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Transcript
SI96-09
Surging Ideas
TVS Diode Application Note
PROTECTION PRODUCTS
Sources of Transients : Lightning
surge waveform is defined as having an exponential
rise to the peak and an exponential decay from that
peak (Figure 2). The pulse is specified by a rise time
from 10 to 90% of the peak value and a decay to 50%
of the peak value. Industry standards such as ANSI/
IEEE C62.41 define a 1.2/50µs voltage waveform and
8/20µs current waveform for induced lightning on
power lines. One of the most common double exponential waveforms for induced lighting in U.S. telecommunication systems is the 10/1000µs impulse waveform
as defined by Telcordia GR-1089 CORE (formerly
Bellcore TR-NWT-001089) and Rural Electrification
Administration REA PE-60. International telecommunication standards such as ITU K17-K20 often specify
the 10/700µs impulse for lightning induced transients.
The telecommunication lightning waveform is different
from the power line waveform because a lightning
strike into a large telecommunication cable is distributed among several internal lines. This has the effect
of slowing down the rise time and increasing the decay
time of the waveform.
IEC 61000-4-5 was set forth by the European Community to define the lightning threat to both power and
telecommunication lines. The standard specifies
double exponential impulses of 1.2/50µs for power
and 10/700µs for telecommunication lines to describe
the threat.
Lightning is an atmospheric discharge of electricity
resulting from the accumulation of static charges,
usually during a thunderstorm. Inside of a thundercloud, static charges are generated by the impact of
water and ice particles and separated in strong air
currents. Lightning occurs when enough charge has
been separated inside the cloud to cause localized
electric breakdown of the air.
Lightning is one of the most common causes of transients in electronic systems. Power and telecommunication systems being the most vulnerable. At any given
time, there are approximately 1800 thunderstorms in
progress around the world generating lightning strikes
on the surface of the earth about 100 times every
second. Each cloud-to-ground event generally contains
3-5 distinct strokes, but as many as twelve have been
observed. Mean peak current for the first stroke is
20kA with subsequent strokes decreasing by 50% or
more. While a direct lightning strike is dramatic, it is
significant to note that lightning produces intense
electric and magnetic fields which can couple into
nearby power lines, communication lines, and circuit
wiring causing catastrophic or latent damage to semiconductor equipment. The magnitude of the induced
voltage varies with the distance from the strike (Figure
1).
References:
1. Stringfellow, Dr Michael F. “Lightning” Power Quality
& Assurance, Sept/Oct 1995
2. Clark, O.M. “Lightning Protection for Computer Data
Lines” EOS/ESD Symposium Proceedings, Sept., 1981
Lightning Standards & Waveforms
Transient voltage waveforms representative of induced
lightning transients are often described by a double
exponential impulse waveform. A double exponential
Induced Voltage in 1m of Wire (V)
10000
1000
100
10
1
0.1
1
10
Distance from Strike (km )
Figure 1 - Lightning Induced Voltages
Revision 9/2000
Figure 2 - Lightning Waveform
1
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