JPS6027883A - Approach of thunderbolt detection system - Google Patents
Approach of thunderbolt detection systemInfo
- Publication number
- JPS6027883A JPS6027883A JP13559083A JP13559083A JPS6027883A JP S6027883 A JPS6027883 A JP S6027883A JP 13559083 A JP13559083 A JP 13559083A JP 13559083 A JP13559083 A JP 13559083A JP S6027883 A JPS6027883 A JP S6027883A
- Authority
- JP
- Japan
- Prior art keywords
- thunderbolt
- electric field
- approach
- cloud
- negative
- Prior art date
- Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
- Pending
Links
- 238000001514 detection method Methods 0.000 title claims description 4
- APTZNLHMIGJTEW-UHFFFAOYSA-N pyraflufen-ethyl Chemical compound C1=C(Cl)C(OCC(=O)OCC)=CC(C=2C(=C(OC(F)F)N(C)N=2)Cl)=C1F APTZNLHMIGJTEW-UHFFFAOYSA-N 0.000 title abstract 8
- 230000005684 electric field Effects 0.000 claims abstract description 16
- 230000003466 anti-cipated effect Effects 0.000 abstract 2
- 230000007423 decrease Effects 0.000 description 4
- 238000010586 diagram Methods 0.000 description 3
- 238000000034 method Methods 0.000 description 2
- 238000010521 absorption reaction Methods 0.000 description 1
- 239000004020 conductor Substances 0.000 description 1
- 230000006378 damage Effects 0.000 description 1
- 238000009792 diffusion process Methods 0.000 description 1
- 230000000694 effects Effects 0.000 description 1
Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01W—METEOROLOGY
- G01W1/00—Meteorology
- G01W1/16—Measuring atmospheric potential differences, e.g. due to electrical charges in clouds
Landscapes
- Environmental & Geological Engineering (AREA)
- Engineering & Computer Science (AREA)
- Life Sciences & Earth Sciences (AREA)
- Atmospheric Sciences (AREA)
- Biodiversity & Conservation Biology (AREA)
- Ecology (AREA)
- Environmental Sciences (AREA)
- Emergency Protection Circuit Devices (AREA)
Abstract
Description
【発明の詳細な説明】
通常の場合。雷の雲底と地表面の間には。雲底の電荷と
は逆の極性の空間電荷が存在することが知られている。[Detailed Description of the Invention] Normal case. between the base of the lightning cloud and the ground surface. It is known that there is a space charge with the opposite polarity to the charge at the cloud base.
それらの状況を電気力線を用いて表現すれば第1図のご
とくなる(ただし雲底を負電荷と仮定する)、図におけ
る記号の−は雲の負電荷。Oは空1%III電荷。If these situations are expressed using electric lines of force, the result will be as shown in Figure 1 (assuming that the base of the cloud has a negative charge). The symbol - in the figure represents the negative charge of the cloud. O is empty 1% III charge.
+は地表面電荷6↑を電気力線とする。地表面電位にく
らべ。空間電荷の影響をうけて雲底直下の電位の傾きが
強いうえ、上空になるほど気圧が低いことも誘因になっ
て。リーダーは雲底側から発進することが多い。その反
面電界の強さは。電気力線の密度が大きい程強くなるの
で。落雷の直前でも地表電界はl0KV/II位であま
り強くならない、第2図は。その雲から落雷があった場
合で。雲の負電荷は急激に減少するが。空間電荷の分布
はすぐに変化しない(一部分は落雷の際の放電路から出
る下向き放電路によって中和される)。大地は導体であ
るから直ちに一電荷が現われ、地表面電界は図示のごと
く逆転してかなり強大になる。+ indicates the ground surface charge 6↑ as electric lines of force. Compared to the ground surface potential. This is due to the strong slope of the electric potential just below the cloud base due to the effect of space charge, and the fact that the atmospheric pressure decreases as you get higher up in the sky. The leader often launches from the base of the cloud. On the other hand, the strength of the electric field is. The higher the density of the electric lines of force, the stronger they become. Even just before a lightning strike, the ground electric field does not become very strong at about 10 KV/II, as shown in Figure 2. If lightning strikes from that cloud. Although the negative charge of the cloud decreases rapidly. The space charge distribution does not change immediately (some of it is neutralized by the downward discharge path that leaves the discharge path during a lightning strike). Since the earth is a conductor, a charge appears immediately, and the electric field on the earth's surface reverses as shown in the figure and becomes quite strong.
次にこの原理をわかりやすく説明するために具体的な数
学を用いる。例えば雲底と大地間との距離をIKm、大
地と雲底との間の電位差を約1億ボルトとして。Next, we will use concrete mathematics to explain this principle in an easy-to-understand manner. For example, assume that the distance between the cloud base and the ground is IKm, and the potential difference between the ground and the cloud base is approximately 100 million volts.
もし空間電荷がないとすれば。地表の電界値Xは実測値
Xoは1♂V/m位であるから。その差はX X6=
9 X IOV / mとなる。If there is no space charge. The actual measured value Xo of the electric field value X on the earth's surface is about 1♂V/m. The difference is X X6=
9×IOV/m.
