Overview of Primitive Object Volatile Explorer (PrOVE) CubeSat or Smallsat concept

Here we describe the Primitive Object Volatile Explorer (PrOVE), a smallsat mission concept to study the surface structure and volatile inventory of comets in their perihelion passage phase when volatile activity is near peak. CubeSat infrastructure imposes limits on propulsion systems, which are compounded by sensitivity to the spacecraft disposal state from the launch platform and potential launch delays. We propose circumventing launch platform complications by using waypoints in space to park a deep space SmallSat or CubeSat while awaiting the opportunity to enter a trajectory to flyby a suitable target. In our Planetary Science Deep Space SmallSat Studies (PSDS3) project, we investigated scientific goals, waypoint options, potential concept of operations (ConOps) for periodic and new comets, spacecraft bus infrastructure requirements, launch platforms, and mission operations and phases. Our payload would include two low-risk instruments: a visible image (VisCAM) for 5-10 m resolution surface maps; and a highly versatile multispectral Comet CAMera (ComCAM) will measure 1) H2O, CO2, CO, and organics non-thermal fluorescence signatures in the 2-5 μm MWIR, and 2) 7-10 and 8-14 μm thermal (LWIR) emission. This payload would return unique data not obtainable from ground-based telescopes and complement data from Earth-orbiting observatories. Thus, the PrOVE mission would (1) acquire visible surface maps, (2) investigate chemical heterogeneity of a comet nucleus by quantifying volatile species abundance and changes with solar insolation, (3) map the spatial distribution of volatiles and determine any variations, and (4) determine the frequency and distribution of outbursts.

[1]  Anita L. Cochran,et al.  Evolution of H2O, CO, and CO2 production in Comet C/2009 P1 Garradd during the 2011-2012 apparition , 2014, 1412.7410.

[2]  D. Elbaz,et al.  Mid-Infrared Spectral Diagnosis of Submillimeter Galaxies , 2007, 0711.1553.

[3]  K. Tsiganis,et al.  Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets , 2005, Nature.

[4]  K. Tsiganis,et al.  Chaotic capture of Jupiter's Trojan asteroids in the early Solar System , 2005, Nature.

[5]  M. DiSanti,et al.  Reservoirs for Comets: Compositional Differences Based on Infrared Observations , 2008 .

[6]  Harold F. Levison,et al.  Capture of the Sun's Oort Cloud from Stars in Its Birth Cluster , 2010, Science.

[7]  K. E. Gordon,et al.  Touch And Go Camera System (TAGCAMS) for the OSIRIS-REx Asteroid Sample Return Mission , 2018 .

[8]  Steven B. Charnley,et al.  The Chemical Composition of Comets—Emerging Taxonomies and Natal Heritage , 2011 .

[9]  Karen J. Meech,et al.  Debiasing the NEOWISE Cryogenic Mission Comet Populations , 2017 .

[10]  Emmanuel Lellouch,et al.  The infrared spectrum of comet C/1995 O1 (Hale-Bopp) at 4.6 AU from the Sun , 1996 .

[11]  Jeffrey Paul Morgenthaler,et al.  Observations of the forbidden oxygen lines in DIXI target Comet 103P/Hartley , 2013 .

[12]  Tony L. Farnham,et al.  Narrowband photometric results for comet 46P/Wirtanen , 1998 .

[13]  James D. Spinhirne,et al.  Stereo Cloud Heights From Multispectral IR Imagery via Region-of-Interest Segmentation , 2006, IEEE Transactions on Geoscience and Remote Sensing.

[14]  Hans Rickman,et al.  Origin and Evolution of the Cometary Reservoirs , 2014 .

[15]  Harold F. Levison,et al.  The Calibration of the Hubble Space Telescope Kuiper Belt Object Search:Setting the Record Straight , 1998, astro-ph/9806210.

[16]  Michel Combes,et al.  The 2.5-12 μm spectrum of comet halley from the IKS-VEGA experiment , 1988 .

[17]  Paul D. Feldman,et al.  The CO2/CO Abundance Ratio in 1P/Halley and Several Other Comets Observed by IUE and HST , 1997 .

[18]  H. Melosh,et al.  Deep Impact: Excavating Comet Tempel 1 , 2005, Science.

[19]  J. Sunshine,et al.  Asymmetries in the distribution of H2O and CO2 in the inner coma of Comet 9P/Tempel 1 as observed by Deep Impact , 2007 .

[20]  H. Melosh,et al.  EPOXI at Comet Hartley 2 , 2011, Science.

[21]  A. McEwen,et al.  Lunar Reconnaissance Orbiter Camera (LROC) Instrument Overview , 2010 .

[22]  Cliff Brambora,et al.  Nature of and lessons learned from Lunar Ice Cube and the first deep space cubesat 'cluster' , 2018, Optical Engineering + Applications.

[23]  L. Edwards,et al.  Context Camera Investigation on board the Mars Reconnaissance Orbiter , 2007 .

[24]  Jason McPhate,et al.  Detection of CO Cameron band emission in comet P/Hartley 2 (1991 XV) with the Hubble Space Telescope , 1994 .

[25]  M. Malin,et al.  The Thermal Emission Imaging System (THEMIS) for the Mars 2001 Odyssey Mission , 2004 .

[26]  Lori M. Feaga,et al.  Uncorrelated volatile behavior during the 2011 apparition of comet C/2009 P1 Garradd , 2013 .

[27]  Jacques Crovisier,et al.  THE PARENT VOLATILE COMPOSITION OF 6P/d’ARREST AND A CHEMICAL COMPARISON OF JUPITER-FAMILY COMETS MEASURED AT INFRARED WAVELENGTHS , 2009 .

[28]  M. E. Brown,et al.  The Size Distribution of Trans-Neptunian Bodies* , 2004 .

[29]  Munetaka Ueno,et al.  AKARI NEAR-INFRARED SPECTROSCOPIC SURVEY FOR CO2 IN 18 COMETS , 2012 .

[30]  John K. Davies,et al.  The outgassing and composition of Comet 19P/Borrelly from radio observations , 2004 .

[31]  Uwe Fink,et al.  A survey of 39 comets using CCD spectroscopy , 1995 .

[32]  Harold F. Levison,et al.  Late evolution of planetary systems , 2008 .

[33]  Michael D. Smith,et al.  Planetary Spectrum Generator: An accurate online radiative transfer suite for atmospheres, comets, small bodies and exoplanets , 2018, Journal of Quantitative Spectroscopy and Radiative Transfer.

[34]  Peter H. Schultz,et al.  COMETARY VOLATILES AND THE ORIGIN OF COMETS , 2012 .

[35]  J. Crovisier,et al.  Recent results and future prospects for the spectroscopy of comets , 2006 .

[36]  Brett Gladman,et al.  The Kuiper Belt and the Solar System's Comet Disk , 2005, Science.

[37]  Robert L. Millis,et al.  The ensemble properties of comets: Results from narrowband photometry of 85 comets , 1995 .