Abstract

Magnesium-rich silicates are ubiquitous both terrestrially and astronomically, where they are often present as small particles. Nanosized Mg-rich silicate particles are likely to be particularly important for understanding the formation, processing, and properties of cosmic dust grains. Although astronomical observations and laboratory studies have revealed much about such silicate dust, our knowledge of this hugely important class of nanosolids largely rests on top-down comparisons with the properties of bulk silicates. Herein, we provide a foundational bottom-up study of the structure and properties of Mg-rich nanosilicates based on carefully procured atomistic models. Specifically, we employ state-of-the-art global optimization methods to search for the most stable structures of silicate nanoclusters with olivine (Mg2SiO4)N and pyroxene (MgSiO3)N compositions with N = 1–10. To ensure the reliability of our searches, we develop a new interatomic potential that has been especially tuned for nanosilicates. Subsequently, we refine these searches and calculate a range of physicochemical properties of the most stable nanoclusters using accurate density functional theory based electronic structure calculations. We report a detailed analysis of structural and energy properties, charge distributions, and infrared vibrational spectra, where in all cases we compare our finding for nanosilicates with those of the corresponding bulk silicate crystals. For most properties considered, we find large differences with respect to the bulk limit, underlining the limitations of a top-down approach for describing these species. Overall, our work provides a new platform for an accurate and detailed understanding of nanoscale silicates.

Highlights

  • Silicates constitute the largest fraction of solid matter in the universe

  • Much of this silicate cosmic dust is formed around evolved oxygen-rich stars where it nucleates from small nanoscale clusters to form micrometer-sized grains, which are injected into the interstellar medium (ISM).[6]

  • Through the development of an interatomic potential (IP) that has been tuned for describing the structures and energetics of nanosilicates, we perform extensive global optimization searches to find new candidate global minimum (GM) isomers for olivine (Mg2SiO4)N and pyroxene (MgSiO3)N nanoclusters for N = 1−10

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Summary

Introduction

Bulk silicates form the basis for the geology of the earth’s crust and mantle,[1] weathering processes produce mineral nanoparticles which are widely distributed throughout many terrestrial systems.[2] Tonnes of small silicate particles enter our atmosphere every day in the form of interplanetary dust particles.[3] all planetary silicates have their origin in such extraterrestrial silicate dust, which is ubiquitously found in numerous astronomical environments.[4,5] Much of this silicate cosmic dust is formed around evolved oxygen-rich stars where it nucleates from small nanoscale clusters to form micrometer-sized grains, which are injected into the interstellar medium (ISM).[6] Before their eventual coalescence into larger bodies in protoplanetary disks, these grains follow a long and tumultuous journey through the ISM. We note that the modeling of brown dwarf atmospheres underlines the likely importance of (nano)silicates in cloud formation and the temperatures of such objects.[10,11]

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