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An Introduction to Space Instrumentation, Edited by K. Oyama and C. Z. Cheng, 193–202. Low energy particle spectrometer for 3-axis stabilized spacecraft Yoshifumi Saito Institute of Space and Astronautical Science, 3-1-1 Yoshinodai, Chuo, Sagamihara, Kanagawa 252-5210, Japan Most of the recent satellite-borne instrumentation for low energy charged particle measurement adopts tophat type electrostatic analyzers. Since the top-hat type electrostatic analyzers have wide field of view of 2π radian with uniform transmission characteristics, they are suitable for low energy charged particle measurement by spin-stabilized spacecraft. However, 3-axis stabilized spacecraft is favored in most of the planetary missions due to the affinity with imaging instruments. Therefore, for the future planetary plasma observations, it is quite important to develop lightweight, low-power consumption and compact low energy charged particle analyzers for 3-axis stabilized spacecraft. In order to realize 3-D field of view on 3-axis stabilized spacecraft under limited resources, ASKY-ESA (All SKY-ElectroStaitc Analyzer) was developed. ASKY-ESA consists of FOV (Field Of View) scanning deflectors at the entrance and spherical/toroidal electrostatic deflectors inside. The FOV is electrically scanned between +/−45 degrees around the center of the FOV, which is 45 degrees inclined from the axis of symmetry. Since ASKY-ESA has hemi-spherical field of view, three-dimensional space is covered by two ASKY-ESAs installed on spacecraft panels opposite to each other. ASKY-ESA is also suitable for low energy charged particle measurement on a surface of airless heavenly bodies, for example, the Moon, Martian satellite Phobos, and numerous small objects/asteroids. Key words: Low energy charged particle, electrostatic analyzer, 3-axis stabilized spacecraft. 1. Introduction to the Low Energy Particle Spec- craft can be used, it is easy to adopt option 1). However, it trometer for 3-Axis Stabilized Spacecraft is also true that there are some drawbacks. One of them is 1.1 Aim of the low energy particle spectrometer for 3axis stabilized spacecraft Most of the recent satellite-borne instrumentation for low energy charged particle measurement adopts top-hat type electrostatic analyzers (Carlson et al., 1983; Young et al., 1988). Since the top-hat type electrostatic analyzers have wide field of view of 2π radian with uniform transmission characteristics, they are suitable for low energy charged particle measurement by spin-stabilized spacecraft. However, 3-axis stabilized spacecraft is favored in most of the planetary missions due to the affinity with imaging instruments. Therefore, for the future planetary plasma observations, it is quite important to develop light-weight, low-power consumption and compact (requires as small area on the spacecraft as possible) low energy charged particle analyzers for 3-axis stabilized spacecraft. In order to realize 3-D field of view on 3-axis stabilized spacecraft, there are three options as follows: 1) using low energy particle spectrometers for spin-stabilized spacecraft with rotation tables, 2) using multiple low energy particle spectrometers for spin-stabilized spacecraft so that necessary angular directions are simultaneously observed, and 3) using one or two sensors that have wide field of view. There are several examples of the option 1). CAPS on CASSINI (Young et al., 2004) uses a rotation table that sweeps the field of view of the charged particle analyzers with two-dimensional field of view. ASPERA3 on Mars Express (Barabash et al., 2006) and ASPERA4 on Venus Express also use rotation tables. Since welldeveloped electrostatic analyzers for spin-stabilized spacec TERRAPUB, 2013. Copyright the limited scan speed of the mechanical rotation tables that leads to the limited time resolution. Another drawback is that the required power is larger than adopting option 3). The option 2) is simple but it requires much more resources including power, mass and installation area on the spacecraft than the other two options. The installation of the sensors is difficult if three-dimensional space should be covered with high angular resolution. Due to this reason, there is no example that the option 2) is really used for covering three-dimensional field of view on a 3-axis-stabilized spacecraft. Instead, the option 2) is planned to be used for high time resolution