JPH0429030B2 - - Google Patents
Info
- Publication number
- JPH0429030B2 JPH0429030B2 JP1293798A JP29379889A JPH0429030B2 JP H0429030 B2 JPH0429030 B2 JP H0429030B2 JP 1293798 A JP1293798 A JP 1293798A JP 29379889 A JP29379889 A JP 29379889A JP H0429030 B2 JPH0429030 B2 JP H0429030B2
- Authority
- JP
- Japan
- Prior art keywords
- signal
- radio wave
- arrival
- amplitude value
- distance
- 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
- 239000005433 ionosphere Substances 0.000 claims description 25
- 238000000034 method Methods 0.000 claims description 19
- 238000012937 correction Methods 0.000 claims description 11
- 238000005259 measurement Methods 0.000 claims description 6
- 238000009434 installation Methods 0.000 claims description 5
- 238000010586 diagram Methods 0.000 description 15
- 230000006870 function Effects 0.000 description 8
- 238000012935 Averaging Methods 0.000 description 7
- 230000007423 decrease Effects 0.000 description 6
- 238000001514 detection method Methods 0.000 description 6
- 238000006243 chemical reaction Methods 0.000 description 5
- 230000007274 generation of a signal involved in cell-cell signaling Effects 0.000 description 5
- 238000000691 measurement method Methods 0.000 description 5
- 230000000694 effects Effects 0.000 description 4
- 239000004065 semiconductor Substances 0.000 description 4
- 230000010354 integration Effects 0.000 description 3
- 230000010363 phase shift Effects 0.000 description 3
- 230000003321 amplification Effects 0.000 description 1
- 238000007796 conventional method Methods 0.000 description 1
- 230000003111 delayed effect Effects 0.000 description 1
- 238000005516 engineering process Methods 0.000 description 1
- 238000007689 inspection Methods 0.000 description 1
- 238000003199 nucleic acid amplification method Methods 0.000 description 1
- 230000000737 periodic effect Effects 0.000 description 1
- 238000012545 processing Methods 0.000 description 1
- 230000000630 rising effect Effects 0.000 description 1
- 229920006395 saturated elastomer Polymers 0.000 description 1
- 230000001360 synchronised effect Effects 0.000 description 1
Landscapes
- Radar Systems Or Details Thereof (AREA)
Description
【発明の詳細な説明】
〔産業上の利用分野〕
本発明は円周上に間隔配置した無指向性アンテ
ナを順次に切替えて走査しながら電波を受信する
ことにより得られる受信信号中の前記切替えによ
り生ずる位相変化の位相差を検出した信号にもと
づいて方位信号を得る無線方向探知方法、つま
り、いわゆる静止形ドツプラ方式の無線方向探知
方法に、地平面に対する垂直面内における電波の
到来角度を測定定する機能とアンテナの設置位置
から電波の発射点までの距離を計測する機能とを
付加する方法およびその方法を実施する装置に関
するものである。[Detailed Description of the Invention] [Industrial Application Field] The present invention provides the switching in the received signal obtained by receiving radio waves while scanning by sequentially switching omnidirectional antennas arranged at intervals on the circumference. A radio direction finding method that obtains a direction signal based on a signal that detects the phase difference of the phase change caused by the radio direction finding method, that is, a so-called stationary Doppler radio direction finding method, involves measuring the arrival angle of radio waves in a plane perpendicular to the horizon. The present invention relates to a method for adding a function to measure the distance from an antenna installation position to a radio wave emission point, and an apparatus for implementing the method.
静止形ドツプラ方式の方向探知方法としては、
その実施装置により説明すると、
第1図イの如く同一特性を有する多数の無指向
性アンテナA1〜Aoを円周上に等間隔に配置して、
アンテナの中央に設けてアンテナ切替走査回路に
導き、これを順次切替え走査して受信機に接続す
る。
The stationary Doppler direction finding method is as follows:
To explain it using an implementation device, as shown in Fig. 1A, a large number of omnidirectional antennas A 1 to A o having the same characteristics are arranged at equal intervals on the circumference,
It is installed in the center of the antenna and led to an antenna switching scanning circuit, which is sequentially switched and scanned and connected to a receiver.
しかるとき電波が地平面に対して水平に伝播す
ると仮定すれば、受信信号の位相成分φoは電波
の到来方向とアンテナの相対位置に従つて第(1)式
の如く表わされ、第1図ハのような正弦波的段階
状に変化することになる。 If we assume that the radio waves propagate horizontally to the horizon, the phase component φ o of the received signal can be expressed as shown in equation (1) according to the arrival direction of the radio waves and the relative position of the antenna, and the first It changes in a sinusoidal stepwise manner as shown in Figure C.
φo=πD/λ・cos(nα−θ) ……(1)
D:アンテナ直径
λ:受信電波の波長
α:隣同志のアンテナ間の角度
θ:基準Nに対する到来電波の角度
n:アンテナ素子数(1〜n)
ここでm=πD/λとおき、このmは変調指数と呼
ばれるもので得られた方位信号の振幅そのもので
ある。 φ o = πD/λ・cos(nα−θ) ……(1) D: Antenna diameter λ: Wavelength of received radio waves α: Angle between adjacent antennas θ: Angle of incoming radio waves with respect to reference N n: Antenna element Number (1 to n) Here, m=πD/λ, where m is the amplitude itself of the azimuth signal obtained by what is called a modulation index.
従つて、この受信信号を増幅検波すると第1図
ハのような方位信号が得られるので、基準点N、
つまり、基準方位からこの方位信号の最大振幅点
(又は零クロス点t1、あるいはt2を求め、これに
90゜を加算又は減算する)迄計数すると電波の到
来方向を測定することができるようにしたもの
が、特公昭56−35828・特開昭56−137169などに
より開示されている。 Therefore, when this received signal is amplified and detected, a direction signal as shown in Fig. 1C is obtained, so the reference point N,
In other words, find the maximum amplitude point (or zero cross point t 1 or t 2 ) of this azimuth signal from the reference azimuth, and
Japanese Patent Publication No. 56-35828 and Japanese Patent Application Laid-Open No. 56-137169 disclose devices in which the direction of arrival of radio waves can be measured by counting up to 90 degrees (adding or subtracting 90 degrees).
また、地平面に対する垂直面内における電波の
到来角度、いわゆる入射を仰角または俯角により
測定する方法としては、従来、インタヘフエロメ
ータ方式よるもの、つまり、線上に間隔配置した
複数のアンテナにより電波の受信して得られる各
受信信号の受信位相の変化により入射角を検出す
る方法などが周知である。 In addition, the conventional method for measuring the angle of arrival of radio waves in a plane perpendicular to the horizon, so-called angle of incidence, using the angle of elevation or depression is the interferometer method, in which radio waves are measured using multiple antennas spaced apart in a line. A method of detecting the angle of incidence based on a change in the reception phase of each received signal is well known.
そして、上記の入射角と電離層の高さとにもと
づいてアンテナから受信電波の発射地点までの距
離を算定し、この距離値と無線方向探知によつて
得られた方位値とにより電波の発射地点を知るす
ることができる。 Then, the distance from the antenna to the emission point of the received radio waves is calculated based on the above incident angle and the height of the ionosphere, and the emission point of the radio waves is determined using this distance value and the azimuth value obtained by radio direction finding. You can know.
上記のような静止形ドツプラ方式の無線方向探
知方法を用いた装置は、既に広く普及しており、
こうした装置を設置した電波鑑視施においても、
上の入射角を測定するとともに、測定した入射角
にもとづいて電波の発射地点を知ることができる
ように設備することが望まれている。
Devices using the stationary Doppler radio direction finding method as described above are already widely used.
Even in radio wave inspection facilities that have installed such devices,
It is desired to have equipment that can measure the above incident angle and determine the emission point of radio waves based on the measured incident angle.
そこで、上記のようなインタフエロメータ方式
のものを新たに増設することなく、既設の静止形
ドツプラ方式の無線方向探知施設を用いて上記の
入射角および発射地点までの距離を測定し得るも
のが提供されれば設備投資を軽減でき、至極、便
利である。 Therefore, there is a method that can measure the above-mentioned angle of incidence and distance to the launch point using the existing stationary Doppler radio direction finding facility without adding a new interferometer system. If provided, equipment investment can be reduced and it is extremely convenient.
また、親規の施設の場合にも比較的安価な投資
で済ませられるという利点がある。 Furthermore, in the case of a parent-owned facility, there is an advantage in that it requires relatively low investment.
このため、そうした測定方法をどのように構成
して提供するか、という課題がある。 Therefore, there is a problem of how to configure and provide such a measurement method.
