Correspondence between the measuring and seismograph record of the power that are introduced to a/the real existence Kamae thing at the time of an/the earthquake

2003年宫城-肯-北部地震(PGA 2037ga)、2004年新泻-Ken-Cyuetsu地震(PGA 1750al)和1995年兵库-肯-南部地震(PGA 818al)记录到的一些强震加速作用。然而，几乎没有直接测量地震对结构产生什么样的应力或应变的实例。在过去地震造成的各种破坏结构中，可以看到极其具体的破坏结构。它不能证明起源于冲击力，因为这样的记录在地震仪中是不存在的，尽管冲击力的存在是对此的猜测。可以想象，地震仪的测量记录中并不包含所有的地震动特征。为此，我们在大阪市立大学进行了地震加速度应变测量系统的建设。地震波和应变波之间的可调性，我们从测量记录中积累数据。此外，我们还进行了地震反应分析，通过分析阐明了地震反应的特点。

Some strong motion accelerations recorded in the 2003 Miyagi-Ken-Hokubu earthquake (PGA 2037gal), the 2004 Niigata-Ken-Cyuetsu earthquake (PGA 1750gal) and Hyogo-Ken-Nanbu Earthquake (PGA 818gal) in 1995. However, there is not the example that measured whether what kind of stress or strain occurred to a structure by an earthquake directly almost. The extremely specific destruction structure is seen, into the various destruction structures that resulted with the earthquake in the past. It is not able to prove to originate from impact force, because the record like that does not exist in the seismograph, although the existence of impact force is guessed to this. It is conceivable that all the characteristics of the ground motions are not included in the measuring record of the seismograph. Accordingly, it is thought that the relevancy with the record of a usual seismograph does not attach in the destruction of the structure.Thereupon, we did the construction of the measuring system that the acceleration and strain by an earthquake measure in Osaka City University. The adjustability between an earthquake wave and strain wave we do the accumulation of the data from the measuring record. Furthermore, we did a seismic response analysis, to clarify a seismic response characteristic by the analysis.