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STRV 1A: EXPERIMENTS



Neutralizer

       The Charge Alleviation Experiment was designed to test an active method of discharging differential electrostatic charge which often builds up on spacecraft surfaces at geostationary altitudes. This electrostatic charge can discharge by arcing to a surface at a lower electrostatic potential and clearly represents a serious threat to the health of the spacecraft.

       The experiment employs a low energy plasma generator which emits xenon ions and electrons into the vicinity of the spacecraft. If a surface electrostaticpotential exists, the experiment would demonstrate whether is canbe reduced by the presence of the low energy plasma. In order to guarantee the presence of a high surface potential and have the ability to monitor the level of the potential, and electrostatic charge detector is also aboard STRV-1a. The Langmuir probe and Cold Ion Detectors on the spacecraft serve as plasma diagnostics equipment.

       The device that produces the plasma is a hollow cathode derived from the DRA UK-10 ion engine. Xenon is used as the engine propellent and is therefore used in the charge alleviation experiment.


Cold Ion Detector

       This detector is designed to measure the energy spectrum of incident, low-energy ions. The detector is operated on a regular basis to record the natural plasma background. If a means of operating the Charge Alleviation experiment is found, the detector will be used to help characterise the xenon plasma.


Langmuir Probe

       A Langmuir probe is mounted close to the neutraliser cathode in order to measure the local electron temperature. electron number density and plasma potential. The probe has been fully verified in orbit. The probe successfully detected the presence of xenon plasma from the cathode during vacuum chamber tests prior to launch. These results are shown in Fig. 6. The electron temperature associated with the steeper part of the curve (0 to 5V sweep) corresponds very well with the predictions of the output of the cathode. The flatter portion of the curve is either a second electron energy, or more likely a secondary ionisation effect.


Surface Charge Detector

       The CDE experiment has been developed at DRA Farnborough to measure surface charge directly using the Pockels Effect. This electro-optical phenomenon occurs when plane-polarised laser light passes through a crystal situated in an electric field. The degree of rotation of the plane of polarisation of the light is related to the magnitude of the field. The surface charge is determined by measuring the rotation angle. In the short time available for the development of this experiment it was possible to show that sufficient miniturisation of the design was (just) possible and that solutions to the delicate problems of optical arrangement and alignment could be found. The resulting flight unit has a mass of 600g and a power consumption of 2W, and also included a small radiation dosimeter, provided by ESA. Pre-flight calibration of the device was performed both with conventional high voltage power supplies and, more realistically, by irradiation of suitable sample of kapton placed in the device as a test piece.


Atomic Oxygen Erosion

       This University of Southampton experiment measures the rate of erosion of a selected number of spacecraft materials due to the action of atomic oxygen (AO) in the upper atmosphere. The experiment comprised 12 silver resistance sensors. As silver is converted to its non-conducting oxide the resistance increases. This increase can be measured and converted into silver loss. The erosion resistance of test materials is measured by coating the thin silver films with overlays of the test material. When this coating is breached the silver starts to oxidise and a resistance increase is observed. Knowledge of the fluence experienced and the thickness of the coating enables the erosion rate to be calculated. Silver sensors coated with polyethylene, PTFE, carbon and silica were flown. The flight spare of the experiment has been exposed to AO in the ESTEC pulsed-laser source. Thus a direct comparison between a flight experiment and a ground based simulation will be possible.

       Ground-based testing of the ability of different structural and thermal materials and coatings to withstand erosion is extremely useful; however such tests do not reproduce the simultaneous conditions of vacuum, oxygen flux, temperature and energy distribution that occurs in space. STRV-1a provides a valuable opportunity to perform such tests since the initial perigee altitude is only 300 km.

       The resistance of the thin silver films (1850 Å) started to increase immediately after launch and increased to the maximum of the measurement range after 280 and 330 orbits respectively. The form of the raw data of resistance as a function of fluence in the laboratory experiment and resistance as a function of orbit for the flight experiment is similar. The resistance change was converted to silver loss to facilitate analysis. The initial stage of the oxidation process was linear until approximately 300 Å of silver had been oxidised. The rate of oxidation then decayed to a low rate parabolic growth. The linear stage is thought to be surface reaction-controlled and the parabolic stage diffusion- limited.

       The resistance of both thick silver films remains unchanged. This suggests either a contamination problem or component failure in the electronic circuit. Analysis of future results should resolve this issue.

       No increase in the resistance of the carbon, silica or polyethylene sensors has vet been observed. On the basis of flux estimates (ESABASE), reported erosion yields for these materials and the thickness of the overlay coatings, these results are as expected.

       It should be noted that the coating thicknesses were selected on the basis of an earlier launch date and a lower perigee which would have provided a more concentrated AO environment.

