JPS60249080A - Method and device for geological analysis by aerial measurement of gamma rays - Google Patents

Method and device for geological analysis by aerial measurement of gamma rays

Info

Publication number
JPS60249080A
JPS60249080A JP59104659A JP10465984A JPS60249080A JP S60249080 A JPS60249080 A JP S60249080A JP 59104659 A JP59104659 A JP 59104659A JP 10465984 A JP10465984 A JP 10465984A JP S60249080 A JPS60249080 A JP S60249080A
Authority
JP
Japan
Prior art keywords
changes
ground surface
gamma rays
daughter element
altitude
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.)
Granted
Application number
JP59104659A
Other languages
Japanese (ja)
Other versions
JPH0369077B2 (en
Inventor
Harumi Araki
春視 荒木
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
Aero Asahi Corp
Original Assignee
Aero Asahi Corp
Priority date (The priority date 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 date listed.)
Filing date
Publication date
Application filed by Aero Asahi Corp filed Critical Aero Asahi Corp
Priority to JP59104659A priority Critical patent/JPS60249080A/en
Publication of JPS60249080A publication Critical patent/JPS60249080A/en
Publication of JPH0369077B2 publication Critical patent/JPH0369077B2/ja
Granted legal-status Critical Current

Links

Abstract

PURPOSE:To detect automatically a dislocation, crack and hot water vein by detecting the gamma rays of different energy bands from the object land by the gamma ray detecting members mounted on an aerial flying body and measuring at the same time the change in the altitude from the ground surface and the temp. of the ground surface as well as the change of the dose ratio with each energy band. CONSTITUTION:The outputs from the environmental gamma ray detector 10, gamma ray detector 12 for <40>K system, gamma ray detector 14 for <238>U system and gamma ray detector 16 for <232>Th mounted on the flying body are respectively converted to logarithm by logarithm circuits 18, 20, 22, 24. The outputs from the circuits 18, 20, 24 are fed to subtractor circuits 26, 28, 30, by which the dose ratios K/U, K/Th and U/Th of the respective gamma rays are determined and are fed together with the output from the circuit 18 and the outputs from a radio altimeter 32, a pressure altimeter 34, a speedometer 36 and a radiation thermometer 38 to an arithmetic circuit 40. The circuit 40 determines the presence of the dislocation, crack and hot water vein from the input data, actuates an alarm member 42 if necessary and records the input data into a recorder 44.

Description

【発明の詳細な説明】 [産業上の利用分野] 本発明は、ガンマ線の空中測定による地質解析法及びそ
の装置に関する。
DETAILED DESCRIPTION OF THE INVENTION [Field of Industrial Application] The present invention relates to a geological analysis method and apparatus using gamma ray aerial measurement.

[従来技術] 断層・亀裂・温水脈に関する探査には、従来、放射能探
査、弾性波探査、電気探査といった方法が使われてきた
が、特殊な技術・熟練を必要とするだけでなく、技術体
系の未確立、或いは探査解析の期間と経済効率の点で充
分に実用性のある方法ではなかった。
[Prior art] Methods such as radioactivity exploration, elastic wave exploration, and electrical exploration have traditionally been used to explore faults, cracks, and warm water veins, but these methods not only require special techniques and skills, but also require Either the system had not been established or the method was not sufficiently practical in terms of exploration and analysis period and economic efficiency.

[発明が解決しようどする問題点] 本発明は、特別な知識・技術を必要とせずに、断層・亀
裂・温水脈の存在する可能性のある場所を自動的に検索
できる探査方法及び装置を提案することを目的とする。
[Problems to be solved by the invention] The present invention provides an exploration method and device that can automatically search for locations where faults, cracks, and warm water veins may exist without requiring special knowledge or technology. The purpose is to make suggestions.

E問題点を解決するための手段] 本発明に係る地質解析法及び装置は、空中でガンマ線検
出器を移動させながら、環境ガンマ線の0に系列ガンマ
線及び))PU系系列ガン綿線232Th系列ガンマ線
のカント数をめ、同時に81測された地表面高度及び地
表面温度、対地速度並びに時刻から、地表面における地
形傾斜変換線、谷底部及び稜線部を自動的に抽出し、そ
の位置での環境ガンマ線のカント数、ラドン娘元素”’
B i とカリウム90にのカント数比xlQBr /
″″K、トロン娘元素2o? T yと力IJ +クム
″’にのカント数比″”T 12 / ’。
Means for Solving Problem E] The geological analysis method and device according to the present invention detect environmental gamma rays, 0-series gamma rays and)) PU-based gun cotton wire 232Th-series gamma rays while moving a gamma ray detector in the air. From the ground surface altitude, ground surface temperature, ground speed, and time measured simultaneously, the topographic slope conversion lines, valley bottoms, and ridges on the ground surface are automatically extracted, and the environment at that location is calculated. Cant number of gamma rays, radon daughter element"'
Cant number ratio between B i and potassium 90 xlQBr /
″″K, Tron Musume Element 2o? The Kant number ratio of T y and force IJ + cum'' is T 12 / '.

