地震学报
地震學報
지진학보
ACTA SEISMOLOGICA SINICA
2015年
2期
335-346
,共12页
朱永莉%黎大虎%龙承厚%孙泽涛
硃永莉%黎大虎%龍承厚%孫澤濤
주영리%려대호%룡승후%손택도
宏观仪器烈度%宏观考察烈度%强震动记录%反应谱
宏觀儀器烈度%宏觀攷察烈度%彊震動記錄%反應譜
굉관의기열도%굉관고찰열도%강진동기록%반응보
macroscopic instrumental intensity%macroscopic inspection intensi-ty%strong motion record%response spectrum
强震观测资料包括强震动时程记录资料和宏观震害调查资料两大类,前者是定量的微观数据,后者则是定性的宏观指标。本文明晰给出了微观仪器烈度与宏观仪器烈度、微观考察烈度与宏观考察烈度的概念,并在此基础上提出了只有在宏观仪器烈度与宏观考察烈度之间进行比较才具有实质性的意义;同时对国内外常见的仪器烈度算法进行了比较性研究,得出了袁一凡仪器烈度算法可靠性更高的结论;最后以四川地区历年来重要震例的强震动记录为依据,对修正的袁一凡仪器烈度算法的可靠性进行了比较应用。结果表明,对袁一凡仪器烈度算法修正与扩展的应用是可行的,同时也验证了将微观仪器烈度与宏观考察烈度直接进行比较会存在较大的差距。
彊震觀測資料包括彊震動時程記錄資料和宏觀震害調查資料兩大類,前者是定量的微觀數據,後者則是定性的宏觀指標。本文明晰給齣瞭微觀儀器烈度與宏觀儀器烈度、微觀攷察烈度與宏觀攷察烈度的概唸,併在此基礎上提齣瞭隻有在宏觀儀器烈度與宏觀攷察烈度之間進行比較纔具有實質性的意義;同時對國內外常見的儀器烈度算法進行瞭比較性研究,得齣瞭袁一凡儀器烈度算法可靠性更高的結論;最後以四川地區歷年來重要震例的彊震動記錄為依據,對脩正的袁一凡儀器烈度算法的可靠性進行瞭比較應用。結果錶明,對袁一凡儀器烈度算法脩正與擴展的應用是可行的,同時也驗證瞭將微觀儀器烈度與宏觀攷察烈度直接進行比較會存在較大的差距。
강진관측자료포괄강진동시정기록자료화굉관진해조사자료량대류,전자시정량적미관수거,후자칙시정성적굉관지표。본문명석급출료미관의기열도여굉관의기열도、미관고찰열도여굉관고찰열도적개념,병재차기출상제출료지유재굉관의기열도여굉관고찰열도지간진행비교재구유실질성적의의;동시대국내외상견적의기열도산법진행료비교성연구,득출료원일범의기열도산법가고성경고적결론;최후이사천지구력년래중요진례적강진동기록위의거,대수정적원일범의기열도산법적가고성진행료비교응용。결과표명,대원일범의기열도산법수정여확전적응용시가행적,동시야험증료장미관의기열도여굉관고찰열도직접진행비교회존재교대적차거。
Strong motion observation data is classified into two categories,one is strong motion time history data,the other is seismic damage investigation data. The former is the microscopic quantitative data,and the latter is the macro-scopic qualitative indexes.Firstly we define the concept of microscopic instru-mental intensity and macroscopic instrumental intensity,microscopic inspection intensity and macroscopic inspection intensity in the present paper.And then we propose it is significant to compare macroscopic instrumental intensity with macroscopic inspection intensity.Meanwhile we also conduct a comparative study about the instrumental intensity algorithms at home and abroad.The results indicate that Yuan’s instrumental intensity algorithm is more reliable. In addition,based on the strong motion records of Sichuan earthquakes,the modified Yuan’s algorithm is applied to calculate seismic intensity.The results show that it is feasible to revise and expand the Yuan’s instrumental intensity algorithm,and also prove that there exists large difference when the micro-scopic instrumental intensity is compared with macroscopic inspection intensity directly.