Aerosol silica as a possible candidate for the heterogeneous formation of nitric acid hydrates in the stratosphere

16Citations
Citations of this article
13Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

The liquid-solid phase transitions in nanometer-size HNO3/H2O solution droplets obtained on fumed silica (a counterpart of aerosol silica) have been studied with differential scanning calorimetry (DSC). "Soft" transitions, reduction in the freezing and melting temperatures, Tf and Tm, and enthalpies, ΔHf and ΔHm, are interpreted to be caused by very small size of droplets. The observed difference between ΔHf and ΔHm can serve as an evidence of temperature dependence of the enthalpy of fusion for hydrates. Freezing of droplets with stoichiometry close to nitric acid trihydrate (NAT) at temperature 4 K warmer than the ice frost point indicates that, in the stratosphere, silica particles can serve as nuclei for heterogeneous freezing of NAT. Copyright 1999 by the American Geophysical Union.

Cite

CITATION STYLE

APA

Bogdan, A., & Kulmala, M. (1999). Aerosol silica as a possible candidate for the heterogeneous formation of nitric acid hydrates in the stratosphere. Geophysical Research Letters, 26(10), 1433–1436. https://doi.org/10.1029/1999GL900254

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free