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2002, Advances in Space Research
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4 pages
1 file
Micro-balances have been used in the past for volatile deposition monitoring in laboratory and in space environment. In order to determine their suitability to measure mass deposition in the form of solid particles, some topical aspects must be characterised, such as the sensitivity versus temperature and grain mass and the sticking efficiency versus grain speed. These parameters have been retrieved for different sensor configurations, i.e. with and without an adhesive coating, used in the perspective of improving the sensor particle collection efficiency. Our studies show that the adhesive coating improves the sensor sticking efficiency only for fast (100-400 m se') grains. However, the stability of the output signal with temperature is worse in the coated configuration by a factor of about ten. These results provide important inputs in the view of using micro-balances for dust monitoring. In particular, they have been carefully considered for the selection of the configuration of micro-balances, included as subsystems of the GIADA experiment onboard the ESA ROSETTA mission and aimed at studying flux and dynamic properties of cometary grains.
Advances in Space Research, 2007
The ESA ROSETTA mission will perform a rendezvous with comet 67P/Churyumov-Gerasimenko and will follow and study it from about 3.25 AU to perihelion at 1.34 AU and, during the foreseen extended mission, up to 2 AU post-perihelion, in order to observe for the first time the onset of activity of a comet and to follow its evolution. The GIADA (Grain Impact Analyser and Dust Accumulator) instrument, on board the ROSETTA orbiter, is aimed to analyse physical and dynamical properties of individual particles ejected by the nucleus and to monitor the dust flux and spatial distribution as a function of time. To achieve these scientific goals, GIADA is composed of different modules: an optical detection system, to monitor the light scattered by single particles entering the instrument, an impact sensor, to detect the momentum carried by the particles, and five micro-balances, to measure the dust flux from different directions. In this work we will describe the technical characteristics and the scientific performances of the flight model of the instrument. The preliminary results of GIADA calibration demonstrate that the instrument is perfectly compatible with design specifications and is suitable to achieve unprecedented scientific results about cometary dust physics.
Space Science Reviews, 2007
The Grain Impact Analyser and Dust Accumulator (GIADA) onboard the ROSETTA mission to comet 67P/Churyumov-Gerasimenko is devoted to study the cometary dust environment. Thanks to the rendezvous configuration of the mission, GIADA will be plunged in the dust environment of the coma and will be able to explore dust flux evolution and grain dynamic properties with position and time. This will represent a unique opportunity to perform measurements on key parameters that no ground-based observation or fly-by mission is able to obtain and that no tail or coma model elaborated so far has been able to properly simulate. The coma and nucleus properties shall be, then, clarified with consequent improvement of models describing inner and outer coma evolution, but also of models about nucleus emission during different phases of its evolution. GIADA shall be capable to measure mass/size of single particles larger than about 15 μm together with momentum in the range 6.5 × 10 −10 ÷ 4.0 × 10 −4 kg m s −1 for velocities up to about 300 m s −1. For micron/submicron particles the cumulative mass shall be detected with sensitivity 10 −10 g. These performances are suitable to provide a statistically relevant set of data about dust physical and dynamic properties in the dust environment expected for the target comet 67P/Churyumov-Gerasimenko. Pre-flight measurements and post-launch checkouts demonstrate that GIADA is behaving as expected according to the design specifications.
Icarus
Context. The Philae lander of the Rosetta mission, aimed at the in situ investigation of comet 67P/Churyumov-Gerasimenko, was deployed to the surface of the comet nucleus on 12 November 2014 at 2.99 AU heliocentric distance. The Dust Impact Monitor (DIM) as part of the Surface Electric Sounding and Acoustic Monitoring Experiment (SESAME) on the lander employed piezoelectric detectors to detect the submillimetre-and millimetre-sized dust and ice particles emitted from the nucleus. Aims. We determine the upper limit of the ambient flux of particles in the measurement range of DIM based on the measurements performed with the instrument during Philae's descent to its nominal landing site Agilkia at distances of about 22 km, 18 km, and 5 km from the nucleus barycentre and at the final landing site Abydos. Methods. The geometric factor of the DIM sensor was calculated assuming an isotropic ambient flux of the submillimetreand millimetre-sized particles. For the measurement intervals when no particles were detected the maximum true impact rate was calculated by assuming Poisson distribution of the impacts, and it was given as the detection limit at a 95% confidence level. The shading by the comet environment at Abydos was estimated by simulating the pattern of illumination on Philae and consequently the topography around the lander. Results. Based on measurements performed with DIM, the upper limit of the flux of particles in the measurement range of the instrument was of the order of 10 −8 − 10 −7 m −2 s −1 sr −1 during descent. The upper limit of the ambient flux of the submillimetre-and millimetre-sized dust and ice particles at Abydos was estimated to be 1.6 • 10 −9 m −2 s −1 sr −1 on 13 and 14 November 2014. A correction factor of roughly 1/3 for the field of view of the sensors was calculated based on an analysis of the pattern of illumination on Philae. Conclusions. Considering particle speeds below escape velocity, the upper limit for the volume density of particles in the measurement range of DIM was constrained to 10 −11 m −3 − 10 −12 m −3. Results of the calculations performed with the GIPSI tool on the expected particle fluxes during the descent of Philae were compatible with the non-detection of compact particles by the DIM instrument.
