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Frederik Granzow Doktor

Publications and source records attributed to Frederik Granzow Doktor.

2 recordsLinked to original sources

Photoelectron and electron microscopy investigation of laboratory grown Mg-silicate space dust analogues

The atomic structure at the surface of interstellar silicate dust particles likely plays a key role in a variety of chemical processes occurring in star- and planet-forming regions of the interstellar medium (ISM). Here, we use the photoelectric effect to characterize, in situ, the local chemical structure of Mg-silicate nanoparticulate films, and ex situ electron microscopy to trace changes to morphology resulting from different starting compositions. Nanoparticulate films are prepared via co-deposition of Si, Mg and O atoms on a graphitic substrate under ultra-high vacuum (UHV) and are characterised with X-ray photoelectron spectroscopy and near edge X-ray absorption fine structure measurements. Analysis, supported by density functional theory calculations, shows that adjusting the Mg-to-Si ratio from 3.5 to 1.8 changes particle composition from a mixture of MgO and Mg-silicate towards predominantly Mg-silicate. Annealing in UHV also pushes the composition towards Mg-silicate, however, non-stoichiometric chemical motifs are always observed, presenting a distribution of potentially catalytically active sites. Electron microscopy images show composition-dependent film morphologies that restructure differently upon thermal annealing. The Mg-silicate nanoparticulate films presented here are characterised as a 2D version of ISM analogue dust particles prepared via laser ablation and are therefore a more readily suitable model for surface science investigations into the catalytic properties of interstellar Mg-silicate dust.

astro-ph.GA↗

How nanoscale physics shapes ice formation in the Universe: Rethinking gas freeze-out on dust grains

In cold molecular clouds, gas freeze-out onto dust grains initiates interstellar ice formation, yet sticking probabilities of heavy species are often assumed to be near unity at low temperature. Recent laboratory measurements on realistic grain analogues show that this assumption can fail. Using CO as a prototype, we investigate how nanoscale surface morphology controls adsorption and ice growth at 10 K on highly oriented pyrolytic graphite and carbon soot. X-ray photoelectron spectroscopy, low-temperature scanning tunneling microscopy, kinetic Monte Carlo simulations, and a thermodynamic description are combined to relate molecular retention to local surface structure. CO does not adsorb with unit sticking on graphite: adsorption proceeds through monolayer growth, a reduced-retention crossover near monolayer completion, and delayed multilayer growth. STM shows that CO remains highly mobile on graphite terraces and is stabilized mainly at island edges and terrace steps. On soot, the same sequence occurs at much higher exposures and with substantially lower sticking coefficients, while simulations show preferential retention in concave regions and poor wetting of convex asperities. These results indicate that low-temperature sticking is governed by post-impact exploration and competition between stabilization and escape. Nanoscale morphology amplifies this mechanism, reducing effective sticking probabilities and delaying gas freeze-out on realistic dust grains.

astro-ph.IM↗