実際は空間電荷があるので、その空間電荷にもとづく地
表の逆電界をυとすると、こflX)が上記の差値9×
1♂v/mになる(x−(x)fJs実際の地表電界値
Xす・そこで近傍に落雷があって0頭上の雲の電荷がほ
とんど零になったとすると、空間電荷の大部分が一瞬と
りのこされるので、これによる地表電呻フは。逆方向で
略9万V/mに折い値となる。従って落雷直前のものに
くらべ、逆向きの相当強い電界を発生する1例え落雷直
前のものと反対方向のかなり大きいコロナ電流が発生す
る。具体的数字で表わすと。落雷以前の地表電界X6
= I X 10V/ mによるコロナ電流に比較して
。In reality, there is a space charge, so if the reverse electric field on the earth's surface based on that space charge is υ, then flX) is the difference value 9×
1♂v/m (x-(x)fJs Actual ground electric field value The ground electric field caused by this is approximately 90,000 V/m in the opposite direction.Therefore, compared to the electric field immediately before a lightning strike, it generates a considerably stronger electric field in the opposite direction. A fairly large corona current in the opposite direction is generated. Expressed in concrete numbers. Surface electric field X6 before the lightning strike
= I x compared to the corona current by 10V/m.
(X)よりx11v/mの反対記号の空間電荷による逆
向きのコロナ電流に変化し。その絶対値はかなり大きく
なる(実際には雲底の電荷−は完全に零にならないし。From (X), it changes to a corona current in the opposite direction due to the space charge of the opposite sign of x11v/m. Its absolute value becomes quite large (in reality, the charge at the base of the cloud does not become completely zero).
空間電荷も一部中和されるのてテX)は計算値よりは小
さくなる)。The space charge is also partially neutralized, so the value is smaller than the calculated value).
次に時間の経過とともに、雲底の一電荷は増加し。Then, as time passes, the charge at the cloud base increases.
空間電荷は拡散または地面えの吸収によって一時的に減
少するので。X6の値は次第に減少し6零値を通って落
雷直前の値に帰る。この時点では、空間電荷も地表面の
植物や建物などから発生するコロナ放電により再び増加
し、(x) x xoの値も落雷前の状態へもどったも
のと考えられる。Space charge is temporarily reduced by diffusion or absorption by the ground. The value of X6 gradually decreases, passes through 6 zero values, and returns to the value immediately before the lightning strike. At this point, it is thought that the space charge increases again due to corona discharge generated from plants and buildings on the ground surface, and the value of (x) x xo also returns to the state before the lightning strike.
上述した落雷時における地表電界の急反転を検出すると
、落雷点が近接していることがわかり。落雷の危険性を
警報することが可能である。Detecting the sudden reversal of the ground electric field during a lightning strike as described above indicates that the lightning strike point is close to each other. It is possible to warn of the danger of lightning.
本発明が最も有効に利用されるのは。コンピューター等
の弱電機器を含む信号回線や。その電源をしゃ断して、
落雷による破壊を防止する場合のように。あまり早くか
ら切ってしまうと不便で困るから、ギリギリまで切らず
、落雷を受ける危険が切迫した時点の直前で、それらの
線路を切ることが望そまれる場合である・
一実施例を図で示せば第3図のごとくなり、Cυはコロ
ナ針電極、(2ンは中心が零目盛のマイクロ電流計。(
3)接地電極。(4)メーターリレー。(5)正電流接
点(以下aという) 、 (6)負電流接点(以下すと
いう9゜(7)保持回路C復帰時間0,1〜0,5秒位
うをもつリレー。(8)同上。Where can the present invention be most effectively utilized? Signal lines including computers and other light electrical equipment. Cut off the power,
As in the case of preventing destruction from lightning strikes. It would be inconvenient to cut the lines too early, so it is desirable not to cut them until the last minute, but to cut the lines just before the danger of being struck by lightning is imminent. An example is shown in the figure. As shown in Figure 3, Cυ is a corona needle electrode, and Cυ is a microammeter with a zero scale in the center.
3) Ground electrode. (4) Meter relay. (5) Positive current contact (hereinafter referred to as a), (6) Negative current contact (hereinafter referred to as A), (7) Relay with holding circuit C return time of about 0.1 to 0.5 seconds. (8) Same as above. .
(9)a及びbが同時に働作した場合に働くリレー、
(10)落W地点接近非常信号である。(9) A relay that operates when a and b operate simultaneously;
(10) This is an emergency signal approaching the W drop point.
即わち。雷雲が接近した場合。雲底の負電荷に対応した
負のコロナ電流が増加するが、その雲から落雷すれば。That is. When thunderclouds approach. The negative corona current corresponding to the negative charge at the cloud base increases, but if lightning strikes from that cloud.
前述した理由でコロナ電流の極性が急反転し。For the reason mentioned above, the polarity of the corona current suddenly reverses.
