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Historical Seismograms - Evidence from the AD 2000 Izu Islands ...

Historical Seismograms - Evidence from the AD 2000 Izu Islands ...

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440 Yasuhiro Umeda and Katsuyoshi It0I Wiechert1 Strong-motion III19?0 Go 'go '60 ?O '80II ..LOW- gain[:.,..::,~;:,.-..::;.-* ........ ..:*: i :*.:.*.: . .. ,::-.-.::':..-.._. ._I ong - period=I I 1 I 1 I IFirst year m?? Second year mi Third yearFigure 1. Microfilming schedule.The first frame of <strong>the</strong> microfilm is a resolution chart for <strong>the</strong> focus and <strong>the</strong> exposurecorrections. The second to <strong>the</strong> eighth frames contain information on how touse <strong>the</strong> microfilm. The second frame shows <strong>the</strong> roll number and <strong>the</strong> dates of <strong>the</strong>seismograms being filmed. The third frame shows <strong>the</strong> station name, address, latitude,longitude, etc. The fourth frame (Figure 2) shows <strong>the</strong> name of <strong>the</strong> instrumentand its constants along with <strong>the</strong> response curves. The fifth frame (Figure 3) showsphotographs of <strong>the</strong> Wiechert seismographs; <strong>the</strong> direction of ground displacement on<strong>the</strong> original seismogram is also drawn on <strong>the</strong> right side of this frame. The originalseismograms are smoked paper records.The sixth frame (Figure 4) indicates <strong>the</strong> filming format. The seismogram of <strong>the</strong>Wiechert instrument is a ring-shaped paper with a total length of 180 cm. Eachseismogram is folded in two, as shown in <strong>the</strong> upper left of Figure 4. Two sides of<strong>the</strong> seismogram, i.e. A- and B-plane, are filmed in two frames of <strong>the</strong> microfilm. Oneside of <strong>the</strong> three-component seismogram is filmed on one frame, and <strong>the</strong> o<strong>the</strong>r sideis filmed on <strong>the</strong> successive frame, as shown in <strong>the</strong> bottom of Figure 4. Generally,<strong>the</strong> side on which some information is described on <strong>the</strong> seismogram is chosen as<strong>the</strong> A-plane. The three-component seismogram is arranged <strong>from</strong> top to bottomin <strong>the</strong> order of vertical, east-west, and north-south components. If <strong>the</strong> east-westcomponent is missing, <strong>the</strong> middle place in <strong>the</strong> frame is blank, as shown in Figure4. A small label (10 x 3.5 cm) is affixed in <strong>the</strong> margin of each seismogram. Thestation, instrument, A- or B-plane, year, component, data on/off time, and a scaleindicating <strong>the</strong> original record length per minute are given on this label. Since <strong>the</strong>drive speed of <strong>the</strong> recording sheet is 3 cm per minute, <strong>the</strong> length of one recordline (180 cm) is one hour. Time is Japanese Standard Time (JST), and UniversalCoordinate Time (UTC) is JST minus 9 hours.The seventh frame, sometimes 7th to 9th frames, is an inventory sheet (Figure 5 )indicating whe<strong>the</strong>r <strong>the</strong> seismograms are present or missing. A blank column indicatesthat <strong>the</strong> records are saved, whereas an oblique line in a column indicatesa missing record. When large amplitude seismic waves were recorded and/or <strong>the</strong>instrument was adjusted, a new recording sheet was set on twice or three times ina day. In this case, <strong>the</strong> number of seismograms per day is described in <strong>the</strong> column."C" in <strong>the</strong> column indicates that <strong>the</strong> calibration signals, i.e. free period, dampingratio and <strong>the</strong> static magnification of <strong>the</strong> instrument are recorded on <strong>the</strong> seismogram.

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