ORCID Profile
0000-0002-2121-6375
Current Organisations
KTH Royal Institute of Technology
,
The University of Edinburgh
,
Queen's University Belfast
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Publisher: AIP Publishing
Date: 04-2023
DOI: 10.1063/5.0146424
Abstract: Covalent amorphous semiconductors, such as amorphous silicon (a-Si) and germanium (a-Ge), are commonly believed to have localized electronic states at the top of the valence band and the bottom of the conduction band. Electrical conductivity is thought to occur through the hopping mechanism via these localized states. The carrier mobility of these materials is usually very low, in the order of ∼10−3–10−2 cm2/Vs at room temperature. In this study, we show that pure high-density amorphous Ge has exceptionally high carrier mobility, in the order of ∼100 cm2/Vs, and a high hole concentration of ∼1018 cm−3. The temperature-dependent conductivity of the material is also very-well defined with two distinctive regions, extrinsic and intrinsic conductivity, as in crystalline Ge. These results provide direct evidence for a largely preserved band structure and non-localized states within the valence band in high-density amorphous Ge, as previously suggested by Tauc et al. from optical characterization alone.
Publisher: Copernicus GmbH
Date: 23-09-2022
Abstract: & class=& quot age& quot title=& quot Page 1& quot & & class=& quot layoutArea& quot & & class=& quot column& quot & & & & strong& Introduction& /strong& & & & & The Asteroid Terrestrial Last-impact Alert System (ATLAS Tonry et al., 2018) is a network of robotic telescopes which scan the sky searching for transient phenomena from potentially hazardous Near Earth Objects to distant supernovae. The units at Haleakala and Mauna Loa have been operating since 2015 and 2017 respectively and together they can scan the visible night sky every two nights down to a limiting magnitude of ~19.5 mag in wideband orange and cyan filters. We have matched the ephemerides of ~445,000 asteroids to ATLAS pointings from these two units up to January 2022, providing us with a photometric database of 9.6& #215 & sup& & /sup& detections.& & & & We can investigate the surface scattering properties of asteroids by observing the change in brightness as a function of the observer-asteroid-Sun phase angle. A well determined phase curve is required to obtain an accurate absolute magnitude for an asteroid, and hence its size if albedo is known. The form of the phase curve depends on the scattering properties of the surface, primarily its composition and roughness, and is described by one or more slope parameters. These slope parameters can be used as a proxy for taxonomic information when more detailed measurements such as spectra are unavailable (e.g. Mahlke et al., 2021).& & & class=& quot age& quot title=& quot Page 1& quot & & class=& quot layoutArea& quot & & class=& quot column& quot & & & & strong& Methods& /strong& & & & & We have analysed the phase curves of all asteroids in our dataset of selected ATLAS photometry, considering & em& o& /em& and & em& c& /em& filter data separately. We fit a variety of phase curve models to the data using Levenberg-Marquadt least squares fitting but we focused on the results for the & em& HG& /em& (Bowell et al., 1989) and & em& HG& /em& & sub& & /sub& & sup& *& /sup& (Penttil& #228 et al., 2016) phase curve models specifically. We found that outlying photometric detections were present in the dataset due to brightness contamination from nearby stars/galaxies or incorrect matching of ephemerides. Such data points were dealt with by initial cuts and an iterative sigma clip during fitting.& & & & For simplicity we did not account for rotational brightness variation in the phase curve model as for most asteroids this is not accurately constrained. Rotation effects manifest as an additional variation in brightness which leads to greater uncertainty in determining phase curve parameters. However, we show in our results that the fitted phase curve parameters of an ensemble of objects with sufficient phase angle coverage are still useful for science on a population statistics level. Furthermore, we automatically identify asteroids in the dataset that show a significant apparition effect. The phase curves of these objects display shifts in absolute brightness between different apparitions, caused by changes in the asteroid aspect angle as viewed from Earth.