Instrument Information |
|
IDENTIFIER | urn:nasa:pds:context:instrument:acp.hp::1.0 |
NAME |
AEROSOL COLLECTOR PYROLYSER |
TYPE |
SPECTROMETER |
DESCRIPTION |
Instrument Overview =================== See [ISRAELETAL2002] ACP's main objective is the chemical analysis of the aerosols in Titan's atmosphere. For this purpose, it will sample the aerosols during descent and prepare the collected matter (by evaporation, pyrolysis and gas products transfer) for analysis by the Huygens Gas Chromatograph Mass Spectrometer (GCMS). ACP's products transfer line (PTL) directly interfaces with an ACP-devoted GCMS feed tube. GCMS is used by ACP for about 20% of its operating time, based on a cooperative agreement between Service d'Aeronomie du CNRS (ACP) and NASA Goddard Space Flight Center (GCMS). Scientific Objectives ===================== The approach for selecting ACP's scientific objectives was to rely on the micro-physics models and on the results of specific laboratory studies. Two methods of producing Titan-like aerosols in the laboratory have been investigated. The first involves identifying these aerosols within the complex organic material that is often observed in the laboratory from simulating the photolytic and radiolytic processes expected in Titan's atmosphere. This material roughly corresponds to what Sagan's group labels 'tholins'. The second route for producing the yellowish aerosols that might correspond to those of Titan is by polymerising organic molecules using UV. The best candidate is C2H2, which polymerises more easily than C2H4 or HCN. These polymers are expected to form the aggregates that are needed to reconcile polarimetric and photometric results [WEST&SMITH1991; CABANEETAL1993; RANNOUETAL1994]. The optical properties of tholins and C2H2 polymers are in agreement with Voyager's observations. The chemical processes leading to these different particle types are not expected to occur in the same altitude ranges, owing to the diversity of the possible energy sources and their related vertical distribution. The polymerisation of C2H2 through the action of solar UV photons is expected, from current modelling, to yield C2nH2 at altitudes greater than ~ 500 km. The synthesis, in large amounts, of polymers of the form (C2H2)n in the lower stratosphere may be considered as rather unlikely, but depends on how the acetylene polymerises long-ward of 190 nm [CHASSEFIERE&CAB1995]. The formation of C-H-N tholin oligomers by the action of suprathermal Saturn plasma electrons, around 900-1000 km, or of energetic radiation belt particles at 350-400 km altitude, is shown to be the most plausible mechanism for explaining the haze's formation. Laboratory experiments providing the best reproduction of Titan's stratospheric conditions are needed to test, for example, the gas phase behaviour of tholin aerosols, and the optical properties of tholin or poly-C2H2 particles. In the low stratosphere, aerosol particles settling down from the upper levels may act as condensation nuclei. Below ~ 80 km, this should lead to the deposition of thin layers (< 0.01 um) of condensed gases (e.g. HC3N, HCN, C4H10) on the sub-um particles. This first stage is followed by a more consistent increase in the particle size, up to a few um, where the condensation of CO2, C3H8, C2H2 and C3H6 occurs, between 67 km and 63 km [FREREETAL1990]. The main condensation processes occur near the tropopause, with the condensation of C2H6 below 62 km, and in the troposphere, where CH4 and N2 condense on the resulting particle, which may yield cloud droplets ( ~ 100 um, see Toon et al., 1992). Another source of condensation nuclei may be the particles produced directly at these altitudes by the radiolysis of organic gases. The energy deposition of cosmic rays peaks near 60 km and, as on Earth, lightning may exist in the low troposphere. Tholins obtained from the sparking of He-CH4 and N2-CH4 mixtures have been studied with the ACP experiment in mind [ISRAELETAL1991; RAULINETAL1992]. The pyrolysis gas chromatography (Py-GC) of tholins produced at 77 K shows them to include saturated and unsaturated carbon chains in their structure; N-containing groups appear in the case of N2-CH4 sparking. The thermal desorption profile of these tholins clearly showed two peaks, the first corresponding to the distillation of condensed species, the second to the pyrolysis. The mass spectrometer (MS) study of the evaporated oligomers and pyrolysis products showed that a wide range of alkylated aromatic compounds evolved from the sample, which indicates that such solids contain a 3-D polymer with a high degree of branching. In other work [EHRENFREUNDETAL1995], the main peaks related to N-compounds observed in the GCMS are HCN, CH3CN, C2H5CN and longer chain nitriles. Only the saturated hydrocarbons are observed. The study of the evolution with temperature shows that HCN is a dissociation product during the whole Py-GC analysis process, which may imply that the nitriles can form thermostable structures in the tholins. From the above and from previous assessment, two classes of scientific objectives have been adopted: Primary objectives, can be satisfied from measurements made during Probe entry by ACP coupled with GCMS: 1. Determine the chemical makeup of the photochemical aerosol, i.e. infer the relative numbers of constituent molecules (C, H, N, O) composing the aerosol. 