EFFECTS OF LIGHTNING
Statistics indicate that approximately 5000 thunderstorms happen on
earth simultaneously with danger for persons, structures, and material.
The average intensity of a lightning flash is estimated to be of 20000
amps, however lightning intensities of up to 200000 amps were registered.
Each year about two million flashes of lightning occur on the Iberian
peninsula, causing death to persons and animals. In industry the
damage and failures due to lightning are estimated to be in the
range of thousands of millions of Spanish Pesetas.
The frequency and the intensity of thunderstorms in an area are
determined by the characteristics of the area, however the risk
of lightning can vary within a certain region. The knowledge about
the areas with high lightning risk is an important information in
order to effectivly determine the most appropriate type of lightning
protection.
The effects of lightning can be produced by direct lightning strokes
or by indirect causes.
While a direct stroke may generate disasterous consequences for
structures, persons and animals, indirect effects produced by lightning
are frequently noticed and usually they produce significant economic
losses. Indirect effects of lightning are observed when the lightning
flash strikes close to a structure and produces by induction surge
voltages in the electrical conductors.
LIGHTNING FLASHES:
Under certain athmospheric conditions the loads within a cloud
get separated, where the negative loads move to the bottom of the
cloud and the positive loads to the top of it. The electrical potential
within the cloud can reach the range of millions of volts.
On the surface of the earth this effect is produced in a similar
way, however with opposite polarity.
The electrical field between the bottom of the cloud and the surface
of the earth under the cloud can become so strong that small electrical
discharges from the cloud will be produced which are called downward
leaders. When these discharges reach the surface of the earth, an
upgoing steam of positive load is generated. When the upgoing steam
meets with the discharges, then the circuit becomes closed and a
discharge current between 10 to 200 kA can be produced.
In the illustrations on the left it is shown how the small discharges
from the cloud and the upgoing streams, which finally lead to the
flash of lightning, are initiated.
Protection against lightning:
The decision to protect an installation against lightning by means
of a Lightning Protection System (LPS) depends on parameters such
as the probability of lightning in the area, its intensity and the
potential consequences for people, material and the functioning
of the installation.
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In order to provide an appropriate protection,
the installation has to be equipped with two types of protections:
an external protection against a direct impact of a lightning
stroke (lightning rod, wire air-termination system or mesh
air-termination system), and an internal protection against
surge voltages produced by lightning strokes in the proximity
or on conductors of the electrical network.
The external and the internal protection require a good earthing
system to evacuate the lightning currents, and equal potentiality
within the earthing system, both of the protection system
and of the electrical circuits to be protected.
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