基本情報
- 所属
- 国立研究開発法人宇宙航空研究開発機構 宇宙科学研究所 太陽系科学研究系 助教東京大学 大学院理学系研究科 地球惑星科学専攻 助教
- 学位
- 理学博士(名古屋大学)理学修士(名古屋大学)
- 連絡先
- hayakawa
planeta.sci.isas.jaxa.jp
- J-GLOBAL ID
- 200901009402364446
- researchmap会員ID
- 1000363026
経歴
3-
2007年9月 - 現在
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2003年10月 - 2007年8月
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1990年3月 - 2003年9月
学歴
2-
- 1989年
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- 1984年
論文
66-
Icarus 420 116204-116204 2024年9月15日 査読有り
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2024年7月3日++ 1. IntroductionThe Hayabusa2 spacecraft is currently cruising through deep space for the extended mission Hayabusa2#. The spacecraft is scheduled to flyby asteroid 2002 CC21 in 2026 and rendezvous with asteroid 1998 KY26 in 2031. Hayabusa2's VIS cameras include the ONC-T (Onborad Navigation Camera - Telescopic) and the wide-angle ONC-W1 and ONC-W2 (Figure 1). ONC-T, with its high sensitivity and multi-band observation capability, is the primary scientific instrument [1]. During the long cruise, ecliptic light observations [2] and exoplanet observations [3] continue as ONC-T observations. On the other hand, we are exploring ways to further utilize ONC cameras during the cruisng phase, and in this study, we examine how to utilize ONC-W2 and plan to process the data. Figure 1. Schematic view of the configuration of ONC-T, W1, and W2 (after [4]). Blue line indicates the solar array paddle.++ 2. Characteristics of ONC-W2The disadvantages and advantages of using the ONC-W2 for distant objects are as follows.[Disadvantages] Low sensitivity and stray light- The sensitivity of the ONC-W2 is not sufficient to observe distant objects because it is designed to observe the surface of an asteroid with disk-resolved situation.- The stray light from the multi-layer insulation at the edge of ONC-W2's FOV is very large for long exposure observation.[Advantage] Wide range of observable direction- The ONC-W2 camera can observe a wide area, whereas the ONC-T camera can only point in a narrow directions due to the limitations of the solar array paddle. Since the W2 camera faces the side of the solar array paddle (in the +Z direction of the spacecraft), it can cover 48% of the entire sky by turning the spacecraft attitude around the +Z axis and pointing the camera in different directions without losing power.Due to its low sensitivity but wide field of view, W2 could be used, for example, to continuously observe bright new comets for several days or weeks. The most recent such possibility is the comet C/2023 A3 (Tsuchinshan-ATLAS). An example about the estimation of observable period is shown in Section 4.++ 3. Preparation of data processing methodsNew ONC-W2 applications will require additional tools different from those for Ryugu images. We are working on a list of necessary data processing methods and calibration tasks.+ Stray lightPrevious calibration studies have shown that the presence or absence of stray light in W2 depends on the attitude of the spacecraft [5]. When stray light does occur, the degree of stray light is significant (Figure 2). The primary countermeasure is to adopt an attitude that minimizes stray light, but it is also necessary to develop image processing methods to remove stray light. Figure 2. An example of ONC-W2 long exposure (44.6s) image with stray light. White dots are mainly hot pixels.+ Sensitivity checkThe sensitivity of ONC-W2 prior to Ryugu arrival has been confirmed by [5]. However, because of sensitivity changes due to the Ryugu touchdown and changes over time, it is necessary to confirm the current sensitivity. As a quick check tool, we have prepared a method to estimate the sensitivity statistically from multiple stars. Figure 3 below plots the relationship between the stars V mag and integrated DN from 43 frames observed in 2016, with stray light removed. These stars include variable stars, but the effect is expected to be smaller by using a large number of stars.  Figure 3. Relationship between the stars Vmag and integrated intensity (DN) of long exposure (44.6s) images.++ 4. Observation opportunitiesWe are also considering the preparation of methods and tools for narrowing down suitable observation opportunities for ONC-W2. The following is the case study of comet C/2023 A3.Figure 4 shows the timing of the comet's entry into the FOV of ONC-W2. The orbit of the comet was obtained from JPL Horizons Sytem [6]. In this figure, the entire space as seen from the spacecraft is projected in a simple cylindrical projection. The spacecraft is oriented with the solar array paddle (+Z) pointing toward the sun and the W2 camera side toward the lower ecliptic plane. The red dots are the direction of the comet calculated every other day. The comet was found to cross the FOV from August 20 to August 28, 2024. Further observation will be possible by changing the attitude of the spacecraft. Figure 5 shows the total magnitude of Comet C/2023 A3 as expected from the position of Hayabusa2, which is expected to be 2-3 magnitude at the end of August, bright enough to be observed by ONC-W2. At this time, the Earth is on the opposite side of the Sun, making it difficult to observe this comet. Therefore, observation of this comet by a spacecraft would be highly valuable as data. We plan to conduct an observational test with ONC-W2 during this period. We will present a preliminary report  in this presentation. Figure 4: Calculated timing of comet crossing in ONC-W2 field of view. Figure 5. Predicted total magnitude of Comet C/2023 A3 from the position of Hayabusa2.