本発明は、上記のような
円周上に等間隔配置した無指向性アンテナを順
次に切替えて走査しながら電波を受信して受信信
号を得るとともに、切替えによつて生じた受信信
号中の位相変化により電波の到来方向に関連づけ
られてSIN波状に変化する成分、つまり、SIN波
状変化成分をもつ信号の方位信号として得ること
により、方位信号にもとづいて電波の到来方向を
探知するとともに電波の到来方向にもとづいて電
波の発射点の位置を計測する無線方向距離測定方
法において、
上記の方位信号に含まれるSIN波状変化成分の
振幅を計測した値を計測振幅値m′として得る振
幅計測と、
電波が地平面を伝播して到来した場合に得られ
るべき計測振幅値m′に相当する振幅値、つまり、
相当振幅値mを作成成する相当振幅値作成と、
上記の計測振幅値m′と相当振幅値mとにより、
m′/m=cosβ
の関係式にもとづいて、地平面に垂直な面内にお
ける電波の到来角度、つまり、到来入射角βを得
る垂直面内到来角測定と、
電離層の高さhと地球半径fを上記の到来入射
角βとにより、
2{cos-1〔r/r+hcosβ〕−β}r=Q
の関係式にもとづいて上記無指向性アンテナの設
置地点から電波の発射点までの距離Qを算定する
発射点演算と
を設ける方法とその方法を具体化した装置を提供
することにより上記の課題を解決し得るようにし
たものである。
The present invention obtains a received signal by receiving radio waves while scanning by sequentially switching the omnidirectional antennas arranged at equal intervals on the circumference as described above, and also detects the phase difference in the received signal caused by the switching. By obtaining a direction signal of a signal that has a SIN wave-like component that is related to the arrival direction of the radio wave due to change, that is, a SIN wave-like change component, the direction of arrival of the radio wave can be detected based on the direction signal, and the arrival direction of the radio wave can be detected. In the wireless direction distance measurement method that measures the position of the emission point of radio waves based on the direction, there is an amplitude measurement method in which the amplitude of the SIN wave-like change component included in the above-mentioned azimuth signal is obtained as the measured amplitude value m'; The amplitude value corresponding to the measured amplitude value m′ that should be obtained when the wave propagates through the horizon, that is,
By creating the equivalent amplitude value m, and using the above measured amplitude value m' and the equivalent amplitude value m, based on the relational expression m'/m=cosβ, in the plane perpendicular to the horizon, By measuring the arrival angle in the vertical plane to obtain the arrival angle of the radio wave, that is, the arrival incident angle β, and by determining the height h of the ionosphere and the earth radius f from the above arrival incidence angle β, 2 {cos -1 [r/r + hcos β] -β}r=Q A method for calculating the distance Q from the installation point of the omnidirectional antenna to a radio wave emission point based on the relational expression, and a device embodying the method are provided. This makes it possible to solve the above problems.
以下、実施例を図面により説明する。 Examples will be described below with reference to the drawings.
第1図ロにおいて、もし、仰角βもつて上空よ
り到来る電波を、直径Dなる円周上に無指向性ア
ンテナを配置した第1図イのアンテナ群によつて
電波を受信したとすると、電波の到来方向におけ
る第(1)式のアンテナ直径Dは、見掛上、小さくな
り、従つて、φnも小さくなるので、第1図ハの
方位信号の振幅mも、それに応じて小さくなる。 In Figure 1 B, if a radio wave arriving from the sky with an elevation angle β is received by the antenna group in Figure 1 A, which has omnidirectional antennas arranged on the circumference of a circle with a diameter D, then The antenna diameter D in equation (1) in the direction of arrival of the radio wave apparently becomes smaller, and therefore φn also becomes smaller, so the amplitude m of the azimuth signal in FIG. 1C also becomes smaller accordingly.
すなわち第1図ロに於て、電波が水平面に対し
てβなる角度をもつて到来すると、電波の波面が
A4アンテナに到達してから180゜反対方向にある
Ao-2アンテナは到達る迄の距離、すなわち実効
アンテナ直径D′は
D′=D・cosβ ……(2)
となりcosβに比例して減少することになる。 In other words, in Figure 1B, when a radio wave arrives at an angle β with respect to the horizontal plane, the wavefront of the radio wave becomes
A 180° in the opposite direction after reaching the 4 antenna
The distance that the A o-2 antenna reaches, ie, the effective antenna diameter D', is D'=D·cosβ (2), and decreases in proportion to cosβ.
従つて仰角を持つて受信された電波のドブラ効
果によつて生ずる位相変化φ′oは
φ′o=(π/λD′)・cos(nα−θ)
=(π/λD・cosβ)・cos(nα−θ)
=(m・cosβ・cos(nα−θ) ……(3)
(3)式に於ける変調指数m′は
m′=m・cosβ ……(4)
となり電波の仰角βの余弦に比例して変調指数
m′が小さくなり、従つて位相変化φ′oも小さくな
るので第1図ハの方位信号の振幅も小さくなる。 Therefore, the phase change φ′ o caused by the Dobra effect of radio waves received with an elevation angle is φ′ o = (π/λD′)・cos(nα−θ) = (π/λD・cosβ)・cos (nα−θ) = (m・cosβ・cos(nα−θ) ……(3) The modulation index m′ in equation (3) is m′=m・cosβ ……(4) and the elevation angle β of the radio wave modulation index proportional to the cosine of
Since m' becomes smaller and therefore the phase change φ' o also becomes smaller, the amplitude of the azimuth signal in FIG. 1C also becomes smaller.
従つて仰角零、すなわち地表波の電波を受信し
た時の方位信号の振幅mを求めてこれを基準値と
してメモリに記憶しておき、仰角βで到来した電
波の方位信号振幅すなわちm′を測定すれば第(4)
式より電波の仰角βを求めることが出来るのであ
る。 Therefore, find the amplitude m of the azimuth signal when the ground wave is received at zero elevation angle, store it in memory as a reference value, and measure the azimuth signal amplitude m' of the radio wave that arrives at the elevation angle β. Then (4)
The elevation angle β of the radio wave can be found from the formula.
つまり、電波が地平面を伝播して到来した場合
に得られれるべき振幅mと、実際に測定して得ら
れる振幅m′とによる三角函数にもとづいて、地
平面と垂直な面内における電波の到来角度βを求
めるわけである。 In other words, based on the trigonometric function of the amplitude m that should be obtained when the radio wave propagates through the horizon and the amplitude m' that is actually measured, the radio wave in a plane perpendicular to the horizon is calculated. The angle of arrival β is found.
次に上で求めた仰角により電波発射点を推定す
る原理について説明する。第2図は到来電波の仰
角βと電離層の高さhによつて距離を推定する原
理図である。 Next, the principle of estimating the radio wave emission point using the elevation angle determined above will be explained. FIG. 2 is a diagram showing the principle of estimating distance based on the elevation angle β of the arriving radio wave and the height h of the ionosphere.
円弧Pは地球表面、Oは地球の中心点、rは地
球の半径、Sは電波発射点、Rは電波受信点、Q
はSとの円弧のさ、YはSとRをはさむ角、hは
電離層の高さ、βは到来電波の大地に対する仰角
(入射角)であつて、電波がS点から発射されて
電離層高さHの点で反射してR点で受信した様子
を示している。電離層反射波がR点に於て仰角0
受信される時の電離層高さはH0であり、電離層
高さが高くなつてHになる電波の仰角はβとな
る。 Arc P is the earth's surface, O is the center of the earth, r is the radius of the earth, S is the radio wave emission point, R is the radio wave reception point, Q
is the length of the arc with S, Y is the angle between S and R, h is the height of the ionosphere, and β is the angle of elevation (angle of incidence) of the incoming radio wave with respect to the ground, and the height of the ionosphere when the radio wave is emitted from point S is The figure shows how the signal is reflected at point H and received at point R. The ionospheric reflected wave has an elevation angle of 0 at point R.
The height of the ionosphere at the time of reception is H0 , and the angle of elevation of the radio wave becomes H as the height of the ionosphere increases is β.
従つて電波反射波の仰角β、電離層の高さh、
電波発射点Sと電波受信点Rを地球の中心点Oか
ら見た角度Yとの間には、第(5)式のような関係が
存在するのでこれを変形し第(6)式のような関係が
得られる。 Therefore, the elevation angle β of the radio wave reflected wave, the height h of the ionosphere,
Since there is a relationship as shown in equation (5) between the radio wave emitting point S and the radio wave receiving point R as seen from the center point O of the earth, the relationship shown in equation (5) can be modified as shown in equation (6). A good relationship can be obtained.
SIN(90゜+β)/r+h=SIN(90゜−β−Y/2)
/r……(5)
cosβ/r+h=cos(β+Y/2)/rcos(β+Y/
2)
=r/r+hcosβ+Y/2=cos-1〔r/r+hcos
β〕Y
=2cos-1〔r/r+hcosβ〕−2β ……(6)
更に円弧の長さQとSとRをはさむ角Yとの間
には次の関係がある。 SIN(90°+β)/r+h=SIN(90°−β−Y/2)
/r...(5) cosβ/r+h=cos(β+Y/2)/rcos(β+Y/
2) =r/r+hcosβ+Y/2=cos -1 [r/r+hcos
β]Y =2cos -1 [r/r+hcosβ] -2β ...(6) Furthermore, the following relationship exists between the length Q of the circular arc and the angle Y sandwiching S and R.
Q=Y/2π・2πr=Yr
=2{cos-1〔r/r+hcosβ〕−β}r ……(7)
rは地球の半径で約6378Km(理科年表による)、
hは測定地点で実測された電離層の高さで既知の
値であるからβを求めれば、電波発射点迄の距離
Qを求めることが出るのである。 Q=Y/2π・2πr=Yr=2{cos -1 [r/r+hcosβ]−β}r...(7) r is the radius of the earth, approximately 6378 km (according to the Science Chronology),
Since h is the height of the ionosphere actually measured at the measurement point and is a known value, by finding β, the distance Q to the radio wave emission point can be found.
つまり、地平面と垂直な面内における電波の到
来角度βと、地球半径rと、電離層の高さhとに
よる三角函数にもとづいて、電波の発射点までの
距離Qを求めるわけである。 That is, the distance Q to the emission point of the radio wave is determined based on a trigonometric function of the arrival angle β of the radio wave in a plane perpendicular to the horizon, the radius r of the earth, and the height h of the ionosphere.
次に、本発明の実施装置について、実施例を説
明する。 Next, an example of an implementation apparatus of the present invention will be described.