measurements of low energy charged particles on a spin-stabilized spacecraft (Saito et al., 2009). Although the option 3) requires additional development of the electrostatic deflectors and stepping high voltage power supplies, it is a feasible option under limited resources. The low energy particle spectrometer for 3-axis stabilized spacecraft described in this paper also adopts this option 3). Most of the examples of option 3) that were developed before 2000s were for low energy charged particles below 1 keV/q. DYMIO on MARS96 (Berthelier et al., 1998) and FONEMA on MARS96 (Fedorov et al., 1998) are the examples. FONEMA used hyperbolic mirror at the entrance of the analyzer in order to cover hemi-spherical field of view. Recently a couple of new instruments that can be categorized into option 3) for low energy charged particles over 1 keV/q are developed. FIPS on MESSENGER is an example that covers nearly hemi-spherical field of view using novel electrostatic optics. PICAM on BepiColombo/MPO (Orsini et al., 2010) is a plasma camera originally proposed by Vaisberg et al. (2005) that also can cover hemi-spherical field of view by utilizing parabolic 193 194 Y. SAITO: LOW ENERGY PARTICLE SPECTROMETER FOR 3-AXIS STABILIZED SPACECRAFT Fig. 1. An example of ASKY-ESA (MAP-PACE-ESA-S2 on Kaguya). Left hand side figure shows the outlook of the analyzer. A cross section of the electron optics part is shown in the right hand side figure. Fig. 2. Electrostatic potential distribution around the deflectors when +3200 V is applied to the upper (a) and lower (b) deflectors while the lower (a) and upper (b) deflectors are grounded. mirror at the entrance. Although it is not hemi-sphere, Ion Mass Analyzer (IMA) that is a part of ASPERA-3 on Mars Express (Barabash et al., 2006) and ASPERA-4 on Venus Express can cover similar size of the solid angle. IMA has a wide annular field of view centered by the annular 2π radian field of view of the standard top-hat type analyzer by electrically scanning its field of view by +/−45 deg. The latest example of option 3) is MAP-PACE on Japanese lunar orbiter Kaguya (Saito et al., 2008a, 2010) that is described in this paper in detail. 1.2 Principle of low energy particle spectrometer for 3-axis stabilized spacecraft ASKY-ESA(All SKY-ElectroStaitc Analyzer) shown in Fig. 1 is an example of low energy particle spectrometer for 3-axis stabilized spacecraft. ASKY-ESA belongs to the option 3) discussed in Subsection 1.1. It is MAP-PACE-ESAS2 on Kaguya. It consists of FOV (Field Of View) scanning deflectors at the entrance and toroidal electrodes inside. The FOV is electrically scanned between +/−45 degrees around the center of the FOV, which is 45 degrees inclined from the axis of symmetry. The three-dimensional electron distribution function is observed with two ASKY-ESA sensors that are installed on the two panels of the spacecraft opposite to each other. The curved upper and lower FOV scanning deflectors are supplied with high voltages which are swept between 0 V and +4 kV. The inner toroidal electrode is also supplied with a high voltage swept between 0 V and +3 kV simultaneously with the FOV scanning deflectors. The electrons that pass through the FOV scanning deflectors enter into the toroidal deflectors. Only electrons in a specific energy range can travel further down to the exit of the toroidal deflectors. The electrons that pass through the toroidal deflectors enter a Micro-Channel Plate (MCP) and are intensified to detectable charge pulses. Between the toroidal deflectors and MCP, there exists a slit and grid supplied with a slightly negative voltage (−4.0 V) in order Y. SAITO: LOW ENERGY PARTICLE SPECTROMETER FOR 3-AXIS STABILIZED SPACECRAFT 195 Fig. 3. An example of the electron trajectories when positive voltage is applied to the upper (a) and lower (b) deflectors, respectively. White lines show the trajectories of the detected electrons. Color in the figure indicates the electrostatic potential. to reject the secondary electrons that give spurious counts. The charge pulses intensified by the MCP are received by a one-dimensional circular resistive anode (Yokota and Saito, 2008). The positions where the charge pulses are detected correspond to the incident azimuthal directions of the electrons. 