++6. ConclusionWe examine how to utilize Hayabusa2 ONC-W2 camera in the cruising phase. Due to its low sensitivity but wide field of view, ONC-W2 could be used to continuously observe bright new comets for several days or weeks. We plan to conduct an observational test of the the comet C/2023 A3 in August. We will present a preliminary report  in this presentation.++ Acknowledgement: We thank the Haybusa2# systems and science teams for discussing the feasibility of the operation.++ References: [1] Sugita et al. (2019) Science 364, eaaw0422. doi.org/10.1126/science.aaw0422 [2] Tsumura et al. (2023) Earth Planets Space 75, 121. doi.org/10.1186/s40623-023-01856-x [3] Yumoto et al. (2024) 55th LPSC, Abstract 1774.  [4] Kouyama et al. (2021) Icarus 360, 114353. doi.org/10.1016/j.icarus.2021.114353  [5] Tatsumi et al. (2019) Icarus 325,153-195. doi.org/10.1016/j.icarus.2019.01.015 [6] NASA JPL Horizons System. https://ssd.jpl.nasa.gov/horizons/app.html#/
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Icarus 417 116122-116122 2024年7月 査読有り
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Communications Earth & Environment 4(1) 2023年9月27日 査読有りAbstract Returned samples from Cb-type asteroid (162173) Ryugu exhibit very dark spectra in visible and near-infrared ranges, generally consistent with the Hayabusa2 observations. A critical difference is that a structural water absorption of hydrous silicates is around twice as deep in the returned samples compared with those of Ryugu’s surface, suggesting Ryugu surface is more dehydrated. Here we use laboratory experiments data to indicate the spectral differences between returned samples and asteroid surface are best explained if Ryugu surface has (1) higher porosity, (2) larger particle size, and (3) more space-weathered condition, with the last being the most effective. On Ryugu, space weathering by micrometeoroid bombardments promoting dehydration seem to be more effective than that by solar-wind implantation. Extremely homogeneous spectra of the Ryugu’s global surface is in contrast with the heterogeneous S-type asteroid (25143) Itokawa’s spectra, which suggests space weathering has proceeded more rapidly on Cb-type asteroids than S-type asteroids.
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Earth, Planets and Space 75(1) 2023年8月22日 査読有りAbstract Zodiacal light (ZL) is sunlight scattered by interplanetary dust particles (IDPs) at optical wavelengths. The spatial distribution of IDPs in the Solar System may hold an important key to understanding the evolution of the Solar System and material transportation within it. The number density of IDPs can be expressed as n(r)∼r−α, and the exponent α∼1.3 was obtained by previous observations from interplanetary space by Helios 1/2 and Pioneer 10/11 in the 1970s and 1980s. However, no direct measurements of α based on ZL observations from interplanetary space outside Earth’s orbit have been performed since then. Here, we introduce initial results for the radial profile of the ZL at optical wavelengths observed over the range 0.76−1.06 au by ONC-T aboard the Hayabusa2# mission in 2021-2022. The ZL brightness we obtained is well reproduced by a model brightness, although there is a small excess of the observed ZL brightness over the model brightness at around 0.9 au. The radial power-law index we obtained is α=1.30±0.08, which is consistent with previous results based on ZL observations. The dominant source of uncertainty arises from the uncertainty in estimating the diffuse Galactic light (DGL). Graphical Abstract
MISC
55-
第50回月・惑星シンポジウム = Proceedings of the 50th ISAS Lunar and Planetary Symposium 2017年8月第50回月・惑星シンポジウム (2017年8月3-4日. 宇宙航空研究開発機構宇宙科学研究所(JAXA)(ISAS)), 相模原市, 神奈川県著者人数: 15名資料番号: SA6000200016
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遊・星・人: 日本惑星科学会誌 22(3) 152-158 2013年9月 査読有り招待有りはやぶさ2には小型の衝突装置(SCI)が搭載されており,これは秒速2kmで小惑星表面に衝突してクレーターを形成する.このクレーターは小惑星内部を覗くための小窓であり,リモートセンシング観測やサンプル回収から,小惑星表面の宇宙風化や浅内部構造に関する知見を得る.一方, SCIが衝突する様子は分離カメラ(DCAM3)により撮影され,イジェクタカーテンの拡大する様子や小惑星周囲を飛び交うダストを観察する. SCIによる小惑星への衝突は宇宙衝突実験ともいえる.我々はこの世界で最初の小惑星における宇宙衝突実験の機会を利用して,微小重力下における「本物の小惑星物質」のクレーター形成過程を明らかにする.
