We present an experimental method combining acoustic levitation with polarising optical microscopy (AL-POM) to probe optically birefringent particles, such as the nanostructured surfactant atmospheric aerosol proxy studied here. Birefringent particles were subjected to a step increase in humidity. A decrease in birefringence was measured over time as a result of a nanostructure change, confirmed by complementary synchrotron X-ray scattering. A multi-layer water uptake model was created and fitted to the experimental data, revealing a water diffusion coefficient increase by ca. 5-6 orders of magnitude upon phase transition. This has implications for the timescale of water uptake in surfactant-containing aerosols and their atmospheric lifetimes. This experimental setup has strong potential to be used in conjunction with other levitation methods and in different contexts concerning birefringent materials such as crystallisation.
UR - http://www.scopus.com/inward/record.url?scp=85174163502&partnerID=8YFLogxK
U2 - 10.1039/d3ea00083d
DO - 10.1039/d3ea00083d
M3 - Article (Academic Journal)
AN - SCOPUS:85174163502
SN - 2634-3606
VL - 3
SP - 1642
EP - 1650
JO - Environmental Science: Atmospheres
JF - Environmental Science: Atmospheres
IS - 11
ER -