2. Instrument 2.1 Sensor, dimension, weight, favorable place to be installed in rocket and satellite The curved upper and lower FOV scanning deflectors of ASKY-ESA is numerically designed so that hemi-sphere can be covered with voltage as low as possible. In order to prevent generating electron beams when illuminated by the sunlight, positive voltage is applied to both upper and lower deflectors. The shape of the curved upper and lower deflectors of MAP-PACE-ESA-S2 on Kaguya is proportional to x 2.4 and x 2.9 , respectively, where x axis is the center of the field of view. Figures 2(a) and (b) shows the potential distribution around the deflectors when +3200 V is applied to the upper/lower deflector while the lower/upper deflector is grounded. Figures 3(a) and (b) shows an example of the electron trajectories when positive voltage is applied to the upper/lower deflector, respectively. Figure 4 shows the relation between Vdef /Vin and the incident angle of the electrons where Vdef is the voltage applied to the deflector and Vin is the voltage applied to the inner sphere. The detailed characteristics of ASKY-ESA including the design principle of the deflection system are reported by Yokota et al. (2005). The size of ASKY-ESA is different depending on the purpose of the analyzer. MAP-PACE-ESA-S1 that is the paired analyzer with MAP-PACE-ESA-S2 (see Fig. 1) on Kaguya is another example of ASKY-ESA. Although the outer size of the analyzers ESA-S1 and ESA-S2 is the same, the gap Fig. 4. Relation between Vdef /Vin and the incident angle of the electrons where Vdef is the voltage applied to the deflector and Vin is the voltage applied to the inner sphere. The data points show the deflection angle averaged over all the azimuthal channels. The vertical line shows the incident angle range covered by all the azimuthal channels. between the toroidal deflectors of ESA-S1 is larger than that of ESA-S2, the maximum energy and energy resolution of ESA-S1 is lower than ESA-S2 while the g-factor of ESAS1 is larger than ESA-S2. Since ESA-S1 mainly observes electrons from the Moon surface, larger geometrical factor is necessary. Figures 5 and 6 show other examples of ASKY-ESA: MAP-PACE-IEA and MAP-PACE-IMA on Kaguya. IEA and IMA are ion energy analyzer and ion energy mass an- 196 Y. SAITO: LOW ENERGY PARTICLE SPECTROMETER FOR 3-AXIS STABILIZED SPACECRAFT Fig. 5. An example of ASKY-ESA (MAP-PACE-IEA on Kaguya). Fig. 6. An example of ASKY-ESA (MAP-PACE-IMA on Kaguya). alyzer, respectively. IMA consists of an energy analyzer, which has a similar structure to the ESA shown in Fig. 1, and an LEF (Linear Electric Field) TOF (Time Of Flight) ion mass analyzer (McComas and Nordholt, 1990; Yokota and Saito, 2005; Yokota et al., 2005). IEA consists only of an energy analyzer that is the same as the energy analyzer of IMA. Since ASKY-ESA has hemi-spherical field of view, three-dimensional space is covered by two ASKY-ESAs installed on spacecraft panels opposite to each other. Figure 7 shows an example of the ASKY-ESAs on a 3-axis stabilized spacecraft. ASKY-ESA is also suitable for plasma measurements on a surface of airless heavenly bodies, for example, the Moon, Martian satellite Phobos, and numerous small objects/asteroids. Only placing one ASKY-ESA directly on a surface of the airless heavenly bodies, the necessary hemi-spherical field of view can be covered without any additional rotation tables. Tables 1 and 2 summarize the characteristics, size and weight of the MAP-PACE electron and ion ASKY-ESA sensors on Kaguya, respectively. 2.2 Electronics block diagram, command, timing signal from data processing unit Figure 8 shows a functional block diagram of MAPPACE ASKY-ESA sensors on Kaguya. MAP is composed of two subsystems MAP-PACE (Saito et al., 2008a, 2010) and MAP-LMAG (Lunar MAGnetometer) (Shimizu et al., 2008; Takahashi et al., 2009; Tsunakawa et al., 2010). In order to minimize the mass and power, the control electronics for the MAP-PACE sensors and MAP-LMAG sensors Y. SAITO: LOW ENERGY PARTICLE SPECTROMETER FOR 3-AXIS STABILIZED SPACECRAFT 197 Fig. 7. An example of ASKY-ESA on a 3-axis stabilized spacecraft (Kaguya). A pair of ion ASKY-ESAs (MAP-PACE-IEA and MAP-PACE-IMA) and a pair of electron ASKY-ESAs (MAP-PACE-ESA-S1 and MAP-PACE-ESA-S2) are on spacecraft panels opposite to each other. Table 1. Characteristics of electron ASKY-ESA: MAP-PACE-ESA-S1 and S2 on Kaguya. Energy range Energy resolution Energy sweep Step Field of view FOV sweep range Angular resolution g-factor (5◦ × 22.5◦ ) Time resolution Analyzer type Average radius Gap Eccentricity Size Weight ESA-S1 6 eV–9 keV 15% (FWHM) 32 2π