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日本惑星科学会秋期講演会予稿集 2012 19-19 2012年10月24日
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Lunar Planet. Sci. XXXII, 1497-1498 2001年
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Lunar Planet. Sci. XXXII, 1495-1496 2001年
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Lunar Planet. Sci. XXXII, 1497-1498 2001年
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Lunar Planet. Sci. XXXII, 1495-1496 2001年
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Proc. Fourth Int. Conf. On the Exploration and Utilisation of the Moon: ESA SP-462 462 187-190 2000年
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Proc. Fourth Int. Conf. On the Exploration and Utilization of the Moon:ESA SP-462 462 107-114 2000年
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Proceeding of International Workshop on Penetrometry in the Solar System 125-136 2000年
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Inst. Space Astron. Sci. Rep. No.677 677 1-21 2000年A hard landing probe "penetrator" has been thought to be a very useful tool for planetary exploration, because it provides cost-effective capability of deploying scientific instruments on planetary surface and subsurface. But development of the penetrator for planetary exploration requires better understanding penetration dynamics in geological materials. The present paper describes some experimental results on the penetrator dynamics obtained during the course of the development of the LUNAR-A penetrator. Special emphasis is placed on understanding the effect of the oblique incidence and the attack angle of the penetrator on penetration depth and a final attitude at the rest position. Many impact experiments into a simulated lunar surface material are made using penetrators 30 mm in diameter, and the penetration characteristics (penetration path length and inflection angle) are investigated as functions of impact velocity, penetrator shape, impact angle and attack angle. The results indicate that the torque applied to the penetrator in cases of the impact with a finite attack angle changes the penetration characteristics significantly. The experimental data also suggests that the impact angle does not have a substantial effect on penetration path length and that the truncation of the nose tip from a conical nose is efficient to stabilize the penetration orientation.
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PROCEEDINGS OF THE FOURTH INTERNATIONAL CONFERENCE ON EXPLORATION AND UTILISATION OF THE MOON 462 107-114 2000年The Japanese lunar penetrator mission, LUNAR-A, is planned to be launched in February 2003. This mission aims to study the lunar interior by using seismometers and heat flow probes on board the lunar penetrators. Two penetrators will be deployed on the lunar surface; one on the nearside, and another on the farside. The seismic study will be made by observing various deep moonquakes at two widely different penetrator sites. fin particular, observations of the amplitudes and travel-times of nearside deep moonquake events at the farside station will reveal core size of the moon, if it exists. Heat flow experiments are also made at two sites in order to better constrain the average lunar heat flow. Obtaining the new data on the core size and the average lunar heat now are crucial to understand the bulk abundance of the siderophile and refractory elements, which in turn are essential to understand the origin of the moon.
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Proceeding of International Workshop on Penetrometry in the Solar System 125-136 2000年
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The Institute of Space and Astronautical Science report 677 1-21 2000年A hard landing probe "penetrator" has been thought to be a very useful tool for planetary exploration, because it provides cost-effective capability of deploying scientific instruments on planetary surface and subsurface. But development of the penetrator for planetary exploration requires better understanding penetration dynamics in geological materials. The present paper describes some experimental results on the penetrator dynamics obtained during the course of the development of the LUNAR-A penetrator. Special emphasis is placed on understanding the effect of the oblique incidence and the attack angle of the penetrator on penetration depth and a final attitude at the rest position. Many impact experiments into a simulated lunar surface material are made using penetrators 30 mm in diameter, and the penetration characteristics (penetration path length and inflection angle) are investigated as functions of impact velocity, penetrator shape, impact angle and attack angle. The results indicate that the torque applied to the penetrator in cases of the impact with a finite attack angle changes the penetration characteristics significantly. The experimental data also suggests that the impact angle does not have a substantial effect on penetration path length and that the truncation of the nose tip from a conical nose is efficient to stabilize the penetration orientation.