2. Obtain the relative abundances of condensed organics (e.g. C2H2, C2H6, HC3N, HCN) in a column average throughout the stratosphere. Compare with the abundance of constituent molecules in the aerosol nucleation sites. 3. Obtain the relative abundances of condensed organics (principally CH4, plus organics listed above) in a column averaged over the upper troposphere. Compare with the abundances of constituent molecules in the aerosol nucleation sites. Secondary objectives of fundamental interest can also be satisfied with the aid of additional information acquired by other Probe instruments (mainly the Descent Imager/Spectral Radiometer): 4. Obtain absolute abundance for all condensed species, averaged over the stratosphere and upper troposphere respectively. 5. Determine the mean sizes of aerosol nucleation sites averaged over the stratosphere, and compare with those in the upper troposphere. 6. Detection of non-condensable species, such as CO, eventually trapped in aerosols. Functional Description ====================== The gas products transferred from ACP are analysed by GCMS (NIEMANNETAL2002). A sampling system is required for sampling the aerosols in the 135-32 km and 22-17 km altitude regions of Titan's atmosphere. These altitude ranges refer to the Probe's nominal descent profile [LEBRETON&MATSON1997]. The sampling system requires an inlet (sampling) tube (ST) extending beyond the boundary layer (estimated to be few mm thick): the end protrudes 28 mm from the Probe's fore dome. During sampling, the collecting target's temperature must be as close as possible to that of Titan's atmosphere in order to help retain the more volatile aerosol and cloud particle components. The target is a filter (FIL), made in stainless steel (Beckaert ST10), that can be moved along the inlet tube. When the filter is in its sampling position, its front face extends a few mm beyond the inlet tube. This increases aerosol collection by direct impaction at high altitude, where the pump does not operate (see below). Before descent, the filter is held in its storage position inside the oven (OV). During descent, a mechanism (FIM) can move the filter to its sampling position and return it into the oven. The oven is a pyrolysis furnace where a heating element (OH) can heat the filter and hence the sampled aerosols to 250 deg C or 600 deg C. A motorised gate valve (GV) can be activated to close the furnace after filter retraction. Three normally-closed monostable valves (V1, V2, VT) are mounted on the oven's body. V1 supplies a labelled gas (15N2) to carry the gas sample from the oven to the transfer lines through V2. The venting valve VT allows the oven's gas content to be vented to Titan's atmosphere. VT is also usually activated during certain sequences for purging operations or under pressure control before transfers (see below). Also, VT can be opened at any time during descent as a safety measure if the oven pressure rises above 3.2 bar; it closes when the pressure falls to 2.7 bar. A drag fan kinetic pump (PU) ensures the flow of Titan's atmosphere through the filter, at a rate depending on altitude. An exhaust tube (ET), with a one-shot isolation valve (P2), allows the gas to be vented externally. The gas flow, on reaching the level of the GV, follows a path perpendicular to the oven/GV assembly. The result is that the circulation is independent of the GV status (closed or open). When it is switched off, PU acts as a flow-blocking device. The pressurisation system for storing N2 gas and controlling its flow to the oven begins with a gas tank (GT) at 40 bar. Oven filling is controlled by a pressure transducer (PS) associated with valve V1. A relief valve (RV, set at 4.1 bar) in the internal gas transfer line protects GCMS against accidental ACP overpressure. The whole internal circuit is pressurised during ground operations and the early part of the flight to Saturn. After the Jupiter flyby, about 3 years after launch, ACP's internal circuit is evacuated by opening P2. In addition, valves V1, V2 and VT are opened briefly during each cruise phase checkout. The gate valve mechanism (GVM) is locked during launch, and unlocked shortly after. It must be locked again for a short time before Probe entry; this is done during the last cruise checkout sequence. The inlet tube end is closed by a sealing cover (SC), which will be opened at the beginning of descent. A connecting tube (Product Transfer Line, PTL) between ACP and GCMS transfers the pyrolysis products. Valve P1 isolates the ACP internal circuit from the product transfer lines. This one-shot isolation valve is opened at the beginning of descent (T0+2 min) for an initial venting of the internal (ITL) and the external (PTL) exit transfer lines. The IVA one-shot valve isolates the PTL at its GCMS extremity. The T1, T2 and T3 special ports are for ground tests. The V2 and VT electrovalves, P1 and PTL can be heated by special heaters (HV1 for V1, HV2 for V2, HVT for VT, HP1 for P1 and HPTL for PTL). In addition, heater HV1 is controlled by a thermostat, activated when the temperature falls below -5 deg C. This prevents leakage caused by Titan's low temperatures. Measurement Strategy ==================== The operations sequences result from the following requirements: 1. Determining the compositions of the particle cores (non-volatile and volatile components) is conducted mainly in the low stratosphere and down to the tropopause (above 30 km). In the higher part of the descent (above 80 km), it is expected that aerosols will be obtained by direct impaction on the filter. Below 80 km, where the pump becomes effective, the samples are obtained by filtration. 