JPS5852191B2 - P-wave/S-wave logging source - Google Patents
P-wave/S-wave logging sourceInfo
- Publication number
- JPS5852191B2 JPS5852191B2 JP54172279A JP17227979A JPS5852191B2 JP S5852191 B2 JPS5852191 B2 JP S5852191B2 JP 54172279 A JP54172279 A JP 54172279A JP 17227979 A JP17227979 A JP 17227979A JP S5852191 B2 JPS5852191 B2 JP S5852191B2
- Authority
- JP
- Japan
- Prior art keywords
- waves
- wave
- source
- rigid body
- hole
- 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.)
- Expired
Links
- 238000010586 diagram Methods 0.000 description 6
- XLYOFNOQVPJJNP-UHFFFAOYSA-N water Substances O XLYOFNOQVPJJNP-UHFFFAOYSA-N 0.000 description 6
- XEEYBQQBJWHFJM-UHFFFAOYSA-N Iron Chemical compound [Fe] XEEYBQQBJWHFJM-UHFFFAOYSA-N 0.000 description 4
- 238000000034 method Methods 0.000 description 4
- 230000000694 effects Effects 0.000 description 3
- 238000005259 measurement Methods 0.000 description 3
- 229910052742 iron Inorganic materials 0.000 description 2
- 239000002184 metal Substances 0.000 description 2
- 229910052751 metal Inorganic materials 0.000 description 2
- 239000003566 sealing material Substances 0.000 description 2
- 238000000926 separation method Methods 0.000 description 2
- 230000002457 bidirectional effect Effects 0.000 description 1
- 230000000903 blocking effect Effects 0.000 description 1
- 238000012790 confirmation Methods 0.000 description 1
- 238000007796 conventional method Methods 0.000 description 1
- 238000011156 evaluation Methods 0.000 description 1
- 238000003780 insertion Methods 0.000 description 1
- 230000037431 insertion Effects 0.000 description 1
- 239000000463 material Substances 0.000 description 1
- 230000002093 peripheral effect Effects 0.000 description 1
- 230000001902 propagating effect Effects 0.000 description 1
- 230000005855 radiation Effects 0.000 description 1
- 238000007789 sealing Methods 0.000 description 1
Landscapes
- Geophysics And Detection Of Objects (AREA)
Description
【発明の詳細な説明】
本発明は、孔内水を有する孔井内で使用するPS検層用
の根源に関し、更に詳しくは剛体と被衝突板との衝突を
利用して、該被衝突板を急速に運動させ、背向性の強い
力とともに孔内に圧縮力を発生させ、S波と同時にP波
を輻射させるようにしたP波・S波検層用の根源に関す
るものである。DETAILED DESCRIPTION OF THE INVENTION The present invention relates to a source for PS logging used in a well containing borehole water, and more specifically, the present invention relates to a source for PS logging used in a well containing borehole water. This relates to the source for P-wave/S-wave logging, which is made to move rapidly, generate compressive force in the hole along with a strong backward force, and radiate P-waves at the same time as S-waves.
PS検層は、孔丼中で地下の弾性波速度、すなわちP波
(縦波)速度とS波(横波)速度を直接測定し、その値
から地下の弾性的性質を調査する方法である。PS logging is a method of directly measuring underground elastic wave velocities, that is, P-wave (longitudinal wave) velocity and S-wave (transverse wave) velocity, in a hole bowl, and investigating the elastic properties of the underground from these values.
近年、地震工学や資源工学等の方面から、地下深部にお
ける高精度の弾性波のデータが要求されている。In recent years, highly accurate elastic wave data deep underground has been required from fields such as earthquake engineering and resource engineering.
これに対し、地下深部の弾性波を測定する装置は、P波
検層器だけが実用器として普及しているにすぎない。On the other hand, the P-wave logging device is the only device that has become widespread as a practical device for measuring elastic waves deep underground.
