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| uk.tech.digital-tv (Digital TV - General) (uk.tech.digital-tv) Discussion of all matters technical in origin related to the reception of digital television transmissions, be they via satellite, terrestrial or cable. Advertising is forbidden, with no exceptions. |
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#1
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Interesting post - if I can add a few points;
Lightning ground strikes occur when the potential difference between the cloud and earth is allowed to build up to such a voltage that the resistance of the air breaks down and the air is ionised. To do this you need lots of volts just to get there and enough power (volts x amps) to actually get the work done. When this happens the resistance of air collapses and the floodgates are opened for huge currents to flow. Before this happens the current is still flowing but to a much lesser extent. However wet air has a much lower resistance than dry air and this causes the centre of the cloud (where it is actually raining) to discharge quicker to earth and lose a lot of its potential difference. Because of this, strikes through rainfall are almost unheard of - cloud to ground lightning almost always occurs around the edges of the cloud where air resistance is greatest. Try it yourself, pull the spark plug connectors off the spark plugs in your car, pour water over the plugs and plug in again and then try to start the car. The water dissipates the spark to earth before it can reach a high-enough level to break down the air resistance in the cylinder. Back to your post! When the aerial is in an area of high potential difference compared to earth, the unplugged connector acts like a mini ioniser, producing a stream of negative ions into the room. However despite the voltage difference between it and (say) the earth on a nearby mains socket it cannot deliver a flash because the current isn't available - this would require the resistance in the air above the aerial to break down too. So although your sums are dead on, you aren't going to get a flash unless a large amount of current becomes available in the vicinity of the aerial. Bizarely this can happen through a nearby strike, and suddenly all the aerials in a block that have happily been acting as ionisers for ten minutes suddenly get enough current from the cloud (which has finally managed to reduce the resistance of the surrounding air to almost zero) to zap all the televisions in one go! Sounds like a job for Wrights Aerials! |
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#2
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Sounds like a job for Wrights Aerials!
Super! Some years ago I was on the roof of a retail store very close to Bradford railway station (Forster Sq I thing it's called). It was a sunny day, very bright but also very windy. A black clound came across very quickly. I thouight there might be lightning and told the two blokes with me that we must get off the roof very quickly. They thought I was crazy because the sun was still shining and on the face of it it was still a nice day, but I insisted and we set off across the very big roof to the ladder. At the monent when the first man was on the ground, the second half way up the ladder and I was still on the roof lightning struck a railway engine, only a few yards away from us. I happened to be looking in that direction and was momentarily blinded. The man half way up the ladder got a fright but didn't fall. The man on the ground was knocked to the floor. This took place when the IRA was active and the people in the shop thought they'd been bombed. The staff came bursting out of the loading bay really scared. One bloke just broke down and curled up into a ball and sobbed. Meanwhile the engine that had been struck burst into flames. Then a torrential downpour started, and although the staff had their indoor clothing on they wouldn't go back in the shop because they still thought there had been a bomb and they thought there might be another. They all got absolutely soaked to the skin, but they wouldn't go in. It was a weird experience. We finished the job in somber mood. Bill |
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#3
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"Duncan Ross" wrote in message Interesting post - if I can add a few points; Lightning ground strikes occur when the potential difference between the cloud and earth is allowed to build up to such a voltage that the resistance of the air breaks down and the air is ionised. To do this you need lots of volts just to get there and enough power (volts x amps) to actually get the work done. Right. It is the quantity of electricity that determines the potential difference between points (measured in Coulombs?) Big capacitors carry higher volts than small ones. Remember this is static or stored electricity not dynamic electricity as produced by a battery or generator. When this happens the resistance of air collapses and the floodgates are opened for huge currents to flow. Before this happens the current is still flowing but to a much lesser extent. However