& & & / & & / & & / & & class=& quot age& quot title=& quot Page 2& quot & & class=& quot layoutArea& quot & & class=& quot column& quot & & & The resulting phase curve parameters were then filtered down to a subset of nearly 100,000 objects with high quality phase curves suitable for comparing the surface properties of different asteroid populations. Objects were selected that have sufficient phase angle coverage, high number of observations, low formal uncertainties from the fitting process, and no strong apparition effects.& & & & & strong& Results& /strong& & & & class=& quot age& quot title=& quot Page 2& quot & & class=& quot layoutArea& quot & & class=& quot column& quot & & & We have derived phase curve parameters for a large number of asteroids obtained in a consistent manner from a single survey over a long baseline and we find this dataset to be useful for a range of science cases. We shall present results comparing the distribution of phase parameters and surface colours measured in the ATLAS & em& c& /em& -& & em& o& /em& filters of different asteroid populations. Considering the Jupiter Trojans, we can compare the properties of the leading and trailing dynamical groups and also assess trends in the & #8220 Red& #8221 and & #8220 Less-Red& #8221 compositional classes (Wong & Brown, 2016).& & & & Alongside this phase curve database we have generated a list of ~5000 Main Belt and Jupiter Trojan asteroids that exhibit strong apparition effects. Such objects must have high spin axis obliquity and would make interesting targets for studies of asteroid spin axis evolution and shape modelling via lightcurve inversion. Only 25% of the objects in our list are currently present in the Asteroid Lightcurve Database (LCDB Warner et al., 2021).& & & & In general our work highlights the possibilities and potential limitations of sparsely s led photometric surveys for investigating the properties of large numbers of asteroids. The upcoming Legacy Survey of Space and Time (LSST) will discover a huge number of new asteroids, however, characterisation of these objects will depend on survey design choices such as cadence and filter selection as well as follow up c aigns from other surveys/observers.& & & & & img src=& quot & quot alt=& quot & quot /& & & & class=& quot age& quot title=& quot Page 3& quot & & class=& quot section& quot & & class=& quot layoutArea& quot & & class=& quot column& quot & & & Figure 1: ATLAS photometry for 766 Moguntia, an asteroid that shows clear apparition effects. Left: Phase curves for each apparition, fixing & em& G& /em& = 0.15 and fitting only for & em& H& /em& . Observations are colour-coded by apparition. Right: Absolute magnitude of Moguntia over time, where each observation has been corrected for distance and phase effects. Error bars indicate the fitted & em& H& /em& and standard deviation of the residuals for each apparition, highlighting the shifts in brightness between apparitions and rotational brightness variations.& & & / & & / & & / & & / & & class=& quot age& quot title=& quot Page 2& quot & & class=& quot layoutArea& quot & & class=& quot column& quot & & & & strong& Acknowledgements& /strong& & & & & This work has made use of data from the Asteroid Terrestrial-impact Last Alert System (ATLAS) project. ATLAS is primarily funded to search for near earth asteroids through NASA grants NN12AR55G, 80NSSC18K0284, and 80NSSC18K1575 byproducts of the NEO search include images and catalogs from the survey area. The ATLAS science products have been made possible through the contributions of the University of Hawaii Institute for Astronomy, the Queen& #8217 s University Belfast, the Space Telescope Science Institute, the South African Astronomical Observatory (SAAO), and the Millennium Institute of Astrophysics (MAS), Chile.& & & class=& quot age& quot title=& quot Page 3& quot & & class=& quot section& quot & & class=& quot layoutArea& quot & & class=& quot column& quot & & & & strong& References& /strong& & & & & Bowell, E., Hapke, B., Domingue, D., et al. 1989, Application of Photometric Models to Asteroids., 524& #8211 & & & & Mahlke, M., Carry, B., & Denneau, L. 2021, Icarus, 354, 114094& & & & Penttil& #228 , A., Shevchenko, V., Wilkman, O., & Muinonen, K. 2016, Planetary and Space Science, 123, 117& & & & Tonry, J. L., Denneau, L., Heinze, A. N., et al. 2018, Publications of the Astronomical Society of the Pacific, 130, 064505& & & & Warner, B. D., Harris, A. W., & Pravec, P. 2021, Asteroid Lightcurve Database (LCDB) Bundle V4.0 Wong, I. & Brown, M. E. 2016, The Astronomical Journal, 152, 90& & & / & & / & & / & & / & & & & & & & / & & / & & / & & / & & / & & / & & / & & / & & / & & / & & / & & / &
Location: United Kingdom of Great Britain and Northern Ireland
Location: United Kingdom of Great Britain and Northern Ireland
No related grants have been discovered for James Robinson.