それは、P波が弾性波のうち最も速い速度で伝搬するた
めその確認が比較的平易なのに対して、S波は、それよ
り速く伝播する波(主としてP波)によって、その波形
がみだれやすく、確認が困難なためである。This is because P waves propagate at the fastest speed among elastic waves, so it is relatively easy to confirm, whereas S waves have a waveform that is easily distorted by waves that propagate faster (mainly P waves). This is because it is difficult.
これに対し、P波の輻射を抑制し、S波のみを効果的に
輻射させうるような方法が提案されている(特開昭54
−107401号公報参照)。In response to this, a method has been proposed that can suppress the radiation of P waves and effectively radiate only S waves (Japanese Patent Laid-Open No. 54
(Refer to Publication No.-107401).
これは、根源体内の運動機構を動作させることによって
孔軸と直交する一方向の根源力を孔内水を介して正負の
間接加圧として孔壁面に加え、それによってその根源力
と直交する方向に卓越した指向性をもつS波を輻射させ
るものである。This applies a source force in one direction perpendicular to the hole axis to the hole wall surface as positive and negative indirect pressure through the water in the hole by operating a motion mechanism within the source body, thereby applying a source force in a direction perpendicular to the source force. It radiates S-waves with excellent directivity.
確かにこの方法はP波の発生を抑え純粋なS波を輻射で
きるすぐれた方法である。This method is certainly an excellent method for suppressing the generation of P waves and radiating pure S waves.
しかし、実際に地下の弾性的性質を適確に調査するため
には、P波とS波を同時に観測することが必要である。However, in order to actually accurately investigate the elastic properties of the underground, it is necessary to observe P waves and S waves simultaneously.
すなわち、P波およびS波に基づく物理量を計測し、そ
れらを合成して別のファクター、例えばポアソン比を求
めていくような場合がそれである。That is, this is the case where physical quantities based on P waves and S waves are measured and then combined to obtain another factor, such as Poisson's ratio.
もし、S波のみを輻射する根源を用いるならば、一連の
ゾンデの別の位置にP波用の根源を別個設けるか、もし
くはS波の観測とは別に改めてP波用のゾンデを降ろし
て観測せねばならないことになる。If a source that radiates only S waves is used, a separate source for P waves should be installed at a different position in the series of sondes, or a sonde for P waves should be lowered and observed separately from the S wave observation. It will have to be done.
ところが、このような構成では同じ位置でP波とS波の
加振を行えるという保障は全くなく、特に深度が深いほ
ど同じ位置で加振することは困難となるし P波とS波
を別の根源で行うため、双方の観測量を合成して得た別
の物理量のデータとしての信頼性、誤差の評価等に問題
が残る。However, with such a configuration, there is no guarantee that P waves and S waves can be excited at the same location, and the deeper the depth, the more difficult it becomes to excite at the same location. Because this is done at the source of the data, there remain problems with reliability and error evaluation as data of separate physical quantities obtained by combining both observed quantities.
従って、同時にP波とS波を輻射でき、しかも発生する
P波とS波が振幅的にみて極端に差が生じないような、
すなわちP波の振幅が大きすぎてS波がかくれてしまわ
ないような、根源の開発が望まれている。Therefore, P waves and S waves can be radiated at the same time, and the generated P waves and S waves do not have an extreme difference in amplitude.
In other words, it is desired to develop a source that prevents the S waves from being hidden due to the amplitude of the P waves being too large.
本発明は、かかる従来技術の実情とそれに対する種々の
要望に鑑みてなされたものであって、その目的は、孔内
においてP波とS波を同時に発生させることができ、し
かも観測に際してP波とS波の分離がよく、両方の波の
確認も平易に行えるような根源を提供することである。The present invention has been made in view of the actual state of the prior art and various demands therefor, and its purpose is to be able to simultaneously generate P waves and S waves in a hole, and to generate P waves during observation. The objective is to provide a source that allows good separation of the and S waves and allows easy confirmation of both waves.
以下、図面に基づき本発明について詳述する。Hereinafter, the present invention will be explained in detail based on the drawings.