str. 45◦ ± 45◦ (Pol) 5◦ (Pol) × 8◦ (Az) (FWHM) 5.3 × 10−4 cm2 str keV/keV (efficiency is not included) 1s Toroidal analyzer 30 mm 5 mm 5 mm 170 mm × 170 mm × 249 mm 2.16 kg are contained in one package, MAP-E (MAgnetic field and Plasma experiment-Electronics). Detected electron/ion signals are pre-amplified and transmitted from each sensor to MAP-E that includes a position detection circuit, TOF measurement circuit and count RAMs. MAP-E also controls high voltage power supplies in each sensor head with analog signals. MAP-PACE sensors are controlled by a CPU board called SI-OBC (Science Instrument-OnBoard Computer). MAP-E also consists of another CPU board called TC-OBC (Telemetry Command-OnBoard Computer) that is responsible for interfacing with spacecraft via a 1553B interface. Figure 9 shows a more detailed block diagram of the analyzer head part of MAP-PACE-ESA-S2 that includes ESA-S2 9 eV–16 keV 10% (FWHM) 32 2π str. (<9 keV) 45◦ ± 45◦ (Pol) 5◦ (Pol) × 8◦ (Az) (FWHM) 1.2 × 10−4 cm2 str keV/keV (efficiency is not included) 1s Toroidal analyzer 30 mm 3 mm 5 mm 170 mm × 170 mm × 249 mm 2.16 kg ASKY-ESA shown in Fig. 1, preamplifier and high voltage power supply. Since circular 1-dimensional resistive anode (Yokota and Saito, 2008) is used for ESA-S2, the used preamplifiers are two charge sensitive amplifiers (AMPTEK A225). By comparing the charge ratio from the two terminals connected to the circular 1-dimensional resistive anode, the position of the incident charged particles can be detected. Since several micro-seconds are necessary to detect the charge ratio, sum of the timing out signals from two charge sensitive amplifiers is also counted as “event count” when the pulse height is above the threshold level. The sensor head of MAP-PACE-ESA-S2 can be controlled with high voltage control signals and two signals “peak hold reset” and “strobe” that are used to control posi- 198 Y. SAITO: LOW ENERGY PARTICLE SPECTROMETER FOR 3-AXIS STABILIZED SPACECRAFT Table 2. Characteristics of ion ASKY-ESA: MAP-PACE-IEA and IMA on Kaguya. Energy range Energy resolution Energy sweep Step Mass range Mass resolution Field of view FOV sweep range Angular resolution g-factor (5◦ × 22.5◦ ) Time resolution Analyzer type Average radius Gap Size Weight IEA 7 eV/q–28 keV/q 5% (FWHM) 32 N.A. N.A. 2π str. (<7 keV/q) 45◦ ± 45◦ (Pol) 5◦ (Pol) × 10◦ (Az) (FWHM) 2.1 × 10−4 (attn.: off) cm2 str keV/keV 3.8 × 10−6 (attn.: on) cm2 str keV/keV (efficiency is not included) 1s Spherical analyzer 55 mm 4 mm 220 mm × 400 mm × 307 mm 4.23 kg IMA 7 eV/q–28 keV/q 5% (FWHM) 32 1–60 m/m ∼ 15 2π str. (<7 keV/q) 45◦ ± 45◦ (Pol) 5◦ (Pol) × 10◦ (Az) (FWHM) 4.5 × 10−4 cm2 str keV/keV (efficiency is not included) 1s Spherical analyzer 55 mm 4 mm 220 mm × 400 mm × 400 mm 6.55 kg Fig. 8. Functional block diagram of MAP-PACE on Kaguya. tion sensing preamplifier. The raw bit rate of the MAP-PACE ASKY-ESA sensors are shown in Table 3. Since the main purpose of MAPPACE-IEA is to measure solar wind ions, the necessary angular resolution is high. The raw bit rate of ion energy mass spectrometer MAP-PACE-IMA is much higher than energy spectrometer due to the additional information of ion species. Since the telemetry rate (42 kbps) allocated to KaguyaMAP-PACE ASKY-ESA sensors was much lower than the raw data rate, the onboard computer SI-OBC (see Fig. 8) reduced the quantity of data in order that the data sent to the ground would fit into the allocated telemetry rate. The data processing for reducing the quantity of data includes data compression, pitch angle sorting of electron data, integrating mass channels and angular sectors and selecting the angular sampling points of the solar wind ions by tracking solar wind direction. Arithmetic compression that is one of the reversible data compression algorithms was used for data compression. Y. SAITO: LOW ENERGY PARTICLE SPECTROMETER FOR 3-AXIS STABILIZED SPACECRAFT 199 Fig. 9. Functional block diagram of ESA-S2. Table 3. Raw bit rate of the Kaguya-MAP-PACE ASKY-ESA sensors. Raw bit rate Telemetry rate 2.3 ESA-S1 64 kbps (max) (16 az * 8 pol * 32 energy * 16 bits/1 sec) 42 kbps ESA-S2 64 kbps (max) (16 az * 8 pol * 32 energy * 16 bits/1 sec) 42 kbps Excellent part and disadvantages, and weak points of the instrument The major advantage of ASKY-ESA comparing the standard top-hat type electrostatic analyzer with +/−45 deg. field of view scanning deflector is as follows: (1) it is easier to find the installation