wet air has a much lower resistance than dry air and this causes the centre of the cloud (where it is actually raining) to discharge quicker to earth and lose a lot of its potential difference. Right. But this would only be true as long as the rate of ionisation matches the rate at which the quantity of electricity (electrons) is being generated. Some thunderstorms generate electric fields fast enough to cause frequent flashes whilst others are quite slow. (The recent one was quite slow where I lived) Because of this, strikes through rainfall are almost unheard of - cloud to ground lightning almost always occurs around the edges of the cloud where air resistance is greatest. You seem to be arguing that the discharge will take a longer and harder path ignoring a shorter path of lower resistance? When the aerial is in an area of high potential difference compared to earth, the unplugged connector acts like a mini ioniser, producing a stream of negative ions into the room. However despite the voltage difference between it and (say) the earth on a nearby mains socket it cannot deliver a flash because the current isn't available - this would require the resistance in the air above the aerial to break down too. So although your sums are dead on, you aren't going to get a flash unless a large amount of current becomes available in the vicinity of the aerial. Well certainly ionisation into the air would serve to inhibit the voltage reaching high enough for breakdown. It is rather like trying to fill a bucket with a hole, but this will only occur for as long as the ionisation flow can match the current flow which will increase as the stress between ground and cloud increases (building up to a strike). Pour more water into a bucket than flows out through the hole and the water level will rise until it runs over the top. If the voltage does reach breakdown point (on an unplugged lead), and we have heard cases in this thread when it has, it is because the quantity of electricity gathered is sufficient to generate the potential difference needed and sufficient to cause breakdown even if not sufficient to sustain it. The same is true of a full lightning strike except on a larger scale, the lightning path only last long enough for the charge to discharge, it does not sustain longer than that. (we are talking tiny amounts of time of course). Bizarely this can happen through a nearby strike, and suddenly all the aerials in a block that have happily been acting as ionisers for ten minutes They will only ionise current into the air if unplugged of course, otherwise the current flows into and through the TV (a much larger hole in the bucket). Damage will occur once this current gets too high (due to the rising electrical field) or, if the aerial is unplugged, the ionisation cannot match the current flow and the voltage rises to the flash point. There are two distinct circumstances here. suddenly get enough current from the cloud (which has finally managed to reduce the resistance of the surrounding air to almost zero) to zap all the televisions in one go! The short circuit will only be in the narrow corridor where the lightning discharge occurs, the surrounding air will still have the same resistance surely? Also, if the resistance of surrounding air does drop to zero as you suggest, why would the current then flow down a cable (with resistance) and through the TV (also with resistance) when it can take a more direct path through this zero resistance air, or is the air only zero resistant down to the roof top? Sorry but that is not logical. Surely once the nearby strike occurs the potential difference between cloud and ground would instantly drop to zero due to the short circuit, collapsing the electrical field in the air with it and the potential difference between aerial top and ground? Thus any current flow down the aerial cable (if not already burnt out) would instantly drop not rise as you suggest? Ohms law still applies. Thus the flash from the unconnected aerial or TV/cable damage due to excess current must surely have occurred a finite time before the strike, driven by the high electrical field between the ground and the aerial? -- Les Hellawell Greetings from : YORKSHIRE - The White Rose County |
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#4
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"Wrightsaerials" wrote in message ... Sounds like a job for Wrights Aerials! Super! Some years ago I was on the roof of a retail store very close to Bradford railway station (Forster Sq I thing it's called). It was a sunny day, very bright but also very windy. A black clound came across very quickly. I thouight there might be lightning and told the two blokes with me that we must get off the roof very quickly. They thought I was crazy because the sun was still shining and on the face of it it was still a nice day, but I insisted and we set off across the very big roof to the ladder. At the monent when the first man was on the ground, the second half way up the ladder and I was still on the roof lightning struck a railway engine, only a few yards away from us. I happened to be looking in that direction and was momentarily blinded. Was there a bang? I once saw lightning strike a nearby pole mounted YEB sub-station only about 30-40ft away from my rear window. It burnt out one of the cables which dropped to the ground setting poles and remaining cables shaking violently all down the field. The only noise was a slight 'fizzing' sound and no bang. Duncan please note: it was raining at the time. -- Les Hellawell Greetings from : YORKSHIRE - The White Rose County |