まず、本発明に係る根源の基本構成とその動作原理から
説明する。First, the basic configuration and operating principle of the present invention will be explained.
第1図に示すように、根源1は、孔内水2を有する孔井
3内において使用される。As shown in FIG. 1, the source 1 is used in a borehole 3 with borehole water 2. As shown in FIG.
根源1の内部には一方向に運動自在に設けた剛体4があ
り、この剛体4の端面と間隔をおいて対向する被衝突板
5が外方へ突出可能に設けられる。Inside the source 1 is a rigid body 4 that is movable in one direction, and a collision plate 5 that faces the end face of the rigid body 4 at a distance is provided so as to be able to protrude outward.
なお、根源1の内部はゴムシール6にまり液密的となっ
ている。Note that the inside of the source 1 is surrounded by a rubber seal 6 and is liquid-tight.
さて、このような構造において、剛体4をX方向に運動
させ、被衝突板5に衝突させる。Now, in such a structure, the rigid body 4 is moved in the X direction and is caused to collide with the collided plate 5.
すると、この衝突により被衝突板5はX方向に衝撃的に
運動し、孔内水2を介してX方向の孔壁にのみ力を及ぼ
すと同時に孔内では被衝突板5が移動した分だけ圧力が
上昇する。Then, due to this collision, the impacted plate 5 moves impulsively in the X direction, exerting force only on the hole wall in the X direction via the hole water 2, and at the same time, within the hole, a force is generated by the amount of movement of the impacted plate 5. Pressure increases.
そのため、孔径に比して大きな距離にある孔軸方向の観
測点では、X方向の力によって起振されたS波のみなら
ず、衝撃的な圧力変化によって生じたP波も観測するこ
とができるのである。Therefore, at observation points in the hole axis direction that are located at a large distance compared to the hole diameter, it is possible to observe not only S waves caused by forces in the X direction, but also P waves caused by impulsive pressure changes. It is.
このような構成とすると、第1に、衝突を利用している
ために、発生する力は単純なパルス様となり、記録紙上
P波とS波の分離を良くすることができ、第2に衝突の
向きを逆にすればS波のみが反転し、S波の確認を平易
にできる等の効果が期待される。With this configuration, firstly, since the collision is used, the generated force becomes a simple pulse-like force, which improves the separation of the P wave and S wave on the recording paper, and secondly, the collision If the direction is reversed, only the S waves will be reversed, which is expected to have the effect of making it easier to confirm the S waves.
根源1内の剛体4は、通常、第2図に示すように、電磁
力によって駆動される。The rigid body 4 within the source 1 is typically driven by electromagnetic forces, as shown in FIG.
すなわち、ハウジング側にはコイル10a、10bを収
容した磁性ヨーク11が取付けられ、剛体4は筒状の磁
性プランジャ12とその両端に取付けられている衝突体
13a、13bからなる。That is, a magnetic yoke 11 containing coils 10a and 10b is attached to the housing side, and the rigid body 4 consists of a cylindrical magnetic plunger 12 and collision bodies 13a and 13b attached to both ends thereof.
コイル10a。10bは、いわゆる双方向ソレノイドを
形成しており、スイッチ14で電流を流すコイルを選択
することにより、剛体4をX方向あるいは逆の−X方尚
のどちらにでも駆動することができる。Coil 10a. 10b forms a so-called bidirectional solenoid, and by selecting the coil through which current flows with the switch 14, the rigid body 4 can be driven in either the X direction or the opposite -X direction.
根源1の詳細を第3図および第4図に示す。Details of source 1 are shown in FIGS. 3 and 4.
円柱状のハウジング20には、その中心軸に直角な方向
に貫通孔が設けられ、該貫通孔の内部に剛体4等が収容
される。The cylindrical housing 20 is provided with a through hole in a direction perpendicular to its central axis, and the rigid body 4 and the like are housed inside the through hole.