第3図は上記の測定方法を具体化した実施装置
を示す系統図である。第4図はDAC(DIGITAL
TO ANALOG CONVERTER)の回路例を、
第5図は本発明による周波数補正回路の1実施例
を示す。第6図は第3図に示す位相比較回路8の
詳細を示す図、第7図、第8図は各部の動作波形
図を示す。第9図は電離層高さ300Kmで反射した
電波の各仰角に対する方位信号の振幅m′と電波
発射源迄の距離を計算したデータ値とこのデータ
値をメモリに記憶するためのメモリ配置を示す図
である。 FIG. 3 is a system diagram showing an implementation apparatus embodying the above measurement method. Figure 4 shows the DAC (DIGITAL)
TO ANALOG CONVERTER) circuit example,
FIG. 5 shows one embodiment of a frequency correction circuit according to the invention. FIG. 6 is a diagram showing details of the phase comparator circuit 8 shown in FIG. 3, and FIGS. 7 and 8 are operational waveform diagrams of each part. Figure 9 is a diagram showing the calculated data value of the amplitude m' of the azimuth signal for each elevation angle of the radio wave reflected at the ionosphere height of 300 km, the distance to the radio wave emission source, and the memory arrangement for storing this data value in memory. It is.
第3図に於て1は中心に補助アンテナA0を、
又円周上に等間隔に1〜n迄無指向性アンテナを
配置したアンテナ群である。2は基準信号発生回
路でクロツクパルスを発生し、これを分周して各
目的の周のパルスを発生する。 In Figure 3, 1 has the auxiliary antenna A 0 in the center,
It is also an antenna group in which omnidirectional antennas 1 to n are arranged at equal intervals on the circumference. 2 is a reference signal generating circuit which generates a clock pulse, which is frequency-divided to generate pulses of each desired frequency.
3は前記アンテナ群の中心に設けた各アンテナ
素子を切替えるためのアンテナ切替走査回路でダ
イオードに流れる電流を制御して各アンテナ出力
を順次切替えてその出力を受信機4に接続する。
4は一つの周波数ツマミを操作することにより、
両チヤンネル共に受信周波数を同時に調整出来る
ような主受信機、従受信機により構成された2チ
ヤンネル受信機で補助アンテナA0の出力を一方
のチヤンネルに、アンテナ切替回路出力を他方の
チヤンネルに接続しそれぞれ増幅する。 Reference numeral 3 denotes an antenna switching scanning circuit for switching each antenna element provided at the center of the antenna group, which controls the current flowing through the diode to sequentially switch the output of each antenna, and connects the output to the receiver 4.
4 is by operating one frequency knob,
A two-channel receiver consisting of a main receiver and a sub-receiver that can adjust the receiving frequency of both channels simultaneously, connects the output of the auxiliary antenna A 0 to one channel and the output of the antenna switching circuit to the other channel. Amplify each.
5はFM成分除去回路と周波数弁別回路よりな
る方位信号検出回路で、主及び従受信機からの出
力をそれぞれ周波数変換し、その出力を混合回路
により更に周波数変換して周波数変化を伴う受信
電波の変調成分を除去して、アンテナ切替にもと
ずくドブラ効果による成分のみを含んだ信号とす
る。 5 is an azimuth signal detection circuit consisting of an FM component removal circuit and a frequency discrimination circuit, which frequency-converts the outputs from the main and sub-receivers, and further converts the frequency of the output by a mixing circuit to detect received radio waves with frequency changes. The modulation component is removed to create a signal containing only the component due to the Dobra effect based on antenna switching.
このFM成分除回路の目的は、周波数変調を受
けた電波を受信するとアンテナ切替走査による方
位信号に、もともと電波に附与されている大きな
変調波が重畳して到来電波の方位が定まらなくな
るので、FM成分除去回路を通して安定な方位を
指示させるために用いるのであつて、受信電波が
FM変調を受けていない場合でもこの回路を通す
ことによつて、不都合を生ずることなく目的のア
ンテナ切替走査による信号成分のみを取すことが
出来るのである。 The purpose of this FM component removal circuit is that when a frequency-modulated radio wave is received, a large modulated wave originally attached to the radio wave is superimposed on the azimuth signal generated by antenna switching scanning, and the direction of the incoming radio wave becomes unstable. It is used to indicate a stable direction through the FM component removal circuit, and the received radio waves are
By passing the signal through this circuit even when it is not undergoing FM modulation, it is possible to extract only the signal component resulting from the intended antenna switching scan without causing any inconvenience.
次にFM成分除去回路の出力な周波数弁別回
路、例えばデイスクリ又はPLL等のような回路
を通して、前アンテナ切替走査によつて生じたド
ブラ効による方位信号を検出する。 Next, the azimuth signal due to the Dobra effect caused by the front antenna switching scan is detected through a frequency discrimination circuit, such as a disk drive or PLL circuit, which is the output of the FM component removal circuit.
6は周波数補正回路で、周波数に逆比例してそ
の振幅が増加する方位信号、すなわち方位信号検
出回路5の出力を入力として受信周波数信号F1
(複数ビツトで構成されたバイナリデイジタル信
号)によつて周波数が低くなると、周波数補回路
6の増幅度をあげ方位信号出力aが周波数に無関
係に一定の値となるように動作する。 Reference numeral 6 denotes a frequency correction circuit, which inputs the azimuth signal whose amplitude increases in inverse proportion to the frequency, that is, the output of the azimuth signal detection circuit 5, and outputs the received frequency signal F1.
When the frequency becomes lower due to (a binary digital signal composed of a plurality of bits), the amplification degree of the frequency compensating circuit 6 is increased so that the azimuth signal output a becomes a constant value regardless of the frequency.
この周波数補正回路6による補正は、上記の第
(1)式により説明したように、受信電波の波長λが
大きくなると、つまり、周波数が低くなると、そ
れに比例して変調指数m(方位信号の振幅)が逆
に小さくなるため、入射βによつて小さくなつた
量のほかに、周波数によつて小さくなつた量が加
わるから、広い周波数帯にわつて方向探知を行う
場合には、そのままで、上記の第(4)式の条件が成
立しなくなつてしまうので、これを救済するため
に設けるたものである。 The correction by this frequency correction circuit 6 is performed by the above-mentioned
As explained using equation (1), as the wavelength λ of the received radio wave increases, that is, as the frequency decreases, the modulation index m (amplitude of the azimuth signal) decreases proportionally. In addition to the amount that decreases with frequency, the amount that decreases with frequency is added, so when direction finding is performed over a wide frequency band, the condition of equation (4) above holds as it is. This was created to save people from losing their lives.
なお第7図aの方位信号は第1ハの信号と同じ
であるが簡単のため階段的変化を省略し、その平
均のSIN波で表わしてあり、しかも周波数補正回
路を通したことにより周波数に無関係に一定振幅
の信号である。第4図には説明のための一般的な
DAC用の回路例を、又第5図に本発明による周
波数補正回路の一実施例を示す。 The direction signal in Figure 7a is the same as the signal in Figure 1C, but for simplicity, the step change is omitted and it is expressed as an average SIN wave, and by passing it through a frequency correction circuit, the frequency can be changed. It is a signal of constant amplitude regardless. Figure 4 shows general information for explanation.
An example of a circuit for a DAC is shown in FIG. 5, and an embodiment of a frequency correction circuit according to the present invention is shown in FIG.
図に於て61は例えばAD7523Jのようなマル
チブライングDAC用ICで、62は二入力を持つ
オペレーシヨンアンプである。第4のDAC用IC
61のデータ入力端子T1に複数ビツト(例えば
8ビツトあるいは12ビツト等)のDIGITAL信号
F1を加え、基準入力端子T2(VREF)にアナ
ログ基準電圧F2を加えると端子T3(RF)に
入力F1と入力F2の積F3が出力するように動
作するのでF1が増加すれば出力F3も増加し、
F1,F2,F3の間には次の関係がある。 In the figure, 61 is a multi-bright DAC IC such as AD7523J, and 62 is an operational amplifier with two inputs. 4th DAC IC
When a digital signal F1 of multiple bits (e.g. 8 bits or 12 bits) is applied to the data input terminal T1 of the 61, and an analog reference voltage F2 is applied to the reference input terminal T2 (VREF), the input F1 is input to the terminal T3 (RF). It operates so that the product F3 of F2 is output, so if F1 increases, the output F3 also increases,
The following relationship exists between F1, F2, and F3.
F1×F2=F3 ……(8)
従つて、第5図のように、入力T1には複数ビ
ツトの受信周波数DIGITAL信号F1を入力し、
端子T3には受信周波数によつて振幅の変化する
方位信号、つまり方位信号検出回路5の出力を加
えると端子T2に出力される信号F2は(8)式より
F2=F3/F1
となる。F1は受信周波数に比例するDIGITAL
信号であるから、比例常をkとすればF1=kfと
表わされる。 F1×F2=F3...(8) Therefore, as shown in FIG. 5, input the multi-bit reception frequency DIGITAL signal F1 to the input T1,
When an azimuth signal whose amplitude changes depending on the reception frequency, that is, the output of the azimuth signal detection circuit 5 is added to the terminal T3, the signal F2 outputted to the terminal T2 becomes F2=F3/F1 from equation (8). F1 is DIGITAL proportional to the receiving frequency
Since it is a signal, if the proportional constant is k, it can be expressed as F1=kf.
又端子T3の信号F3は方位信号で、同様に受
信周波数に比例して振幅が変化するから比例常数
をk′とすればF3=k′fと表わされ、
F2=F3/F1=k′f/kf=k′/k(一定常数)
となり端子T2には受信周波数に無関係に振幅一
定の方位信号が得られることになる。 Also, the signal F3 at terminal T3 is an azimuth signal, and the amplitude similarly changes in proportion to the reception frequency, so if the proportionality constant is k', then it can be expressed as F3 = k'f, and F2 = F3 / F1 = k'f/kf=k'/k (constant constant), so that an azimuth signal with a constant amplitude is obtained at the terminal T2 regardless of the reception frequency.