2. The second sample must be collected within the troposphere above the deep methane clouds (20 km). 3. Owing to mass constraints, the instrument is equipped with a single collector that must be used again after cleaning the oven, filter and product transfer lines. 4. The samples are analysed by using GCMS for a fixed portion of its life (approximately 20 min), knowing that this instrument must make at least one direct chromatographic analysis of the atmosphere's composition before surface impact. In addition, because of the very short descent profile (120 min minimum), it was decided to make three transfers for each sample, each transfer using the direct MS mode. These will use, in turn, the oven at ambient temperature, 250 deg C and 600 deg C. A complete GCMS analysis, requiring about 10 min, is provided only for the first sample's pyrolysis sequence (transfer after 600 deg C heating). These pyrolysis products have to wait until GCMS has analysed the contents of the two gas enrichment cells that were sampled in the upper atmosphere. This implies that the use of the three gas chromatograph columns for analysing ACP aerosol pyrolysis products obtained at 600 deg C occurs at T0+73 min (nominal altitude 25 km). Operational Sequences ===================== A detailed timeline has been formulated to mesh with GCMS' own. It is based on the following sequences that ACP must operate during the descent phase. Sequence 1 Initial venting and preparation for the first sampling operation between ACP initialisation (at T0+1 min 40 s) and the filter in its sampling position (at T0+6 min 45 s, nominal altitude 130 km). Sequence 2 First sampling in the low stratosphere. This period ends when the filter is retracted into the oven (GV locked) at T0+60 min 00 s (nominal altitude 32 km). Sequence 3 Heating the filter (ambient, 250 deg C, 600 deg C) and gas product transfers to GCMS at T0+74 min 00 s (nominal altitude 24 km). Sequence 4 Oven and transfer lines cleaning, and preparation for the second sampling operation with the filter in its sampling position at T0+77 min 00 s (nominal altitude 22 km). Sequence 5 Second sampling in the upper troposphere. This period ends when the filter is retracted into the closed oven, at T0+89 min 00 s (nominal altitude 17 km). Sequence 6 Heating the filter (ambient, 250 deg C, 600 deg C) and gas product transfers to GCMS ends at T0+108 min 00 s (nominal altitude 9 km). During sequence 1, after the high entry velocity has been reduced and the Probe's protective front shield has been jettisoned - eliminating the risk of contamination from the front shield - the following operations begin at T0+1 min 40 s. P3 is opened, and flushing and venting the internal circuit begins by filling the circuit with N2 through V1 and V2 down to P1 (GV is closed). Venting is obtained by opening VT. The whole process is repeated after opening valve P1. The mechanism for ejecting the sealing cover (SC) is then activated, and in-flight calibration of the oven pressure sensor (PS) is performed to compensate for any offset accumulated during cruise. GV is then opened and the filter is moved into its sampling position. Sequence 2 begins immediately, with its two sampling modes. The first leaves the pump unit inactive (until approximately T0+23 min 30 s), so that sampling is by direct impaction. The second turns the pump unit, so that sampling is mainly by filtration. Once the pump is switched off, the filter is retracted and the oven gate is closed. Retraction and oven closing is accomplished in only 13 s in order to avoid any evaporation of certain condensates in the aerosols. The whole of sequence 2 takes about 55 min. Sequence 3 deals with: 1. the preparation of aerosols for producing evaporates and pyrolysis products; 2. the transfer of gas products to the ACP line (feed tube to GCMS); 3. the analysis either by the sole direct MS mode or the complete mode (GCMS + direct MS). The programme for aerosol preparation and transfer consists of three phases: Phase (a) transfer of the gas products obtained while the filter is in the unheated oven. At the time of transfer, the filter has considerably warmed since oven closing, and the temperature gradient is sufficient to produce some evaporates. Phase (b) transfer of gas products obtained after heating the filter to Tf=250 deg C. In order to avoid excessive pressure in the oven and hence in the ACP feed tube in GCMS, the oven is linked before heating to the atmosphere by briefly opening VT. In addition, to avoid condensations of gas samples, transfer lines ITL and PTL (valves and tubing) are heated as much as possible