貫通孔の内周壁には純鉄製のヨーク11. a 、 1
l bとそれに組込まれたコイル10a、10bが位
置する。A pure iron yoke 11 is attached to the inner peripheral wall of the through hole. a, 1
lb and the coils 10a and 10b incorporated therein are located.
純鉄製のプランジャ12と衝突体13a 、13bとか
らなる剛体4は、スパイラル状板バネ21a、21bに
よって該貫通孔の中心軸に沿って非接触的に移動可能に
支持される。A rigid body 4 consisting of a pure iron plunger 12 and collision bodies 13a and 13b is supported by spiral leaf springs 21a and 21b so as to be movable in a non-contact manner along the central axis of the through hole.
スパイラル状の板バネ21a。21bは、CIJソング
2,23によって止着される。A spiral leaf spring 21a. 21b is fixed by CIJ songs 2 and 23.
また、剛体4の両端と間隔をおいて対向するように被衝
突板5a、5bが位置し、それらの外側はゴム製の防水
用シール材6a、6bで覆われ、それらは固定金具24
、押え金具25、及びネジ26によってハウジング20
に固定される。In addition, collision plates 5a and 5b are positioned so as to face both ends of the rigid body 4 with a space therebetween, and their outsides are covered with rubber waterproof sealing materials 6a and 6b.
, the presser fitting 25 and the screw 26 fix the housing 20.
Fixed.
なお符号27は0リングシールである。Note that the reference numeral 27 is an O-ring seal.
被衝突板5a。5bの内端部は固定金属24に当接して
いるため、外方へのみ突出可能で、内方への変位は生じ
ない。Collision plate 5a. Since the inner end portion of 5b is in contact with the fixed metal 24, it can only protrude outward and will not be displaced inward.
またゴム製の防水シール材6a 、5bで覆われている
ため、被衝突板5a 、sbが剛体4との衝突によって
外方へ突出してもハウジング20の内部に孔内水が浸入
することはない。In addition, since it is covered with rubber waterproof sealing materials 6a and 5b, even if the collided plates 5a and sb protrude outward due to a collision with the rigid body 4, water in the hole will not infiltrate into the inside of the housing 20. .
このような根源は、受信器等とともに一連のゾンデとし
て孔井内に挿入される。Such sources are inserted into the borehole as a series of sondes along with receivers and the like.
実際にP波、S波検層に応用した例を第5図に示す。Figure 5 shows an example of actual application to P-wave and S-wave logging.
下から、ゾンデ29の挿入を容易にするための重り30
、それぞれP波用の上下動受振素子とS波相の水平動受
振素子が組込まれている2個の漂遊型受振器31.32
、S波の受振を防害する孔中音波を遮断するためのフィ
ルタチューブ33、プリアンプ34、ゾンデ本体を伝播
する防害波を防ぐためのダンパ35、本発明に係る根源
36、該根源36を駆動させる根源ドライバ37がこの
順序で連続しており、シーブ39を介してウィンチ40
で孔井3内の所定位置まで上げ下ろしされる。From below, a weight 30 for facilitating the insertion of the sonde 29
, two stray type geophones 31 and 32 each incorporating a vertical motion receiving element for P waves and a horizontal motion receiving element for S wave phase.
, a filter tube 33 for blocking in-hole sound waves that prevent the reception of S waves, a preamplifier 34, a damper 35 for preventing damage waves propagating through the sonde body, a source 36 according to the present invention, and driving the source 36. The source drivers 37 are successive in this order, and the winch 40 is connected via the sheave 39.
It is raised and lowered to a predetermined position within the well 3.
地表には、フィルタチューブ33にガスを供給するため
のガスシリンダ41.及び制御装置42や記録装置(例
えば電磁オシログラフ)43が配置される。On the ground surface, there is a gas cylinder 41. for supplying gas to the filter tube 33. A control device 42 and a recording device (for example, an electromagnetic oscilloscope) 43 are arranged.
