Characterization of the temperature and humidity-dependent phase diagram of amorphous nanoscale organic aerosols

被引:38
|
作者
Rothfuss, Nicholas E. [1 ]
Petters, Markus D. [1 ]
机构
[1] North Carolina State Univ, Dept Marine Earth & Atmospher Sci, Raleigh, NC 26795 USA
基金
美国能源部;
关键词
GLASS-TRANSITION TEMPERATURE; HETEROGENEOUS ICE NUCLEATION; CONDENSATION NUCLEI CCN; RELATIVE-HUMIDITY; WATER TRANSPORT; CHEMICAL-COMPOSITION; FUNCTIONAL-GROUPS; VISCOSITY; PARTICLES; SUCROSE;
D O I
10.1039/c6cp08593h
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Atmospheric aerosols can exist in amorphous semi-solid or glassy phase states. These states are determined by the temperature (T) and relative humidity (RH). New measurements of viscosity for amorphous semi-solid nanometer size sucrose particles as a function of T and RH are reported. Viscosity is measured by inducing coagulation between two particles and probing the thermodynamic states that induce the particle to relax into a sphere. It is shown that the glass transition temperature can be obtained by extrapolation to 10(12) Pa s from the measured temperature-dependent viscosity in the 10(6) to 10(7) Pa s range. The experimental methodology was refined to allow isothermal probing of RH dependence and to increase the range of temperatures over which the dry temperature dependence can be studied. Several experiments where one monomer was sodium dodecyl sulfate (SDS), which remains solid at high RH, are also reported. These sucrose-SDS dimers were observed to relax into a sphere at T and RH similar to those observed in sucrose-sucrose dimers, suggesting that amorphous sucrose will flow over an insoluble particle at a viscosity similar to that characteristic of coalescence between two sucrose particles. Possible physical and analytical implications of this observation are considered. The data reported here suggest that semi-solid viscosity between 10(4) and 10(12) Pa s can be modelled over a wide range of T and RH using an adapted Vogel-Fulcher-Tammann equation and the Gordon-Taylor mixing rule. Sensitivity of modelled viscosity to variations in dry glass transition temperature, Gordon-Taylor constant, and aerosol hygroscopicity are explored, along with implications for atmospheric processes such as ice nucleation of glassy organic aerosols in the upper free troposphere. The reported measurement and modelling framework provides a template for characterizing the phase diagram of other amorphous aerosol systems, including secondary organic aerosols.
引用
收藏
页码:6532 / 6545
页数:14
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