position on the spacecraft since the latter analyzer has to be installed at the corner of the spacecraft or on a extendable boom while the former analyzer can be installed on any spacecraft panels (2) it is also possible to use ASKY-ESA on a surface of airless heavenly bodies. ASKY-ESA also has an advantage from the viewpoint of the time resolution. While the time resolution of the standard top-hat type electrostatic analyzers for spin-stabilized spacecraft is limited by the spin period of the spacecraft unless multiple sensors are simultaneously used, ASKY-ESA’s time resolution is determined by the speed of the high voltage sweep that can be controlled by the instrument team only installing two ASKY-ESAs on either a spin-stabilized spacecraft or 3-axis stabilized spacecraft,. Although the counting statistics depending on the measured ion/electron flux and the saturation of the detector limit the actual time resolution, time resolution independent of the spacecraft motion is a big advantage. Another advantage is the equally weighted division of the hemi-spherical field IEA 1 Mbps (max) (64 az * 32 pol * 32 energy * 16 bits/1 sec) 42 kbps IMA 16 Mbps (max) (64 az * 32pol * 32 energy * 16 bits * 16 mass/1 sec) 42 kbps of view. Although the standard top-hat type electrostatic analyzers on a spin-stabilized spacecraft has much denser angular coverage in the pole direction than the equatorial direction with respect to the spin axis, ASKY-ESAs angular coverage is nearly equal if the angular division in the polar coordinate system with respect to the spin axis is equal. In addition to the advantages shown above, there also exist some disadvantages. Since ASKY-ESA utilizes electrostatic deflectors to cover hemi-spherical FOV, the maximum voltage of the stepper high voltage power supply limits the maximum detectable energy. Although the FOV scanning deflector is designed so that the deflection efficiency should be as high as possible, about twice the maximum voltage applied to the deflectors is the highest energy of the charged particle when the field of view scanning range is +/−45 deg. Another disadvantage of the ASKY-ESA is the severe requirements on the magnetic cleanliness and surface potential uniformity of the spacecraft. Since the orbit of the electrons/ions coming from the horizontal direction to the sensor passes close to the spacecraft body, they are easily affected by the surface potential of the spacecraft and magnetic field around the spacecraft body. Sometimes the EMC requirements of ASKY-ESA on the DC magnetic field are severer than that of magnetometers. Since magnetometers 200 Y. SAITO: LOW ENERGY PARTICLE SPECTROMETER FOR 3-AXIS STABILIZED SPACECRAFT Fig. 10. Ion populations on the dayside of the Moon. Panel (a) shows a summary of low-energy ion population on the dayside of the Moon. Panel (b) is an omni-directional E-t spectrogram from IMA. The vertical scale is the energy of ions while the horizontal axis is time. The color of each bin depicts the ion differential ion flux, in each energy bin at the time of observations. All the populations shown in Panel (a) can be found in Panel (b). Panels (c) and (d) are altitude of Kaguya, magnetic field intensity and direction in the Geocentric Solar Ecliptic (GSE) polar coordinate system observed by MAP-LMAG. Panels (e) and (f) show the solar zenith angle and latitudinal/longitudinal position of Kaguya in the Mean Earth/Polar Axis (ME) coordinate system. are usually separated from the spacecraft using extendable mast or boom, magnetometer sensors can be far from the magnetic field source on the spacecraft. However, the orbit of the charged particle cannot be far from the spacecraft if the ASKY-ESA is directly installed on a spacecraft panel. Of course, if ASKY-ESA is installed at the corner of the spacecraft, these requirements on the magnetic cleanliness can be highly relaxed. 2.4 Results obtained so far by MAP-PACE on Kaguya MAP-PACE on Japanese lunar orbiter Kaguya (Saito et al., 2008a, 2010) is an example of the ASKY-ESA sensors. MAP-PACE made observations of low energy charged particles around the Moon. Kaguya was inserted into a circular lunar polar orbit of 100 km altitude and continued observation for nearly 1.5 years until it impacted the Moon on 10 June 2009. During the last 5 months, the orbit was lowered to ∼50 km-altitude, and some orbits had further lower perilune altitude of ∼10 km. Besides the solar wind, MAPPACE-IMA (anti-moon looking ion analyzer) found four clearly distinguishable ion populations on the dayside of the Moon (see Fig. 10). 