within the constraint of the allocated power; 90 deg C is the objective. During the transfer time (~ 1 min), the filter temperature is maintained by holding Tf at 250 deg C. Phase (c) transfer of the gas products obtained after heating the filter to 600 deg C. This pyrolysis phase is also preceded by briefly opening VT to reduce pressure to atmospheric. During transfer, the valves and tubes are heated within the power constraint as in phase (b); the goal is again 90 deg C. In order to transfer the gas samples with minimal dilution from the effluent gas (15N2), each injection into GCMS is done by pressurising the oven to 2.5 bar with N2 (V1 controlled, V2 closed) and then rapidly depressurising it (fast actuation of V2 and VAB). The estimated mass flow rate at injection is 3-9 mg/s at 2 bar N2. The same cycle is used for each analysis that occurs after phase (a), (b) and (c). As there are two sampling operations (one high altitude, one low altitude), the complete ACP programme equates to six transfer cycles. Each transfer cycle comprises two sub-cycles. The 'scientific sub-cycle' is devoted to analysing the oven contents by a series of six injections (V1 closed) of 0.875 s (V2 and VAB open) each, each followed by an MS analysis period of 4.750 s. This period for MS analysis is longer than the time required by GCMS for a full mass scan. After completion of the sixth MS analysis, VT and VAA are opened (VL4 is closed) for 5 s to evacuate any residual traces of pyrolysis products in the sampled volume. A second sub-cycle follows, devoted to a background analysis. Two 0.875 s injections are each followed by an MS analysis of 4.750 s. A second 5 s vent (VAA and VT open) completes the transfer cycle. The oven pressure must be controlled during each transfer for a correct GCMS analysis. An optimal interface requires that the pressure in the GCMS feed tube is maintained above 1.9 bar. Also, efficient sample transfer requires pre-injection pressurisation of the oven to 2.5 bar. During the pressurisation period (625 ms) a control loop uses the oven's pressure sensor to stay within the 2.5 bar limit (by closing V1 if needed). During injection, the control loop ensures a minimum 1.9 bar in the oven by opening V1 if necessary. (Note that V1 is closed by the software as part of the transfer cycle in any case at the end of the 625 ms pressurisation period). Furthermore, because of the unknown aerosol load collected on the filter, we have to accommodate any unforeseen increase in oven pressure after heating. The oven pressure is therefore checked before each transfer cycle. If it is above the nominal 2.7 bar, VT is opened until this value is reached. Owing to the peak power limit imposed by the Probe system (83 W on the ML3 main power line), there is a conflict between heating the oven and the transfer lines during the transfer cycle. It was thus imperative that a temperature control priority be selected by the software. The result is that heating the oven and holding it constant during the transfer of gas products to GCMS has first priority. Second priority is given to heating VT, P1 and PTL. In addition, during the preparation phase sub-sequence before oven heating, the temperature control loop of the transfer lines activates their heating for 1-2 min at 120 deg C. For sequence 4, before the second sampling stage, the filter, oven walls and transfer lines must be well cleaned. The oven and filter are cleaned, first, by extending oven heating by 1 min in order to complete filter outgassing (filter temperature is 600 deg C at the end of sequence 3's last transfer). Immediately after, the oven is filled to 2.5 bar within 3 s by activating the oven's pressure control loop to open V1. Then, the oven is vented by opening VT for about 6 s, reducing the pressure down to ambient atmospheric. Cleaning the transfer lines downstream of V2 is achieved first by switching on heaters HV2 and HP1 (plus PTL), set at the maximum 120 deg C for 90 s. Then, a fill-vent phase is started for the oven and transfer lines by: 1. switching on the oven's pressure control loop (filled at a maximum 2.7 bar) while valve V2 is opened for approximately 3 s; 2. venting the two circuits when reducing the internal pressure to the external level at the two ends. The oven is vented by opening VT (6 s), while the transfer lines downstream of V2 are vented through GCMS by opening VAA (few seconds). This fill-vent operation is repeated once. There is no background analysis from the MS in order not to contaminate the GCMS instrument unnecessarily. At the end of sequence 4, ACP is ready for a second sampling sequence. For sequence 5, sampling is performed by filtration in the cloud region. The altitude range is fixed by the time at which the pyrolysis products analyses must be finished so that GCMS is freed for direct GCMS analysis of the atmosphere. It means that the second sampling phase, which starts T0+77 min (nominal descent profile, 22 km) must be finished at T0+88 min 30 s (17 km nominal descent profile). Then, after about 11 min of sampling, the filter is moved back into the oven, which is closed for preparation and analysis. Before dealing with the next sequence, there is a standby period of 9 min in