2 00 1 The Giant Flare of 1998 August 27 from SGR 1900 + 14 : II . Radiative Mechanism and Physical Constraints on the Source
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چکیده
The extraordinary 1998 August 27 giant flare places strong constraints on the physical properties of its source, SGR 1900+14. We make detailed comparisons of the published data with the magnetar model, which identifies the Soft Gamma Repeaters as neutron stars endowed with ∼ 10 15 G magnetic fields. The giant flare evolved through three stages, whose radiative mechanisms we address in turn. The extreme peak luminosity L > 10 6 L edd , hard spectrum, and rapid variability of the initial ∼ 0.5 s spike emission all point to an expanding pair fireball with very low baryon contamination. We argue that this energy must have been deposited directly through shearing and reconnection of a magnetar-strength external magnetic field. Low-order torsional oscillations of the star fail to transmit energy rapidly enough to the exterior, if the surface field is much weaker. A triggering mechanism is proposed, whereby a helical distortion of the core magnetic field induces large-scale fracturing in the crust and a twisting deformation of the crust and exterior magnetic field. After the – 2 – initial spike (whose ∼ 0.4 s duration can be related to the Alfvén-crossing time of the core), very hot (T ∼ < 1 MeV) plasma rich in electron-positron pairs remains confined close to the star on closed magnetic field lines. The envelope of the August 27 flare can be accurately fit, after ∼ 40 s, by the contracting surface of such a " trapped fireball. " The form of this fit gives evidence that the temperature of the trapped pair plasma decreases outward from its center. We quantify the effects of direct neutrino-pair emission on the X-ray light curve, thereby deducing a lower bound µ min ∼ 1 × 10 32 G-cm 3 to the magnetic moment of the confining field – comparable to the strongest fields measured in radio pulsars. The radiative flux during the intermediate ∼ 40 s of the burst appears to exceed the trapped fireball fit. The lack of strong rotational modulation and intermediate hardness of this smooth tail are consistent with the emission from an extended pair corona, in which O-mode photons are heated by Compton scattering. This feature could represent residual seismic activity within the star, and accounts for ∼ 10 percent of the total flare fluence. We consider in detail the critical luminosity, below which a stable balance can be maintained between heating and radiative cooling in …
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GEOTAIL observation of SGR 1900 + 14 giant flare on 27 August 1998
The soft gamma repeater (SGR) 1900+14 emitted the giant flare on 27 August 1998. Most gammaray detectors saturated during the initial spike of the giant flare because of the intense flux. However the plasma particle detector onboard GEOTAIL observed the first 300 ms time profile with a time resolution of 5.577 ms and the initial spike of the giant flare was first resolved. The time profile show...
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A radio afterglow was detected following the 1998 August 27 giant flare from the soft gamma repeater (SGR) 1900 14. Its short-lived behavior is quite different from the radio nebula of SGR 1806 20, but very similar to radio afterglows from classic gamma-ray bursts (GRBs). Motivated by this, we attempt to explain it with the external shock model as invoked in the standard theory of GRB afterglow...
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