1) Solar wind protons backscattered at the lunar surface (Saito et al., 2008b), 2) solar wind protons reflected by magnetic anomalies on the lunar surface, 3) reflected/backscattered protons picked-up by the solar wind, and 4) ions originating from the lunar surface/lunar exosphere (Yokota et al., 2009; Tanaka et al., 2009; Saito et al., 2010). Using low altitude data, MAP-PACE revealed the plasma structure over lunar magnetic anomalies on the dayside of the Moon. At ∼25 km altitude over magnetic anomalies on the Moon, deceleration of the solar wind ions, acceleration of the solar wind electrons parallel to the magnetic field, and heating of the ions reflected by magnetic anomalies were simultaneously observed. Deceleration of the solar wind ions was observed for both two major solar wind ion compositions: protons and alpha particles. Deceleration of the solar wind had the same E/q (E: deceleration energy, q: charge) for both protons and alpha particles. In addition, the acceleration energy of the electrons was almost the same as the deceleration energy of the ions. It indicates the existence of anti-moonward electric field over the magnetic anomaly above the altitude of Kaguya. On the other hand, the reflected ions had lower energy than the incident solar wind ions. Since the kinetic energy of the ions magnetically reflected by magnetic anomalies on the lunar surface will not change, it suggests the existence of an additional non-adiabatic dissipative interaction between solar wind ions and lunar magnetic anomalies below Kaguya. Y. SAITO: LOW ENERGY PARTICLE SPECTROMETER FOR 3-AXIS STABILIZED SPACECRAFT 201 In the lunar wake region, MAP-PACE found two differ- References ent types of ion entry into the lunar wake. As for the Type-1 Barabash, S., R. Lundin, H. Andersson, K. Brinkfeldt, A. Grigoriev, H. entry, solar wind protons enter into the lunar wake in the Gunell, M. Holmström, M. Yamauchi, K. Asamura, P. Bochsler, P. Wurz, R. Cerulli-Irelli, A. Mura, A. Milillo, M. Maggi, S. Orsini, A. direction perpendicular to the magnetic field. They gain J. Coates, D. R. Linder, D. O. Kataria, C. C. Curtis, K. C. Hsieh, B. kinetic energy in one hemi-sphere while lose in the other R. Sandel, R. A. Frahm, J. R. Sharber, J. D. Winningham, M. Grande, hemi-sphere (Nishino et al., 2009a). As for the Type 2 enE. Kallio, H. Koskinen, P. Riihelä, W. Schmidt, T. Säles, J. U. Kozyra, try, solar wind protons reflected/backscattered on the dayN. Krupp, J. Woch, S. Livi, J. G. Luhmann, S. McKenna-Lawlor, E. C. Roelof, D. J. Williams, J.-A. Sauvaud, A. Fedorov, and J.-J. Thoside of the Moon are picked-up by the solar wind and enter caven, The analyzer of space plasmas and energetic atoms (Aspera-3) into the deepest lunar wake (Nishino et al., 2009b, 2010). for the Mars Express Mission, Space Sci. Rev., 126, 113–164, 2006, The newly obtained knowledge about the solar winddoi:10.1007/s11214-006-9124-8. Moon interaction by Kaguya must contribute to the under- Berthelier, J.-J., J.-M. Illiano, R. R. Hodges, J. Covinhes, M. Godefroy, G. Gogly, J. Guillou, F. Legoff, F. Leblanc, Z. Racic, P. Rouchette, D. standing of the plasma environment around non-magnetized Krankowsky, D. Dorflinger, O. Vaisberg, V. Smirnov, and N. Kolesova, solar system objects. 3. Toward Future Improvements 3.1 Which part should be improved? The MAP-PACE sensors on Kaguya that is an example of the ASKY-ESA have several points that should be improved for the future usage of the similar kind of the analyzers. 1) Although 1-dimensional circular resistive anode was used for MAP-PACE sensors, it should be replaced by delay-line anode (Saito et al., 2006) or discrete anode with ASIC (Saito et al., 2009) that have much faster data processing speed. Besides the data processing speed, the resistive anode used for MAP-PACE had characteristics that the position detection resolution was worse at the edge of the anode than at the center of the anode. This lead to wide blind angle around the edge of the anode. 2) The poles to support the spherical grid at the entrance of the analyzer (see Figs. 1, 5 and 6) should be made as thin as possible in order to minimize the blockage of the field of view. 3) The field of view scanning deflectors of MAP-PACE were made of aluminum alloy with mirror finished surface in order to reflect back the incident solar UV. However, the mirror finished aluminum alloy surface also scatters incident charged particles with high efficiency. Since these scattered particles can be noise counts, the deflectors should be serrated and blackened in order to reduce the scattering. 