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ETH-Zentrum
Phone: +41 44 633 36 25 |
Sea salt particles belong to the major aerosol components globally. They affect many aspects of the troposphere, e.g., atmospheric radiation, cloud physics, meteorology and atmospheric chemistry. Sea salt aerosols are of great importance for atmospheric chemistry. They have a large reservoir of halogens, which are highly reactive and have a substantial impact on the chemistry of hydrocarbons or ozone in the atmosphere. Such halogens can be released to the atmosphere by heterogeneous reactions between the aerosol and gas phase species, such as sulfuric or nitric acid.
Since heterogeneous reactions usually occur in the near surface region (~ the outermost 100 monolayers) of the condensed phase, we are especially interested in physical and chemical processes within this region of liquid or solid salt particles. Such processes include water adsorption, partitioning of ions between different phases, uptake of gas phase components into the condensed phase, chemical reaction and diffusive transport inside the condensed phase.
Using Rutherford Backscattering Spectrometry allows us to measure directly elemental concentration profiles down to a depth of about one micrometer with a typical resolution of 50 nm in salt crystals. This enables us to combine physical and chemical processes on the surface as well as inside the condensed phase to an overall picture. For further information about this technique, please visit http://www.eaglabs.com/training.
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