正のコロナ電流がかなり流出する。時間の経過とともに
雲底の負電荷は増加し。マイクロアンメーターの電流値
は減って。零を通って落雷前の値に帰る。メーターの指
針がaまたはb(雲の極性が十の場合ンだけに感じた場
合を注意報とし、 a、 bが同時に働作した場合非常
警報とTる・0n(0より仄U〕2穂り阿カよK(ゴI
tずれか1つの作用をなさしむる。A significant amount of positive corona current flows out. As time passes, the negative charge at the cloud base increases. The current value of the microammeter decreases. It passes through zero and returns to the value before the lightning strike. If the meter pointer is a or b (if the polarity of the cloud is 10), it will be considered as a warning, and if a and b are activated at the same time, it will be an emergency warning. Riakayo K (go I)
perform one action.
イ、警報器が作動して警報を出す(警報器の場合は手働
のスイッチによっても復帰することができるン。B. The alarm will activate and issue an alarm (in the case of an alarm, it can also be reset by a manual switch).
口、予知の電気信号は・継電器に送られ遮断器を開閉せ
しめるなどの各種自動制御に用いる。The predicted electrical signals are sent to relays and used for various automatic controls such as opening and closing circuit breakers.
そのほか、コロナ電流の測定には電流計を用いて測定す
る方法だけを限定していない。デジタルメーター等に使
われる電子回路でもよい。In addition, the method of measuring corona current is not limited to using an ammeter. An electronic circuit used in digital meters etc. may also be used.
また・コロナ針電極のかわりに回転型電界強度測定器を
使用して同様な方法を実施することも可能であるかくの
ごとく。本発明の落雷点接近検知方式によれば、地表面
電界の急反転という簡単な現象を利用し。It is also possible to carry out the same method using a rotating electric field strength measuring device instead of the corona needle electrode. According to the lightning point approach detection method of the present invention, a simple phenomenon of a sudden reversal of the electric field on the ground surface is used.
人間の五感では知ることが難かしい落雷の接近を。正確
に検出することが出来るので。弱電器のt保護対策に使
用した場合は。あまり早くから電源や信号回路を切るよ
うなことなく。ギリギリまで切らず、落雷が予想される
直前に電源回路等を切ることが出来るので誠に有益な発
明である。The approach of lightning is difficult to detect with the human five senses. Because it can be detected accurately. When used for protection against light electrical appliances. Do not turn off the power supply or signal circuit too early. This is a really useful invention because it allows you to cut off power circuits, etc. just before a lightning strike is expected, without cutting them off until the last minute.
第1図
雷雲の雲底と地表面の電位。空間電荷等の関係を電気力
線を用いて示す図。
第2図
第1図のものが落雷(太い矢印)によりどう変化するか
を同じく電気力線で示した図。
第3図
本発明による落雷点接近検知方式の一実施例を示すブロ
ックごとの結線図。Figure 1. Cloud base and ground surface potential of a thundercloud. A diagram showing the relationship between space charges and the like using lines of electric force. Figure 2: A diagram showing how the thing in Figure 1 changes due to a lightning strike (thick arrow), also using electric lines of force. FIG. 3 is a wiring diagram for each block showing an embodiment of the lightning strike point approach detection method according to the present invention.
Claims (1)
警報するか、または信号する落雷点接近検知方式By detecting sudden changes in the ground electric field. A lightning point approach detection method that warns or signals that a lightning point is approaching.
Priority Applications (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP13559083A JPS6027883A (en) | 1983-07-25 | 1983-07-25 | Approach of thunderbolt detection system |
Applications Claiming Priority (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP13559083A JPS6027883A (en) | 1983-07-25 | 1983-07-25 | Approach of thunderbolt detection system |
Publications (1)
| Publication Number | Publication Date |
|---|---|
| JPS6027883A true JPS6027883A (en) | 1985-02-12 |
Family
ID=15155378
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| JP13559083A Pending JPS6027883A (en) | 1983-07-25 | 1983-07-25 | Approach of thunderbolt detection system |
Country Status (1)
| Country | Link |
|---|---|
| JP (1) | JPS6027883A (en) |
Cited By (2)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| FR2676547A1 (en) * | 1990-04-27 | 1992-11-20 | Central Lightning Protection C | Lightning alarm device |
| US5296842A (en) * | 1990-04-30 | 1994-03-22 | Central Lightning Protection Co., Ltd. | Thunder alarm |
Citations (1)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| JPS54131986A (en) * | 1978-04-05 | 1979-10-13 | Koizumi Toshio | Thunder alarm utilizing corona discharge |
-
1983
- 1983-07-25 JP JP13559083A patent/JPS6027883A/en active Pending
Patent Citations (1)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| JPS54131986A (en) * | 1978-04-05 | 1979-10-13 | Koizumi Toshio | Thunder alarm utilizing corona discharge |
Cited By (2)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| FR2676547A1 (en) * | 1990-04-27 | 1992-11-20 | Central Lightning Protection C | Lightning alarm device |
| US5296842A (en) * | 1990-04-30 | 1994-03-22 | Central Lightning Protection Co., Ltd. | Thunder alarm |
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