INTRODUCTION
The ultra high voltage direct current (UHVDC) transmission technology in China has witnessed huge progress and massive achievements in the past decades, evolving from transmitting hydropower in the South at the very beginning to transmitting thermal power and clean energy in the North at present [1]. The environment and climate of the North and South are quite distinct, leading to some new issues confronted in developing high voltage direct current (HVDC) transmission in the North. It is found by using electromagnetic environment experiments that under the HVDC transmission lines in the North the ground total electric field (GTEF) at the side of negative pole shall be abnormally enhanced and the increase can be twice to three times as high as that in the normal case, when it is dry and air polluted [2, 3]. This phenomenon has rarely been observed in the South. It is believed to be associated with the airborne suspended particles which are charged and hardly moving in the ion flow field [2, 3]. Total electric field is the superposition of space-charge-free electric field stimulated by the stressed conductors and the space charge electric field generated by the ions. The GTEF is directly connected with the environment protection and sustainable development of UHVDC projects [4]. Hence, it is of key importance to control and mitigate the adverse effects of suspended particles on the total electric field of HVDC transmission lines. This paper is devoted to studying the particle charging mechanisms in the ion flow field of HVDC lines and their models, in order to lay foundations for constructing a reasonable mathematical model to predict GTEF. In addition, particle charging models also have a value in studying the deposition of charged particles onto the conductor surfaces, which changes the surface morphologies and thus affects the corona characteristics of conductors [5] and corona audible noise [6].
When a particle is exposed to ions in an electric field, these ions will collide with the particle and transfer their charges as a result of Brownian motion and electric-field driven motion. These two charging mechanisms can be found in lots of circumstances, such as electrostatic precipitation [7], electrical measurement of aerosols [8, 9] and charging of droplets and aerosols in cloud [10]. To comprehend and model these two mechanisms, some models have been brought forward in the literature. For field charging, Pauthenier and Moreau-Hanot derived the Pauthenier's model in 1932 [7] and it has been widely used since their work. However, some experimental results indicate that there exist appreciable discrepancies between this model and the experimental data [11‒13]. Besides, no one in aerosol science knew how to deal with a lossy particle which has permittivity and conductivity at the same time since Pauthenier's model is applicable to either purely dielectric or ideally conductive particle. These issues were addressed in Reference [14] by using Maxwell-Wagner relaxation theory and the so-called Maxwell-Wagner relaxation model was proposed. The validity of this new model has been demonstrated in unipolar case [14], but not in bipolar case yet.
For diffusion charging, the most widely used model is Fuchs' model and its improvements (hereafter all of them are called Fuchs' model). This type of model is first proposed by Fuchs [15] based on the work of Natanson [16] and later improved by Hoppel and Frick [17, 18], Stommel and Riebel [19]. The basic idea of Fuchs' model is that there is a limiting spherical shell dissecting the space around a particle into two non-overlapping zones, in one of which tightly close to the particle the ions behave as free molecules and in the other of which ions are treated as continuum, and on the interface of the two zones, namely the limiting spherical shell, the ionic fluxes in the two zones are matched. Fuchs' model has been validated by many experimental works [20‒23]. The other model is approximation solution of the Boltzmann equation based model [24‒26], which is too complex and rarely used relative to Fuchs' model.
To predict the GTEF in the presence of particles, some works incorporated the Pauthenier's model and Fuchs' model into the ion flow field of HVDC lines [27‒30]. There is a controversy on how to deal with the bipolar ions in the charging models. Some previous works intuitively thought a particle charging in the space full of bipolar ions is equivalent to one charging in a virtual space filled with net ion density, namely the algebraic sum of positive and negative ion densities. Models using this idea is termed equivalent unipolar charging models (EUCM). This idea may stem from the charging models in electrostatic precipitation where ions are unipolar. While some other works believe the net density flux, namely the algebraic sum of positive and negative ion density fluxes to the particle, should be used. Models using this idea is termed bipolar charging models (BCM). Since these two types of models have been applied in the charging of particles suspended around HVDC lines, it is of need to systematically compare them and justify their validities. While this point has not been addressed in previous works. It should be noted that in previous BCM models in References [27‒29], the Pauthenier's model, instead of the Maxwell-Wagner relaxation model, is employed.
In addition to those above-mentioned issues, experimental results show that GTEF in the presence of airborne suspended particles depends on relative humidity (RH). This coupling effect of airborne particles and humidity on GTEF has rarely been identified and reported in the literature and the physical mechanism underlying it needs to be explored.
To deal with the forgoing issues, firstly the EUCM and BCM for modelling field and diffusion charging mechanisms in bipolar ion environment are introduced in this paper, among which the Maxwell-Wagner relaxation mechanism is proposed to be inserted. Secondly, the EUCM and BCM are analysed and validated by comparisons with experimental data. Thirdly, the experimental result that GTEF in the presence of airborne suspended particles depends on RH is qualitatively analysed using the BCM. Lastly, a new charging model combining field and diffusion charging mechanism is proposed for airborne particles suspended around HVDC lines, which is validated by experimental results reported previously.