K及びトロン娘元素とラドン娘元素のカント数比”’T
9./ 3i、並びに地表面温度変化率等を計算したう
えで、断層・亀裂及びに地熱の有無と規模、並びに表面
水の有無を判断し、断層・亀裂・地下水脈・温泉脈を探
査することを特徴とする。
Cant number ratio of K and thoron daughter element and radon daughter element "'T
9. / 3i and the rate of change in ground surface temperature, etc., to determine the presence and scale of geothermal heat in faults, cracks, and the presence or absence of surface water, and to explore faults, cracks, underground water veins, and hot spring veins. Features.

[発明の原理] 本発明者は、断層・亀裂のある場所で地下水の供給され
る可能性のあるときは地下水脈が存在する可能性があり
、加えて地熱のある所には温泉脈の存在する可能性があ
り、断層・亀裂の存在と表流水・伏流水の存在、それに
地熱の存否の可能性が、空中ガンマ線と地表面温僚、地
表面高度、対地速度及び飛行時間等から探知できること
を発見した。
[Principle of the Invention] The present inventor believes that if there is a possibility of underground water supply in a place where there is a fault or crack, there is a possibility that a groundwater vein exists, and in addition, a hot spring vein exists in a place where there is geothermal heat. The existence of faults and cracks, the existence of surface water and underground water, and the possibility of the presence or absence of geothermal heat can be detected from airborne gamma rays, ground surface heating, ground surface altitude, ground speed, flight time, etc. discovered.

岩石中にある放射性元素のウラン222U、トリウム2
317 h、カリウムIa Kは、放射線を放出して安
定元素へと壊変していく途中で、ウランからラドン””
Rn、t−IJウムから2ao T nといったガス状
元素を経るが、この時期に地温が高いほどラドンガス及
びトロンガスの圧力は高まり、亀裂に沿ってガスの移動
が生じる。ところが、ラドンの半減期は、3,825日
であるのに対しトロンの半減期は54.5秒であり、相
互に大きな差があるので、移動により元素間の比率が変
わる。従って、地中に亀裂があれば、放射性元素の分離
が進行し、′に系列のガンマ線量に対する U系列のガ
ンマ線比及び21” T h系列のガンマ線比が相対的
に増加し、また地熱の高い地区はど”’T h系列のガ
ンマ線量の2ゝ2U系列のガンマ線量に対重る比率が相
対的に低くなる。断層や亀裂等は一般に地形傾斜変換線
、谷底部及び稜線部で地表に露出するが、これらの地域
において、2′に系列/ U系列のガンマ線量比及び’
に系列/””Th系列のガンマ線量比が相対的に低くな
っているときには断層、亀裂、地下水脈の存在を予測さ
せ、 U系列/ Th系列のガンマ線量比が相対的に高
くなっているときには地熱の高温部の存在を予想させ、
′に系列/ U系列のガンマ線量比が相対的に低く且つ
132U系列/232T h系列のガンマ線量比が相対
的に高いときは、温泉脈の存在を予想させる。本発明は
、こうした1ネルギー帯の異なるガンマ線の線量比が相
対的に異常な変化を示す地形傾斜変換線、谷底部又は稜
線部から断層・亀裂・温水脈を探し出すことを特徴とづ
る。
Radioactive elements uranium-222U and thorium-2 found in rocks
317 h, Potassium Ia K is in the process of emitting radiation and decaying into a stable element, changing from uranium to radon.
Gaseous elements such as Rn, t-IJum and 2aoTn are passed through, but the higher the ground temperature is during this period, the higher the pressure of radon gas and thoron gas, causing gas movement along the cracks. However, the half-life of radon is 3,825 days, while that of thoron is 54.5 seconds, and there is a large difference between them, so the ratio between the elements changes due to movement. Therefore, if there is a crack in the ground, the separation of radioactive elements progresses, and the gamma ray ratio of the U series and the gamma ray ratio of the 21" Th series relative to the gamma ray dose of the ' series increases. The ratio of the gamma radiation dose of the H series to the gamma dose of the 2ゝ2U series is relatively low in the area. Faults, cracks, etc. are generally exposed on the ground at topographical slope conversion lines, valley bottoms, and ridgelines, but in these areas, the gamma dose ratio of the 2' series/U series and '
The presence of faults, cracks, and underground water veins is predicted when the gamma dose ratio of the series/Th series is relatively low, and when the gamma dose ratio of the U series/Th series is relatively high. Predicting the existence of geothermal high temperature areas,
When the gamma ray dose ratio of the ' series/U series is relatively low and the gamma dose ratio of the 132U series/232Th series is relatively high, the presence of hot spring veins is predicted. The present invention is characterized by searching for faults, fissures, and warm water veins from topographic slope conversion lines, valley bottoms, or ridgelines where the dose ratios of different gamma rays in one energy band exhibit relatively abnormal changes.