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#5
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In message , Les Hellawell
writes "Duncan Ross" wrote in message Interesting post - if I can add a few points; Lightning ground strikes occur when the potential difference between the cloud and earth is allowed to build up to such a voltage that the resistance of the air breaks down and the air is ionised. To do this you need lots of volts just to get there and enough power (volts x amps) to actually get the work done. Right. It is the quantity of electricity that determines the potential difference between points (measured in Coulombs?) Big capacitors carry higher volts than small ones. Remember this is static or stored electricity not dynamic electricity as produced by a battery or generator. Well, no. For a given quantity of charge (in Coulombs) a small capacitor will show a higher voltage than a small one. Mike -- M.J.Powell |
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#6
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"Les Hellawell" wrote in message Was there a bang? There often is. I was once having breakfast in the Boar's Head (PH / Hotel) in Bishops Stortford (formerly the palace) when lightening struck the church spire about 30m away on the other side of the road and passed down the conductor. It was summer and the door was open. The flash rendered me temporarily blind (~10s), and the bang meant I couldn't hear anything for about a minute. When at school lightnening struck the building opposite (~50m) - the bang was much worse than the flash. |
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#7
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#8
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In message , Les Hellawell
writes "Wrightsaerials" wrote in message ... Sounds like a job for Wrights Aerials! Super! Some years ago I was on the roof of a retail store very close to Bradford railway station (Forster Sq I thing it's called). It was a sunny day, very bright but also very windy. A black clound came across very quickly. I thouight there might be lightning and told the two blokes with me that we must get off the roof very quickly. They thought I was crazy because the sun was still shining and on the face of it it was still a nice day, but I insisted and we set off across the very big roof to the ladder. At the monent when the first man was on the ground, the second half way up the ladder and I was still on the roof lightning struck a railway engine, only a few yards away from us. I happened to be looking in that direction and was momentarily blinded. Was there a bang? I once saw lightning strike a nearby pole mounted YEB sub-station only about 30-40ft away from my rear window. It burnt out one of the cables which dropped to the ground setting poles and remaining cables shaking violently all down the field. The only noise was a slight 'fizzing' sound and no bang. Duncan please note: it was raining at the time. I was driving home many years ago, through Moss Side, listening to R4 LW when the radio suddenly started a loud screaming noise. After a few seconds a huge lightning flash hit the ground about 50 yards away. Normal reception then. I assume the screaming noise was corona from the whip aerial. Mike -- M.J.Powell |
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#9
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In message , Les Hellawell
writes "M. J. Powell" wrote in message In message , Les Hellawell writes "Duncan Ross" wrote in message Interesting post - if I can add a few points; Lightning ground strikes occur when the potential difference between the cloud and earth is allowed to build up to such a voltage that the resistance of the air breaks down and the air is ionised. To do this you need lots of volts just to get there and enough power (volts x amps) to actually get the work done. Right. It is the quantity of electricity that determines the potential difference between points (measured in Coulombs?) Big capacitors carry higher volts than small ones. Remember this is static or stored electricity not dynamic electricity as produced by a battery or generator. Well, no. For a given quantity of charge (in Coulombs) a small capacitor will show a higher voltage than a small one. Looking it up v = q/c (Nelkon again :-) Thinks: Halve c and you double v. Yes you are right, I stand corrected. but voltage is proportional to quantity which is what I was trying to get at. I am afraid my electrical theory has got a little rusty down the years :-( Right! And nobody noticed that my second 'small' should have been 'large'! Mike -- M.J.Powell |
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#10
