Uk work on ExoMars for Aurora


Advanced Environmental Package (AEP+) – looking at the weather on Mars



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Advanced Environmental Package (AEP+) – looking at the weather on Mars

UK Institutes: Oxford University, Open University

Contact Simon Calcutt, calcutt@atm.ox.ac.uk , John Zarnecki, j.c.zarnecki@open.ac.uk Tel. +44 (0)1908 659599 Mobile: +44 (0)778 9900099
The investigation and understanding of the Martian surface environment is crucial for a number of reasons: Firstly, it determines the habitability of the Martian surface, for microbial life as well as for future human explorers. Secondly, the near-surface environment governs the exchange of heat, dust and water between the planetary surface and atmosphere and thus holds the key to unravelling current atmospheric processes as well as climate evolution. Thirdly, a better understanding of the surface environment in general, and turbulence and dust processes in particular, will be necessary for safe landing and operation of any future missions.
The AEP+ package, already selected by ESA for inclusion in the ExoMars mission, will measure atmospheric pressure, temperature and humidity, as well as wind speed and direction, dust momentum and optical depth. The AEP+ package will be led jointly by the Open University and Oxford University, drawing on their extensive experience in Mars meteorological instrumentation from the Beagle 2 Environmental Sensor Suite (ESS) as well as designs for the (now cancelled) NetLander ATMospheric Instrument Suite (ATMIS) and other missions. The proposed instrument suite has a modular design making it robust and flexible, minimising sensitivity to programmatic and technical risk. The sensor suite will be based on improved variants of instruments already deployed on previous missions resulting in a powerful yet resource-efficient instrument package.
This experiment will help characterise the Martian environment and provide answers to the following:


  • What's the weather like at the ExoMars landing site?

  • Could any living organisms survive in this environment?

  • How are global dust storms started?

  • How and where is water to be found on the planet?

  • How turbulent is the atmosphere of Mars?

Oxford University has a PPARC grant for evaluating prototype wind sensors, and to upgrade their Mars wind tunnel.


UV-VIS Spectrometer

UK Institutes: Open University, SSTL

Contact John Zarnecki, j.c.zarnecki@open.ac.uk Tel. +44 (0)1908 659599 Mobile: +44 (0)778 9900099
The OU are currently working on a one year ESA contract to develop the prototype, and will shortly start work on a PPARC grant (in conjunction with the Space Optics Group at SSTL) to develop the front end fibre-optic interface.
Ultraviolet (UV) and Visible (VIS) radiation play an important role in planetary environments, ranging from the photochemistry of upper atmospheres to the study of astrobiology. Visible light is required for photosynthesis, whilst UV can be extremely damaging to biological structures. The accurate determination of the solar UV/VIS flux reaching the surface of Mars is addressed by this proposal through the design, development and delivery of a space-qualified spectroscopic instrument for ExoMars.
The UV flux reaching the Martian surface has never before been directly measured. This instrument aims to achieve for the first time, high resolution spectra of the UV and visible flux present at the Martian surface.
The UV-VIS spectrometer (UVIS) is a miniature high-resolution spectroscopic instrument designed for inclusion on a Martian lander to address these unresolved issues. With extremely low mass and low power requirements (<300 g and <100 mW respectively), it provides an ideal candidate for any Martian science payload, giving a very significant science return in the form of a spectrum covering the UV and visible spectrum (200-650nm) at high resolution (1-2 nm).
Panoramic Camera – our eyes on Mars

Institutes: UCL, UWA, UCL/Birkbeck, University of Leicester, University of Surrey.