なお周波数信号F1の反対極性の信号1が得
られる場合には、第4図の接続とし端子T2に方
位信号検出回路5の出力を加えれば端子T3には
周波数に無関係に常に一定な振幅の方位信号が得
られる。 If a signal 1 with the opposite polarity to the frequency signal F1 is obtained, by making the connection shown in Figure 4 and adding the output of the azimuth signal detection circuit 5 to the terminal T2, the azimuth signal with a constant amplitude is always output to the terminal T3 regardless of the frequency. I get a signal.
7はオペアンプとダイオードで構成した両波整
流回路で周波数補正回路6の出力、第7図aをb
のような両波整流信号とすると同時に、cのよう
な方位信号aと周期の一致した矩形波を発生す
る。 7 is a double-wave rectifier circuit composed of an operational amplifier and a diode, and the output of the frequency correction circuit 6.
At the same time, a rectangular wave having the same period as the azimuth signal a as shown in c is generated.
8は位相比較回路で第6図のように内部信号発
生器81と掛算器82、半導体スイツチ83,
ADC(ANALOG TO DIGITAL
CONVERTER)84、ラツチ回路85,
EXCLUSIVE OR GATE86より構成されてい
る。前述してある通り検波した方位信号号aから
電波到来方位を求めるためには、方位信号の最大
振幅点を求め(又は0クロス点を求めこれに90゜
を加算又減算して方位とする)電波の到来方位と
すれば良いのであるが、第2図のように、電離層
反射して伝播してくるような遠方の電波の場合に
は、方位信号には雑音信号が多く含まれ、そのま
までは、方位が変動して測定が困難なりやすい。 8 is a phase comparator circuit that includes an internal signal generator 81, a multiplier 82, a semiconductor switch 83,
ADC (ANALOG TO DIGITAL)
CONVERTER) 84, latch circuit 85,
Consists of EXCLUSIVE OR GATE86. As mentioned above, in order to find the radio wave arrival direction from the detected direction signal a, find the maximum amplitude point of the direction signal (or find the 0 cross point and add or subtract 90 degrees to it to determine the direction) It is sufficient to use the direction of arrival of the radio waves, but as shown in Figure 2, in the case of far-off radio waves that propagate by being reflected from the ionosphere, the direction signal contains many noise signals, , the direction tends to fluctuate, making measurement difficult.
そのため内部信号発生回路を設けて方位信号と
同一周期のSIN波の両波整流波(第7図e)を作
り、この信号と方位信号bとを掛算して得られる
波形の面積を求めて平均処理を行い、この結果に
より前記内部信号発生回路出力の位相を制御して
より正確で安定な方位を求めることが出来るので
ある。 Therefore, an internal signal generation circuit is installed to generate a double rectified SIN wave with the same period as the direction signal (Fig. 7e), and the area of the waveform obtained by multiplying this signal by the direction signal b is calculated and averaged. The process is performed, and the phase of the output of the internal signal generation circuit is controlled based on the result, thereby making it possible to obtain a more accurate and stable heading.
又、方位信号はいつも第7図aのような比較的
きれいなSIN波であるとは限らず電波の状況によ
つて複雑な形の波形となり高次高調波を含むよう
になると、もし内部信号として矩形波用いると両
信号の高調波(例えば3次高調波、5次高調波
等)同志の位相差成分が出力に重畳してくるの
で、内部信号がSIN波(基本波)の時に対して方
位誤差を生ずることになる。このため前述のよう
に、二つの信号の一方、つまり内部信号をSIN
ROMによりSIN波として方位信号と掛算すれば
方位信号の方が高調波を含んだ波形であつても基
本波以外の周波数成分については掛算した結果の
平均値は0となるので、方位誤差に対する影響は
なくなり正しい方位を指示することが出来るので
ある。 In addition, the direction signal is not always a relatively clean SIN wave as shown in Figure 7a, but depending on the radio wave situation, it becomes a complicated waveform and contains high-order harmonics, and if it becomes an internal signal. When using a rectangular wave, the phase difference component between the harmonics of both signals (e.g. 3rd harmonic, 5th harmonic, etc.) will be superimposed on the output, so when the internal signal is a SIN wave (fundamental wave), the direction will be different. This will result in an error. Therefore, as mentioned above, one of the two signals, that is, the internal signal, is
When multiplied by the azimuth signal as a SIN wave using ROM, even if the azimuth signal has a waveform that includes harmonics, the average value of the multiplication results for frequency components other than the fundamental wave will be 0, so this will affect the azimuth error. This means that the correct direction can be pointed out.
ここで、上記の方位信号aと内部信号のSIN波
と信号eおよび位相の制御の関係を要約して第7
図により説明すると、電波が基準方位Nの方向か
ら到来したときには、方位信号aのSIN波状の信
号は第7図aのθ0に対応するVの波形になつて現
れ、また、方位信号aを両波整流波した方位信号
bは第7図bのVの波形になつて現れる。 Here, we will summarize the relationship between the azimuth signal a, the SIN wave of the internal signal, the signal e, and the phase control.
To explain with a diagram, when a radio wave arrives from the direction of the reference direction N, the SIN wave-like signal of the direction signal a appears as a waveform of V corresponding to θ 0 in FIG. The direction signal b obtained by rectifying both waves appears as a waveform V in FIG. 7b.
一方、内部信号のSIN波は、最初、方位信号a
が電波が基準方位Nの方向から到来したときの波
形、つまり、Vの波形に対して90゜の位相差をも
つSIN波で発生されるが、この内部信号のSIN波
の両波整流波の信号eの波形は第7図eのθ0に対
応するVの波形になつて現れる。 On the other hand, the SIN wave of the internal signal is initially the azimuth signal a
is generated as a SIN wave with a phase difference of 90° with respect to the waveform when the radio wave arrives from the direction of the reference direction N, that is, the waveform of V, but the rectified wave of both SIN waves of this internal signal The waveform of signal e appears as a waveform of V corresponding to θ 0 in FIG. 7e.
電波の到来方向がθ1またはθ2の方向に変化して
方位信号aがθ1またはθ2に対応するUまたはWの
波形になる。 The arrival direction of the radio wave changes to the direction of θ 1 or θ 2 , and the azimuth signal a becomes a waveform of U or W corresponding to θ 1 or θ 2 .
そこで、信号eと方位信号bとを掛算して得ら
れる信号の平均値、つまり、後記の第7図f〜i
の波形で説明する信号の平均値の信号を作り、こ
の平均値の信号で内部信号のSIN波の位相を移相
して、方位信号aのSIN波状の信号と90゜の位相
差になるように制御すると、内部信号のSIN波が
θ1またはθ2に位相点に移ることになり、この間の
移相量、つまり、θ1またはθ2が電波の到来方向な
るわけである。 Therefore, the average value of the signal obtained by multiplying the signal e and the azimuth signal b, that is, the average value of the signal obtained by multiplying the signal e and the azimuth signal b, that is, the
Create a signal with the average value of the signals explained with the waveform, and use this average value signal to shift the phase of the SIN wave of the internal signal so that it has a phase difference of 90 degrees with the SIN wave signal of the direction signal a. When controlled, the SIN wave of the internal signal shifts to the phase point θ 1 or θ 2 , and the amount of phase shift during this time, that is, θ 1 or θ 2 is the arrival direction of the radio wave.
第6図は本発明の位相比較回路の一実施例を示
す。 FIG. 6 shows an embodiment of the phase comparator circuit of the present invention.
811はプリセツタブルアツプダウンバイナリ
カウンタで複数ビツトからなるプリセツト端子に
プリセツト入力F4を与えてアンテナ基準信号発
生回路2より与えられたクロツクCLKによりダ
ウン計数し、出力側に複数ビツトのカウンタ出力
が得られる。 Reference numeral 811 is a presettable up-down binary counter which applies a preset input F4 to a preset terminal consisting of multiple bits, performs down counting using the clock CLK applied from the antenna reference signal generation circuit 2, and obtains a multi-bit counter output on the output side. It will be done.
812はROM(READ ONLY MEMORY)
でSIN波の半周期又は1周期分が記憶されてお
り、SIN ROMの入力側にプリセツタブルアツプ
ダウンバイナリカウンタ812の出力でアドレス
L内部に記憶してあるSIN波eの変化をする
DIGITAL信号が得られる。 812 is ROM (READ ONLY MEMORY)
A half cycle or one cycle of the SIN wave is stored in the input side of the SIN ROM, and the output of the presettable up-down binary counter 812 changes the SIN wave e stored at address L.
DIGITAL signal can be obtained.
82は第4図のようなDAC用ICとオペアンプ
で構成した掛算回路で、一方の入力端子に前記
SIN波のDIGITAL信号を与えて、他方の入力端
子に前述した方位信号の両波整流波bを加えて両
入力の掛算を行い、第7図jのようなアナログ出
力を作り、これを半導体スイツチ83を通して
ADC84に入力する。ADC84はSC(スタート
コンバージヨン)信号の立上りで変換を開始し、
変換終了時にEOC(エンド オブ コンバージヨ
ン)信号を発生し、この信号より半導体スイツチ
を導通させて掛算回路出力第7図jをADCの入
力端子加える。前記SCは円周上に配置したアン
テナを順次切替えて1回転する時間をT=1/fa
(fa:アンテナ1回転の周波数)、アンテナの数を
nとすればT/n=1/nfaの周期のパルスを用いる。 82 is a multiplication circuit composed of a DAC IC and an operational amplifier as shown in Fig. 4, and one input terminal has the above-mentioned
Apply the SIN wave DIGITAL signal, add the above-mentioned double-wave rectified wave b of the azimuth signal to the other input terminal, multiply both inputs, create an analog output as shown in Figure 7j, and send this to the semiconductor switch. through 83
Input to ADC84. The ADC84 starts conversion at the rising edge of the SC (start conversion) signal,
At the end of conversion, an EOC (end of convergence) signal is generated, which turns on the semiconductor switch and applies the multiplication circuit output (Fig. 7j) to the input terminal of the ADC. The above SC sequentially switches the antennas arranged on the circumference and takes the time to make one rotation as T=1/fa (fa: frequency of one antenna rotation), and if the number of antennas is n, then T/n=1/nfa. Use periodic pulses.