本発明の発明者にJ、る日本各地の既知の断層・亀裂・
温水脈の上空での各核種のエネルギー領域のガンマ線、
飛行高度、対地高度、地表面温度、対地速度及び飛行時
間等の測定の結果、飛行高度から対地高度を差引いた地
表面高度の時間差高を対地速度と飛行時間との楢で除し
てめた地形傾斜(tanθ)の変化率、及び地表面温度
の時間差値を対地速度と飛行時間との積で除した温度変
化率を使用して、断層・亀裂の外観上からの可能な場所
及び表流水・伏流水の有無の可能性を知ることのできる
ことが発見されている。即ち、断層や亀裂は、地形傾斜
の変化率の大きな所で存在する可能性が高く、また、表
流水・伏流水の存在する所では、地表面温度が周囲に比
べ数度異なる。本発明は、この地形データから抽出され
た、可能性としての断層・亀裂の存在が内部的な要因か
らも支持されるものであるか否かを判定する手段たりう
るちのであり、具体的には、ガンマ線のラドン娘元素を
カリウムとのカント数比 Bi/にで比較して1lJi
層付近ではこの比が通常2倍以上になっていること、表
流水・伏流水の存在〜により地表面温度が周辺より数度
以上変化すること、地熱地帯ではトロン娘元素とラドン
娘元素のカント数比”’t” 1! /”5’B iが
低下し、通常地帯の80%以下になっていること、とい
う基準に基づき判断する。
Known faults, cracks, and
Gamma rays in the energy range of each nuclide above the warm water vein,
As a result of measuring flight altitude, altitude above ground, surface temperature, ground speed, flight time, etc., the time difference height of ground surface altitude, which is obtained by subtracting altitude above ground from flight altitude, was calculated by dividing the difference between ground speed and flight time. Using the rate of change in the topographical slope (tanθ) and the rate of temperature change obtained by dividing the time difference value of the ground surface temperature by the product of ground speed and flight time, possible locations of faults and cracks from the appearance and surface water can be determined.・It has been discovered that it is possible to know the possibility of the presence or absence of underground water. In other words, faults and cracks are likely to exist in places where the rate of change in topographical slope is large, and in places where surface water or underground water exists, the ground surface temperature differs by several degrees compared to the surrounding area. The present invention provides a means for determining whether or not the possible existence of faults/cracks extracted from this topographical data is also supported by internal factors. is 1lJi by comparing the cant number ratio Bi/of the radon daughter element of gamma rays with potassium.
This ratio is usually more than double near the layer, the surface temperature changes by several degrees or more from the surrounding area due to the presence of surface water and underground water, and in geothermal areas, the cant of thoron daughter elements and radon daughter elements Number ratio "'t" 1! Judgment is made based on the criterion that 5'B i has decreased to 80% or less of the normal zone.

[実施例の説明] 第1図は、本発明を実施するためにヘリコプタに積載づ
る装置の概略ブロック図を示す。10は、環境ガンマ線
用のシンチレータ及び波高分析器からなる検出器であり
、12は、’に系列ガンマ線用の検出器、14は233
U系列用ガン7線の検出器、16は2uT 6系列用ガ
ンマ線の検出器である。各検出器10乃至16の出力は
それぞれ、対数化回路18乃至24によって対数化され
る。対数化回路20の出力と対数化回路22の出力は、
減算回路26で減算される。
DESCRIPTION OF THE EMBODIMENTS FIG. 1 shows a schematic block diagram of equipment mounted on a helicopter to carry out the invention. 10 is a detector consisting of a scintillator and a pulse height analyzer for environmental gamma rays, 12 is a detector for series gamma rays, and 14 is 233
16 is a gamma ray detector for the 2uT 6 series. The output of each detector 10-16 is logarithmized by a logarithmization circuit 18-24, respectively. The output of the logarithmization circuit 20 and the output of the logarithmization circuit 22 are
The subtraction circuit 26 performs subtraction.