測定系のブロック図を第6図に示す。A block diagram of the measurement system is shown in Figure 6.
測定系制御回路50で起振方向NもしくはRおよび入力
切換51,52,53をコントロールする。A measurement system control circuit 50 controls the vibration direction N or R and input switches 51, 52, and 53.
直流高電圧源54からは根源ドライバ3Tへ電力が供給
される。Power is supplied from the DC high voltage source 54 to the source driver 3T.
トリガパルス源55によって根源ドライバ37にトリガ
パルスが印加され、剛体4を予め定められたNもしくは
R方向に駆動し、被衝突板5に衝突させ、S波とP波を
輻射させると共に、前記トリガパルスで6チヤンネル波
形記憶装置56をスタートさせる。A trigger pulse is applied to the root driver 37 by the trigger pulse source 55 to drive the rigid body 4 in a predetermined N or R direction to collide with the colliding plate 5 and radiate S waves and P waves. Start the six channel waveform storage device 56 with a pulse.
輻射されたS波及びP波は、漂遊型受振器31,32で
検知され、プリアンプで増幅させてから地表の6チヤン
ネル波形記憶装置56に送られ、8チヤンネル電磁オシ
ログラフ43で記録紙にタイムマークと共に記録が取ら
れる。The radiated S waves and P waves are detected by stray geophones 31 and 32, amplified by a preamplifier, and sent to a 6-channel waveform storage device 56 on the ground surface.The radiated S-waves and P-waves are recorded on recording paper by an 8-channel electromagnetic oscilloscope 43. A record is taken along with the mark.
その一例を第7図に示す。P波とS波がほぼ同程度の振
幅で記録されている。An example is shown in FIG. P waves and S waves are recorded with approximately the same amplitude.
S波の確認は、起振方向を変えること(NとR)によっ
て波形が反転していることから確実に行える。The S wave can be reliably confirmed by changing the direction of vibration (N and R) since the waveform is reversed.
これらのデータからP波・S波の速度分布等の解析を行
うのは、従来同様の手法による。Analyzing the velocity distribution of P waves and S waves from these data is performed using the same conventional method.
本発明の装置の効果をより一層高めるためには、前記の
ように被衝突板5は内方には変位しないようなストッパ
の役割を果す部材に当接するように配置するとともに、
該被衝突板5は金属のような剛性材料製とし、また、被
衝突板5とハウジングとを液密的にするシール部材は、
剛体4と被衝突板5との衝突に影響を及ぼさない程度に
弱いバネ定数をもった部材で作るのが良い。In order to further enhance the effect of the device of the present invention, as described above, the collision plate 5 is arranged so as to come into contact with a member that serves as a stopper so as not to be displaced inwardly, and
The colliding plate 5 is made of a rigid material such as metal, and the sealing member that makes the colliding plate 5 and the housing liquid-tight is:
It is preferable to use a member having a spring constant that is weak enough not to affect the collision between the rigid body 4 and the colliding plate 5.
本発明は上記のように構成されているから、同じ位置で
P波とS波を輻射でき、双方の観測値を組合せて得た別
の物理量のデータとしての信頼性が高く指向性を持った
力によって発生するS波と全体として圧縮の力によって
発生するP波は共に孔軸上にその振幅の指向性のピーク
を持っており、それ故、根源と受振器を一体のゾンデに
組み入れた本格的検層器として非常に有利であるし、衝
突の方向を逆にすればS波の波形は反転するがP波は反
転せず、S波の確認を容易に行えるうえ、衝突を利用し
ているから、発生する力は時間的にみれば波形がパルス
様となり、シンプルでかつパルス幅は狭く、そのため記
録紙上、P波とS波の分離が良く、また小型のわりには
強力な力を発生させることができる等、従来技術にはな
いすぐれた効果を奏しうるものである。Since the present invention is configured as described above, P waves and S waves can be radiated at the same position, and the observed values of both can be combined to provide highly reliable and directional data of another physical quantity. Both the S wave generated by the force and the P wave generated by the compressive force as a whole have their amplitude directivity peaks on the hole axis, and therefore a full-scale sonde incorporating the source and the geophone into a single sonde. It is very advantageous as a well-logging device, and if the direction of the collision is reversed, the waveform of the S wave will be reversed, but the waveform of the P wave will not be reversed, making it easy to confirm the S wave. Therefore, the generated force has a pulse-like waveform in terms of time, and the pulse width is simple and narrow, so the P wave and S wave can be separated well on recording paper, and it generates a strong force despite its small size. It is possible to achieve superior effects that are not available in the prior art.