つまり第1図ハの方位信号の振幅の変化が急峻
でない平坦部分の値をAD変換するのである。な
おAD変換が開始されると同時にEOC信号が
“L”になり、半導体スイツチ83を断として変
換中にはデーターが変化しないようにする。AD
変換された複数ビツトの出力はラツチ回路85に
ラツチした後次の回路に転送される。 In other words, the value of the flat portion in which the amplitude of the azimuth signal shown in FIG. Note that at the same time as the AD conversion is started, the EOC signal becomes "L" and the semiconductor switch 83 is turned off so that the data does not change during the conversion. A.D.
The converted multi-bit output is latched in a latch circuit 85 and then transferred to the next circuit.
86はエクスクルーシブオアゲート
(EXCLUSIVE OR GATE)で方位信号bと同
期した矩形波cと内部信号の最上ビツト、つまり
プリセツタブルアツプダウンカウンタ811の最
上ビツト出力dを入力として、第7図kの極性信
号を出力し、前述のラツチ回路85の出力と一諸
に次のDIGITAL平均回路9に転送する。 86 is an EXCLUSIVE OR GATE which inputs a rectangular wave c synchronized with the azimuth signal b and the uppermost bit of the internal signal, that is, the uppermost bit output d of the presettable up-down counter 811, and calculates the polarity shown in FIG. 7 k. The signal is output and transferred together with the output of the latch circuit 85 described above to the next DIGITAL averaging circuit 9.
9はメモリを持つたDIGITAL平均回路で、8
の位相比較回路出力を入力として極性信号kにじ
て第7図jの波形の面積を積算平均する。この平
均結果を一時的に平均回路内のメモリに記憶し
て、これを前記位相比較回路のプリセツタブルア
ツプダウンバイナリカウンタ811のプリセツト
入力F4として加えて、プリセツタブルアツプダ
ウンバイナリカウンタの出力信号の位相を進め又
は遅らせて方位信号と内部信号の位相差が互に
90゜になるようにじよじよ位相を動かし、最終的
にjの波形が対称、つまり1周期の積算結果が0
になる迄制御し安定する。 9 is a DIGITAL averaging circuit with memory, 8
The area of the waveform shown in FIG. 7j is cumulatively averaged according to the polarity signal k using the output of the phase comparator circuit of FIG. This average result is temporarily stored in the memory in the averaging circuit, and is added as the preset input F4 of the presettable up-down binary counter 811 of the phase comparator circuit to output the output signal of the presettable up-down binary counter. By advancing or delaying the phase of the direction signal and the internal signal, the phase difference between the direction signal and the internal signal is
Gradually move the phase so that it becomes 90°, and finally the waveform of j is symmetrical, that is, the integration result for one period is 0.
It is controlled until it becomes stable.
プリセツトした数値は前述のように一時的にメ
モリに積算記憶してあるので、その総和は内部信
号を基準点N、つまり、基準方位に対応する位相
点から方位信号と90゜の位相差をもつ位相点まで
移相し終えるまでの移相量に相当するものであ
り、結局、基準方位からの電波の到来方位とな
る。これを表示器12に転送し適当な表示周期に
従つて表示せしめるのである。11は振幅比較
器、10はメモリで電波の仰角に対する振幅m,
m′、及び電波発射源迄の距離Qのデータを記憶
する。受信した電波の方位信号の振幅m′を測定
し、メモリに記憶してあるmとにより仰角βの大
きさをその都度計算して求めるのは計算装置を必
要としたり又計算に時間がかるなど実際的でな
い。又仰角βと基準の振幅mと測定した振幅
m′とには第(4)式の関係があるのは前述の通りで
あるが、電離層の高さそのものが大きな広がりを
持つたものであり、又その状態は常に変化してい
るものであるからβをあまりこまかく求めて見て
も意味がないので数度おきに求めるのが実際的で
ある。 As mentioned above, the preset values are temporarily accumulated and stored in the memory, so the summation is the internal signal that has a phase difference of 90° from the azimuth signal from the reference point N, that is, the phase point corresponding to the reference azimuth. This corresponds to the amount of phase shift until the phase shift reaches the phase point, and ultimately becomes the arrival direction of the radio wave from the reference direction. This is transferred to the display 12 and displayed according to an appropriate display cycle. 11 is an amplitude comparator, and 10 is a memory that measures the amplitude m for the elevation angle of the radio wave,
m' and the distance Q to the radio wave emission source are stored. Measuring the amplitude m' of the direction signal of the received radio wave and calculating the magnitude of the elevation angle β each time using m stored in memory requires a calculation device and is time-consuming. Not on point. Also, the elevation angle β, the reference amplitude m, and the measured amplitude
As mentioned above, there is a relationship between m' and equation (4), but the height of the ionosphere itself has a large spread, and its state is constantly changing. Since there is no point in calculating and looking at β in too much detail, it is practical to calculate it every few degrees.
従つて仰角0度の時の振幅値mをある値、例え
ば2560mV(10進)と定めるとrは既知であるか
ら本発明の実施例ではhをある値、例えば300Km
として角βに対する振幅m′及び距離Qを計算す
ると第9図のデータ値が得られるので、これを前
記メモリ10に第9図メモリ配置に示したように
各アドレスごとに記憶しておく。 Therefore, if the amplitude value m when the elevation angle is 0 degrees is set to a certain value, for example 2560 mV (decimal), r is already known, so in the embodiment of the present invention, h is set to a certain value, for example 300 Km.
By calculating the amplitude m' and distance Q for the angle β, the data values shown in FIG. 9 are obtained, and these are stored in the memory 10 for each address as shown in the memory arrangement in FIG.
電波を測定し方位信号が得られるとその方位信
号の振幅m′と、第9図のメモリ配置に従つてメ
モリ10に記憶されたm′を順次振幅比較回路に
読出して電波を受信して得られた方位信号の振幅
m′と比較してその値が一致又は一番近い時のβ
及びQが電離層高さ300Kmの時の仰角及び電波発
射源迄の距離である。例を示せば今電波を受信し
た時の方位信号の振幅が2557mVだつたとすれ
ば、第9図のデータ値のm′の値を順々に比較す
ると2番目のm′=2558mVに最も近いのでこの時
の仰角及び距離はβ=0002度、Q=3838Kmとなり
これを読出し次の表示器12に転送し、電波の到
来方位仰角及び電波発射源迄の距離を同時に瞬間
的に表示せしめるのである。 When a radio wave is measured and a direction signal is obtained, the amplitude m' of the direction signal and m' stored in the memory 10 according to the memory arrangement shown in FIG. amplitude of the direction signal
β when the value matches or is closest compared to m′
and Q is the elevation angle and distance to the radio wave emission source when the ionosphere height is 300 km. For example, if the amplitude of the direction signal when the radio wave was just received was 2557 mV, then if we compare the m' values of the data values in Figure 9 in order, we will find the one closest to the second m' = 2558 mV. Therefore, the elevation angle and distance at this time are β = 0002 degrees and Q = 3838 km, which are read out and transferred to the next display 12, which instantly displays the arrival direction and elevation angle of the radio wave and the distance to the radio wave emission source at the same time. .
次に総合動作を説明する。 Next, the overall operation will be explained.
アンテナA1〜Aoで受信した出力は、アンテナ
走査基準信号発生回路2より得られた切替信号に
よりアンテナ切替走査回路3で各アンテナを順次
に切替えて2チヤンネル受信機4の一方のRF入
力へ、又補助アンテナA0の出力は他方のRF入力
端子にそれぞれ加えて増幅し、そのIF出力を方
位信号検出回路5の入力にそれぞれ加える。 The outputs received by the antennas A1 to Ao are sent to one RF input of the two-channel receiver 4 by sequentially switching each antenna in the antenna switching scanning circuit 3 using the switching signal obtained from the antenna scanning reference signal generation circuit 2. , and the outputs of the auxiliary antenna A0 are respectively applied to the other RF input terminals and amplified, and the IF outputs thereof are applied to the inputs of the azimuth signal detection circuit 5, respectively.
二つのIF入力を周波数変換し電波に与えられ
ている周波数変調成分を除去し、アンテナ回転に
よる変調成分のみとした後周波数弁別回路により
方位信号を抽出する。 The two IF inputs are frequency-converted to remove the frequency modulation components given to the radio waves, leaving only the modulation components due to antenna rotation, and then the azimuth signal is extracted by a frequency discrimination circuit.
この信号は周波数に比例してその振幅が増加す
るので、次の周波数補正回路6を通して周波数情
報F1により周波数に無関係に常に一定振幅の出
力が得られる。この信号の一部を増幅して第7図
cの矩形波信号とし又他の一部を両波整流回路7
により両波整流した第7図bの方位信号と共に位
相比較回路8に加える。 Since the amplitude of this signal increases in proportion to the frequency, an output with a constant amplitude is always obtained regardless of the frequency using the frequency information F1 through the next frequency correction circuit 6. A part of this signal is amplified to form the rectangular wave signal shown in FIG.
The signal is applied to the phase comparator circuit 8 along with the azimuth signal shown in FIG.
この方位信号bとプリセツタブルアツプダウン
バイナリカウンタ811、およびSINROM81
2で得られた第7図eの信号を掛算回路82によ
り掛算すれば第7図jのようなアナログ積出力が
得られる。 This direction signal b, presettable up-down binary counter 811, and SINROM 81
If the signal shown in FIG. 7e obtained in step 2 is multiplied by the multiplication circuit 82, an analog product output as shown in FIG. 7j can be obtained.
