JPS6296587U - - Google Patents
Info
- Publication number
- JPS6296587U JPS6296587U JP18845285U JP18845285U JPS6296587U JP S6296587 U JPS6296587 U JP S6296587U JP 18845285 U JP18845285 U JP 18845285U JP 18845285 U JP18845285 U JP 18845285U JP S6296587 U JPS6296587 U JP S6296587U
- Authority
- JP
- Japan
- Prior art keywords
- waves
- wave
- borehole
- waveform
- record
- Prior art date
- Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
- Pending
Links
- 230000000630 rising effect Effects 0.000 description 1
Landscapes
- Geophysics And Detection Of Objects (AREA)
Description
そこで参考までに第1図に一般に標準的な波形
を示しましたが、この図でもわかる様に必らず第
一番目に(COMPRESSIONAL WAV
E)P波と言うものが来て次に(SHEAR W
AVE)S波が来るのである。地震でもわかる様
に第一に下からつき上げる様な振動がP波であり
、それから横にゆれる波がS波である。従つて現
在S波を確実に発生させて地層の測定をしようと
研究されているが残念ながら現在迄のところこれ
が解決されていない。そこで本考案ではこの点を
みごとに解決したのが第2図、第3図のS波のみ
の波形である。又、波形が完全なS波であると云
う事を証明する為には波形の立上りが完全に逆の
状態になることである。第2図、第3図を見れば
わかる通り、P波は少しもなく完全にS波のみで
逆転していることがわかる。この様にするには第
4図で示した様に孔内にてアームを孔壁に同列に
圧着し、その発信号から上下にすべるS波振動を
発信し、受信側もS波のみを受信する受振子を取
り付けてあるのでS波のみを感じる第2図、第3
図の様な完全なS波の波形が得られるのである。
Therefore, for reference, we have shown generally standard waveforms in Figure 1, but as you can see in this figure, the first waveform (COMPRESSIONAL WAV
E) Something called P wave comes and then (SHEAR W
AVE) S waves are coming. As you can see in earthquakes, the first vibrations that rise up from below are P waves, and the waves that sway laterally are S waves. Therefore, research is currently being carried out to measure the strata by reliably generating S waves, but unfortunately this problem has not been solved to date. Therefore, in the present invention, this point has been successfully solved by the waveforms of only the S waves shown in FIGS. 2 and 3. Also, in order to prove that the waveform is a perfect S wave, the rising edge of the waveform must be completely reversed. As you can see from Figures 2 and 3, the P waves are completely reversed with only the S waves. To do this, as shown in Figure 4, the arm is pressed into the hole in the same line as the wall of the hole, the emitted signal emits S-wave vibration that slides up and down, and the receiving side also receives only the S-wave. Since a transducer is attached, only S waves can be felt in Figures 2 and 3.
A complete S-wave waveform as shown in the figure can be obtained.
Claims (1)
に圧着し数千米の深度の所からでも連続的にS波
のみを発受信して地上で記録出来る様にしたS波
検層装置。 This is an S-wave logging device that automatically affixes measuring equipment to the borehole wall in a borehole so that it can continuously transmit and receive only S-waves and record them on the ground even from a depth of several thousand meters.
Priority Applications (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
JP18845285U JPS6296587U (en) | 1985-12-09 | 1985-12-09 |
Applications Claiming Priority (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
JP18845285U JPS6296587U (en) | 1985-12-09 | 1985-12-09 |
Publications (1)
Publication Number | Publication Date |
---|---|
JPS6296587U true JPS6296587U (en) | 1987-06-19 |
Family
ID=31139831
Family Applications (1)
Application Number | Title | Priority Date | Filing Date |
---|---|---|---|
JP18845285U Pending JPS6296587U (en) | 1985-12-09 | 1985-12-09 |
Country Status (1)
Country | Link |
---|---|
JP (1) | JPS6296587U (en) |
-
1985
- 1985-12-09 JP JP18845285U patent/JPS6296587U/ja active Pending
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