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ZÁVACKÁ, K. NEDĚLA, V. OLBERT, M. TIHLAŘÍKOVÁ, E. VETRÁKOVÁ, Ľ. YANG, X. HEGER, D.
Originální název
Temperature and Concentration Affect Particle Size Upon Sublimation of Saline Ice: Implications for Sea Salt Aerosol Production in Polar Regions
Typ
článek v časopise ve Web of Science, Jimp
Jazyk
angličtina
Originální abstrakt
Using an environmental scanning electron microscope, we quantified for the first time aerosol-sized salt particles formed during the sublimation of sea ice as a function of temperature and concentration. The sublimation temperature of the ice is a dominating physical factor to determine the size of the residua: Below -20 degrees C, micron-sized pieces of salt emerge, whereas above the temperature large chunks of salt are detected. Another such aspect influencing the distribution of sizes in salt particles is the concentration: Micron-sized particles are observed exclusively at salinities below 3.5 psu, while below 0.085 psu particles with a median smaller than 6 mu m arise from sea ices at any subzero temperature. Moreover, when a chunk of salt sublimes at less than -30 degrees C to be dried and warmed later, a large number of sub-micron crystals will appear. We relate our findings to the production of the polar atmospheric sea salt aerosols.
Klíčová slova
sea salt aerosols; ozone depletion; sublimation; microscopy; eutectic temperature; bromine explosion
Autoři
ZÁVACKÁ, K.; NEDĚLA, V.; OLBERT, M.; TIHLAŘÍKOVÁ, E.; VETRÁKOVÁ, Ľ.; YANG, X.; HEGER, D.
Vydáno
28. 4. 2022
Nakladatel
AMER GEOPHYSICAL UNION
Místo
WASHINGTON
ISSN
0094-8276
Periodikum
GEOPHYSICAL RESEARCH LETTERS
Ročník
49
Číslo
8
Stát
Spojené státy americké
Strany od
1
Strany do
10
Strany počet
URL
https://doi.org/10.1029/2021GL097098
BibTex
@article{BUT178375, author="Kamila {Závacká} and Vilém {Neděla} and Martin {Olbert} and Eva {Tihlaříková} and Ľubica {Vetráková} and Xin {Yang} and Dominik {Heger}", title="Temperature and Concentration Affect Particle Size Upon Sublimation of Saline Ice: Implications for Sea Salt Aerosol Production in Polar Regions", journal="GEOPHYSICAL RESEARCH LETTERS", year="2022", volume="49", number="8", pages="1--10", doi="10.1029/2021GL097098", issn="0094-8276", url="https://doi.org/10.1029/2021GL097098" }