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The Comet Astrobiology Exploration Sample Return (CAESAR) MissionThe Comet Astrobiology Exploration Sample Return (CAESAR) mission will acquire and return to Earth for laboratory analysis a minimum of 80 grams of surface material from the nucleus of comet 67P/Chur-yumov-Gerasimenko (67P). CAESAR will characterize the surface region sampled, preserve the collected sample in a pristine state, and return evolved volatiles by capturing them in a separate gas reservoir. NASA Goddard Space Flight Center provides project management, systems engineering, safety and mission assurance, contamination control, mission operations, and many other important functions. Northrop Grumman Space Systems will build the spacecraft, based on Dawn mission heritage, which like CAESAR, uses solar electric propulsion. CAESAR was selected by for Phase A study in the New Frontiers 4 Competition and will be proposed to New Frontiers 5.Collection of a sample from the surface of comet 67P is facilitated by a set of cameras that together provide images to support sample site selection, perform optical navigation, and document the sample before, during, and after col-lection. The sample is collected at the end of an arm during a 5-second touch-and-go (TAG) maneuver with the Sample Acquisition System (SAS)designed by Honeybee Robotics for the surface properties of comet 67P observed by the Rosetta mission. After sample collection, and while the sample is still cold (< -80°C), the TAG Arm inserts the sample container into the Sample Containment System (SCS) mounted inside the Sample Return Capsule (SRC). The SCS is sealed, preventing the sample from escaping into space. The sample is slowly warmed inside the SCS to enable sublimation of volatiles, which are collected in the Gas Containment System (GCS), a passively cooled gas reservoir. Separating the volatiles from the solid sample protects the solid sample from alteration. Once all sublimated H2O is transferred to the GCS, the GCS is sealed to capture the volatile sit contains, and the SCS is vented to space to maintain the solid sample under vacuum. The SCS vent is closed before Earth entry to prevent atmospheric contamination. Detailed laboratory analyses of the sample from 67P will trace the history of volatile reservoirs, delineate the chemical pathways that led from simple interstellar species to complex molecules, constrain the evolution of the comet, and evaluate the role of comets in delivering water and prebiotic organics to the early Earth. CAESAR will achieve these goals by carrying out coordinated sample analyses that will link macroscopic properties of the comet with microscale mineralogy, chemistry, and isotopic studies of volatiles and solids. Most of the sample (≥75%) will be set aside for analyses by generations of scientists using continually advancing tools and methods, yielding an enduring scientific treasure that only sample return can provide. This presentation will review development conducted during NF4 Phase A and discuss the NF5 mission concept.


Document ID
20205005754
Acquisition Source
Johnson Space Center
Document Type
Presentation
Authors
A G Hayes
(Cornell University Ithaca, New York, United States)
K Nakamura-Messenger
(Johnson Space Center Houston, Texas, United States)
S W Squyres
(Cornell University Ithaca, New York, United States)
D P Glavin
(Goddard Space Flight Center Greenbelt, Maryland, United States)
D F Mitchell
(Goddard Space Flight Center Greenbelt, Maryland, United States)
V E Moran
(Goddard Space Flight Center Greenbelt, Maryland, United States)
M B Houghton
(Goddard Space Flight Center Greenbelt, Maryland, United States)
D Douglas-Bradshaw
(Goddard Space Flight Center Greenbelt, Maryland, United States)
D S Lauretta
(University of Arizona Tucson, Arizona, United States)
K Yamada
(Japan Aerospace Exploration Agency Tokyo, Japan)
S Okazaki
(Japan Aerospace Exploration Agency Tokyo, Japan)
Y Satoh
(Japan Aerospace Exploration Agency Tokyo, Japan)
Y Maru
(Japan Aerospace Exploration Agency Tokyo, Japan)
T Nakao