order to wait for GCMS as it completes its analysis of sample cell number 3. Sequence 6 is a copy of sequence 3 but during phase (c) there is no time left for GCMS to analyse the pyrolysis products through the columns - only the MS mode is used. Purging and background analysis are, as in sequence 3, performed after phase (a) and again after phase (b/c). At the end of the transfer (phase c) of the products to GCMS (T0+108 min), ACP is prepared for being turned off until T0+110 km (8 km nominal altitude). Mechanical Configuration ======================== The instrument housing is made of aluminium alloy and consists of a single unit mounted on the lower part of the experiment platform. The rectangular box carries six attachment lugs on its base. The electronics system (ACPE) has its own structure attached at six points on one side of the instrument's main body, in which the mechanical and pneumatic subsystem is located. ACP's maximum dimensions are 220x200x206 (H) mm. In addition to the inlet and exhaust tubes, and to the GCMS product transfer tube, there is an extension accommodating movement of the filter mechanism's rack. ACP's total mass is 6.7 kg (including 5% margin), shared between 4.5 kg for the mechanical box and 2.2 kg for the electronics box. The aerosols sampling inlet tube extends downwards to penetrate the Probe's fore dome. To provide efficient evacuation of Titan's atmospheric gas after sampling and filtering, the exhaust tube exits upwards, passing through the experiment platform and the top platform. By siting ACP close to GCMS, the inlet tube is close to the Probe's axis and PTL is as short as possible. A very strict procedure for limiting chemical contamination was followed during instrument fabrication. The objective values specified for the internal circuit of the gas transfer subsystem are <50 ppb for the organic compounds expected during aerosol chemical analysis and for gases such as CO2, CO and H2O. The internal surfaces of all the transfer tubes have been passivated ('silanised'). A cleanliness plan was followed first at the level of each equipment element and then at the instrument level. After assembly, the whole ACP was baked under vacuum for several days at 120 deg C. Also, organic materials were not used in the GV and filter mechanisms. Their bearings, in particular, are not lubricated. In order to maintain the high cleanliness level during the instrument's ground storage and its first part of the cruise, ACP's internal gas circuit was filled to 2.5 bar with pure nitrogen. The internal circuit is hermetically closed off, by three sealing devices, at the level of the sampling and exhaust tubes and at the interface between the ACP housing and the PTL. The specified instrument overall helium leak rate of 10^-7 mbar litre s^-1 was found to be sufficient to hold the gas circuit pressurised for more than 4 years. The two apertures leading to the atmosphere are sealed by specially-developed devices: the sealing cover (SC) for the sampling tube and the one-shot P2 valve for the exhaust tube. SC is screwed to the bottom of the sampling tube (ST); the tightness requirement is satisfied by a stainless steel O-ring gasket. SC's cap will be spring-ejected towards Titan at 11 m/s; the requirement was for 8.6 m/s in order to avoid back-collision with Huygens. The cap and spring, totalling 80 g, are held in position on SC's body by tin-silver solder. Ejection will be within 2 min of switching on the 53 W heater (SCH), as the alloy melts at about 150 deg C. Correct ejection is checked by a Hall effect sensor (HSC). The P2 concept is identical: melting a brazing allows a spring to eject the sealing cover, freeing the outlet gas exhaust. The P1 one-shot isolation valve between the ACP housing and PTL. Electronics =========== Hardware design --------------- ACP's electronic system (ACPE) is composed of four functional blocks: DC/DC converter, control unit, monitoring unit and drive unit. The structure has two frames and a base plate, both made of aluminium alloy. The first frame contains two parallel printed circuit boards (PCBs), one for the control unit (ACPCU) and one for the drive unit (ACPDU). The second frame, which has an integrated top plate, contains the monitoring unit (ACPMU) PCB and the components for the DC/DC converter block. After final integration the two frames are screwed together; the base plate is attached to the first frame, interfacing with the ACP mechanical main box. Huygens supplies ACP with three 28 V power lines: main lines ML1 and ML3 and protected line PL2. ACPDC's main functions are: (1) to provide ML1 input with DC conversion for supplying other electronics functional blocks; and (2) to provide all power lines with EMI filters. Conversion of ML1 DC is performed through a circuit that uses in series an SAE, AFC 461 F/CH for transient suppression, an SAE AT 02815 TF/CH for DC/DC conversion and one specific EMI filter to each output of the converter (0, +5, -15, +15 V). ACPDU drives all the electromechanical devices (electrovalves, heaters, motors) of the mechanical box. DU is galvanically isolated from the drive logic in CU. ACPMU conditions and monitors the temperature and pressure analogue signals coming