Mautner M N, Abdelsayed V, El-Shall M S, Thrower J D, Green S D, Collings M P, McCoustra M R S
Department of Chemistry, Virginia Commonwealth University, Richmond 23284, USA.
Faraday Discuss. 2006;133:103-12; discussion 191-230, 449-52. doi: 10.1039/b518207g.
Dust particles and their interaction with gases play important roles in star formation and in solar nebulae. Appropriate model dust grains are needed for the laboratory simulation of gas-grain interactions. Nanoparticles formed from carbonaceous meteorites may be particularly suitable, as these particles are formed from materials that were formed originally from interstellar/nebula dust. Extending our previous studies with grounded meteorite powders, we demonstrate here the production of nanoparticles formed from meteorites using the laser desorption/controlled condensation method developed in our laboratory. The product nanoparticle aggregates have porous, web-like morphologies similar to interstellar dust grains, indicating that they can present large specific surface areas for gas/grain interactions. In this paper, we present polarisation modulation reflection-absorption infrared spectra (PM-RAIRS) of supported thin films and compare these spectra with the known silicate bands in the spectra of interstellar dust recorded during the ISO mission. We also report an ultrahigh vacuum (UHV) temperature programmed desorption (TPD) study of the adsorption of CO on the supported nanoparticle films. The latter allow us to estimate the CO binding energy on the meteorite nanoparticles as 13.5 +/- 3.0 kJ mol(-1), cf. a value of 9.8 +/- 0.2 kJ mol(-1) for CO binding to a water ice substrate. Such thermochemical data can be useful for computational modelling of gas-grain interactions under the diverse conditions in interstellar clouds and solar nebulae.
尘埃颗粒及其与气体的相互作用在恒星形成和太阳星云中起着重要作用。实验室模拟气粒相互作用需要合适的模型尘埃颗粒。由碳质陨石形成的纳米颗粒可能特别合适,因为这些颗粒由最初源自星际/星云尘埃的物质形成。在我们之前对磨碎的陨石粉末研究的基础上,我们在此展示了利用我们实验室开发的激光解吸/控制冷凝法由陨石制备纳米颗粒。产物纳米颗粒聚集体具有类似于星际尘埃颗粒的多孔、网状形态,这表明它们可为气/粒相互作用提供大的比表面积。在本文中,我们给出了负载薄膜的偏振调制反射吸收红外光谱(PM - RAIRS),并将这些光谱与在ISO任务期间记录的星际尘埃光谱中的已知硅酸盐谱带进行比较。我们还报告了对负载纳米颗粒薄膜上CO吸附的超高真空(UHV)程序升温脱附(TPD)研究。后者使我们能够估计CO在陨石纳米颗粒上的结合能为13.5±3.0 kJ mol⁻¹,相比之下,CO与水冰底物结合的值为9.8±0.2 kJ mol⁻¹。这样的热化学数据对于在星际云团和太阳星云的不同条件下气粒相互作用的计算建模可能是有用的。