TiNet - A Concept Study for a Titan Geophysical Network LANGE Caroline, DEMBROVSKIS Andis, GROßE Jens, KOCH Aaron, MAIWALD Volker, QUANTIUS Dominik, ROSTA.

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Presentation transcript:

TiNet - A Concept Study for a Titan Geophysical Network LANGE Caroline, DEMBROVSKIS Andis, GROßE Jens, KOCH Aaron, MAIWALD Volker, QUANTIUS Dominik, ROSTA Roland, WAGENBACH Susanne, ZABEL Paul, VAN ZOEST Tim, SOHL Frank, KNAPMEYER Martin IPPW-9, 2012, Toulouse, France Chart 1

Study Overview Context: HGF Alliance for Planetary Evolution and Life Assess the potential for emergence and evolution of life on a planetary body Concept Car missions to answer the relevant scientific questions Go beyond the current NASA and ESA planning (low importance of cost and politics considerations) Why a geophysical network on Titan? Big research theme: interior of planetary bodies, and the interaction of interior- surface-atmosphere Titan due to its concurrent similarity with icy satellites as well as terrestrial planets + its uniqueness with regard to its surface conditions, atmosphere, interior is a key to increase the understanding of this topic How it was done: CE-Study at the DLR Concurrent Engineering Facility performed in October Postprocessing ongoing Chart 2

Geosaucer – a mission scenario to learn from… Titan Geophysics Package aka „Geosaucer“  feasibility study (2008) in the frame of the NASA/ESA TSSM (Titan Saturn System Mission) study 14 kg instruments and support package accommodated in Montgolfiere heat shield Instruments: magnetometer, seismometer, radio science X-band communication with patch antennas RTG + secondary batteries Backshell Montgolfiere Frontshell MMRTG* Payload Envelope Frontshield Instruments support S/S *Multi-Mission RTG Chart 3

Scientific Objectives Measure tidally induced surface displacements + forced librations of outer ice shell Measure time-variable magnetic field (induced and inducing) to determine location and thickness of internal ocean Measure the level of seismic activity; determine the structure of outer ice shell and deduce clues on internal ocean Measure regolith properties Measure atmospheric composition Optional: Determine the Titan lake composition Chart 4

Science Traceability Matrix Science ObjectiveMeasurementInstrumentPriority Pressure, Temperature, WindsPressure, temperature, windsIn-situ MET stationMid Atmospheric compositionChemical constituents and isotopic compositions GC/MSMid N2, NH3, CH4, CO originsIsotopic ratiosGC/MSHigh H2O and CH4 abundancesHumidity measurementsHumidity sensorLow Regolith chemical propertiesOrganic fallout speciationRaman spectrometer, LIBS, GC/MS High Regolith physical propertiesPermittivity and magnetic suszeptibility Permittivity probeMid Amount of cryovolcanismsTribolelectric effectTriboelectric sensorsLow Internal differentiation of the deep interior Tides, heat flow, seismicity, rotational state Radio Science, Seismometer, Heat flow probe, High Magnetic field environmentElectrical field, induced and inducing magnetic fields, and their time rates of change Magnetometer, permittivity probe High Interior composition: thickness and rigidity of ice layer; thickness, depth and electrical conductivity of liquid water ocean Tides, seismicity, permittivity, rotational state Radio Science, seismometer, permittivity probe High Chart 5

Mission Requirements and Constraints Mission goal: The mission shall establish a network of instrumented landing units on the surface of Titan, which operate simultaneously to measure geophysical parameters of the body Mission requirements: The mission shall be set in the timeframe. The mission lifetime shall be as a minimum 1 and maximum 2 Titan days. The landing sites shall fullfill the following requirements: 3 stations globally distributed are minimum for seismic measurements Sites shall: Be restricted to illuminated hemisphere Cover pole, mid-latitudes (45 deg, leading or trailing hemisphere) and equator (sub- resp. anti-saturnian hemisphere)  global dispersion A local dispersion shall be realized with the sub-landers (3-5 sub- lander) Chart 6

System Requirements The total mass of all units shall be < 320 kg (including EDL- subsystem / Thermal Protection) Functional requirements: The landing units shall be able to land on solid surface and in liquids The landing units (Remote units) shall be able to communicate their science and H/K data from any landing site and on-surface attitude to a relay satellite The landing units shall conduct science experiments autonomously Performance requirements: The landing units shall have a lifetime between 1 (T) and 2 (G) Titan days (1 Titan day = 15 Earth days) Chart 7

