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Showing posts with label Lightning Discharge. Show all posts
Showing posts with label Lightning Discharge. Show all posts

Friday, January 3, 2014

Shielding in 380kV HV Transmission Lines

     380 kV transmission overhead lines seem to be vulnerable to lightning discharges since they are, mostly, the things that have largest height in field. Lightning discharges most likely prefer to breakdown the air through overhead lines in plain fields. This is a very bad condition for power system since it may result temporary overvoltages, insulation failures or partial energy cuts. That's why overhead lines should be protected against lightning discharges. Most of the time, the protection is satisfied using lightning rods, especially in substations. Actually, sometimes it is inevitable for HV transmission lines to be exposed to lightning discharges. Therefore, the excessive energy should be directed to a point which causes much less damage to power system. Shielding is a kind of protection against the harmful effects of lightning discharges, which is always used in high voltage transmission lines unless it is protected by lightning rods or any other conductor that has higher altitude. Shielding requires to direct the lightning strokes to ground wire instead of phase wires. This aim is satisfied by simply placing the ground wire at a higher place than phase wires so that the nearly all of the strokes are directed towards ground wire. The shielding position of wires can be determined using shielding angle, theta, which is defined as the angle between tower direction and the line passing through ground wire and outermost phase wire. Figure 1 is showing an effective shielding. 

Figure 1: Effective Shielding

     The most important thing to take into consideration for effective shielding is determining the shielding angle. While high shielding angle may result to missing some strokes to phase wires, low shielding angle may result to extra unnecessary tower cost and construction handicaps. Let me try to explain the method for choosing the best procedure for determining shielding angle. 

     Lightning Stroke History in Field
     Provide the lightning stroke historical data for determining the characteristics of the strokes to be protected. Then determine the maximum protection level ,in other words, determine the stroke energies that are most likely to happen and eliminate the extreme (rarely happened) events. If we try to protect the line for even extreme cases, the construction cost will increase dramatically. By using the historical data for lightning strokes we can determine the equipotential lines. Please note that the higher the electrical charges collected in a stroke the the higher the shielding angle is. In other words, if the charge enclosed in a lightning stroke is high, the stroke starts at a longer height. Thus, high shielding angle is enough. However if the charges in a lightning stroke is less which means the lightning stroke starts discharging at the distances closer to earth, then the low shielding angle is needed which can be possible only with high tower length. Please take a look at the graphs shown in figure 2, 3 and 4, they give the relations between shielding angle and lightning strokes.

Figure 2: Percentage of Strokes vs Lightning (kA)

Figure 3: Protective Angle vs Lightning (kA)
Figure 4: Percent Lightning Strokes vs Angle

     It had better to represent a noneffective shielding, figure 5 represents a non effective shielding. 

Figure 5: Noneffective Shielding

Figure 6 shows a practical application of shielding in a thermal plant in Turkey.

Figure 6: Practical Shielding in Kemerköy Thermal Plant, Muğla / TURKEY







Friday, October 11, 2013

Lightning Discharges

     As a result of natural environmental phenomena, there may exist lots of  positive and negative charge centers in the air. The distance between those charge centers may vary up to 500 km long and their charge distribution changes. If the electric field density in the vicinity of a negative charge center reaches a critical value ,typically 10 kV/cm, the small length of air is started to be ionized and an ionized channel is formed. This ionized channel is also called "streamer". The critical electric field value for ionization is directly proportional to the breakdown value of air. This breakdown value can be changed by humidity and temperature but ionization is most likely start in large water droplets in air. 
     As I said, the distance between the positive and negative charges centers in air may vary up to 500 km ,thus, the excessive negative charges may prefer to discharge through ground (another positive charge center) which is much more closer to negative charge center. After first streamer ,about a couple of ten microseconds later, the second streamer arises and it follows the same way with the first streamer but it goes a little bit further than the first streamer. This process continues a number of times ,each time the ionized channel propagates 10 to 200 metres, up to the ionized channel is reached to a critical distance to ground. This process is called "stepped leader". Each time the stepped leader propagates in air, an excessive amount of negative charges move towards ground. When the stepped leader reaches to a distance of 10 to 50 metres from earth, the field intensity of the earth (positive charge center) reaches a sufficient value to form an upwards streamer in order to make connection between stepped leader and earth. Then the excessive amount of current flows from earth to clouds along ionized path so that the negative charges neutralized. This neutralizing current is called "return stroke". The figure below explains the whole characteristics of lightning discharges.

Figure 1: Lightning Discharge Phenomenon

Reference: EE575 - Advanced High Voltage Techniques (METU)