減算回路26の出力は、 K系列のガンマ線量と(J系
列のガンマ線量の比を示す。同様に、減算回路28は、
対数化回路20の出力と対数化回路24の出力との差を
計算し、減算回路30は、対数化回路22の出力と対数
化回路24の出力の差を計算する。その他に、電波高度
計32、気圧高度計34、速度計36及び放射温度計3
8を積載する。これらからのデータは、前述の地形傾斜
の変化率及び温度変化率を計算するために利用される。
The output of the subtraction circuit 26 indicates the ratio of the K-series gamma ray dose to the J-series gamma ray dose.Similarly, the subtraction circuit 28
The difference between the output of the logarithmization circuit 20 and the output of the logarithmization circuit 24 is calculated, and the subtraction circuit 30 calculates the difference between the output of the logarithmization circuit 22 and the output of the logarithmization circuit 24. In addition, a radio altimeter 32, a barometric altimeter 34, a speedometer 36, and a radiation thermometer 3
Load 8. Data from these are utilized to calculate the rate of change of terrain slope and rate of temperature change described above.

環境ガンマ線用の検出器10は、対象物及びバックグラ
ウンドの影響を監視するために用いる。
Detector 10 for environmental gamma rays is used to monitor object and background effects.

対数化回路18の出力、減算回路26.28.30の出
力及び装置32.34.36.38の出力は、演算回路
40に供給される。演算回路40は、前述の各判断要素
について対応条件を満たすか否かを演算し、必要なとき
に出力を出して、R報部材42を作動させる。
The output of the logarithmization circuit 18, the output of the subtraction circuit 26, 28, 30 and the output of the device 32, 34, 36, 38 are fed to an arithmetic circuit 40. The arithmetic circuit 40 calculates whether or not the corresponding conditions are satisfied for each of the above-mentioned judgment elements, outputs an output when necessary, and operates the R-reporting member 42.

警報部材42は、光又は音により閉測者に例えば温泉脈
の発見を知らせる。また、これら装置18,26乃至3
8の出力は、地上での精密な解析のために、データ・レ
コーダ44に記録しておく。
The alarm member 42 notifies the surveyor of the discovery of a hot spring vein, for example, by means of light or sound. In addition, these devices 18, 26 to 3
The output of 8 is recorded in a data recorder 44 for precise analysis on the ground.

該当地域d後に確認し易くづるために、このjJンマ線
計測と同期して、ガンマ線探査地域の可視光映像及び熱
赤外線映像をビデオ・テープ・レコーダに同期記録して
おくのが好ましい。
In order to easily confirm the gamma ray survey after the corresponding area d, it is preferable to record visible light images and thermal infrared ray images of the gamma ray exploration area on a video tape recorder in synchronization with this jJ gamma ray measurement.

第1図には図示しなかつICが、この解析装置には、各
ガンマ線検出器10〜16及び演算回路40等を同期し
て動作させ、また、データのサンプリング時間及び周期
を決定するクロック回路が設けられている。
Although not shown in FIG. 1, this analysis device includes a clock circuit that operates the gamma ray detectors 10 to 16, the arithmetic circuit 40, etc. in synchronization, and determines the data sampling time and period. It is provided.

第2図は、温泉脈についての計測データをグラフ化した
ものである。横軸は飛行時間又は飛行距離を示す。グラ
フの上部は、飛行高度(1、対地高度△h及び地表面高
度112.△11を通常の縦軸目盛で示し、下部は、環
境ガンマ線(chi)、 K系列ガンマ線(ch2)、
 U系列ガンマ線(ch3)及びx!2Th系列ガンマ
線(ch4)を縦軸対数目盛で示す。上向きの矢印で示
した部分は、谷の部分であり、且つ232U系列と)3
2−r−h系列のガンマ線□□□比が著しく大ぎくなっ
ていることから、温泉脈の存在を示唆している。
Figure 2 is a graph of measurement data regarding hot spring veins. The horizontal axis indicates flight time or flight distance. The upper part of the graph shows flight altitude (1, ground altitude △h and ground surface altitude 112. △11) on the normal vertical axis scale, and the lower part shows environmental gamma rays (chi), K series gamma rays (ch2),
U-series gamma rays (ch3) and x! 2Th series gamma rays (ch4) are shown on a logarithmic scale on the vertical axis. The part indicated by the upward arrow is the valley part, and is the 232U series) 3
The significantly large ratio of gamma rays in the 2-rh series suggests the existence of hot spring veins.