Contact Andrew Coates, ajc@mssl.ucl.ac.uk, Tel 01483 204145
This wide-angle panoramic camera (PanCam) is an essential element of the ExoMars Rover, led by UCL’s Mullard Space Science Laboratory (Andrew Coates, Andrew Griffiths). PanCam images will set the context for the ExoMars life detection experiments. As well as mapping, in 3D, the rover's immediate surroundings it will look at the distant scene to identify future targets of interest. PanCam will observe the drilling activities, look at rock layering, structure and composition, and examine the rover's traverse for newly exposed material. It will also look for any macroscopic evidence for biological activity.
The wide-angle camera is a stereo pair based on Beagle heritage. Just like our eyes, it senses depth and shape on the surface using 'machine vision' techniques, and spectral information gives geology (composition) and atmospheric information. PanCam will make the vital three dimensional models of the rover's surroundings. The PPARC R&D investment will allow explore if hyperspectral techniques (imaging over a range of wavelengths from 400-1000nm visible and near infrared) could replace fixed filters. Possible terrestrial uses of the technology include hostile environment robotics, e.g. the nuclear industry and bomb disposal.
Using attenuation of sunlight near sunrise and sunset, PanCam will measure the height profile of water vapour in the atmosphere. This water vapour is then blown away by the solar wind at the top of the atmosphere as Mars lacks a global magnetic field. Over billions of years, Mars dehydrates.
The High Resolution Camera part of PanCam (DLR, Germany provided) gives complementary images, effectively a zoom lens for detailed imagery of interesting targets and for high resolution panoramas.
PanCam images will be used for planning the rover's route across the Martian surface, in particular scientific site selection. Panoramas will be taken to examine the geology at each stopping point.
Major international collaborators are DLR, Joanneum Research (Austria), and Space X (Switzerland) and the Science Team includes a wider international team.
Robust EDLS (Entry, Descent and Landing Systems)

Institutions: LogicaCMG, Vorticity Ltd, Fluid Gravity, SSTL, University of Manchester, Open University, INSYS, Analyticon, University of Dundee

Contact: Andrew Hide, LogicaCMG, Email: andrew.hide@logicacmg.com Tel +44 7866 560239
A team led by LogicaCMG is developing technology aimed at ensuring a successful landing for ExoMars. The team combines the essential expertise to address the most critical phase of the ExoMars mission; the deceleration from hypersonic velocities at the top of the Martian atmosphere to a soft landing on the surface. This works builds on a successful track record with the Huygen’s probe which landed on Titan in January 2005.
The PPARC R&D investment will produce improved models of the Martian atmosphere and develop novel ways to determine location and speed during the descent through the atmosphere.

The research will focus on:



  • Entry point accuracy determination

  • Entry & Descent error propagation analysis

  • Transverse Velocity determination towards the end of the landing phase


Fluid Inertial Simulation – a gentle touchdown on Mars

Institution: Vorticity Ltd



Contact Steve Lingard steve.lingard@vorticity-systems.com Tel 01865 893 212 Mobile 07710 546654


Parachutes are an essential part of the ExoMars EDLS.


To land on Mars the parachute must be deployed at twice the speed of sound in order to give it time to decelerate the probe and be descending vertically by the time it reaches the surface. Designing a successful parachute requires understanding of how it is affected by supersonic flow. Simulating how parachutes work is complicated even at low speeds since the parachute is flexible and the airflow affects the shape of the parachute and in turn the shape of the parachute affects the airflow. This is called fluid structure interaction (FSI). At supersonic speeds the disturbance to the flow caused by the probe strongly affects the parachute.
The drag efficiency of the parachute falls rapidly above the speed of sound and the parachute can suffer rapid and repeated inflation and collapse. These oscillations could overstress the parachute structure and cause failure. To design a reliable parachute for ExoMars demands a full understanding of these phenomena.
Recent advances in computational power and techniques will enable Vorticity Ltd to simulate and understand the airflow around a flexible parachute leading to an improved parachute system with minimal instability risks.
The PPARC funding will enable the efficiency of different parachutes designs under different landing conditions to be modelled and evaluated.
Other work with a UK involvement:
Mars Organic Detector & Mars Oxidant Instrument (MOD and MOI)

Institution: Imperial College London



Contact: Mark Sephton, Tel: +44 (0)20 7594 6542, m.a.sephton@imperial.ac.uk
The Mars Organic Detector (MOD) instrument package searches for trace levels of specific organic molecules, amino acids and polycyclic aromatic hydrocarbons (PAH). These compound classes span all likely organic assemblages that may be detected on Mars. All life as we know it uses amino acids, while sedimentary (fossil) organic matter almost invariably contains some PAH; meteoritic organic matter contains both.
In MOD, mineral samples are heated to release the target compounds in gas form. From this form, PAH samples examined with a near-UV laser will fluoresce (emit light) naturally and can be examined with a spectroscope. To detect amino acids the sample holder will be covered with a chemical that reacts with them to fluoresce.
MOD is integrated with the Mars Oxidant Instrument (MOI), which is designed to characterise the chemical species and reactions responsible for the highly reactive nature of the Martian soil and perhaps the alteration and depletion of organic compounds that comprise the evidence of putative Martian life. In other words, if MOD does not detect organic compounds on Mars, MOI can tell us why.
The instrument, together with the drill, will allow scientists to understand the fate of organic molecules on Mars, by studying the distribution of organics and oxidants in the subsurface with unprecedented sensitivity. MOD/MOI is considered a fundamental instrument to achieve the mission's scientific objectives.
Magnetometer