このプリセツタブルアツプダウンバイナリカウ
ンタのプリセツト入力には次のDIGITAL平均回
路より必要な数値F4がプリセツトされ、内部信
号出力の位相を前後に進み遅れするように制御す
る。 A necessary value F4 is preset from the next DIGITAL averaging circuit to the preset input of this presettable up-down binary counter, and the phase of the internal signal output is controlled to advance or lag forward or backward.
掛算回路82の出力はADC回路84により
DIGITAL値として前述した極性信号第7図kと
共に平均回路に加えて極性信号の符号に従つて、
1周期又は数周期間積算し平均する。 The output of the multiplication circuit 82 is output by the ADC circuit 84.
According to the sign of the polarity signal in addition to the average circuit along with the polarity signal (Fig. 7k) described above as the DIGITAL value,
Accumulate and average over one cycle or several cycles.
今、第7図jの,,,の各区間の面積
を=A1,=A2,=A1,=A2とすれば、
各区間の面積を極性信号kに応じて和と差を取れ
ば
+++=2(A1−A2) ……(9)
−+−=2(A1+A2) ……(10)
となり(9)式は第7図jの面積の差すなわち位相誤
差成分であり、(10)式は面積の総和つまり平均の振
幅値となるのである。 Now, if the areas of the sections , , in Fig. 7j are =A 1 , =A 2 , =A 1 , =A 2 , then
If we take the sum and difference of the area of each section according to the polarity signal k, we get +++=2(A 1 −A 2 ) ...(9) −+−=2(A 1 +A 2 ) ...(10) ( Equation 9) is the area difference in FIG. 7j, that is, the phase error component, and Equation (10) is the sum of the areas, that is, the average amplitude value.
従つて方位信号a−Vと内部信号e−Vが完全
に90゜位相差の時には、面積A1とA2は等しいので
(9)式の結果は零となり、内部信号の位相もその点
で安定化し基準Nからの位相θ0となる。 Therefore, when the azimuth signal a-V and the internal signal e-V have a completely 90° phase difference, the areas A1 and A2 are equal, so
The result of equation (9) becomes zero, and the phase of the internal signal also stabilizes at that point, becoming the phase θ 0 from the reference N.
ここで方位信号がa−Uのように変化した瞬間
には内部信号d,eの位相は末だ制御されていな
いので、元のままつまりd−V,e−Vであるか
ら掛算回路82の出力は方位信号b−Uと内部信
号e−Vとの積であるからfのような信号とな
り、EXCLUSIVE OR GATEの出力つまりc−
Uとd−Vとの積はgのようになる。又方位信号
がa−Wのように変化した場合には方位が変化し
た瞬間には前述の理由により掛算回路の出力及び
EXCLUSIVE OR GATEの出力はh,iのよう
になる。 At the moment when the azimuth signal changes like a-U, the phases of internal signals d and e are not controlled at all, so they remain as they were, that is, d-V, e-V, so the multiplication circuit 82 Since the output is the product of the azimuth signal b-U and the internal signal e-V, it becomes a signal like f, which is the output of EXCLUSIVE OR GATE, that is, c-
The product of U and d-V is g. Also, when the azimuth signal changes like a-W, at the moment the azimuth changes, the output of the multiplication circuit and
The output of EXCLUSIVE OR GATE becomes h, i.
この出力を次の平均回路9により1周期又は数
周期間積算し、平均すると方位信号がa−Uの場
合にはfの信号を積算するのでその平均値は
(−)となり、又方位信号がa−Wの場合にはh
の信号を積算するのでその平均値は(+)とな
る。 This output is integrated by the next averaging circuit 9 for one cycle or several cycles, and when averaged, if the azimuth signal is a-U, the signal of f is integrated, so the average value becomes (-), and the azimuth signal is h in case of a-W
Since the signals are integrated, the average value is (+).
この平均値を前述したプリセツタブルアツプダ
ウンバイナリカウンタのプリセツト入力端子に加
え、基準Nの時点でプリセツトして分周を行う
と、その出力の位相はプリセツト値分だけ前後に
変化する。 When this average value is added to the preset input terminal of the presettable up-down binary counter described above and preset at the time of reference N and frequency division is performed, the phase of the output changes back and forth by the preset value.
第8図はプリセツタブルアツプダウンバイナリ
カウンタのプリセツト入力とカウンタ出力の関係
を示す説明図である。1はプリセツタブルアツプ
ダウンカウンタの出力の総和を示し、最大点がカ
ウンタが最大になつたことを示しておりカウンタ
の総和が順次減少し最小点でカウンタの内容が0
になつたことを、又2〜4はカウンタの最大ビツ
ト出力を示している。 FIG. 8 is an explanatory diagram showing the relationship between the preset input and counter output of the presettable up-down binary counter. 1 indicates the total sum of the output of the presettable up-down counter, and the maximum point indicates that the counter has reached the maximum, and the total sum of the counter decreases sequentially until the minimum point is when the contents of the counter become 0.
2 to 4 indicate the maximum bit output of the counter.
今方位信号が第7図a−Vの状態で内部信号が
前記方位信号と丁度90゜位相差e−Vに制御され
ていたとするとNの時点で平均回路9で積算した
結果によりプリセツトする数値F4をθ0としてプ
リセツトすればプリセツトバイナリーカウンタの
最大出力ビツトの波形は第8図2のようになる。 If the current azimuth signal is in the state shown in Figure 7 a-V and the internal signal is controlled to have a phase difference e-V of exactly 90 degrees from the azimuth signal, then at time N, the preset value F4 is determined by the result of integration by the averaging circuit 9. If it is preset as θ 0 , the waveform of the maximum output bit of the preset binary counter will be as shown in FIG. 8.
次に方位信号が第7図a−Uのように変化した
とすれば、内部信号e−Vは末だ制御されていな
いので、方位信号b−Uと内部信号e−Vの積出
力及びEXCLUSIV OR GATE86の出力、つ
まり第7図のcとdの積出力である極性信号はそ
れぞれf,gとなり、fの面積をgの極性信号に
応じて積算し平均すると結局(−)分が残るの
で、これを前述のメモリに積算しこの合計のθ1を
プリセツタブルアツプダウンカウンタにNの時点
でプリセツトを行う。その結果カウンターの出力
は第8図1の曲線Uのようになりカウンタの最大
出力ビツトは、第8図3のように位相がじよじよ
に遅れて最終的には第7図d−U,e−U,j−
U,k−Uとなり、最初の時点よりΔθだけ位相
が遅れ基準Nよりθ1の点で安定する。 Next, if the azimuth signal changes as shown in Figure 7 a-U, the internal signal e-V is not controlled at all, so the product output of the azimuth signal b-U and internal signal e-V and EXCLUSIV The output of OR GATE 86, that is, the polarity signal which is the product output of c and d in Figure 7, becomes f and g, respectively, and if the area of f is integrated and averaged according to the polarity signal of g, the (-) portion will remain. , this is accumulated in the memory mentioned above, and this total θ1 is preset in the presettable up-down counter at time N. As a result, the output of the counter becomes as shown by curve U in Fig. 8 1, and the maximum output bit of the counter gradually lags in phase as shown in Fig. 8 3, and finally reaches d-U, e in Fig. 7. -U,j-
U, k-U, and the phase is delayed by Δθ from the initial point and stabilizes at the point θ 1 from the reference N.
次に方位信号がa−Wとなつた時は同様動作に
よりΔθだけ位相が進み基準Nからθ2の点で安定
する。このように内部信号d,eの位相は方位信
号の位相に追随することになり、プリセツト値F
4の総和が到来電波の方位となる。 Next, when the azimuth signal becomes a-W, the phase advances by Δθ by the same operation and becomes stable at a point θ 2 from the reference N. In this way, the phase of internal signals d and e follows the phase of the azimuth signal, and the preset value F
The sum of 4 is the direction of the incoming radio wave.
電波の到来方向が求められると次の時点で前述
の(10)式の積算、つまり区間〜の総和を求め方
位信号の振幅m′を求める。このm′を前述したよ
うにメモリ10の内容と比較してその値が一致又
は1番近い値の時の仰角、電波発射源迄の距離を
読出し方位指示器12により瞬間的に方位仰角距
離を表示するのである。 Once the direction of arrival of the radio wave is determined, the amplitude m' of the azimuth signal is determined at the next point in time by calculating the integration of equation (10), that is, the sum of the sections . As described above, this m' is compared with the contents of the memory 10, and when the values match or are the closest value, the elevation angle and the distance to the radio wave emission source are read out and the azimuth/elevation angle/distance is instantaneously determined by the azimuth indicator 12. It is displayed.
普通電離層の高さは送信機から持続時間の短い
インパルス波を一定間隔(例えば1/50(SEC))
で垂直上方に発射し近傍の受信機で直接波と電離
層反射波との時間差をオシロスコープで測定する
のが普通であるが、この値は電離層の平均値であ
る。電離層の幅は一般的には100Km以上にもおよ
ぶ比較的広い幅を持ちこれが時々刻々と変化する
ものである。従つて電離層の高さをあまりこまか
く区切つて測定することは無意味である。 Normally, the height of the ionosphere is determined by transmitting short-duration impulse waves from a transmitter at regular intervals (for example, 1/50 (SEC)).
Normally, the time difference between the direct wave and the reflected wave from the ionosphere is measured using an oscilloscope by emitting it vertically upward and using a nearby receiver to measure the time difference between the direct wave and the reflected wave from the ionosphere, but this value is the average value for the ionosphere. The width of the ionosphere is relatively wide, generally over 100 km, and this width changes from moment to moment. Therefore, it is meaningless to measure the height of the ionosphere in too small sections.