3.2 Unsolved scientific subjects, and necessary improvement of the instruments Since ASKY-ESA deflects the incident angular direction of low energy charged particles, higher voltage is required when charged particles with higher energy should be observed. Although the efficiency of the deflection depends on the design of the field of view scanning deflectors, it is not possible to deflect the incident particles of all the energy range covered by the spherical/toroidal electro-static analyzer when the same high voltage level upper limit is applied. In case of the MAP-PACE-ESA-S2 on Kaguya spacecraft, the maximum energy that could cover 3-dimensional field of view was 9 keV, while that of MAP-PACE-IEA and MAP-PACE-IMA was 7 keV/q. Since the pickup ions around the Moon sometimes have much higher energy than this maximum energy, some of the phenomena related with pick-up acceleration could not be resolved by MAP-PACE observations. Development of new optics to cover hemispherical field of view or further improvement of the angular scanning deflector and high voltage power supply is necessary to resolve this problem. The DYMIO ion mass spectrometer of the Mars 96 Mission, in Measurement Techniques in Space Plasmas—Particles, Geophysical Monograph 102, edited by R. F. Pfaff, J. E. Borovsky, and D. T. Young, The American Geophysical Union, Washington, D.C., U.S.A., 1998, p. 215. Carlson, C. W., F. W. Curtis, G. Paschmann, and E. Michael, An instrument for rapidly measuring plasma distribution functions with high resolution, Adv. Space Res., 2, 67–70, 1983. Fedorov, A. O., O. L. Vaisberg, A. D. Johnstone, A. M. James, and R. D. Woodlife, Rapid non-scanning ion distribution measurements using electrostatic mirror and multichannel collimator for the INTERBALL and MARS-96 missions, Geophysical Monograph 102, edited by R. F. Pfaff, J. E. Borovsky, and D. T. Young, The American Geophysical Union, Washington, D.C., U.S.A., 1998, 221–228. McComas, D. J. and J. E. Nordholt, New approach to 3-D, high sensitivity, high mass resolution space plasma composition measurements, Rev. Sci. Instrum., 61, 3095–3097, 1990. Nishino, M. N., K. Maezawa, M. Fujimoto, Y. Saito, S. Yokota, K. Asamura, T. Tanaka, H. Tsunakawa, M. Matsushima, F. Takahashi, T. Terasawa, H. Shibuya, and H. Shimizu, Pairwise energy gain-loss feature of solar wind protons in the near-Moon wake, Geophys. Res. Lett., 36, L12108, 2009a, doi:10.1029/2009GL039049. Nishino, M. N., M. Fujimoto, K. Maezawa, Y. Saito, S. Yokota, K. Asamura, T. Tanaka, H. Tsunakawa, M. Matsushima, F. Takahashi, T. Terasawa, H. Shibuya, and H. Shimizu, Solar-wind proton access deep into the near-Moon wake, Geophys. Res. Lett., 36, L16103, 2009b, doi:10.1029/2009GL039444. Nishino, M. N., M. Fujimoto, Y. Saito, S. Yokota, Y. Kasahara, Y. Omura, Y. Goto, K. Hashimoto, A. Kumamoto, T. Ono, H. Tsunakawa, M. Matsushima, F. Takahashi, H. Shibuya, H. Shimizu, and T. Terasawa, Effect of the solar wind proton entry into the deepest lunar wake, Geophys. Res. Lett., 37, L12106, 2010, doi:10.1029/2010GL043948. Orsini, S., S. Livi, K. Torkar, S. Barabash, A. Milillo, P. Wurz, A. M. Di Lellis, E. Kallio, and the SERENA team, SERENA: A suite of four instruments (ELENA, STROFIO, PICAM and MIPA) on board BepiColombo-MPO for particle detection in the Hermean environment, Planet. Space Sci., 58, 1–2, 166–181, 2010, doi:10.1016/j.pss.2008.09.012. Saito, M., Y. Saito, T. Mukai, and K. Asamura, Development of a lowenergy charged particle detector with on-anode ASIC for in-situ plasma measurement in the Earth’s magnetosphere, AIP Conf. Proc. 1144, 48, 2009, doi:10.1063/1.3169303. Saito, Y., D. Delcourt, and A. Coates, Low energy ion observation by Mercury Magnetospheric Orbiter: MMO, Advances in Geosciences, Volume 3: Planetary Science, 85–91, 2006. Saito, Y., S. Yokota, K. Asamura, T. Tanaka, R. Akiba, M. Fujimoto, H. Hasegawa, H. Hayakawa, M. Hirahara, M. Hoshino, S. Machida, T. Mukai, T. Nagai, T. Nagatsuma, M. Nakamura, K. Oyama, E. Sagawa, S. Sasaki, K. Seki, and T. Terasawa, Low energy charged particle measurement by MAP-PACE onboard SELENE, Earth Planets Space, 60, 4, 375–386, 2008a. Saito, Y., S. Yokota, T. Tanaka, K. Asamura, M. N. Nishino, M. Fujimoto, H. Tsunakawa, H. Shibuya, M. Matsushima, H. Shimizu, F. Takahashi, T. Mukai, and T. Terasawa, Solar wind proton reflection at the lunar surface: Low energy ion measurement by MAP-PACE onboard SELENE (KAGUYA), Geophys. Res. Lett., 35, L24205, 2008b, doi:10.1029/2008GL036077. Saito, Y., S. Sasaki, M. Fujimoto, K. Maezawa, I. Shinohara, Y. Tsuda, and H. Kojima, High time resolution electron measurement by Fast Electron energy Spectrum Analyzer (FESA), AIP Conf. Proc. 1144, 53, 2009, doi:10.1063/1.3169304. 