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        參數(shù)資料
        型號(hào): P0640EA
        英文描述: SIDAC|77V V(BO) MAX|800MA I(S)|TO-92VAR
        中文描述: SIDAC的| 77V V(下公報(bào))最大| 800mA的我(縣)|對(duì)92VAR
        文件頁數(shù): 136/161頁
        文件大?。?/td> 986K
        代理商: P0640EA
        Lightning
        SIDACtor
        Data Book
        5 - 20
        Teccor Electronics
        (972) 580-7777
        ,*
        Overview
        Lightning is one of nature
        s most common and dangerous phenomena. At any one
        time, there are approximately 2,000 thunderstorms in progress around the globe with
        lightning striking the earth over 100 times per second. During a single year in United
        States, lightning will strike an average of 52 times per square mile, resulting in 100
        deaths, 250 injuries, and over 100 million dollars in damage to equipment property.
        The Lightning Phenomenon
        The formation of lightning is caused by the complex interaction of rain, ice, up drafts,
        and down drafts that occur during a typical thunderstorm. The movement of rain
        droplets and ice within the cloud results in a large build up of electrical charges at the
        top and bottom of the thunder cloud. Normally, positive charges are concentrated at
        the top of the thunderhead while negative charges accumulate near the bottom.
        Lightning itself does not occur until the potential difference between two charges is
        great enough to overcome the insulating resistance of air between them.
        The Formation of Lightning
        Cloud to ground lightning will begin forming as the level of negative charge contained
        in the lower cloud levels begins to increase and attract the positive charge located at
        ground. When the formation of negative charge reaches its peak level, a surge of
        electrons called a stepped leader will begin to head towards the earth. Moving in 50
        meter increments, the stepped leader initiates the electrical path (channel) for the
        lightning strike. As the stepped leader moves closer to the ground, the mutual
        attraction between positive and negative charges results in a positive stream of
        electrons being pulled up from the ground to the stepped leader. The positively
        charged stream is known as a streamer and can rise up out of a tree, roof of a house,
        or even the top of your head. When the streamer and stepped leader make contact, it
        completes the electrical circuit between the cloud and ground. At that instant, an
        explosive flow of electrons travels to ground at half the speed of light and completes
        the formation of the lightning bolt.
        The Lightning Bolt
        The initial flash of a lightning bolt results when the stepped leader and the streamer
        make connection resulting in the conduction of current to ground. Subsequent strokes
        (3-4) occur as large amounts of negative charge move farther up the stepped leader.
        Known as return strokes, these subsequent bolts heat the air to temperatures in
        excess of 50,000
        °
        F and cause the flickering flash that is associated with lightning. The
        total duration of most lightning bolts lasts between 500ms and 1 second.
        During a lightning strike, the associated voltages range from 20,000V to 1,000,000V
        while currents average around 35,000A. However, it should be noted that maximum
        currents associated with lightning have been measured as high as 300,000A.
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