電離層の高さは普通100Km〜500Kmと言われてい
るので、100Km単位で測定したも充分であるから
地上から500Km位迄の間を100Km単位で区切り、そ
れぞれの電離層について計算した第9図のデータ
値及びメモリ配置を作成しこの値を記憶回路10
に記憶させ必要な電離層高さを入力して、その電
離層高さに相当する記憶回路の内容を検索照合し
読み出して指示させるのが実際的である。 The height of the ionosphere is usually said to be between 100km and 500km, so it would be sufficient to measure it in units of 100km, so the data in Figure 9 was calculated for each ionosphere by dividing the range from the ground to about 500km in units of 100km. Create a value and memory arrangement and store this value in the memory circuit 10.
It is practical to input the necessary ionospheric height, search and collate the contents of the memory circuit corresponding to the ionospheric height, read out the contents, and instruct the user.
具体的にはアンテナの近傍から小型発振器によ
り電波を発射して受信し、その時の方位信号の振
幅を基準値mつまり本実施例では2560mVに合せ
るだけでよく調整も極めて簡単である。なおこの
基準値mはADC84が飽和しない範囲で自由に
選定出来る。 Specifically, the adjustment is extremely simple, as it only requires emitting and receiving radio waves from near the antenna using a small oscillator, and adjusting the amplitude of the azimuth signal at that time to the reference value m, that is, 2560 mV in this embodiment. Note that this reference value m can be freely selected within a range in which the ADC 84 is not saturated.
又第3図の6以降の信号処理を特別の関数発生
器を用いてアナログ的に行うことも可能である
が、デジタル化した上でデジタルマイクロコンピ
ユータ等を用いて行うのが実際的である。 It is also possible to perform the signal processing after 6 in FIG. 3 in an analog manner using a special function generator, but it is more practical to digitize the signal and perform it using a digital microcomputer or the like.
本発明によれば、以上のように、 静止形ドツ
プラ方式の無線方向探知方法を用いるものにおい
て、
a 予め地平面に水平に電波が伝播してきた場合
の方位信号の振幅を知つておき、方位信号の振
幅値を計測する機能と演算機能を付加するだけ
で、電波の入射角と発射地点までの距離を測定
できるようになるので、測定方法がきわめて簡
単である。
According to the present invention, as described above, in a method using a stationary Doppler wireless direction finding method, a) the amplitude of the direction signal when radio waves propagate horizontally to the ground is known in advance; The measurement method is extremely simple, as the angle of incidence of the radio wave and the distance to the emission point can be measured simply by adding a function to measure the amplitude value and a calculation function.
b 方位信号の振幅値に対応して入射角と距離を
記憶したメモリを設けだけで、演算機能が不要
なごく簡単な構成のものを提供できる。b. By simply providing a memory that stores the angle of incidence and distance in correspondence with the amplitude value of the azimuth signal, an extremely simple configuration that does not require arithmetic functions can be provided.
c 広い周波数の電波を方向探知するものでは、
方位信号の振幅を周波数に逆比例して大きくす
る機能を設けるだけで、入射角と距離の精度を
確保し得るものを提供できる。c. For direction finding using wide frequency radio waves,
By simply providing a function to increase the amplitude of the azimuth signal in inverse proportion to the frequency, it is possible to provide something that can ensure the accuracy of the incident angle and distance.
などの特長がある。It has the following features.
第1図イはアンテナの配置を示す図、ロは仰角
βで電波が到来する様子を示す図、ハはアンテナ
を切替受信して生じた位相変化成分を示す波形図
である。第2図は電離層反射による電波の仰角の
説明図、第3図は本発明の1実施例を示す系統
図、第4図はDAC(DIGITAL TO ANALOG
CONVERTER)の回路例を、第5図は本発明に
よる周波数補正回路の1実施例を示す。第6図は
位相比較回路の詳細説明図、第7図、第8図は各
部の動作波形図を示す。第9図は仰角に対する振
幅m′及び電波発射源迄の距離を計算したデータ
値とこの結果を記憶回路に記憶させるためのアド
レス配置を示す。
1:アンテナ群、2:アンテナ走査基準信号発
生回路、3:アンテナ切替走査回路、4:受信
機、5:方位信号検出回路、6:周波数補正回
路、7:両波整流回路、8:位相比較回路、9:
DIGITAL平均回路、10:記憶回路、11:振
幅比較回路、12:方位指示器、F1:受信周波
数デジタル信号、F2:ADC用ICの端子の信
号、F3:ADC用ICの端子の信号、F4:プ
リセツタブルアツプダウンカウンタ811へのプ
リセツト数値、D:アンテナ直径、N:基準(真
北)D′:実効アンテナ直径、β:到来電波の大
地に対する仰角(入射角)、r:地球の半径(約
6387Km)、O:地球の中心点、h:電離層の高さ、
S:電波発射点、R:電波受信点、Y:電波発射
点Sと電波受信点Rをかこむ角、P:地球表面、
Q:円弧S・Rの距離、m:変調指数。
FIG. 1A is a diagram showing the arrangement of antennas, B is a diagram showing how radio waves arrive at an elevation angle β, and C is a waveform diagram showing a phase change component generated by switching antennas for reception. Fig. 2 is an explanatory diagram of the elevation angle of radio waves due to ionospheric reflection, Fig. 3 is a system diagram showing one embodiment of the present invention, and Fig. 4 is a DAC (DIGITAL TO ANALOG) diagram.
FIG. 5 shows an example of a frequency correction circuit according to the present invention. FIG. 6 is a detailed explanatory diagram of the phase comparator circuit, and FIGS. 7 and 8 are operational waveform diagrams of each part. FIG. 9 shows the calculated data values of the amplitude m' with respect to the elevation angle and the distance to the radio wave emission source, and the address arrangement for storing the results in the memory circuit. 1: Antenna group, 2: Antenna scanning reference signal generation circuit, 3: Antenna switching scanning circuit, 4: Receiver, 5: Direction signal detection circuit, 6: Frequency correction circuit, 7: Double wave rectification circuit, 8: Phase comparison Circuit, 9:
DIGITAL averaging circuit, 10: Memory circuit, 11: Amplitude comparison circuit, 12: Direction indicator, F1: Reception frequency digital signal, F2: ADC IC terminal signal, F3: ADC IC terminal signal, F4: Preset value to presettable up-down counter 811, D: Antenna diameter, N: Reference (true north) D': Effective antenna diameter, β: Elevation angle (incident angle) of incoming radio waves relative to the ground, r: Radius of the earth ( about
6387Km), O: center point of the earth, h: height of the ionosphere,
S: radio wave emitting point, R: radio wave receiving point, Y: angle surrounding radio wave emitting point S and radio wave receiving point R, P: earth surface,
Q: Distance of arc S/R, m: Modulation index.
Claims (1)
順次に切替えて走査しながら電波を受信して受信
信号を得るとともに、前記切替えによつて生じた
前記受信信号中の位相変化により前記電波の到来
方向に関連づけられてSIN波状に変化する成分
(以下、SIN波状変化成分という)をもつ信号を
方位信号として得ることにより、前記方位信号に
もとづいて前記電波の到来方向を探知するととも
に前記到来方向にもとづいて前記電波の発射点の
位置を計測する無線方向距離測定方法(以下、方
法という)であつて、 a 前記方位信号に含まれる前記SIN波状変化成
分の振幅を計測した値を計測振幅値m′として
得る振幅計測と、 b 前記電波が地平面を伝播して到来した場合に
得られるべき前記計測振幅値m′に相当する振
幅値(以下、相当振幅値という)mを作成する
相当振幅値作成と、 c 前記計測振幅値m′と前記相当振幅値mとに
より、 m′/m=cosβ の関係式にもとづいて、前記地平面に垂直な面
内における前記電波の到来角度(以下、到来入
射角という)βを得る垂直面内到来角測定と、 d 電離層の高さhと地球半径rと前記到来入射
角βとにより、 2{cos-1〔r/r+hcosβ〕−β}r=Q の関係式にもとづいて前記無指向性アンテナの
設置地点から前記電波の発射点までの距離Qを
算定する発射点演算と を具備することを特徴とする方法。 2 円周上に等間隔配置した無指向性アンテナを
順次に切替えて走査しながら電波を受信して受信
信号を得るとともに、前記切替えによつて生じた
前記受信信号中の位相変化により前記電波の到来
方向に関連づけられてSIN波状に変化する成分
(以下、SIN波状変化成分という)をもつ信号を
方位信号として得ることにより、前記方位信号に
もとづいて基準方位に対する前記電波の到来方向
を探知するとともに前記到来方向にもとづいて前
記電波の発射点の位置を計測する無線方向距離計
測装置(以下、装置という)であつて、 a 前記方位信号に含まれる前記SIN波状変化成
分の振幅を計測した値を計測振幅値m′の信号
を計測振幅値信号として得る振幅計測手段と、 b 前記電波が地平面を伝播して到来した場合に
得られるべき前記計測振幅値m′に相当する振
幅値(以下、相当振幅値という)mと、前記計
測振幅値m′とにより、 m′/m=cosβ の関係式にもとづいて算定した前記地平面に垂直
な面内における前記電波の到来角度(以下、到来
入射角という)βと、電離層の高さhと地球半径
rとにより、 2{cos-1〔r/r+hcosβ〕−β}r=Q の関係式にもとづいて算定した前記無指向性アン
テナの設置地点から前記電波の発射点までの距離
Qとのデータのうちから、前記計測振幅値m′と
前記到来入射角βと前記距離Qとの各算定値を対
応させて記憶する振幅対応角度距離距離手段と、 c 前記計測振幅値信号にもとづく読出信号によ
つて、前記記憶のうちから前記計測振幅値
m′に対応する記憶内容を読み出すことにより、
前記距離値Qの信号または前記到来入射角βと
前記距離値Qとの信号を計測読出信号として得
る計測読出手段と を具備することを特徴とする装置。 3 円周上に等間隔配置した無指向性アンテナを
順次に切替えて走査しながら電波を受信して受信
信号を得るとともに、前記切替えによつて生じた
前記受信信号中の位相変化により前記電波の到来
方向に関連づけられてSIN波状に変化する成分
(以下、SIN波状変化成分という)をもつ信号を
方位信号として得ることにより、前記方位信号に
もとづいて基準方位に対する前記電波の到来方向
を探知するとともに前記到来方向にもとづいて前
記電波の発射点の位置を計測する無線方向距離計
測装置(以下、装置という)であつて、 a 前記方位信号を前記電波の周波数にもとづい
て得られる信号によつて前記SIN波状変化成分
の振幅を前記周波に逆比例して増加する補正を
行つた信号を補正方位信号として得る振幅補正
手段と、 b 前記補正方位信号に含まれる前記SIN波状変
化成分の振幅を計測した値を計測振幅値m′の
信号を計測振幅値信号として得る振幅計測手段
と、 c 前記電波が地平面を伝播して到来した場合に
得られるべき前記計測振幅値m′に相当する振
幅値(以下、相当振幅値という)mと、前記計
測振幅値m′とにより、 m′/m=cosβ の関係式にもとづいて算定した前記地平面に垂
直な面内における前記電波の到来角度(以下、
到来入射角という)βと、電離層の高さhと地
球半径rとにより、 2{cos-1〔r/r+hcosβ〕−β}r=Q の関係式にもとづいて算定した前記無指向性ア
ンテナの設置地点から前記電波の発射点までの
距離Qとのデータのうちから、前記計測振幅値
m′と前記到来入射角βと前記距離Qとの各算
定値を対応させて記憶する振幅対応角度距離距
離手段と、 d 前記計測振幅値信号にもとづく読出信号によ
つて、前記記憶のうちから前記計測振幅値
m′に対応する記憶内容を読み出すことにより、
前記距離値Qの信号または前記到来入射角βと
前記距離値Qとの信号を計測読出信号として得
