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Masnori Ohno (ISAS/JAXA). Different spectral correlation between short and long GRBs with Suzaku. Long/Short GRBs are different ?. There are two GRB classes, Long/Short GRBs in T90 distribution Different origin ? Hardness ratio; short/hard, long/soft (Kouvelioutou et al. 1993)
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Masnori Ohno (ISAS/JAXA) Different spectral correlation between short and long GRBs with Suzaku
Long/Short GRBs are different ? • There are two GRB classes, Long/Short GRBs in T90 distribution • Different origin ? • Hardness ratio; short/hard, long/soft (Kouvelioutou et al. 1993) • Spectral properties • (Paciesas et al. 2003, Ghirlanda et al. 2004, Ohno et al. yesterday’s talk.. etc) • How about z distribution ? • <z>~1 from Swift result • GRB080913 (z=6.7 T90,src~1s), Short ? Long ? • Low statistics Ghirlanda et al. 2004 Paciesas et al. 2001 α Epeak
Epeak-Eiso/Liso correlation • Epeak-Liso as the redshift indicator for long GRBs (Yonetoku et al. 2004) • Short GRBs do not satisyf Epeak-Eiso due to much lower energy • (Amati 2006, 2008, Ohno et al. 2007 …etc) • How about Epeak-Liso for short GRBs ?? Total energy (Eiso) Short (WAM) Ep-Eiso relation for Redshift-”unknown” Short GRBs by the WAM Long Long (Amati 2006) Long (WAM sample)
Epeak-Eiso/Liso correlation for short GRBs • Both z and Epeak information • z from Swift, but Swift can not determine Epeak • Wide-band and good statistics is needed for short GRB Epeak Joint analysis between Swift/BAT and Suzaku Wide-band All-sky Monitor is very useful to test these correlations for short GRBs
Suzaku Wide-band All-sky Monitor Suzaku/HXD is surrounded by thick (4cm), large (40cm) 20 high-z BGO crystals for active shielding. Wide-band All-sky Monitor (Suzaku/WAM) cross section top view Yamaoka et al. 09 Energy band: 50—5000 keV Effective area: 400cm2@1MeV Suzaku HXD-WAM Powerful tool for short GRB spectrum
WAM Short GRB correlations (1) sample Swift leads redshift measurement even for short GRBs WAM provides Epeak for 6 redshift-measured short GRBs ! GRB060801 Z=1.13 T90=0.44 GRB051221A Z=0.545 T90=0.22 GRB061006 Z=0.44 T90=0.42 1sec GRB061210 Z=0.41 T90=0.05 GRB070714B Z=0.92 T90=2.56 GRB071227 Z=0.383 T90=0.8 ※T90:50-5000 keV
WAM Short GRB correlations (2) spectral analysis Epeak is obtained from WAM/BAT joint spectral analysis Cutoff PL model is best fit for all sample Lpeak from WAM light curve (16ms time scale) GRB060801 Z=1.13 T90=0.44 GRB051221A Z=0.545 T90=0.22 GRB061006 Z=0.44 T90=0.42 WAM BAT GRB061210 Z=0.41 T90=0.05 GRB070714B Z=0.92 T90=2.56 GRB071227 Z=0.383 T90=0.8
WAM short GRB correlations (3) Epeak-Eiso correlation • Ghirlanda et al. (arXiv 0902.0983) • Long • Short WAM short GRBs Short GRBs do not satisfy Amati relation due to its much lower total energy Similar result to Ghirlanda et al. 2009 Eiso (1052 erg) 10-5 10-4 10-3 0.01 0.1 1 10 100 1000
WAM short GRB correlations (4)Epeak-Liso correlation GRB071227 WAM Short GRBs • Almost data seem to be consistent • within dispersion of Ghirlanda et al result. • Tend to be harder than long GRBs ? • GRB 071227 is clear outlier. • different correlation ? • systematics ? • It is difficult to conclude that short GRBs follow • the Epeak-Liso relation, need more sample ! Lpeak(1sec) (1052 erg) 10-5 10-4 10-3 0.01 0.1 1 10 100 1000
Summary We performed correlation analysis such as Epeak-Eiso and Epeak-Liso relation for short GRBs using BAT/WAM sample. (1) Short GRBs do not satisfy Epeak-Eiso relation (2) Roughly consistent with Epeak-Liso relation, however…. - large dispersion - tend to locate at harder Epeak regime - outlier ? (GRB071227) different correlation ? It is difficult to conclude that we can use the Epeak-Liso relation as the redshift indicator for short GRBs. Need more samples !