from the sensors in the mechanical main box. Under software instruction, ACPCU controls ACP's motors, valves and heaters. For that purpose, it monitors first, inside ACPE, the transfer of actuation commands to ACPDU the flow of digital and analogue inputs from ACPMU. It also monitors all data transfers and synchronisation with ACP external systems such as the Probe, GCMS and ACP's EGSE. The data are transferred in two directions: (1) from the Probe's Command and Data Management Subsystem (CDMS) to ACP - mainly telecommands, descent data broadcast (DDB) and broadcast pulse (BCP); and (2) from ACP to the Probe - statusword and packet telemetry data (PTD). Synchronisation pulses are sent to GCMS for accurate timing of GCMS and ACP valve actuations during transfer periods. For activating and controlling mechanical and pneumatic components, the command signals generated within ACPCU are sent to ACPDU through a J21 connector. Status and sensor readings from ACP elements are transferred, after conditioning, to ACPMU. ACPCU's main components are the 80C85 8-bit microprocessor, the 80C37 direct memory address (DMA), a 4.096 MHz oscillator, two PROMS with 8 kbyte memory each, two RAMS with 8 kbyte memory each, a 12-bit analogue to digital converter (ADC) with a sample and hold amplifier (S&H), two 8-channel multiplexers (MUX) and two FPGAs (field programmable gate arrays). In addition, ACPCU contains memory latches, buffers and optocouplers. The microprocessor uses eight bits for data lines and 16 bits for address lines, eight of which are multiplexed with the address bus. The 4.096 MHz oscillator frequency is divided by one of the FPGAs to provide the non-maskable microprocessor interrupt with selectable clock pulses of 1, 2, 4, 8 or 16 ms. Two other interrupts of the 80C85 are used for BCP pulses every 125 ms (synchronised with the Probe) and overpressure signals. The 12 kbyte program is stored in the two 8 kbyte PROMS. When the ACPE main line (ML1) is powered by the Probe, the 12 kbyte are transferred to the two 8 kbyte RAMS. The remaining 4 kbyte in the RAM serve as data transient memory. DMA. driven by the FPGA timer, is used mainly for fast telemetry (TM) and telecommand (TC) management. Three of DMA's four request inputs are used for TM/TC data transfer from the 4 kbyte of the RAM to the Probe CDMS. The first two are used for nominal and redundant TM transfer, and the third for TC transfer. The monitoring signals (temperature, pressure and status) coming from ACPMU are used by the software for controlling the instrument. Analogue signals (temperature and pressure) are multiplexed and converted to digital signals into ACPCU. A total of 15 analogue input lines is multiplexed through the two MUXs. The MUXs output line selection is performed by one FPGA, then the selected signal is transferred via the S&H to the ADC for analogue to digital conversion. One of the two FPGAs controls the exchange of signals with the Probe (BCP, DDB, TC, TM). It also serves as pump current and speed counter. The other FPGA provides the microprocessor with a timer and a watchdog, and manages the ACPCU and ACPMU multiplexers. This FPGA also controls all the output command signals to ACPDU. Software design --------------- Onboard software is used by ACP's microcontroller to execute the automatic sequences, monitor the status and health of the various subsystems, acquire and interpret TC and format data for TM. Its main functions are to control the mechanical subsystem, collect data and transmit it to the Probe system, provide an interface to command ACP via the Probe, and perform descent measurements synchronised with the rest of the Probe. ACP's software provides four different operational modes: descent; cruise checkout; ground test mode: engineering mode. The first three execute automatically on receipt of the appropriate mission flag and time. The engineering mode is selectable by a specific TC, and is used mainly for integration and test phases. In this mode, all ACP functions can be activated individually by sending the appropriate TC. It is accessible during any automatic sequence. It can also be used to check specified mechanical devices during cruise should any problem arise. Calibration =========== Pyrolysis tests --------------- In order to validate ACP's scientific performance. pyrolysis tests were conducted at LISA in Paris on solid phase material synthesised from experimental simulation. The organic synthesis by electrical irradiation of an N2-CH4 mixture requires a long reaction time (about 20 h). The reactor is a two-part glass vessel with two tungsten electrodes and a metallic filter in the lower part. It is filled to a total pressure of 900 mbar with a mixture of N2 (800 mbar) and CH4 (100 mbar). One of the electrodes is connected to a Tesla coil fed by a low current (80-100 mA) high frequency (80-200 kHz) generator. The other electrode is Earthed. Five irradiation periods of about 4 h each were performed and, between each, the gas phase was removed from the reactor and replaced by a new mixture of N2-CH4 at 900 mbar with the same ratio as the original. During irradiation, the bottom of the reactor was cooled by liquid nitrogen. At the end of the synthesis, 2.3 