2017
DOI: 10.1021/acs.analchem.7b02381
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Atomic Force Microscopy-Infrared Spectroscopy of Individual Atmospheric Aerosol Particles: Subdiffraction Limit Vibrational Spectroscopy and Morphological Analysis

Abstract: Chemical analysis of atmospheric aerosols is an analytical challenge, as aerosol particles are complex chemical mixtures that can contain hundreds to thousands of species in attoliter volumes at the most abundant sizes in the atmosphere (∼100 nm). These particles have global impacts on climate and health, but there are few methods available that combine imaging and the detailed molecular information from vibrational spectroscopy for individual particles <500 nm. Herein, we show the first application of atomic … Show more

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Cited by 61 publications
(103 citation statements)
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“…The following computational scenarios are presented: Scenario 1, Δ shell /r total is a continuous function of the total radius (Δ shell is size resolved), as defined by equation (2); Scenario 2, Δ shell /r total is a fixed mean value for all sizes of particles (i.e., 0.44 for urban case and 0.32 for desert case); and Scenario 3, Δ shell / r total is discretized in two mean values, one for fine and one for coarse mode particles, as presented in section 3.4. It should be mentioned that some studies (Bondy, Kirpes, et al, 2017;Grassian & Tivanski, 2018) showed that particles can be also coated by much thin thickness of shell than the ones assumed 8. Histograms of axis ratio of particles with halo (core part only, denoted as particle cores) and particles without halo (denoted as not coated particles) for (a) urban and (b) desert cases.…”
Section: Optical Propertiesmentioning
confidence: 96%
“…The following computational scenarios are presented: Scenario 1, Δ shell /r total is a continuous function of the total radius (Δ shell is size resolved), as defined by equation (2); Scenario 2, Δ shell /r total is a fixed mean value for all sizes of particles (i.e., 0.44 for urban case and 0.32 for desert case); and Scenario 3, Δ shell / r total is discretized in two mean values, one for fine and one for coarse mode particles, as presented in section 3.4. It should be mentioned that some studies (Bondy, Kirpes, et al, 2017;Grassian & Tivanski, 2018) showed that particles can be also coated by much thin thickness of shell than the ones assumed 8. Histograms of axis ratio of particles with halo (core part only, denoted as particle cores) and particles without halo (denoted as not coated particles) for (a) urban and (b) desert cases.…”
Section: Optical Propertiesmentioning
confidence: 96%
“…More recently, AFM studies have incorporated more detailed analysis of specific properties, such as surface tension (Lee et al, , ) and hygroscopicity (Ghorai et al, ; Morris et al, ). An exciting advancement for AFM has been coupling with a scanning IR laser to conduct photothermal IR spectroscopy (Bondy et al, ; Kwon et al, ; Or et al, ). The operating principle of AFM‐IR is that when the tunable IR laser interacts with the sample at a frequency where it absorbs, the sample expands slightly causing the oscillation of the cantilever to change, and that signal can be converted back to an IR spectrum.…”
Section: Measurement Techniques For Aerosol Mixing Statementioning
confidence: 99%
“…For example, various "bulk" sample analyses conducted in the laboratory have confirmed the liquid-liquid phase separation do exist for the secondary particles [41,46,47]. The presence of the organic core and inorganic shell in individual particles have been confirmed in the laboratory by using optical microscopy and Raman spectroscopy [38,41,42], atomic force microscopy with infrared spectroscopy [48], and environmental scanning electron microscopy and scanning transmission X-ray microscopy [49].…”
Section: Possible Phase Transformation Of Cs Particlesmentioning
confidence: 92%