(Japan Aerospace Exploration Agency Tokyo, Japan)
A Kukita
(Japan Aerospace Exploration Agency Tokyo, Japan)
T Shimoda
(Japan Aerospace Exploration Agency Tokyo, Japan)
T Yamawaki
(Japan Aerospace Exploration Agency Tokyo, Japan)
T Nakamura
(Japan Aerospace Exploration Agency Tokyo, Japan)
J E Parker
(Goddard Space Flight Center Greenbelt, Maryland, United States)
D C Wegel
(Goddard Space Flight Center Greenbelt, Maryland, United States)
H L Peabody
(Goddard Space Flight Center Greenbelt, Maryland, United States)
J P Dworkin
(Goddard Space Flight Center Greenbelt, Maryland, United States)
A N Nguyen
(Jacobs (United States) Dallas, Texas, United States)
S Clemett
(Jacobs (United States) Dallas, Texas, United States)
T J Zega
(Cornell University Ithaca, New York, United States)
E Mazarico
(Goddard Space Flight Center Greenbelt, Maryland, United States)
D Rowlands
(Goddard Space Flight Center Greenbelt, Maryland, United States)
S A Aslam
(Goddard Space Flight Center Greenbelt, Maryland, United States)
N Gorius
(Catholic University of America Washington D.C., District of Columbia, United States)
G Quilligan
(Goddard Space Flight Center Greenbelt, Maryland, United States)
Y Furukawa
(Tohoku University Sendai, Japan)
A Takigawa
(Kyoto University Kyoto, Japan)
G Blake
(California Institute of Technology Pasadena, California, United States)
M J Mumma
(Goddard Space Flight Center Greenbelt, Maryland, United States)
S N Milam
(Goddard Space Flight Center Greenbelt, Maryland, United States)
P A Gerakines
(Goddard Space Flight Center Greenbelt, Maryland, United States)
J I Lunine
(Cornell University Ithaca, New York, United States)
J L Mitchell
(Johnson Space Center Houston, Texas, United States)
L F Pace
(Johnson Space Center Houston, Texas, United States)
C D K Herd
(University of Alberta Edmonton, Alberta, Canada)
S Gorevan
(Honeybee Robotics (United States) Brooklyn, New York, United States)
J Spring
(Honeybee Robotics (United States) Brooklyn, New York, United States)
K Zacny
(Honeybee Robotics (United States) Brooklyn, New York, United States)
P C Chu
(Honeybee Robotics (United States) Brooklyn, New York, United States)
M M Hasegawa
(Goddard Space Flight Center Greenbelt, Maryland, United States)
C Guttler
(Max Planck Society Munich, Germany)
H Sierks
(Max Planck Society Munich, Germany)
J-B Vincent
(German Aerospace Center Cologne, Germany)
N Oklay
(German Aerospace Center Cologne, Germany)
H Campins
(University of Central Florida Orlando, Florida, United States)
Y Fernandez
(University of Central Florida Orlando, Florida, United States)
J Makowski
(Northrop Grumman (United States) Falls Church, Virginia, United States)
D Oberg
(Northrop Grumman (United States) Falls Church, Virginia, United States)
E L Morse
(Northrop Grumman (United States) Falls Church, Virginia, United States)
J M Soderblom
(Massachusetts Institute of Technology Cambridge, Massachusetts, United States)
D Bodewits
(University of Maryland, College Park College Park, Maryland, United States)
M Kelley
(University of Maryland, College Park College Park, Maryland, United States)
B Davidsson
(Jet Propulsion Lab La Cañada Flintridge, California, United States)
J Johnson
(University of Alaska Fairbanks Fairbanks, Alaska, United States)
A Kulchitsky
(University of Alaska Fairbanks Fairbanks, Alaska, United States)
R Kirk
(United States Geological Survey Reston, Virginia, United States)
L Leshin
(Worcester Polytechnic Institute Worcester, Massachusetts, United States)
K Oberg
(Harvard University Cambridge, Massachusetts, United States)
M Ravine
(Malin Space Science Systems (United States) San Diego, California, United States)
Date Acquired
July 31, 2020
Subject Category
Lunar And Planetary Science And Exploration
Meeting Information
Meeting: AGU Fall Meeting 2020
Location: San Francisco
Country: US
Start Date: December 7, 2020
End Date: December 11, 2020
Sponsors: American Geophysical Union
Funding Number(s)
PROJECT: 048290.02.01.01.05
Distribution Limits
Public
Copyright
Portions of document may include copyright protected material.
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