Institution: Imperial College London, University of Edinburgh, University of Liverpool, British Geological Survey, University of Leicester,

Contact: Professor Steven Schwartz, Tel +44 20 7594 7660 s.schwartz@imperial.ac.uk
The magnetometer will make the first localised surface measurements of Mar’s magnetic field. Mars does not have a magnetic dynamo generating a field that protects the planets atmosphere from the solar wind, though it is thought to have had one in the past. Understanding what happened to the dynamo is key to the history of Mars. The magnetometer will contribute to our understanding of Martian history, study how the solar wind interacts with the planet’s atmosphere and characterise the environment for future missions. It will also add to our knowledge of re-surfacing effects on Mars (impacts, volcanoes, tectonics) as they have a effect on the magnetic surface field.
UK groups are working on pre-flight calibration, on-board software and scientific modelling.
Raman/LIBS spectrometer

Institution: Brunel University, CCLRC RAL, e2V, Bradford University



Contact: Chris Castelli, chris.castelli@brunel.ac.uk , Tel +44 (0)1895 266517, Mobile 07919160723
The combined Raman/LIBS (laser induced breakdown spectrometer) instrument is one of the ESA recommended instruments on the Pasteur Rover Exobiology Payload. This instrument will carry out detailed analysis of collected samples of rock within the rover analytical laboratory as well as remote sampling through the use of an external optical sensing head on the rover robotic arm. The powerful combination of the Raman & LIBS techniques will be used to determine the geochemistry, organic content and atomic composition of minerals.


Current design of the spectrometer from the EBB study

Raman spectroscopy has been demonstrated to be a viable non-destructive technique for the analytical interrogation of geological scenarios for life-detection signatures based on the presence of characteristic biochemicals produced by extremophilic organisms for their survival in hostile environments. Several advantages of Raman spectroscopic techniques for the molecular characterisation of extremophiles are easily translatable from terrestrial to extraterrestrial applications including an extended wavenumber range that covers signatures from both organic and inorganic molecular species and the identification of biogeological modifications and relict biomolecules present in the host geological matrices. In the ExoMars programme, this instrument will be seeking to record signatures of any organic materials and biomolecules that may be present.


TNO Science and Industry (Netherlands) leads a consortium of several European partners to develop the Elegant Bread Board model for the instrument under contract from ESA. The UK teams in this collaboration are providing the high performance, miniature CCD camera and front end electronics. This teaming arrangement builds on key technologies developed through the PPARC programme, in particular, space qualified low mass and power custom CCD readout ASICs development by RAL and flight qualified scientific CCDs from e2v. The scientific exploitation of the results is being led by Bradford University who are world leaders in the use of Raman spectra for the study of extremophiles in Mars analogue sites and for many years and have built up expertise in the recognition of biomolecular signatures obtained under a wide range of experimental conditions. Importantly, the Bradford Group is also integrated into the international Raman/LIBS instrument science working team led by Prof. Fernando Rull (University of Valladoid, Spain)
Mars Yard – simulating Mars on Earth

Institution: University of Wales Aberystwyth



Contact: Dave Barnes, dpb@aber.ac.uk Tel +44 01970 621561
The University of Wales Aberystwyth is constructing a Planetary Analogue Terrain Laboratory, informally known as a ‘Mars Yard’. They are equipping a 45 square metre area with soil and rocks that have similar mechanical properties to those found on Mars. The Mars Yard will be used to develop and test the movements of rovers for use on Mars.
Diagram: The Mars Yard will be used to test the same rover chassis concept as is being developed at EADS Astrium. The half scale model at Aberystwyth will be used to test additional designs options.


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