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Protection AgaindDirect Lightning Strokes by Charge Transfer System Roy B. Carpenter Jr. Mark M. Drabkin Lightning Eliminators & Consultants,Inc. 6687 ArapahoeRd Boulder, Colorado,USA Lightning Eliminators & Consultants,Inc. 6687 ArapahoeRd Boulder, Colorado, USA Abstract: Implementation of the Charge Transfer System (CTS) offers a wide range of protection against direct lightning strokes; from the enhancement of the strike collection ability to the total prevention of strokes into the protected premise. Design of such a system requires engineering specifics about the site to be protected and the data related to the lightning activity and weather conditions in that particular location. The engineeringdata for the premise to be protected is usually readily available, but lightning data, statistical and probabilistic by nature, varies from region to region. Some times this data is only partially available, and that createssome complexity for the design process of CTS. The paper discusses the major steps of the engineering approachto the designof CTS. Introduction Protecting a premise against direct lightning strokes by preventing lightning stroke is not exactly a new idea. It was Franklin’s original idea that he could dissipate the thundercloud electricity by installing the pointed iron rod, which would quietly conduct the electricity away. However,. he changed his mind after his lightning rods were hit by lightning insteadof preventing the strokes.He then postulated that it would be better to provide a preferablepath to earth for lightning by erecting the elevated groundedrods. During the past 250 years the Franklin rod successfUlly protected structures from the lightning-caused damage.And that was the & requirementto the lightning protection against direct hits till last 40 - 50 years. In the recent 4 decades,due to the explosive progress in computers/electronicstechnology, the secondaryeffect of the lightning stroke became the major concern in many cases. Generated by lightning current, the strong magnetic field around the downward conductor connectingthe lightning rod to the grounding system causedthe induced voltagesof such a magnitudethat it permanentlydamagedor causedmalfunction of sensitive electronic equipment located nearby. The prevention of the direct lightning strokes into the premise is one of the ways to eliminate the damaging consequencesof the secondaryeffect. 0-7803-5015-4/98/$10.000 1998IEEE Mechanism of preventing the lightning stroke The idea of preventing the lightning stroke is based on the so-called point discharge phenomenon.Sharp edged objects such as leaves of trees , bushes and grass as well as pointed electrodessuch as lightning rods), when exposedto the strong electric field, start to emit current into the surrounding air. This current is a result of an ionization process in the air surroundingthe sharpenedpoints. The strength of the electric field, called the critical initiating field is required to initiate such an ionization process.The magnitude of critical field can vary widely depending on factors like an availability of free electrons in that area, barometric pressure, temperature,etc. As an example,note the following empirical formula (1) used frequently in power transmission and distribution engineering to determine the critical value of the electric field strength which will start a corona from the line conductors: EC,= 23.36(1+ $$&), 0 where 6 is the relative air density factor depending on temperatureand pressure,and ro is the radius of the conductor. For quick estimation of the critical field strength the Peek’s empirical formula, Ecr = 316 (kV/cm), can be used. In calculations of the electric fields due to the lightning, the thunderstormcloud is often representedby a simplified model (see Figure 1) of point charges located on one vertical line. The main positive charge is at the top of the cloud, the negative charge at the bottom of the cloud, and an additional local positive charge at some distance below the negative charge [I]. The electric field at the ground level can then be calculatedby the following equation (2): where: Qposand Qnegare the positive and negative chargesof 1094 a thundercloudcell, qpDs is a local positive chargebelow the thundercloud cell, Hpos,Hnegand hposare the heights of the correspondingchargesabovethe ground level, and D is the horizontal distanceof the point at the Earth’s surfacefrom the thundercloudcell charges. strengthof the electric field, wind velocity past the points, and barometric pressure. Appearance of an additional charge locatedrelatively close to the ground changesthe total electric field E. [4]. Inserting a new componentof total electric field causedby the presenceof the spacecharge qSc,into Equation (2), we introduce Equation (3), which can be used to calculate the new value of the electric field strength with consideration of an additional positive chargeq,, at the height h,, above the ground. + 2QnegHneg *o=- 2Qp.Pp 4m+(Ig,, +Tlp3’* H P*s 29po&oo - 4nq,(h;os+d)3’2 .pos Figure 1. Simplified model of a thundercloud cell Chalmers [2] noted that the electric field of 600 to 1000 V/m at ground level is sufficient to initiate the ionization process from the points at the top of trees. Thesevalues are not in any disagreement with E,, because the electric field, E,, at sharpenedpoints and edges is much stronger than Eo. The field enhancementfactor, which is defmed as b = Ep/Eo , dependson the shape,dimensions,and height of the sharpened point. It is difficult to calculate exact value of k, becausethe analytical solution for most shapesis yet to be developed. However, for the simple forms, like vertical or horizontal conductors,reasonableapproximationscan be made using the equations developed for a conducting prolate semi-ellipsoid [3]. Calculations of the enhancementcoefficient, k, basedon this approximation show that k, can be as great as 100 - 600 dependingon the electrodeheight and radius of curvature. When a stepped leader starts its downward movement, it lowers the main negative charge located at the bottom of the thundercloud cell and may or may not neutralize the local positive charge. The electric fields, Eo, and correspondingly, Ep, have intensified rapidly, approximately in accordance with the vertical component of the average speed of the