演算回路40どしては、具体的には、小型で安価なパー
ソナルコンピュータを用いることができ、従って、各装
置からのデータの各サンプリング値最大値、最小値及び
平均値等を適宜記録させるようにプログラム・ソフトウ
ェアを組むことで、容易に、各エネルギー帯のガンマ線
量の変化を発見することができる。即ち、この実施例の
演算回路40は、地形傾斜(tanθ)が2倍を越えて
変化し、ラドン娘元素とカリウムのカント数比”’Bi
/”Kが2倍以上に変化するとき、断層・亀裂の存在す
る可能性が高いことを指示づる。地形傾斜が2倍以−上
となり、傾斜の正負が変わり、ラドン娘元素と力1戸ン
11のカン1へ数比2″Bi/″′Kが2イ8以上変化
し、さらに地表面濡瓜が数℃以上変化する場合には、ト
ロン娘元素とラドン娘元素のカント数比”’T 11.
 / ”’B +が減少するとき、温泉脈の存在する可
能性が高いことを指示し、反対に Tel 21″B 
Hが増加するとき地下水脈の存在する可能性が高いこと
を指示する。これらの顕著な状況では、演算回路40は
、警報部材42に一アラーム信号を出力覆る。XYプロ
ッタやCRTを用いる場合には、所定のアラーム信号を
プロッタ紙上又はCRT上に出力づる。
Specifically, a small and inexpensive personal computer can be used as the arithmetic circuit 40, and therefore, the maximum value, minimum value, average value, etc. of each sampling value of data from each device can be recorded as appropriate. By incorporating programming and software into the system, changes in gamma ray doses in each energy band can be easily discovered. That is, the arithmetic circuit 40 of this embodiment is configured such that the topographical slope (tan θ) changes by more than twice and the cant number ratio of radon daughter element and potassium “'Bi
/"When K changes by more than twice, it indicates that there is a high possibility of the existence of faults and fissures.The topographical slope becomes more than twice as much, the sign of the slope changes, and the radon daughter element and the force increase. If the number ratio 2''Bi/'''K changes by more than 2i8 and the ground surface wetness changes by more than a few degrees Celsius, the Kant number ratio of the thoron daughter element and the radon daughter element changes. 'T 11.
/ ``'B When + decreases, it indicates that there is a high possibility of the existence of hot spring veins, and on the contrary, Tel 21''B
When H increases, it indicates that there is a high possibility that a groundwater vein exists. In these significant situations, the arithmetic circuit 40 outputs an alarm signal to the alarm member 42. When using an XY plotter or CRT, a predetermined alarm signal is output on the plotter paper or CRT.

データ収集に際しては、通常1秒毎に飛行高度、対地高
度、及び対地速度がデータレコーダに入力されているの
で、飛行距離と地表面高度との関係がわかり、結果とし
て地形断面がデータレコーダに入力されることどなる。
When collecting data, the flight altitude, ground altitude, and ground speed are usually input into the data recorder every second, so the relationship between the flight distance and the ground surface altitude can be determined, and as a result, the terrain cross section is input into the data recorder. I yelled that it was done to me.

と同時に放射温度計38により地表面温度もデータレコ
ーダに入力されているので、土地利用の変化に対応して
地表面温度が変化づる様子も把握できる。地2表面で水
分の多い場所や表流水・伏流水のある谷底部では、周辺
とは数度稈異なる温度(冬では高く、夏では低くなる)
となるのて゛、このデータを地形断面のデータと連動さ
せれば、地下水・温泉水の函養源となる水の存在を、飛
行速度が毎時90kmの場合的25mの間隔で探知しう
ることになる。
At the same time, since the ground surface temperature is also input to the data recorder by the radiation thermometer 38, it is possible to grasp how the ground surface temperature changes in response to changes in land use. In places with a lot of moisture on the earth's surface, and in valley bottoms with surface water and underground water, the temperature differs by several degrees from the surrounding area (higher in winter and lower in summer)
Therefore, if this data is linked with topographical cross-section data, it will be possible to detect the presence of water that serves as a storage source for groundwater and hot spring water at intervals of 25 m, assuming a flight speed of 90 km/h. .