Advances in Space Research, 2002
The Grain Detection System (GDS) is part of the instrument GIADA (Grain Impact Analyser and Dust Accumulator), included in the scientific payload of the ESA Rosetta mission towards comet 46PiWirtanen. GIADA is aimed at analysing the grain dynamic properties and the dust flux evolution in the cometary environment. The GDS is devoted to the detection of single grains entering the instrument, to measure their velocity and to obtain information about their morphology and possibly composition. In this paper we describe the design of the GDS instrument and give some predictions on GDS performances at the comet. In particular, the simulation shows that the GDS will be able to count a total of 4.7 x lo5 particle "events" during all the GIADA operating phase and so satisfy scientific requirements for a statistically reliable analysis of cometary grains. 0 2002 COSPAR. Published by Elsevier Science Ltd. All rights reserved.
Space Science Reviews, 2007
The International Rosetta Mission is set for a rendezvous with Comet 67 P/Churyumov-Gerasimenko in 2014. On its 10 year journey to the comet, the spacecraft will also perform a fly-by of the two asteroids Stein and Lutetia in 2008 and 2010, respectively. The mission goal is to study the origin of comets, the relationship between cometary and interstellar material and its implications with regard to the origin of the Solar System. Measurements will be performed that shed light into the development of cometary activity and the processes in the surface layer of the nucleus and the inner coma.
Measurement Science and Technology, 2012
A new in-beam dust coordinate sensor (DCS) at the Colorado Center for Lunar Dust and Atmospheric Studies (CCLDAS) dust accelerator facility has been constructed and is now in use. The dust sensor operates by measuring the image charges induced on two planes of wire electrodes by passing charged dust particles. Applications for the DCS include the quantitative evaluation and improvements of the focusing and steering elements of the accelerator, and the correlation of particle velocity and mass with impact sites using precision particle location. For focusing and steering improvements, particle positions to 0.25 mm are plotted in real-time. It is possible to determine a typical particle's position within the beamline to < 0.1 mm. The design, simulation and results of the DCS are further discussed.
Advances in Space Research, 1998
We describe the scientific objectives, the design concept and the implementation of the Dust Flux Analyser (DFA) for the ESA Rosetta mission. DFA is designed to detect individual dust particles in order to study their physical and dynamical properties as a function of time and of orbital position, to monitor the spatial distribution of the dust production and correlate it with the nucleus emission sites and to analyse gas-dust interactions and the evolution of the coma. The instrument is composed of three detectors with a common electronic box. The Velocity Measurement System (VMS) will measure the velocity of the incoming dust particles and the dust detector (MOM), its momentum. A separate deposition system (DEP) composed of three quartz microbalances will monitor the cometary dust flux in three directions. DFA will be able to detect dust particles in the size range 5-1000/am and velocity range 0.1-150 m.s 1. Required resources are a mass of 4.9 kg, a power of 3.6 W to 16.7 W and a telemetry of 50 to 512 kBits per hour depending upon the operating modes. 01998 COSPAR. Published by Elsevier Science Lid.
Advances in Space Research, 2004
Among the main directions identified for future Martian exploration, the study of the properties of dust dispersed in the atmosphere, its cycle and the impact on climate are considered of primary relevance. Dust storms, dust devils and the dust ''cycle'' have been identified and studied by past remote and in situ experiments, but little quantitative information is available on these processes, so far. The airborne dust contributes to the determination of the dynamic and thermodynamic evolution of the atmosphere, including the large-scale circulation processes and its impact on the climate of Mars. Moreover, aeolian erosion, redistribution of dust on the surface and weathering processes are mostly known only qualitatively. In order to improve our knowledge of the airborne dust evolution and other atmospheric processes, it is mandatory to measure the amount, mass-size distribution and dynamical properties of solid particles in the Martian atmosphere as a function of time. In this context, there is clearly a need for the implementation of experiments dedicated to study directly atmospheric dust. The Martian atmospheric grain observer (MAGO) experiment is aimed at providing direct quantitative measurements of mass and size distributions of dust particles, a goal that has never been fully achieved so far. The instrument design combines three types of sensors to monitor in situ the dust mass flux (micro balance system, MBS) and single grain properties (grain detection system, GDS + impact sensor, IS). Technical solutions and science capabilities are discussed in this paper.
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