地震学报
地震學報
지진학보
ACTA SEISMOLOGICA SINICA
2014年
4期
711-718
,共8页
权重%两步法%峰值加速度%分布规律
權重%兩步法%峰值加速度%分佈規律
권중%량보법%봉치가속도%분포규률
weight%two-step method%peak ground acceleration%distribution law
通过对距离和震级的分档将权重引入两步回归法:第一步,将地震记录按距离分档,每个记录得到的权重为 w′ij =1/(njn i )(其中 nj 为该记录所在档的地震数,ni 为该记录的地震在此档中的记录数),这种权重的取法不仅使各档的权重相同,而且保证每档中不同地震在各档中的权重也相同;第二步,将地震按震级分档,每次地震得到的权重为 v′k =1/nk (其中nk为该地震所在档的地震数)。以 Joyner 和 Boore 的数据为分析对象进行加权两步法的回归,并与传统两步法回归的结果进行比较。结果表明:传统两步法在近场拟合的小震峰值加速度的估计值偏大,大震峰值加速度的估计值偏小,其衰减曲线在远场的衰减速度过快;而加权两步法则能更好地反映地震动的空间分布规律。
通過對距離和震級的分檔將權重引入兩步迴歸法:第一步,將地震記錄按距離分檔,每箇記錄得到的權重為 w′ij =1/(njn i )(其中 nj 為該記錄所在檔的地震數,ni 為該記錄的地震在此檔中的記錄數),這種權重的取法不僅使各檔的權重相同,而且保證每檔中不同地震在各檔中的權重也相同;第二步,將地震按震級分檔,每次地震得到的權重為 v′k =1/nk (其中nk為該地震所在檔的地震數)。以 Joyner 和 Boore 的數據為分析對象進行加權兩步法的迴歸,併與傳統兩步法迴歸的結果進行比較。結果錶明:傳統兩步法在近場擬閤的小震峰值加速度的估計值偏大,大震峰值加速度的估計值偏小,其衰減麯線在遠場的衰減速度過快;而加權兩步法則能更好地反映地震動的空間分佈規律。
통과대거리화진급적분당장권중인입량보회귀법:제일보,장지진기록안거리분당,매개기록득도적권중위 w′ij =1/(njn i )(기중 nj 위해기록소재당적지진수,ni 위해기록적지진재차당중적기록수),저충권중적취법불부사각당적권중상동,이차보증매당중불동지진재각당중적권중야상동;제이보,장지진안진급분당,매차지진득도적권중위 v′k =1/nk (기중nk위해지진소재당적지진수)。이 Joyner 화 Boore 적수거위분석대상진행가권량보법적회귀,병여전통량보법회귀적결과진행비교。결과표명:전통량보법재근장의합적소진봉치가속도적고계치편대,대진봉치가속도적고계치편소,기쇠감곡선재원장적쇠감속도과쾌;이가권량보법칙능경호지반영지진동적공간분포규률。
Weight is introduced into two-step method by grading distances and magnitude.In the first step,the recordings are divided into several intervals by range of distances.Every recording gets one weight w′ij =1/(njn i )(nj is the number of earthquakes in the interval in which the recording is located,ni is the number of recordings of the earthquake in this interval).Not only does the way of getting weight keep equal weight for every interval,but also promises the same weight for earthquakes in any interval.In the second step,the earth-quakes are divided into several intervals by range of magnitudes.Every earth-quake get one weight v′k =1/nk (nk is the number of earthquakes in the interval in which the earthquake is located).Taking the recordings used by Joyner and Boore (1981 )as instance,comparing results from weighted two-step method with that from traditional one,the results show that values of peak ground ac-celeration (PGA)in near sites fitted by traditional method are higher than that fitted by weighted method for small events and lower for large events,attenua-ting rates are much rapider in far sites;weighted two-step method is better to simulate spatial distribution laws of ground motions than traditional method.