また本発明では、各核種に対応させた空中ガンマ線のカ
ント数を通常5秒間計測しており、毎時90kn+で飛
行するとき地表面を125mの間隔でその間の空中ガン
マ線を測定しCいることになり、通常は飛行高度を対地
高度100mにとっているので、地上の直径500wの
範囲から放出される放剣線の90%を計測している。
In addition, in the present invention, the cant number of airborne gamma rays corresponding to each nuclide is normally measured for 5 seconds, and when flying at 90kn+ per hour, airborne gamma rays are measured at intervals of 125m above the ground surface. Since the flight altitude is normally 100m above the ground, 90% of the radiation emitted from a 500W diameter area on the ground is measured.

なお、本探査装置ではデータ収集時間を0.5秒にまで
短縮でき、5秒間の累積和を0.5秒間にとることによ
って地上解像度を毎時90kmで飛行する場合に12.
5mまで上げることができる。
In addition, with this exploration device, the data collection time can be shortened to 0.5 seconds, and by taking the cumulative sum of 5 seconds to 0.5 seconds, the ground resolution can be reduced to 12.5 seconds when flying at 90 km/hour.
It can be raised up to 5m.

本発明により断層・亀裂・温水脈を面内に自動解析する
には、データ・レコーダ44に記録した地形情報、地表
面温度情報及びガンマ線情報を地上で演算処理して、プ
ロッタ又はCRT上に断層・亀裂・温水脈の存在する可
能性の高い位置を二次元的に表示させればよい。このプ
ログラムは、探査位置データをも処理することを除いて
、基本的には演算回路40の動作プログラムと同じであ
る。
In order to automatically analyze faults, cracks, and warm water veins in a plane according to the present invention, the topographical information, ground surface temperature information, and gamma ray information recorded in the data recorder 44 are processed on the ground, and the faults are displayed on a plotter or CRT.・It is sufficient to display two-dimensionally the locations where cracks and warm water veins are likely to exist. This program is basically the same as the operating program of the arithmetic circuit 40, except that it also processes exploration position data.

[発明の効果] 本発明によれば、空中ガンマ線と各種の飛行情報を演算
処理することにより、断層・亀裂・冑水脈の存在の可能
性の高い位置を即時に、又はプロッタ又はCRTを使っ
て二次元的に発見することができ、しかもその判断のた
めに何ら等特殊の知識・熟練は必要とされない。
[Effects of the Invention] According to the present invention, by processing airborne gamma rays and various types of flight information, positions where there is a high possibility of the existence of faults, cracks, and water veins can be immediately identified, or using a plotter or CRT. It can be discovered two-dimensionally, and no special knowledge or skill is required to make that determination.

【図面の簡単な説明】[Brief explanation of drawings]

第1図は、本発明を実施づるための装置の概略ブロック
図であり、第2図は、測定データの一例を示すグラフで
ある。 10.12,14.16・・・ガンマ線検出器18.2
0,22.24・・・対数化回路 26,28.30・
・・減算回路32・・・電波高度計 34・・・気圧高
度計 36・・・速度計38・・・放銅温度計 40・
・・演算回路 42・・・警報部材44・・・データ・
レコーダ
FIG. 1 is a schematic block diagram of an apparatus for implementing the present invention, and FIG. 2 is a graph showing an example of measurement data. 10.12, 14.16... Gamma ray detector 18.2
0,22.24...logarithmization circuit 26,28.30・
...Subtraction circuit 32...Radio altimeter 34...Barometric altimeter 36...Speed meter 38...Copper thermometer 40.
...Arithmetic circuit 42...Alarm member 44...Data...
recorder

Claims (7)