mg of solids were deposited on the filter. An ACP model (M3) was specifically developed for this sort of science validation and laboratory investigation. It is representative of ACP except for the pump unit and the gas tank, which are not mounted. However, it contains: - the filter transfer mechanism (not motorised) to translate the filter into and out of the oven; - the gate valve mechanism (not motorised) to close off the oven; - the three monostable microvalves used to vent the oven by pumping (VT) to fill the oven with pure nitrogen piston gas (V1), and to transfer the gas phase from the oven to GCMS (V2). The filter could be dismounted from its support and easily replaced. In order to protect the filter's organic solid phase material from oxygen contamination, the following operations were carried out in a glove box filled with nitrogen: - once removed from the reactor, the filter was mounted in M3; - M3's gate valve was closed after enclosing the filter in the oven. Owing to the oven's low leak rate (<10^-3 mbar l s^-1 ), we can be sure that no oxygen contamination of the filter occurred during analysis. The analysis of the pyrolysis products was done at LISA, where a Varian Saturn II GCMS was used (with helium as carrier gas) at an inlet pressure of 1.6 bar. The chromatographic capillary column was a CP-Sil-5 CB column of 25 m length, 0.15 mm inside diameter and 1.20 mm film thickness from Chrompack. The column temperature was controlled thus: 30 deg C for 20 min; raised from 30 deg C to 150 deg C in 30 min at 4.0 deg C/min; 150 deg C for 10 min. The total mass spectra of the GC peaks were thus collected over 60 min. The ion trap detector was able to detect masses of 10-226 amu by using the electronic ionisation mode. The experimental chromatographic conditions were chosen to detect hydrocarbons from C4 to C10, which excludes any information about the light hydrocarbons (C2 and C3) and the heavy hydrocarbons (above C10). Using this experimental approach, we achieved a very good validation of ACP for the 600 deg C pyrolysis sequence that will be performed on the sampled aerosols during Probe descent. The chromatogram obtained by GCMS analysis of the synthesised solid phase yields a pyrogram showing many organic compounds. Some GC peaks appear clearly from the total mass spectra. The others are identified only when they are specific ions with a very high MS sensitivity. According to their mass spectra, 23 gross formulas of more than 25 GC peaks have been identified unambiguously. The numbered peaks were identified and the possible isomers according to their mass spectra were suggested. It immediately appears that no oxygenated organic compounds were detected, showing that the laboratory procedure prevented oxygen contamination of the synthesised solid phase material. The main compounds detected on the pyrogram are mono aromatic hydrocarbons. The most concentrated is benzene (12), followed by toluene (16) and C2-substituted benzene (19, 21, 22). One may conclude that these mono aromatic hydrocarbons are the major constituents of the synthesised solid phase material. If they are thermally stable, they could be completely desorbed into the gas phase at 600 deg C with no variation of their structures. Thus the main constituents are the main compounds desorbed and detected on the pyrogram. One argument limits the validity of this result. Since a bi-aromatic hydrocarbon is observed on the pyrogram (23) and because of the chromatographic conditions (choice of column), we cannot properly observe poly aromatic hydrocarbons. In a previous study, pyrolysis of anthracene, which contains three aromatic cycles, was performed with the same pyrolyser at 600 deg C. The pyrogram showed mainly benzene, toluene, ethenyl-benzene and C8H10 isomers. It shows that poly aromatic hydrocarbons are decomposed at 600 deg C in benzene and in substituted mono aromatic hydrocarbons. The type of compounds detected on anthracene pyrograms depends on the pyrolysis temperature. For example, it was shown that naphthalene (a bi-aromatic hydrocarbon) was clearly observed at a lower pyrolysis temperature. So it is quite possible that the mono aromatic hydrocarbons detected on the pyrogram could be provided by the poly aromatic hydrocarbons present in the solid phase material and thermally decomposed at 600 deg C into mono aromatic hydrocarbons. A small amount of benzonitrile (20) was also detected, which can be similarly produced by thermal decomposition of poly aromatic compounds containing nitrogen atoms. Most of the nitriles observed on the pyrogram have also been detected in the gas phase synthesised by the simulation (3, 4, 7, 8 and 11). The heaviest nitriles detected (14 and 15) could be provided by thermal desorption of the same compounds present in the solid phase or by thermal decomposition of the heaviest molecules. Finally, many hydrocarbons are detected on the pyrogram (1, 2, 5, 6, 9, 10 and 13). They can be provided by the two sources cited above, or by the thermal polymerisation of the lightest alkenes and alkynes. Before performing the above pyrolysis tests, the procedure for testing the cleanliness of the ACP Flight Model, after delivery by SEP, was conducted on M3. The