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Handbook of Electrical Installation Practice - BeKnowledge

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INTRODUCTION<br />

CHAPTER 9<br />

Lightning Protection<br />

J. Sherlock<br />

(Technical Manager, Furse/Thomas & Betts)<br />

P. Woods<br />

(Marketing Manager, Furse/Thomas & Betts)<br />

Traditionally, the subject <strong>of</strong> lightning protection has developed in two directions:<br />

(1) Protecting structures<br />

(2) Protecting electronic systems.<br />

It will be appreciated that, although the topics are related, the sensitivity <strong>of</strong> the two<br />

elements to lightning strikes differs considerably.<br />

It is essential that there should be no confusion as to the precautions that need<br />

to be taken for each condition. For this reason this chapter has been divided into<br />

two stand-alone parts, which in some instances duplicate important data.<br />

PART 1. PROTECTION OF STRUCTURES<br />

Characteristics <strong>of</strong> lightning<br />

Lightning strokes are the visible discharge <strong>of</strong> static electricity accumulated in storm<br />

clouds created by meteorological conditions. Strokes may occur within the cloud,<br />

between clouds, or from the cloud base to earth or earthed structures.<br />

Lightning is formed as a result <strong>of</strong> a natural build-up <strong>of</strong> electrical charge separation<br />

in storm clouds. The base <strong>of</strong> a storm cloud is commonly 5–10km above<br />

the earth’s surface, with the cloud 12km high. The charge at the base <strong>of</strong> the cloud<br />

is usually negative and induces an equal and opposite charge on the earth’s surface<br />

and earthed objects beneath the cloud. Buildings <strong>of</strong> masonry, concrete and timber<br />

are sufficiently conductive to reach the same potential as the earth’s surface.<br />

The earth’s atmosphere contains drifting pockets <strong>of</strong> ionised air, which also take<br />

on a charge <strong>of</strong> opposite polarity to the cloud base, and the presence <strong>of</strong> such a pocket<br />

near the cloud can create a potential difference sufficient to cause electrical breakdown<br />

<strong>of</strong> the air, and a downward leader stroke develops from the cloud, having a<br />

current <strong>of</strong> a few hundred amperes.A step progression can then develop from pocket<br />

to pocket <strong>of</strong> the leader stroke towards the earth in a few microseconds until the tip<br />

<strong>of</strong> the leader is within a distance <strong>of</strong> 50–100m from some point on the earth. At this<br />

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