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Juno Jupiter image

Neil Bowles

Professor of Planetary Science

Sub department

  • Atmospheric, Oceanic and Planetary Physics

Research groups

  • Planetary atmosphere observation analysis
  • Planetary surfaces
  • Solar system
  • Space instrumentation
Neil.Bowles@physics.ox.ac.uk
Telephone: 01865 (2)72097
Atmospheric Physics Clarendon Laboratory, room 307
  • About
  • Publications

Spectral Characterization of Bennu Analogs Using PASCALE: A New Experimental Set‐Up for Simulating the Near‐Surface Conditions of Airless Bodies

Journal of Geophysical Research Planets American Geophysical Union (AGU) 126:2 (2021) e2020je006624

Authors:

KL Donaldson Hanna, NE Bowles, TJ Warren, VE Hamilton, DL Schrader, TJ McCoy, J Temple, A Clack, S Calcutt, DS Lauretta
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Spectral data of aqueously and thermally altered carbonaceous chondrites

University of Oxford (2021)

Authors:

Helena Bates, Kerri Donaldson Hanna, Ashley King, Neil Bowles, Sara Russell

Abstract:

Spectral data created as part of a study into the effects of aqueous and thermal alteration on the spectral signature in the NIR and MIR wavelength ranges. NIR data were collected as reflectance and MIR data were collected as emissivity under both ambient and simulated asteroid environment (SAE) conditions.
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X-ray diffraction data of aqueously and thermally altered carbonaceous chondrites

University of Oxford (2021)

Authors:

Helena Bates, Neil Bowles, Kerri Donaldson Hanna, Sara Russell, Ashley King

Abstract:

Position sensitive detector X-ray diffraction (PSD-XRD) data created as part of a study into the effects of aqueous and thermal alteration on the spectral signature in the NIR and MIR wavelength ranges. Data were collected on an Enraf-Nonius PDS120 X-ray diffractometer with an INEL curved 120o PSD. Each meteorite had two diffraction patterns collected on two 50mg aliquots (HB1 and HB2) of a larger 1.8g mass powdered sample.
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Author Correction: Shape of (101955) Bennu indicative of a rubble pile with internal stiffness

Nature Geoscience Springer Nature 13:11 (2020) 764-764

Authors:

OS Barnouin, MG Daly, EE Palmer, RW Gaskell, JR Weirich, CL Johnson, MM Al Asad, JH Roberts, ME Perry, HCM Susorney, RT Daly, EB Bierhaus, JA Seabrook, RC Espiritu, AH Nair, L Nguyen, GA Neumann, CM Ernst, WV Boynton, MC Nolan, CD Adam, MC Moreau, B Rizk, CY Drouet D’Aubigny, ER Jawin, KJ Walsh, P Michel, SR Schwartz, R-L Ballouz, EM Mazarico, DJ Scheeres, JW McMahon, WF Bottke, S Sugita, N Hirata, N Hirata, S-I Watanabe, KN Burke, DN DellaGiustina, CA Bennett, DS Lauretta
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Studying the composition and mineralogy of the hermean surface with the Mercury Radiometer and Thermal Infrared Spectrometer (MERTIS) for the BepiColombo mission: an update

Space Science Reviews Springer 216:6 (2020) 110

Authors:

H Hiesinger, J Helbert, G Alemanno, Ke Bauch, M D’Amore, A Maturilli, A Morlok, Mp Reitze, C Stangarone, An Stojic, I Varatharajan, I Weber, G Arnold, M Banaszkiewicz, K Bauch, J Benkhoff, A Bischoff, M Blecka, N Bowles, S Calcutt, L Colangeli, S Erard, S Fonti, Bt Greenhagen, O Groussain, H Hirsch, J Jahn, R Killen, J Knollenberg, E Kührt, E Lorenz, I Mann, U Mall, A Maturilli, A Morlok, L Moroz, G Peter, M Rataj, M Robinson, W Skrbek, T Spohn, A Sprague, D Stöffler, A Stojic, F Taylor, I Varatharajan, H Venus, J Warrell, I Walter, I Weber

Abstract:

Launched onboard the BepiColombo Mercury Planetary Orbiter (MPO) in October 2018, the Mercury Radiometer and Thermal Infrared Spectrometer (MERTIS) is on its way to planet Mercury. MERTIS consists of a push-broom IR-spectrometer (TIS) and a radiometer (TIR), which operate in the wavelength regions of 7-14 μm and 7-40 μm, respectively. This wavelength region is characterized by several diagnostic spectral signatures: the Christiansen feature (CF), Reststrahlen bands (RB), and the Transparency feature (TF), which will allow us to identify and map rock-forming silicates, sulfides as well as other minerals. Thus, the instrument is particularly well-suited to study the mineralogy and composition of the hermean surface at a spatial resolution of about 500 m globally and better than 500 m for approximately 5-10% of the surface. The instrument is fully functional onboard the BepiColombo spacecraft and exceeds all requirements (e.g., mass, power, performance). To prepare for the science phase at Mercury, the team developed an innovative operations plan to maximize the scientific output while at the same time saving spacecraft resources (e.g., data downlink). The upcoming fly-bys will be excellent opportunities to further test and adapt our software and operational procedures. In summary, the team is undertaking action at multiple levels, including performing a comprehensive suite of spectroscopic measurements in our laboratories on relevant analog materials, performing extensive spectral modeling, examining space weathering effects, and modeling the thermal behavior of the hermean surface.
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