instrumentation includes a very pure nitrogen gas reservoir, a flow regulator provided by the contractor, and laboratory GCMS. A mixing ratio threshold of 50 ppb was measured for the significant gas components. Validation tests of the direct Mass Spectrometer mode ----------------------------------------------------- Tests were run to verify the ACP transfer cycle and to validate the data obtained by GCMS in the direct MS mode (direct inlet flow into the dedicated ACP ion source of GCMS). Several nominal sequences reproducing the ACP transfer cycle were conducted at LISA using a commercial quadrupole mass spectrometer. The verified transfers correspond to the nominal descent phase when ambient oven temperature analyses are made after the first aerosol sampling period. GCMS valve VAB was replaced by a commercial Buerkert valve to which a commercial Lee-Jeva restrictor, representing FRA, was added. Flow restriction equivalent to that provided by VL4 on Huygens was reproduced by using a capillary fused silica tubing of 10 um internal diameter and 6 cm length. For testing the ACP-MS coupling, the oven was filled at 30 mbar with pure krypton. The mass spectra obtained (mass 84) is representative of the amount of krypton injected. Quantitatively, the decrease in krypton's pressure corresponds exactly to the specifications for transferring the oven's atmospheric content. It confirms that the calibration of the FRA restrictor used for the M3 model (Lee Jeva 80000 Lohm) gives the correct flow for the ACP-GCMS coupling of the Huygens experiment. The observed pressure peaks correspond to the simultaneous opening of V2 and VAB causing an increase in the total pressure and krypton's partial pressure in the V2-VAB line. This phenomena is smoothed on the figure by acquiring one point per second. In the GCMS experiment, a scan of the entire mass spectra will last about 2 s, so the smoothing of the curve obtained should be greater. The calibration programme ------------------------- The programme selected for calibrating the flight models is directly linked to the GCMS calibration plan (see the GCMS paper in this volume). As GCMS will analyse the gas products transferred from ACP, the calibration system at NASA Goddard was used to relate (qualitatively and quantitatively) GCMS' mass spectra to the effluent gases injected from ACP. ACP calibration is a 2-step process and concerns only the gas phase transfer. This is because we do not wish to pollute the Flight Models' ACP internal tubing and GCMS analyser with products of solid samples such as tholins or other complex matter. The tests allowed the evaluation of GCMS' response to the ACP products. The first step directly injected several calibrated gas or gas mixtures containing expected Titan ratios into the ACP feed tube (IVA-VAB). The second step, which requires the calibration gas to pass through ACP first, has been delayed because of the very tight GCMS delivery schedule. This part of the calibration programme will be performed immediately after launch, on the two spare models. The second step was similar but the calibrated gas passed through ACP first. For that, the calibrated gas mixtures were injected from Goddard's calibration bench into the oven using the special inlet T3 (to be pinched off). During the investigation, the oven will be heated according to ACP's timeline before each nominal transfer cycle. The oven pressure will be set to simulate the conditions after the completion of each of the two aerosol sampling phases. The oven's gas tightness when the gate valve is locked is sufficient (leak rate 10^-3 mbar l s^-1) to prevent any change in the calibrated gas concentrations during the analysis process. In the ACP configuration at Goddard, isolation valve P1 will be replaced by a dummy valve with a punctured diaphragm in order to allow passage through to GCMS. During ACP integration on Huygens, the pneumatic connection to GCMS was made by attaching PTL between the two. This was followed by a special procedure for cleaning and filling the PTL with pure N2. Flight Model cleanliness was assured and controlled by following the same procedure as with the M3 model. During post-launch calibration, pyrolysis tests and chromatographic analysis are planned at Goddard using representative mock-ups of the GCMS and ACP Flight Models. |
MODEL IDENTIFIER | |
NAIF INSTRUMENT IDENTIFIER |
not applicable |
SERIAL NUMBER |
not applicable |
REFERENCES |
unk unk unk unk unk Israel, G. et al. (2002), HUYGENS PROBE AEROSOL COLLECTOR PYROLYSER EXPERIMENT, Space Science Review, 104, 433-468 Lebreton, J.P., and Matson, D.L., The Huygens Probe: Science, Payload and Mission Overview, in HUYGENS - Science, Payload and Mission, ESA-SP-1177, 5, 1997 Niemann, H.B., S.K. Atreya, S.J. Bauer, K.Biemann, B. Block, G.R. Carignan, T.M. Donahue, R.L. Frost, D. Gautier, J.A. Haberman, D. Harpold, D.M. Hunten, G. Israel, J.I. Lunine, K. Mauersberger, T.C. Owen, F. Raulin, J.E. Richards, S.H. Way, The Gas Chromatograph Mass Spectroameter for the Huygens Probe, Space Science Review 104, pp 553-591, 2002 unk unk West, R.A., and P.H. Smith, Evidence for aggregate particles in the atmospheres of Titan and Jupiter. Icarus 90, 330-333. 138, 1991 |