stepped leader and the charge distribution along the leader channel. Under influence of the rapidly increasingelectric field, E,, the ionization of the air surrounding the sharpenedpoints is intensified, leading to development of the positive space charge around the sharpenedpoints. The size of such a space chargedependson many factors, the most important being the + 4xq)(H&+Dy %&c 4xq&c+lI+)3’* It can be shown that a relatively small space charge, qSo above the sharpenedpoints, (a small fraction of the charge of the steppedleader) causesa significant reduction of the total electric field strengthat the points. This is becausethe electric field is proportional to the size of the charge but inversly proportionalto the squareof the height of this charge. The more current that is flowing from the sharpenedpoints into the air, and the longer duration of that current flow, the larger the space charge will be. An increasing space charge will weakenthe electric field at the points, The point discharge current will continue to flow until the electric field strength drops below the level where the further ionization will cease to exist. At this particular phaseof the lightning development process,the situation exists where the space chargeabove the sharpenedpoints acts as a shield, making a direct lightning stroke into the points impossible. This well known phenomenon leads to a better understanding as why a lightning rod sometimesfails to attract lightning. Unfortunately, a favorable situation for lightning protection situation with regard to lightning charges and space charge does not remain static during the process of lightning progressing.Qnce developed,the spacecharge is driven away from the points by the forces of electric fields and wind. Traveling far enoughfrom the spacechargewill not shield the points anymore.The field strength at the points will increase again, and new ionization processwill take place. But during each ensuingperiod, the field strengthensmuch more rapidly and becomesstrongerwith each step of the lightning leaderas it descendsfrom a thundercloud , approaching closer and closer to the sharpenedpoints. In such conditions the new spacechargegeneratedmay be not sufficient to influence the electric field and will not have enoughtime to move from the points to provide adequateshielding. The streamerformed in such circumstanceswill eventually result in establishingthe conducting path between the descendingstepped leader and moving upward streamer from the sharpened points. The direct lightning stroke will occur. And this is a desirableevent for the lightning rods or other devices designed to collect lightning strokes. In the case when the space charge is still large enoughand able to reducethe electric field at the points, 1095 even within a very short time given by the stepped leader’s pausesbefore the fmal jump, the direct stroke will be avoided. And that is desirable performance for the lightning strokes prevention system. It becomes obvious from the general discussion of this the lightning stroke preventative mechanism, that the major parametersinfluencing the choice of the attachmentpoint for the descendingsteppedleader at its final stepsare: . charge lowered by the steppedleader, l distance betweentip of the steppedleader and the points, . speedof the steppedleader propagationand the time interval available for formation of the spacecharge of the required size, e magnitude of point dischargecurrent All these parameters are mutually interdependent on each other. The charge deposited on the stepped leader channel varies from a few Coulombs to 10 to 20 C with 5 C being an average value. Another method of an estimation of the averagecharge lowered by the steppedleader is the averagecharge density of 1mC per 1 meter of the channel length. Calculation of the electric field strength at the ground level according to Equation (3) is not valid in the case of the initiation of a steppedleader. Equation (3) has to be modified, taking into consideration that a part of the main negative charge, Qneg,is moving downwards. That part, AQneg,can be defmed at any given time fiom the moment of the stepped leader initiation assuming linear charge density distribution is as follows (Equation (4)): AQ,, = PslYHnep- HT) AQ., or = ps~*(Hneg - v*fh (4) where psiis the steppedleader charge density (assumedbeing constant), Hr is the height of the steppedleadertip at time t, and v is the average speedof the steppedleader. After substitution of these changes into Equation (3) we will produce Equation (5) for the calculation of E0and E,: 4nso(D2+h;,,)3’2 2Pd 1 4’=0 [ (D2+H;)“* - 4mo(D2+h;c)3’2 (D2+&q)1’2 + 1 The distance between the tip of the stepped leader and the sharpened points of the CTS is extremely important at the fmal steps of the leader propagation, where a so-called discrimination process will start when ground objects influence the further path of the leader. If that distance will reach the length of the striking distance (a distance before the fmal jump occurs), the lightning stroke will or will not occur. It will depend on the size of the space charge above the Charge Transfer System. Several methods for calculating the striking distance as a function of the magnitude of the lightning current of the return stroke have been developed [5]. These methods have quite large (up to almost 400%) variation of the striking distance for the same given value of lightning current. The following analytical expression is used widely by power transmission lines engineers: d = 10i”*65, (6) where d is the striking distance in [ml, and I is the amplitude of the lightning current in [kA] The striking distance together with the height of the sharpenedpoints determines the final length of the stepped leader and the size of the charge of the leader channel (without consideration of charge in multiple branches of the leader). This data can be used for an estimation of the space charge that might be generatedby the points during the last steps of the lightning leader. The space charge, qse, is a product of the point-discharge current and duration of that current flowing. Both magnitude and duration of the point-discharge current depend on the electric field strength, which is, in turn, a function of the height and charge of the steppedleader. Investigations of the point-discharge current in laboratory conditions