       After 350 orbits, the resistance of the PTFE-coated sensors had increased to the upper bound of the measurement range. On the basis of a preliminary analysis, it is estimated that the erosion rate is 0.77 x 10-24 cm3 atom-1. This is of the same order as that achieved from the flight spare in the ESTEC facility and higher than that reported for flight experiments. This suggests that synergistic effects between the ultraviolet environment and AO may be influencing the erosion process.

       In conclusion, the experiment has enabled the value of the silver resistance technique as a monitor for the AO environment and the resistance of materials to AO degradation to be evaluated. It is concluded that whilst there is considerable merit in the technique for AO measurement, in common with other thin film techniques the question as to whether a thin film is truly representative of a bulk material must be seriously considered. Further ground-based tests are required to resolve this issue.

       A concentrated programme has recently commenced using the ESTEC facility. This will address some of he issues raised by the flight experiment.

       Flying a second experiment on a satellite such as STRV-1c or - 1d is a goal for future research activities.


Cosmic Ray & Dosimetry

       This experiment is vital to the STRV-1a technology demonstration mission objectives since it is accurately characterising the radiation dose received by the spac.ecraft. This information is clearly essential for determining the performance of solar cells, microelectronics, etc. Actual doses received at specific locations within the spacecraft can be derived by computer modelling the shielding effects of all the spacecraft components. DRA Farnborough has already flown versions of CREDO on Concorde, UoSAT and the Space Shuttle. The APEX mission currently in orbit is also flying a version of the instrument and the data retrieved from this mission will be cross-correlated with that from detectors on both STRV-1 and -1b.

       CREDO measures both the energy and arrival rate of cosmic rays as the particles pass through a 3 cm square array 6f 300 µm thick diodes. The total charge generated in nine energy bands (over 300s intervals) is recorded by the instrument thereby providing a clear picture of the cosmic ray environment of the GTO.

       ParticleS; trapped in the geomagnetic field and other naturally occurring ionising radiation are also measured by CREDO. The instrument includes a network of Radiation Field Effect transistors (RadFET's) located at different positions within STRV-1a. Each RadFET has a 100 nm thick gate oxide layer which traps positive charges generated as particles pass through, thereby altering the threshold voltage of the device. The total received radiation dose is therefore measured by monitoring the threshold voltage of each transistor.


Battery Recharge

       The STRV-1a Power Subsystem incorporates an ESTEC experiment to study a new, more effective means of controlling the charging of a spacecraft battery. The technique involves accurately monitoring the temperatures and terminal voltages of the selected cells of the battery. When charging occurs, the temperature tends to fall, however when charging is complete and more energy is dissipated within the cells, the temperature rises. By measuring the rate of change of the temperature the moment that charging is complete can be accurately detected. This technique does not require any compensation for ageing, temperature, depth of discharge or charging rate.

       Due to battery. anomaly on STRV-1a during August 1994, the BRE was not operated until September 1994. The experiment had to contend with two difficult conditions: a) the operating temperature of the battery. was around 30° C, and b) the battery terminal voltage was below nominal. In the first case there was concern that the dynamic range of the temperature detector would be compromised, since circuit saturation was predicted to commence at 35° C, while the second case dictated that the BRE end-of-charge (EOC) logic was held permanently reset and that the BRE could only be used in monitoring mode with the data being routed to the ground for assessment before any on-board response could be initiated. Thus although the BRE could not directly control the STRV-1a battery' chargers, it was extensively used during the mission as a batteD' thermal dissipation monitor to determine the duration of applied battery, charge. This came about since the depressed battery, terminal voltage also resulted in the operation of the conventional EOC control being compromised.

       The BRE displayed a high degree of sensitivity to battery EOC dissipation whilst at the same time showed itself to be basically insensitive to the dynamic temperature environment of the battery and spacecraft around the orbit. In the course of the STRV-1a mission it successfully detected EOC conditions on a battery whose temperature could vary over the range 20-35° C.

       The BRE also incorporates 6 hybrid power MOSFET's ("HyFETs"). These devices are being calibrated in the radiation environment. The gate voltage of each device is measured and based on ground results, a drift rate of 200 mV/krad was expected. The results to date suggest approximately an order of magnitude less than predicted by software models.

       Several hundred discharge/charge cycles to date on STRV-1a have shown the temperature derivative (Tdt) charge control technique of the BRE to be both a reliable and thermally stable battery management concept. It has proved that the applied charge rates of C/14 and C/7 in conjunction with the pre-selected circuit sensitivity has produced sufficient thermal impulse to the battery when approaching end-of-charge, to allow accurate detection.

       The results from the STRV-la application of the BRE have also led ESA-ESTEC to propose the development of an. enhanced Tdt Detector for application to operational LEO spacecraft.

 

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