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Quantum efficiencies of the XIS CCDs onboard Suzaku. T. Miyauchi, K. Hayashida, K. Torii, M. Namiki, N. Anabuki, S. Katsuda, N. Tawa, D. Matsuura, H. Tsunemi, Osaka Univ. (Japan); H. Nakajima, H. Yamaguchi, H. Matsumoto, T. G. Tsuru, Kyoto Univ. (Japan); T. Kohmura, Kougakuin Univ. (Japan);
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Quantum efficiencies of the XIS CCDs onboard Suzaku T. Miyauchi, K. Hayashida, K. Torii, M. Namiki, N. Anabuki, S. Katsuda, N. Tawa, D. Matsuura, H. Tsunemi, Osaka Univ. (Japan); H. Nakajima, H. Yamaguchi, H. Matsumoto, T. G. Tsuru, Kyoto Univ. (Japan); T. Kohmura, Kougakuin Univ. (Japan); H. Katayama, Japan Aerospace Exploration Agency (Japan); E. Miller, B. LaMarr, S. E. Kissel, M. W. Bautz, Massachusetts Institute of Technology [6266-100]
Outline of the Problem Findings • Some of the observed spectra at low energy (<1keV) were not what we expected • According to the knowledge from previous missions. • Inconsistent among the XIS 4 sensors • QE degradation at low energy is explained by introducing extra carbon absorber in the XIS response (~2005Dec). Contamination is most likely cause. • We performed repeated observations of one source (E0102). Evolution of the QE degradation was found. • XIS response in which extra carbon absorber was prepared and distributed to SWG members and GOs, with empirical model of its time evolution. • Analysis of diffuse sources indicated non-uniformity of the carbon absorber within XIS FOV. Contamination on OBF is most likely cause. • Analysis of atmospheric fluorescent line provided further data for time evolution and non-uniformity. • Detailed spectrum analysis of some sources provided information on the composition of the absorber.
RXJ1856.5-3754 Discovered with ROSAT Nearby (D~120pc) Isolated Neutron Star X-ray spectrum is fitted with a simple blackbody ( against NS atmosphere model). R~4-5km Quark Star ?
RXJ1856 Observed with Suzaku 2005-10/24~26RMF 20051210 a-d for XIS1 Rev0.3 data -10eV offset C-K edge ~0.3keV a: Based on the Cal on the Ground b: a x excess0.15mmC c: Dead Layer =Design Value d: c x excess0.15mmC
Suzaku/XIS ContaminationMeasurements with E0102 • E0102: SNR in SMC, bright in soft X-ray lines • excellent calibrator for low-E gain, QE changes • contamination degrading low-E eff. area of all XIS’s • model • thermal bremss + 24 Gaussian emission lines • Galactic + SMC absorption • pure C absorption from contaminant (varabs) • gain shift -5 eV ~ -15 ev • r2 ~ 1.6 (FIs) to 2.5 (BI) NeIX OVIII NeX MgXI OVII 2005-08-13 2005-08-31 2005-12-16 2006-01-17 2006-02-02
XIS Contamination Rate • empirical correction for observers • contamination rate turnover (?) • SMC NH uncertainty systematic error ±0.02 m independent of epoch change in effective C column: chip slope intercept (1016 cm-2/day) XIS0 1.6 ±0.1 4.4 ±4.0 XIS1 2.7 ±0.1 -9.6 ±15 XIS2 3.1 ±0.1 -3.2 ±14 XIS3 4.1 ±0.5 54. ±50.
Cyg Loop • Nearby Old Super Nova Remnant • 2005Nov 4pointgs C-band CVI-band
C-band/CVI-band map in detector coordinate =Inidicating absorber thickness is not uniform
Center Rim C Absorber thickness is about 1/2 at Rim (2005 Nov)
Atmospheric Fluorescence Line • When the telescope is looking at the shining Earth or its atmosphere, fluorescence lines of the Earth atmosphere (N-K, O-K) by Solar X-rays are contaminated in the observed spectra. • Intensity and line ratio depends on the elevation angle from the Earth rim and the Solar activity. N-K (0.39keV) O-K (0.52keV) DAY EARTH 0 < DYE_ELV < 5 5 < DYE_ELV < 10 10 < DYE_ELV < 20 20 < DYE_ELV < 30
N-K line 2005-8-13 2005-9-4 2005-10-22 2005-11-28 2005-12-24 2006-2-6 Day Earth 0 < DYE_ELV < 5 5 < DYE_ELV < 10 10 < DYE_ELV < 15 15 < DYE_ELV < 20 20 < DYE_ELV < 25 From Anabuki et al.’s poster Atmospheric N-K line Map XIS1(BI) Color code is adjusted for each map
2005-8-13 2005-9-4 2005-10-22 2005-11-28 2005-12-24 2006-2-6 Day Earth 0 < DYE_ELV < 5 5 < DYE_ELV < 10 10 < DYE_ELV < 15 15 < DYE_ELV < 20 20 < DYE_ELV < 25 Atmospheric O-K line Map XIS1(BI)
E0102-72 SN1006_NE_BGD Mrk 3 A2811_offset NGC 4388 MBM12_off Cloud N-K line O-K line N-K line O-K line N-K line O-K line N-K line O-K line N-K line O-K line N-K line O-K line Day Earth Radial Profile(vignetting corrected,normalized by center region)
N-K line O-K line Center 6mm radius / Other area • Mean Free Path in C(2.2g/cc) • 0.182mm for N-K line • 0.375mm for O-K line • Spatial Difference in Carbon contamination thickness can be modeled with Atmospheric N-K, O-K data. • Thickness at the center is evaluated by E0102 and RXJ1856 obs. • Thickness (t,detx,dety) will be modeled/introduced in arfbuilder (or rmfbuilder).
PKS2155-304 NH(Gal)=1.65e20cm~-2 XIS1(BI) NH(Gal)*Pow NH(Gal)*N_C*Pow NH(Gal)*N_C*N_O*Pow XIS3(FI) NH(Gal)*Pow NH(Gal)*N_C*Pow NH(Gal)*N_C*N_O*Pow
N_C vs N_O Cf DEHP(C24H38O4) N_O/N_C=1/6=0.17
If we assume the contaminant is DEHP… XIS1 XIS3 Assuming DEHP NH(Gal)*DEHP*Pow NH(Gal)*DEHP*Pow XIS1 XIS3 Best fit C/O ratio NH(Gal)*N_C*N_O*Pow NH(Gal)*N_C*N_O*Pow The data may not reject the possibility of DEHP.
Contamination 2D model • E0102 +RXJ1856 Obs →Contaminant thickness at Center • Atmospheric N-K/O-K → Difference in Contaminant thickness as a function of radius E(t) is the thickness of the carbon at the center
If we assume the contaminant has significant contribution from Oxygen C:O=6:1
Summary • QE degradation in Suzaku XIS has been studied. • Absorber (Contaminat) thickness: XIS0<XIS1<XIS2<XIS3 • Absorber thickness: Rim ~ 1/2 of the Center. Atmospheric N-K, O-K line is efficient to evaluate the distribution of the absorber. • Contamination Rate was almost constant in 2005, but the rate is decreasing recently. • Carbon is dominant in the contaminant . There is a small contribution of O. PKS2155 results gives O/C <0.13. • Empirical model of the QE degradation as a function of time and location has been made. • Recent RXJ1856 & E0102 observations indicate O contribution might be significant. Assuming O/C =1/6 gives smooth connection in time plot.