る計測読出手段と を具備することを特徴とする装置。[Scope of Claims] 1. Omnidirectional antennas arranged at equal intervals on the circumference are sequentially switched and scanned while receiving radio waves to obtain a received signal, and the received signal generated by the switching is By obtaining a signal having a SIN wave-like component (hereinafter referred to as a SIN wave-like change component) that is related to the direction of arrival of the radio wave due to a phase change as an azimuth signal, the direction of arrival of the radio wave can be determined based on the azimuth signal. A radio direction distance measuring method (hereinafter referred to as the method) for detecting and measuring the position of the emission point of the radio wave based on the direction of arrival, the method comprising: a) measuring the amplitude of the SIN waveform change component included in the direction signal; (b) An amplitude value corresponding to the measured amplitude value m' that should be obtained when the radio wave propagates through the horizon (hereinafter referred to as equivalent amplitude value); c. Create an equivalent amplitude value to create m, and c. From the measured amplitude value m' and the equivalent amplitude value m, based on the relational expression m'/m=cosβ, the radio wave in a plane perpendicular to the horizon 2 {cos -1 [r/r+hcosβ ]-β}r=Q A method comprising: calculation of a distance Q from the installation point of the omnidirectional antenna to the emission point of the radio wave based on the relational expression: -β}r=Q. 2. Omnidirectional antennas arranged at equal intervals on the circumference are sequentially switched and scanned to receive radio waves to obtain a received signal, and the phase change in the received signal caused by the switching causes the radio waves to change. By obtaining a signal having a component that changes like a SIN wave in association with the direction of arrival (hereinafter referred to as a SIN wave change component) as a direction signal, the direction of arrival of the radio wave relative to a reference direction is detected based on the direction signal, and A wireless direction distance measuring device (hereinafter referred to as the device) that measures the position of the emission point of the radio wave based on the direction of arrival, comprising: a) measuring the amplitude of the SIN waveform change component included in the azimuth signal; an amplitude measuring means for obtaining a signal of the measured amplitude value m' as a measured amplitude value signal; b. an amplitude value corresponding to the measured amplitude value m' that should be obtained when the radio wave propagates through the horizon The arrival angle of the radio wave in a plane perpendicular to the horizon (hereinafter referred to as the arrival incident angle) is calculated based on the relational expression m'/m=cosβ using The installation point of the omnidirectional antenna is calculated based on the relational expression: 2 {cos -1 [r/r + hcos β] - β} r = Q, using the angle (referred to as angle) β, the height h of the ionosphere and the radius r of the earth. amplitude-corresponding angle-distance-distance means for storing calculated values of the measured amplitude value m', the arrival angle of incidence β, and the distance Q in correspondence with each other from among the data of the distance Q from to the emission point of the radio wave; and c. The measured amplitude value is retrieved from the memory by a readout signal based on the measured amplitude value signal.
By reading the memory contents corresponding to m′,
An apparatus characterized by comprising measurement readout means for obtaining a signal of the distance value Q or a signal of the arrival angle of incidence β and the distance value Q as a measurement readout signal. 3 Omnidirectional antennas placed at equal intervals on the circumference are sequentially switched and scanned to receive radio waves to obtain a received signal, and the phase change in the received signal caused by the switching causes the radio waves to be By obtaining a signal having a component that changes like a SIN wave in association with the direction of arrival (hereinafter referred to as a SIN wave change component) as a direction signal, the direction of arrival of the radio wave relative to a reference direction is detected based on the direction signal, and A radio direction distance measuring device (hereinafter referred to as the device) that measures the position of the emission point of the radio wave based on the direction of arrival, comprising: a) detecting the direction signal by using a signal obtained based on the frequency of the radio wave; an amplitude correction means for obtaining a corrected azimuth signal, a signal in which the amplitude of the SIN wave-like change component is increased in inverse proportion to the frequency; b) measuring the amplitude of the SIN wave-like change component included in the corrected azimuth signal; c) an amplitude measuring means for obtaining a signal with a measured amplitude value m' as a measured amplitude value signal; The arrival angle of the radio wave in a plane perpendicular to the horizon (hereinafter referred to as the equivalent amplitude value) and the measured amplitude value m' is calculated based on the relational expression m'/m=cosβ (hereinafter referred to as the equivalent amplitude value).
of the omnidirectional antenna, which is calculated based on the relational expression 2{cos -1 [r/r + hcos β] - β} r = Q, using the ionosphere height h and the earth's radius r. The measured amplitude value is determined from among the data regarding the distance Q from the installation point to the emission point of the radio wave.
an amplitude-corresponding angle-distance means for storing the calculated values of m', the arrival angle of incidence β, and the distance Q in correspondence; d. The measured amplitude value
By reading the memory contents corresponding to m′,
An apparatus characterized by comprising measurement readout means for obtaining a signal of the distance value Q or a signal of the arrival angle of incidence β and the distance value Q as a measurement readout signal.
Priority Applications (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP1293798A JPH02167486A (en) | 1989-11-13 | 1989-11-13 | Radio direction and distance detecting device |
Applications Claiming Priority (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP1293798A JPH02167486A (en) | 1989-11-13 | 1989-11-13 | Radio direction and distance detecting device |
Related Parent Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| JP25221683A Division JPS60143793A (en) | 1983-12-29 | 1983-12-29 | Radio direction finder |
Publications (2)
| Publication Number | Publication Date |
|---|---|
| JPH02167486A JPH02167486A (en) | 1990-06-27 |
| JPH0429030B2 true JPH0429030B2 (en) | 1992-05-15 |
Family
ID=17799296
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| JP1293798A Granted JPH02167486A (en) | 1989-11-13 | 1989-11-13 | Radio direction and distance detecting device |
Country Status (1)
| Country | Link |
|---|---|
| JP (1) | JPH02167486A (en) |
-
1989
- 1989-11-13 JP JP1293798A patent/JPH02167486A/en active Granted
Also Published As
| Publication number | Publication date |
|---|---|
| JPH02167486A (en) | 1990-06-27 |
Similar Documents
| Publication | Publication Date | Title |
|---|---|---|
| US8204707B2 (en) | Time delay estimation | |
| US4975710A (en) | Methods and apparatus for direction of arrival measurement and radio navigation aids | |
| US5184135A (en) | Phase measurement of received pseudonoise sequence using digital correlation | |
| Poole | Advanced sounding: 1. The FMCW alternative | |
| EP0458148B1 (en) | Angle of rotation detector | |
| JPH0146835B2 (en) | ||
| JP3808431B2 (en) | Direction finding device | |
| JPH0349075B2 (en) | ||
| Kurniawan et al. | Implementation of automatic I/Q imbalance correction for FMCW radar system | |
| JPH0429029B2 (en) | ||
| JPH0720583U (en) | Wireless direction finder | |
| JPH02167486A (en) | Radio direction and distance detecting device | |
| US6952175B2 (en) | Phase digitizer for signals in imperfect quadrature | |
| RU2165628C1 (en) | Phase direction finder | |
| JPS6316280A (en) | Radio direction finder | |
| JPH0726858B2 (en) | Signal processing circuit for encoder | |
| KR102538624B1 (en) | Method of measuring phase difference for frequency measurement and interferometer direction finding and wideband digital receiver including the same | |
| RU2206901C1 (en) | Phase direction finder | |
| RU2426143C1 (en) | Method of phase direction finding and phase direction finder to this end | |
| JP2001255361A (en) | Direction measurement device | |
| JP2839406B2 (en) | Direction measurement device | |
| JP3404526B2 (en) | Direction finding receiver | |
| JPH06118154A (en) | Direction detector | |
| RU2311656C1 (en) | Phase method for direction finding | |
| RU2346289C1 (en) | Radio reconnaissance station |