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Adv. Space Res. 23(11) 1825-1828 1999年
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MOON AND MARS 23(11) 1825-1828 1999年Lunar heat flow experiment is planned by using two LUNAR-A penetrators which will be deployed on the near-side and far-side of the lunar surface in 2000. Each penetrator has seven absolute and eleven relative temperature sensors. Impact experiments for real-size penetrator models onto a lunar-regolith analogue target confirmed that the sensors and electronics used in the Lunar-A Heat Flow Experiment can survive the shock loading expected during penetration of the penetrator in a lunar regolith. The calibration experiment demonstrates that the temperature sensors have a resolution of 0.01 degrees and that the thermal conductivity device have 10 % accuracy. In order to determine the heat flow value, we need a good thermal model and numerical simulation for the penetrator and the regolith which in turn requires accurate measurements of thermal properties of the penetrator's components. The current numerical models indicate that we will be able to obtain the lunar heat flow values within 20 to 30 percents in precision with this method. (C) 1999 COSPAR. Published by Elsevier Science Ltd.
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日本惑星科学会秋期講演会予稿集 1995 205-205 1995年11月13日The accelerometer onboard LUNAR-A penetrator is developed to estimate the depth of emplacement and information on the physical properties of the lunar regolith. The decceleration record is also indispensable to design the structure of the outer case of lunar penetrator and to investigate quantitatively the shock-resistant capacity for the payload instruments. Investigation of several kinds of sensors' performance and improvement of the data acquisition system are made in order to design the most suitable accelerometer and its electronics for LUNAR-A penetrator. Using the piezoelectric type sensor with annular shear mode, the acceleration profiles with the sufficient accuracy are obtained under the actual flight conditions.
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J. Phys. Earth 41(5) 291-304 1993年
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JOURNAL OF PHYSICS OF THE EARTH 41(5) 291-304 1993年In order to study the effectiveness of GPS (Global Positioning System) differential positioning for the deployed Antarctic penetrator, we made fall tests by changing the release altitude at 160, 330, 680, and 1,000 m above the ground. A two-blade helicopter equipped with a Trimble GPS Pathfinder was used in the experiment at the Aoyama Pasture, Hokkaido, in April 1991. As compared with the precise location (0.1 m accuracy) determined by the GPS doubly differenced phase analysis, post-processed 1 min (less than 60 data points during PDOP<10) average of the helicopter hovering GPS differential navigation data was accurate to 10 m for a horizontal location (hovering method). By knowing the release time to an accuracy of 1 s, the impact location can be predicted by tracing the falling trajectory (trajectory method). Thus estimated position was accurate to 30 m against the precise location. As for a height accuracy, there was an error of +/- 10 m in the hovering method. This error further degraded to +/- 20 m when the coordinates of the reference site were replaced by a time-average (1-2 h duration) of the point-positioning results. The above obtained positioning accuracies are enough for a long-range (300 km profile) seismic explosion experiments of each 5-10 km station separation, because the associated errors result only in 0.2% uncertainty on the estimate of P-wave velocity structures.
書籍等出版物
2-
Primitive Solar Nebula and Origin of the Planets(Terra Publication Press) 1993年
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Primitive Solar Nebula and Origin of the Planets(Terra Publication Press) 1993年
講演・口頭発表等
227-
56th LPSC 2025年3月13日
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Hayabusa 2024 2024年11月13日 招待有り
所属学協会
3-
2009年 - 現在
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1992年 - 現在
Works(作品等)
6共同研究・競争的資金等の研究課題
10-
日本学術振興会 科学研究費助成事業 基盤研究(A) 2015年4月 - 2018年3月
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日本学術振興会 科学研究費助成事業 2000年 - 2002年
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日本学術振興会 科学研究費助成事業 1997年 - 1998年
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日本学術振興会 科学研究費助成事業 1992年 - 1993年
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1984年 - 1990年