Architecture Trades Chart 8

Mission Overview – 1/2 A Cassini-size carrier transports the 3 entry probes to Titan Each probe enters separately and autonomously into the atmosphere, protected by a heat shield An additional deceleration stage (e.g. parachute) is deployed after heat shield separation. Arrival at Titan and Orbit insertion Inter-planetary Cruise with Swingbys Launch in the 2030s Network Deployment, EDL and Operation Chart 9

Mission Overview – 2/2 During descent the each entry probe, later Hub (main unit) releases 3 Remote Units which are diverted by the wind, e.g. using parachutes/paraglider Landing on Titan surface (soil or lake) System start-up and beginning of measurement program Relay of scientific data to the carrier now functioning as an orbiter in a stable polar orbit Chart 10

Instruments Small Instruments for geophysical measurements: (Top left) magnetometer from TU Braunschweig, proposed for Netlander; (Top right) Micro-Seismometer; (Bottom left) Pressure sensor from Mars MetNet lander; (Middle) humidity sensor (MetNet); (Bottom right) Tiltmeter (Lorenz) Chart 11

System Baseline Design - Configuration Entry Probe: Innovative sharp edged design to enhance descent stability. Predefined standardized payload compartments  payload easy excheangeable EDL Entry Probe: Passive system, self- stabilizing Remote Units: Deployment during descent. Parachute for attitude stabilization only Hub: Entry Probe reconfigured Releases Remote Units Passive attitude correction after landing Chart 12

Power Hub: GPHS RTG (NASA development), Pel = 19W max. / Pth = 250 W max. Remote: Assumption 2/3 physical size of GPHS RTG Pel = 10W, Pth = 125W Thermal Active: Heat of RTG is used. Heat switch and radiator to avoid overheating during cruise Heat switch to be enhanced. Heat shield: Basotec Foam, Huygens heritage Communication UHF link for communication between Hub and Remote Units (max. distance: 25km, Pt = 1W) X-Band for uplink to Orbiter, 2Mbit/s (Redundance via UHF link) No DTE Baseline Design cont‘d Chart 13

Mass Budget: Total Mass [kg] Mass including margins [kg] Instrument Mass [kg] Entry Probe Hub Remote Unit Total per Landing Site Total 3 Sites mm 1100 mm 266 mm 1280 mm Chart 14

Chart 15 Thank you! The TiNet Study Team

Backup Slides Chart 16> Lecture > Author Document > Date

InstrumentQuantityMass / unit [kg] Mass Total [kg] Very Broadband Seismometer (Opt 2)12.30 Tiltmeter (Geosystems)10.50 Magnetometer (TU Braunschweig)10.05 Micro-Seismometer/Acoustic sensor (Active) Titan Electric Environment Package – Lander (TEEP-L) MetBoom10.50 Titan Probe Imager, Radiometer Surface Science Package14.20 Total On Hub, but for science during descent: 1 kg descoped HASI 0.4 kg descent camera Instrument Suites: Hub

InstrumentQuantityMass / unit [kg] Mass Total [kg] Micro-Seismometer/Acoustic sensor10.40 Magnetometer (3-axial) Micro-GCMS (Massenspectrometer / MEMS)10.50 MetBoom10.50 Total Instrument Suites: Remote Unit

System Trade 1: Network Architecture -Centralized Architecture -Decentralized Architecture -vs. Chart 19

Centralized vs Decentralized Hub/Remote: Central Station (Hub) + 3 simple instrument packages (Remote Units) Local Network: 3 more „advanced“ instrument packages ProCon Hub/RemoteNo intelligence on subunits required Subunits can be more simple/only instrument „survival“ required Reduced mass on remote units (Comm, Data Handling) Instrument disturbancies/interferences from subsystems are reduced Interfaces and configuration (to instruments) easier to be standardized Option to implement active seismology 2 dedicated designs (Remote Unit and Hub) Local NetworkNo single-point failure (redundancy) Only one single design Single unit has higher applicability for future missions Descent scenario simplified Simpler/more reliable communication scheme Reduced P/L to system mass ratio Chart 20

P/L massEase of Deployment Reconfig.Reliability /Risk Data Rate /Comm Lifetime Hub/Remote +-+-+o Local Network -+-+-o Selected Network Architecture Hub/Remote configuration is the chosen architecture Lake vs. Soil: different equipment (e.g. some instruments exchanged, eventually modified mechanisms), same configuration Chart 21

Trade 2: Deployment Scenario cont‘d Option 1: Hub is carrier for remote units during entry  early separation (height 60km) and descent of RU‘s separately Option 2: deployment after landing Requirements: from science 1-10 km separation; from communication max. 10 km Unit massLanding Disperion Landing stability Reliability /Risk Science Return RU deployment during descent RU deployment after landing Chart 22