【特許請求の範囲】[Claims] (1)空中飛行体に積載しICガンマ線検知部材により
、解析対象地からのエネルギー帯の異なる複数のガンマ
線の線量を測定し、 と同時に、地表面高度及び地表面温度を測定し、 地表面高度の変化、地表面温度の変化及び、上記測定ガ
ンマ線のエネルギー帯毎の線量比の変化から、地質を探
査する ことを特徴とするガンマ線の空中測定による地質解析法
(1) Using an IC gamma ray detection component mounted on an aerial vehicle, the dose of multiple gamma rays in different energy bands from the analysis target area is measured, and at the same time, the ground surface altitude and ground surface temperature are measured, and the ground surface altitude is measured. A geological analysis method by aerial measurement of gamma rays, which is characterized by exploring the geology from changes in ground surface temperature, changes in ground surface temperature, and changes in the dose ratio for each energy band of the measured gamma rays.
(2) 上記ガンマ線が、少なくとも、’に系列ガンマ
線、′32U系列ガンマ線及び Th系列ガンマ線を含
むことを特徴とする特許請求の範囲第(1)項に記載の
方法。
(2) The method according to claim 1, wherein the gamma rays include at least ' series gamma rays, '32U series gamma rays, and Th series gamma rays.
(3)地形傾斜が2倍を越えて変化し、ラドン娘元素と
カリウムのカント数比 Bi/Kが2倍以上変わるとき
、断層・亀裂の存在を指示し、地形傾斜が2倍以上変化
し、傾斜の正負が変化し、ラドン娘元素とカリウムのカ
ント数比2′″B+ / ”Kが2倍以上変化し、地表
面温度が数℃以上変化し、トロン娘元素とラドン娘元素
のカン1〜地形傾斜が2倍以上変化し、傾斜の正負が変
化し、ラドン娘元素とカリウムのカント数比1″Bi/
″0Kが2倍以上変化し、地表面温度が数℃以上変化し
、トロン娘元素とラドン娘元素のカント数比”’T 1
! /” B rが増加するどき、地下水脈の存在を示
す ことを特徴とする特許請求の範囲第(2)項に記載の方
法。
(3) When the topographic slope changes by more than 2 times and the cant number ratio Bi/K of radon daughter element and potassium changes by more than 2 times, it indicates the existence of faults/cracks, and the topographic slope changes by more than 2 times. , the sign of the slope changes, the cant number ratio 2'''B+/''K of radon daughter element and potassium changes by more than twice, the ground surface temperature changes by more than several degrees Celsius, and the cant number ratio of radon daughter element and potassium daughter element changes by more than a few degrees Celsius. 1 - The topographical slope changes by more than 2 times, the sign of the slope changes, and the cant number ratio of radon daughter element and potassium is 1″Bi/
``0K changes by more than twice, the ground surface temperature changes by more than a few degrees Celsius, and the Kant number ratio of thoron daughter element and radon daughter element'''T 1
! 2. A method according to claim 2, characterized in that when B r increases, it indicates the presence of a groundwater vein.
(4)飛行高度及び対地高度の測定値から地表面高度を
得ることを特徴とする特許請求の範囲第(1)項乃至第
(3)項のいずれか1項に記載の方法。
(4) The method according to any one of claims (1) to (3), characterized in that the ground surface altitude is obtained from the measured values of flight altitude and ground altitude.
(5)飛行体と、 当該飛行体に積載され、検知Tネルギー帯の異なる少な
くとも3個のガンマ線検出器と、当該飛行体にf1戟さ
れ、測定地域の地表面高度を測定する部拐と、 当該飛行体に積載され、測定地域の地表面温度を測定す
る部材と、 当該ガンマ線検出器の各出力の間の比を示す信号を得る
比計算部材と、 当該比計算部材の出力、地表面高度データ及び地表面温
度データに基づき、これらが所定の変化を示すどきに所
定の警報信号を発生する演算回路と、 当該演算回路の出力に応答して、所定の警報を発生する
警報部材 とからなることを特徴とするガンマ線の空中測定による
地質解析装置。
(5) a flight vehicle; at least three gamma ray detectors with different detection T energy bands loaded on the flight vehicle; and an aircraft that is f1-controlled by the flight vehicle and measures the ground surface altitude of the measurement area; A member that is loaded on the aircraft and measures the ground surface temperature in the measurement area; a ratio calculation member that obtains a signal indicating the ratio between each output of the gamma ray detector; and the output of the ratio calculation member and the ground surface altitude. It consists of an arithmetic circuit that generates a predetermined alarm signal based on data and ground surface temperature data when these indicate a predetermined change, and an alarm member that generates a predetermined alarm in response to the output of the arithmetic circuit. A geological analysis device that uses gamma ray aerial measurements.
(6) 上記ガンマ線が、少なくとも、″に系列ガンマ
線、′33U系列ガンマ線及び2JLT 1.系列ガン
マ線を含むことを特徴とする特許請求の範囲第(5)項
に記載の装置。
(6) The apparatus according to claim (5), wherein the gamma rays include at least `` series gamma rays, '33U series gamma rays, and 2JLT 1. series gamma rays.
(7) 前記演算回路は、 地形傾斜が2倍を越えて変化し、′ラドン娘元素とカリ
ウl\のカント数比z+QBi、/ KoKが2倍以上
変わるとぎ、断層・亀裂の存在を指示し、地形傾斜が2
倍以上変化し、傾斜の正負が変化し、ラドン娘元素とカ
リ・クムのノJント数比Al5I B+/ Kが248
以上変化し、地表面温度が数℃以上変化し、トロン娘元
素とラドン娘元素のカン1〜数比”’T l! / B
 iが減少するとぎ、温泉脈の存在指示し、 地形傾斜が2倍以上変化し、傾斜の正負が変化し、ラド
ン娘元素とカリウムのカント数比alp B+i”Kが
2倍以上変化し、地表面温度が数℃以上変化し、トロン
娘元素とラドン娘元素のカント数比 T 9. /鋒B
 iが増加するとき、地下水脈のλof 存在を示す ことを特徴とする特許請求の範囲第(6)項に記載の装
置。 ■ 前記地表面高度測定部材が、飛行高度及び対地高度
の測定値から地表面高度を得ることを特徴とする特許請
求の範囲第(5)項乃至第(7)項のいずれか1項に記
載の装置。
(7) The arithmetic circuit indicates the existence of a fault/crack when the topographic slope changes by more than twice and the Cant number ratio z+QBi,/KoK of 'radon daughter element and potassium l\ changes by more than twice. , terrain slope is 2
The sign of the slope changes, and the number ratio Al5I B+/K of radon daughter element and potassium cum is 248.
The ground surface temperature changed by several degrees Celsius or more, and the ratio of the thoron daughter element to the radon daughter element increased.
When i decreases, it indicates the existence of hot spring veins, the topographical slope changes by more than twice, the sign of the slope changes, the cant number ratio alpB+i''K of radon daughter element and potassium changes by more than twice, When the surface temperature changes by several degrees Celsius or more, the Cant number ratio of the thoron daughter element and the radon daughter element T 9. / Feng B
Device according to claim 6, characterized in that when i increases, it indicates the presence of a groundwater vein λof. (2) The ground surface height measuring member obtains the ground surface height from the measured values of the flight altitude and the ground altitude, according to any one of claims (5) to (7). equipment.
JP59104659A 1984-05-25 1984-05-25 Method and device for geological analysis by aerial measurement of gamma rays Granted JPS60249080A (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
JP59104659A JPS60249080A (en) 1984-05-25 1984-05-25 Method and device for geological analysis by aerial measurement of gamma rays