202 Y. SAITO: LOW ENERGY PARTICLE SPECTROMETER FOR 3-AXIS STABILIZED SPACECRAFT Saito, Y., S. Yokota, K. Asamura, T. Tanaka, M. N. Nishino, T. Yamamoto, Y. Terakawa, M. Fujimoto, H. Hasegawa, H. Hayakawa, M. Hirahara, M. Hoshino, S. Machida, T. Mukai, T. Nagai, T. Nagatsuma, T. Nakagawa, M. Nakamura, K. Oyama, E. Sagawa, S. Sasaki, K. Seki, I. Shinohara, T. Terasawa, H. Tsunakawa, H. Shibuya, M. Matsushima, H. Shimizu, and F. Takahashi, In-flight performance and initial results of Plasma energy Angle and Composition Experiment (PACE) on SELENE (Kaguya), Space Sci. Rev., 154, 1–4, 265–303, 2010, doi:10.1007/s11214-010-9647-x. Shimizu, H., F. Takahashi, N. Horii, A. Matsuoka, M. Matsushima, H. Shibuya, and H. Tsunakawa, Ground calibration of the high-sensitivity SELENE lunar magnetometer LMAG, Earth Planets Space, 60, 353, 2008. Takahashi, F., H. Shimizu, M. Matsushima, H. Shibuya, A. Matsuoka, S. Nakazawa, Y. Iijima, H. Otake, and H. Tsunakawa, In-orbit calibration of the lunar magnetometer onboard SELENE (KAGUYA), Earth Planets Space, 61, 1269–1274, 2009. Tanaka, T., Y. Saito, S. Yokota, K. Asamura, M. N. Nishino, H. Tsunakawa, H. Shibuya, M. Matsushima, H. Shimizu, F. Takahashi, M. Fujimoto, T. Mukai, and T. Terasawa., First in situ observation of the Moon-originating ions in the Earth’s Magnetosphere by MAP-PACE on SELENE (KAGUYA), Geophys. Res. Lett., 36, L22106, 2009, doi:10.1029/2009GL040682. Tsunakawa, H., H. Shibuya, F. Takahashi, H. Shimizu, M. Matsushima, A. Matsuoka, S. Nakazawa, H. Otake, and Y. Iijima, Lunar magnetic field observation and initial global mapping of lunar magnetic anomalies by MAP-LMAG onboard SELENE (Kaguya), Space Sci. Rev., 154, 219– 251, 2010. Vaisberg, O. L., L. A. Avanov, A. V. Leibov, V. N. Smirnov, J. Keller, T. Moore, D. Chornay, M. Collier, V. S. Troshin, and V. D. Myagkikh, A panoramic plasma spectrometer: An all-sky camera for charged particles, COSMIC RESEARCH, 43, 5, 373–376, 2005, doi:10.1007/s10604005-0058-9. Yokota, S. and Y. Saito, Estimation of picked-up lunar ions for future compositional remote SIMS analyses of the lunar surface, Earth Planets Space, 57, 281–289, 2005. Yokota, S. and Y. Saito, Circular one-dimensional position-sensitive timeof-flight microchannel plate detector using resistive anode for space plasma measurements, Rev. Sci. Instrum., 79, 013301, 2008. Yokota, S., Y. Saito, K. Asamura, and T. Mukai, Development of an ion energy mass spectrometer for application on board three-axis stabilized spacecraft, Rev. Sci. Instrum., 76, 014501-1–014501-8, 2005. Yokota, S., Y. Saito, K. Asamura, T. Tanaka, M. N. Nishino, H. Tsunakawa, H. Shibuya, M. Matsushima, H. Shimizu, F. Takahashi, M. Fujimoto, T. Mukai, and T. Terasawa, First direct detection of ions originating from the Moon by MAP-PACE IMA onboard SELENE (KAGUYA), Geophys. Res. Lett., 36, L11201, 2009, doi:10.1029/2009GL038185. Young, D. T., S. J. Bame, M. F. Thomesen, R. H. Martin, J. L. Burch, J. A. Marshall, and B. Reinhard, 21/4-radian field-of-view toroidal electrostatic analyzer, Rev. Sci. Instrum., 59, 743–751, 1988. Young, D. T., J. J. Berthelier, M. Blanc, J. L. Burch, A. J. Coates, R. Goldstein, M. Grande, T. W. Hill, R. E. Johnson, V. Kelha, D. J. McComas, E. C. Sittler, K. R. Svenes, K. Szegö, P. Tanskanen, K. Ahola, D. Anderson, S. Bakshi, R. A. Baragiola, B. L. Barraclough, R. K. Black, S. Bolton, T. Booker, R. Bowman, P. Casey, F. J. Crary, D. Delapp, G. Dirks, N. Eaker, H. Funsten, J. D. Furman, J. T. Gosling, H. Hannula, C. Holmlund, H. Huomo, J. M. Illiano, P. Jensen, M. A. Johnson, D. R. Linder, T. Luntama, S. Maurice, K. P. McCabe, K. Mursula, B. T. Narheim, J. E. Nordholt, A. Preece, J. Rudzki, A. Ruitberg, K. Smith, S. Szalai, M. F. Thomsen, K. Viherkanto, J. Vilppola, T. Vollmer, T. E. Wahl, M. Wüest, T. Ylikorpi, and C. Zinsmeyer, Cassini plasma spectrometer investigation, Space Sci. Rev., 114, 1–4, 1–112, 2004, doi:10.1007/s11214-0041406-4. Y. Saito (e-mail: [email protected])