resulted in development of the empirical equations as follows: I = klV2 or I = k2V(V - Vo), (7) where k, and kZ are constants,V is voltage applied across the gap in a laboratory test setup, and V. is the minimal voltage caused initiating the ionization process. Studies of the pointdischarge currents in natural weather conditions led to development of the expression similar to (6) but with considerationof the speedof the wind past the point: I = a(V - V0)(W2 + c2V2)ln, 63) where a, V. and c are constants,V is the potential difference between the points and their surroundings (this voltage is a function of the local electric field, height of the points and their geometry), and W is the speed of the wind past the points. When many points are used for the development of the space charge (like in the CTS), the question is how to estimate the total current flowing from such a system into the air. There are two extremesto answer this question. One of the extremes is that the total current from such a multitude of the points is equal or even less than the single point-discharge current. The other extreme is that the total current output fi-om such a system is equal to a single point-discharge current multiplied by the number of points in the system. There are some theoretical and laboratory studies supporting these extremes. The practical solution of this problem is that the total current 1096 from the multiple points is a function of spacing between the Equation (4). Having the engineeringdata adjacentpoints. The greater this distanceis, the closer the total of a structureto be protected (height.,size, specific current is to the product of a single point-discharge current architecturalor other requirementsor considerations)and and a number of the points. the assumedgeometry of the sharpenedpoints of the The point-discharge current has a pulsed nature. In each strike prevention system, calculate field enhancement pulse the current startsto flow from the point into surrounding coefficient, &, and electric field at the points. air at the moment when the electric field at the point will reach 5. Compute the minimal spacecharge,qsmrequired to have the critical value E,,. This current moving away from the point local electric field reduced to the minimal value Eomin. createsthe space charge, which reduces the field close to the This calculations can be performed using the Equation (4) point. But, because the current depends on the field at the or (5), where E,h/k, should be used as a value for Eomin, point, the weakened field will result in decreasingthe current. 6. Computethe multi-point dischargecurrent, IcTS,required At a certain point, there will be a situation of balance when to develop the spacecharge qsc.This can be done using there will be just enough current to create the spacecharge of the following approximate expression:qse= I,--& where such a size to produce the field at the point that supplies the t is the duration of the point-discharge current flow, which may be estimatedusing lightning data (leader current. But even that balanced situation will not last for any stepsaveragelength and speedof propagation, leader significant period, becauseof the local field change and space pausesduration, etc.). charge migration is influenced by the variables of wind and electric field. At the moment when the electric field reaches 7. Define the number of points required using the total systemcurrent, Ices, a single point-discharge current, Isp, the value E,,,h the current will cease.So the total duration of calculatedaccording to the Equation (7) or (S), and a the single pulse of the point-discharge current will be the system efficiency coefficient which value dependson interval between the moment of initiation and the ceasing of the point spacing and geometry and is usually obtained as the current. This time is strongly dependenton the location of result of laboratory testing. the lightning charges relative to the point and speed of the steppedleader propagation. Conclusion Engineering approach to design of the CTS The performance of a system preventing the occurrence of the The key point to a successful performance of a system direct lightning stroke into the structure protected by such a designedto prevent direct lightning strokes into a structure is system is described. The major engineering steps to design the computation of the number of points and their geometry to such a systemare proposed. produce a space charge which will shield the protected structure. The following design procedure can be offered to References define the major parametersof such a system: [l] Uman M. A. The lightning Discharge, Academic Press, 1. Determine of the worst-case situation. In most casesit Inc., Orlando, Florida, 1987 might be a situation where the lightning steppedleader is [2] ChalmersJ.A. Atmospheric Electricity, PergamonPress within the zone of two - three stepsbefore the “final Ltd., Oxford, 1967 jump”. In another situations the caseof the positive [3] Smythe,W. R., Static and Dynamic Electricity,Mc Grawlightning stroke with the main positive charge located at Hill, New York, 1950 the bottom of the thunderstorm cell. It might be a situation [4] Carpenter,R. B., Drabkin M. M., Improvement of where a thundercloud cell located in close proximity to Lightning Protection Again.qtDirect Lightning Strokes, the structure to be protected. In such a situation, a direct IEEE 1997 International Symposium qn Electromagnetic lightning stroke takes place betweenthe thundercloud cell Compatibility and a streamermoving upwards from the structure (in [5] Golde, R. H. (ed) Lightning Protection, Vol. 2, Academic most casesa tall building or an broadcastingtower) to be Press,New York, 1977 protected. 2. For a chosenworst casesituation, defme the data required for computation of the local electric field strength according to Equation (3). This data should include (if available) local data of lightning activity such as the frequency of occurrenceof lightning flashesto ground, probabilistic distribution of lightning currents in return strokes, chargesaccumulatedin thundercloudsand their distribution, etc. For example, parametersshown on Figure 1 of the simplified model of a thundercloudcell, may vary from location to location, from one country to another. 3. Compute the local electric field strength accordingto the 1097