第1図は本発明の動作原理を示す説明図、第2図は根源
内部の剛体の1駆動原理を示す説明図、第3図は根源の
一実施例の断面図、第4図はその二部破断斜視図、第5
図は使用状態の説明図、第6図は測定系のブロック図、
第7図は得られた波形記録の一例を示す図である。
1・・・・・・根源、3・・・・・・孔井、4・・・・
・・剛体、5・・・・・・被衝突板。Fig. 1 is an explanatory diagram showing the operating principle of the present invention, Fig. 2 is an explanatory diagram showing one driving principle of the rigid body inside the root, Fig. 3 is a sectional view of one embodiment of the root, and Fig. 4 is the second example. Partially broken perspective view, No. 5
The figure is an explanatory diagram of the usage state, Figure 6 is a block diagram of the measurement system,
FIG. 7 is a diagram showing an example of the obtained waveform recording. 1... Root, 3... Koi, 4...
... Rigid body, 5 ... Collided plate.
Claims (1)
の中央に、該根源刃軸に沿って運動自在に設けた可動剛
体と、振動力軸の両端位置にて該剛体の端面と間隔をお
いて対向し、外方に突出可能に設けた被衝突板とを備え
、前記剛体の駆動により被衝突板に衝突可能としたこと
を特徴とするP波・S波検層用根源。1. A movable rigid body provided at the center of the root blade axis perpendicular to the central axis direction of the logging sonde so as to be movable along the root blade axis, and a space between the end faces of the rigid body at both ends of the vibration force axis. A source for P-wave/S-wave logging, characterized in that it is provided with a plate to be collided and provided so as to be able to protrude outward, facing each other at a distance, and to be able to collide with the plate to be collided by driving the rigid body.
Priority Applications (2)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP54172279A JPS5852191B2 (en) | 1979-12-29 | 1979-12-29 | P-wave/S-wave logging source |
| US06/215,929 US4383591A (en) | 1979-12-29 | 1980-12-12 | Apparatus for generating P waves and S waves |
Applications Claiming Priority (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP54172279A JPS5852191B2 (en) | 1979-12-29 | 1979-12-29 | P-wave/S-wave logging source |
Publications (2)
| Publication Number | Publication Date |
|---|---|
| JPS5697892A JPS5697892A (en) | 1981-08-06 |
| JPS5852191B2 true JPS5852191B2 (en) | 1983-11-21 |
Family
ID=15938964
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| JP54172279A Expired JPS5852191B2 (en) | 1979-12-29 | 1979-12-29 | P-wave/S-wave logging source |
Country Status (1)
| Country | Link |
|---|---|
| JP (1) | JPS5852191B2 (en) |
Families Citing this family (3)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| JPS58171689A (en) * | 1982-04-01 | 1983-10-08 | Oyo Chishitsu Kk | Oscillation source of logging for s-wave |
| US4805727A (en) * | 1982-10-28 | 1989-02-21 | The United States Of America As Represented By The United States Department Of Energy | Down hole periodic seismic generator |
| JPH01201187A (en) * | 1988-02-05 | 1989-08-14 | Dia Consultant:Kk | Elastic wave generator |
-
1979
- 1979-12-29 JP JP54172279A patent/JPS5852191B2/en not_active Expired
Also Published As
| Publication number | Publication date |
|---|---|
| JPS5697892A (en) | 1981-08-06 |
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