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
JP59104659A JPS60249080A (en) 1984-05-25 1984-05-25 Method and device for geological analysis by aerial measurement of gamma rays

Publications (2)

Publication Number Publication Date
JPS60249080A true JPS60249080A (en) 1985-12-09
JPH0369077B2 JPH0369077B2 (en) 1991-10-30

Family

ID=14386588

Family Applications (1)

Application Number Title Priority Date Filing Date
JP59104659A Granted JPS60249080A (en) 1984-05-25 1984-05-25 Method and device for geological analysis by aerial measurement of gamma rays

Country Status (1)

Country Link
JP (1) JPS60249080A (en)

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPH01152392A (en) * 1987-12-09 1989-06-14 Asahi Koyo Kk Ground estimation method and its device

Citations (3)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPS5122881A (en) * 1974-08-14 1976-02-23 Tanabe Seiyaku Co Hatsukoho nyoru dd araninno seiho
JPS5225361A (en) * 1975-08-20 1977-02-25 Nishishiba Denki Kk Apparatus for controlling lifting up electromagnet
JPS58169080A (en) * 1982-03-31 1983-10-05 Nogyo Doboku Shikenjo Detection of crack position in bed of ground surface

Patent Citations (3)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPS5122881A (en) * 1974-08-14 1976-02-23 Tanabe Seiyaku Co Hatsukoho nyoru dd araninno seiho
JPS5225361A (en) * 1975-08-20 1977-02-25 Nishishiba Denki Kk Apparatus for controlling lifting up electromagnet
JPS58169080A (en) * 1982-03-31 1983-10-05 Nogyo Doboku Shikenjo Detection of crack position in bed of ground surface

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPH01152392A (en) * 1987-12-09 1989-06-14 Asahi Koyo Kk Ground estimation method and its device

Also Published As

Publication number Publication date
JPH0369077B2 (en) 1991-10-30

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