广西大学学报(自然科学版)
廣西大學學報(自然科學版)
엄서대학학보(자연과학판)
JOURNAL OF GUANGXI UNIVERSITY (NATURAL SCIENCE EDITION)
2015年
3期
680-685
,共6页
伽玛暴%双喷流%外激波模型
伽瑪暴%雙噴流%外激波模型
가마폭%쌍분류%외격파모형
Gamma-ray bursts ( GRBs)%two components jet%external shock
伽玛暴余辉的双拐折行为可以用双喷流成份结构模型得到较好的解释,但至今其物理参数还未解.为给出其相应的物理参数,文中将对具有双喷流成份的伽玛暴光学余辉进行统计分析,用外激波模型时域指数α和频域指数β的关系(closure relation)对数据进行限制,得到 GRB 071003,GRB 080319B,GRB 090426和GRB 100219A共4个具有外激波模型的伽玛暴双成份喷流特征.这些伽玛暴第一个喷流成份的张角都在1°以内,而第二个喷流成份的张角增大到2°ц7°,与单成份喷流的张角一致.其各向同性辐射能量在1051ц1054 erg,电子谱指数p约为2,比典型值2.3硬.长暴能较好符合Amati关系.
伽瑪暴餘輝的雙枴摺行為可以用雙噴流成份結構模型得到較好的解釋,但至今其物理參數還未解.為給齣其相應的物理參數,文中將對具有雙噴流成份的伽瑪暴光學餘輝進行統計分析,用外激波模型時域指數α和頻域指數β的關繫(closure relation)對數據進行限製,得到 GRB 071003,GRB 080319B,GRB 090426和GRB 100219A共4箇具有外激波模型的伽瑪暴雙成份噴流特徵.這些伽瑪暴第一箇噴流成份的張角都在1°以內,而第二箇噴流成份的張角增大到2°ц7°,與單成份噴流的張角一緻.其各嚮同性輻射能量在1051ц1054 erg,電子譜指數p約為2,比典型值2.3硬.長暴能較好符閤Amati關繫.
가마폭여휘적쌍괴절행위가이용쌍분류성빈결구모형득도교호적해석,단지금기물리삼수환미해.위급출기상응적물리삼수,문중장대구유쌍분류성빈적가마폭광학여휘진행통계분석,용외격파모형시역지수α화빈역지수β적관계(closure relation)대수거진행한제,득도 GRB 071003,GRB 080319B,GRB 090426화GRB 100219A공4개구유외격파모형적가마폭쌍성빈분류특정.저사가마폭제일개분류성빈적장각도재1°이내,이제이개분류성빈적장각증대도2°ц7°,여단성빈분류적장각일치.기각향동성복사능량재1051ц1054 erg,전자보지수p약위2,비전형치2.3경.장폭능교호부합Amati관계.
Two components jet model can interpreter the behaviors of two breaks for gamma-ray bursts ( GRBs) afterglow. The two components jet break in the optical afterglow is studied is this work. A completed well-sample optical light-curves were included, using the empirical fitting andα-β closure relation of external forward shock model. 4 GRBs ( GRB 071003,GRB 080319B,GRB 090426 and GRB 100219A) are claimed as two components jets of the external forward shock mod-el. All of the jet opening angle of the first component is smaller than 1°,and they increase to 2°ц7° for the second component, which is consistent with the single component jet GRBs. The isotropic equivalent radiation energies vary from 1051 erg to 1054 erg and the electron spectral index p is about 2 , which is harder than the typical value of p=2 . 3 . The three long duration GRBs ( GRB 071003 , GRB 080319B and GRB 100219A) are consistent with the Amati relation.