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"Duncan Ross" wrote in message ... From: "Les Hellawell" Date: 24/07/2003 20:57 GMT Daylight Time Message-id: Because of this, strikes through rainfall are almost unheard of - cloud to ground lightning almost always occurs around the edges of the cloud where air resistance is greatest. You seem to be arguing that the discharge will take a longer and harder path ignoring a shorter path of lower resistance? No, the ground to cloud potential difference in the area of rainfall is much lower than the potential difference around it. In addition wet air conducts, and a spark cannot pass through a conductor, only across an insulator (dry air). You are restating your argument not answering the question. How can a voltage build in one part of the cloud sufficient to discharge a long way to earth if an adjacent area of cloud has (according to your argument) a low resistance path to earth? Surely, in these circumstance the discharge would be between these areas of cloud - the shortest/easiest path in this case? Yes the wetter path to earth may have a lower insulation resistance but it wont be zero and I doubt if it will be significantly less than the 25,000V figure quoted. All this means is that a discharge can occur at a lower voltage in a wet zone than in a dry one, so a 'dry' discharge will have more potential energy than a 'wet' one and be more dangerous. As to whether the leakage is enough to prevent a strike, who really knows? I don't. it all depends on the circumstances and severity of the storm. The stormclouds can reach very high into the sky. I have seen the hammerheads from aircraft and once flew into Venice Airport near one. It was fantastic descending between great towers of solid white. You could hardly see the ground above the airport as it was like looking into a murky pond. Getting off the aircraft was like stepping into a Turkish Bath. The slow moving storm reached the coast that same night about 0100 and was a real humdinger. suddenly get enough current from the cloud (which has finally managed to reduce the resistance of the surrounding air to almost zero) to zap all the televisions in one go! The short circuit will only be in the narrow corridor where the lightning discharge occurs, the surrounding air will still have the same resistance surely? This is from inductance, a large current flowing down a nearby conductor (the lightning channel) will induce a smaller current flow in the aerial conductor - this is the current flow that it was waiting for to kick things off. Inductance induces voltage not current. Current is proportional to the voltage induced if electrical resistance is not infinite. So you introduce a new circumstance by introducing the electromagnetic pulse caused by a lightning discharge? OK. Yes this will indeed induce a voltage spike in adjacent conductors. The magnitude will reduce in proportion to the square of the distance from the lightning. I doubt if this will be very large (enough perhaps to induce a crackle on a radio?) but I simply do not know. This momentary increase in p.d. induced in the conductor may indeed be enough to cause a flash if the existing voltage is just on or below the threshold (and has not yet started to collapse due to this same adjacent short circuit in the lightning path) but current will only start to flow ONCE the breakdown has occured and it has a path to flow through. Let's just consider an unplugged aerial lead here which is insulated at the bottom by air between the nearest ground point and its plug and, therefore, has a path of electrical resistance approaching infinity - there will be ionisation leakage as you mention to ground. (Note: The insulation resistance of air is a different thing entirely from its almost infinite electrical resistance.) Insulation resistance of an insulator (whether air, plastic mica etc) is measured purely in term of the potential difference or electrical stress that it can withstand. As already stated air can withstand about 25,000v/inch. Insulation breakdown occurs when the voltage limit is reached. (that's a full stop there) Only AFTER breakdown has occurred does a discharge current start to flow though it. How long this current lasts, depends on the quantity of charge stored (in static or stored electricity) and this is proportional to the voltage before the breakdown occured. Putting it the other way round: For a given situation a doubling of the voltage means a doubling of the charge stored (in the cable in this case*). So, the discharge current does not have to come from (your zero resistant) air above the aerial as you suggest but is already stored in the cable. *I have a feeling this is not quite so simple as the potential difference between ground and aerial top will still exist in this moment in time even though the flash has short circuited the bottom of the cable. Strewth who knows what happens under these circumstances! ps thanks for the interesting debate forcing me to clarify my thinking here. I hope others are not finding it too boring :-) -- Les Hellawell Greetings from : YORKSHIRE - The White Rose County |
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