FUNDAMENTAL MODELS FOR PARTICLE CHARGING BY UNIPOLAR IONS
Diffusion charging – the Fuchs' model
When the electric field is ignored and a particle is suspended in a medium full of ions, some of these ions collide with the particle under the action of Brownian motion and thus charge the particle without the help of electric field. Fuchs' model has been proposed to describe the diffusion charging, in which the particle-ion attachment coefficient for diffusion charging R
D is [31, 32]
where R
D(a, q
D) is the attachment coefficient between ions and particles with charge q
D and radius a; D
i is the diffusion coefficient of ions and its value can be derived by use of Stokes-Einstein Relationship k
i = eD
i/k
b
T in which k
i is the ion mobility; k
b is the Boltzmann constant; T is the gas temperature in unit K; δ is the radius of limiting sphere, which is given by [31]
where λi is the mean free path. F
i is a ratio constant given by
In Equations (1) and (6), ϕ(r) is the electrostatic potential of the ions in the field of the particle at the distance r
In Fuchs' model, the values of mass, mobility, diffusion coefficient, mean free path and mean thermal velocity need to be known to calculate the particle charge q
D. These parameters are called ion properties. They are dependent on each other and given any two of them, the other three can be derived. Normally, mass and mobility are set to be known, and diffusion coefficient can be derived by the Stokes-Einstein Relationship, mean thermal velocity by Equation (4), and mean free path by
For particle charging in air, m a = 28.8 amu. amu is short for atomic mass unit and 1 amu = 1.66 × 10−27 kg.
Field charging – the Maxwell-Wagner relaxation model
When the Brownian motion of ions is ignored and a particle is suspended in a medium full of ions and stressed with an external electric field, these ions are driven by the field to deposit on the particle and thus it gets charged. The charging equation in Maxwell-Wagner relaxation model is formulated as
where
and
where σ1 and σ2 are the conductivities of the medium and particle, respectively. This τ MW is called Maxwell-Wagner relaxation time constant. More discussions on the Maxwell-Wagner relaxation model can be found in Reference [14].
FUNDAMENTAL MODELS FOR PARTICLE CHARGING BY BIPOLAR IONS
In this section, we will first introduce the two types of models. Especially the bipolar charging model that includes Maxwell-Wagner relaxation for bipolar ion environment is proposed.
Equivalent unipolar charging models
The EUCM for diffusion charging is formulated as
Bipolar charging models
Diffusion charging
The BCM for diffusion charging is formulated as
Let the total charging current entering into the particle be zero, namely dq
D/dt = 0, we have
Using the ion density ratio γ, the diffusion charging Equation (17) can be reformulated as
It can be inferred from this equation that given gas temperature, ion mobilities, particle radius, and positive or negative ion density, the ion density ratio γ is the decisive factor during the diffusion charging process. When γ→0 or +∞, Equation (20) reduces to Equation (8).
Field charging
The BCM for field charging is proposed based on the Maxwell-Wagner relaxation model and it is formulated as
Let the total charging current entering into the particle be zero, namely dq
E/dt = 0, we have
Define the state where dq
E/dt = 0 as an equilibrium one. The charge q
Eeq at the equilibrium state can be computed by Equation (22), which is given by
Since dq
Eeq/dt = 0, f(a,t) must be independent of time t. When the relaxation time τ
MW is finite and the charging time t
pc→∞, the Maxwell-Relaxation process is over and f(a,t) is constant in this case and given by
In practical cases, the charging time t
pc is finite. If τMW << t
pc, the Maxwell-Relaxation process is finished very quickly comparing to the charging process and f(a,t) is constant in the end and given by equation. If τMW >> t
pc, the Maxwell-Relaxation process is just started by the end of charging, f(a,t) is considered to be constant and given by
If τ MW is comparable to t pc, namely τ MW ∼ t pc, f(a,t) can be even considered as constant, and thus Equation (23) is not valid in this case. Based on forgoing analysis, our bipolar field charging model predicts that only when the relaxation time constant τ MW is incomparable to the charging time t pc, an equilibrium can be reached. In Pauthenier's model, Maxwell-Wagner relaxation is not existent, which can be considered as a limiting case where τMW >> t pc. Hence, in this model, the equilibrium state can always be reached. This is one of the differences between Pauthenier's Model and Maxwell-Wagner relaxation model, which is not covered in Reference [14].
Under the condition that f(a,t) can be considered constant, Equation (23) can be reformulated as
where q
s is the saturation charge given as
It can be inferred from this equation that given gas temperature, ion mobilities, particle radius, and positive or negative ion density, the ion density ratio γ is the decisive factor during the field charging process. When γ→0 or +∞, Equation (28) reduces to Equation (11).
The comparisons of the models and their validities
The biggest difference between EUCM and BCM is treating the charging current flowing into the particle in a distinct way. EUCM states that the net charge forms the charging current, while BCM argues that both positive and negative ion charge the charge at the same time and the net charging current equals to the total charging current. To deepen our understanding of this difference, a numerical study is conducted in the following to give a quantitative impression. The parameters used in the numerical study are listed in Table 1.
TABLE 1 The parameters used in this section
Parameter | Symbol | Unit | Value |
Vacuum permittivity | ε 0 | F/m | 8.85 × 10−12 |
Air permittivity | ε 1 | F/m | 1ε 0 |
Particle permittivity | ε 2 | F/m | 2.46ε 0 |
Air conductivity | σ 1 | S/m | 2 × 10−14 |
Particle conductivity | σ 2 | S/m | 4 × 10−16 |
Particle radius | a | μm | 0.075, 0.15, 5.5 |
Electric field | E 0 | kV/cm | 0.5 |
Particle charging time | t cp | s | 0.69 |
Air molecule mass | m a | amu | 29 |
Positive ion mass | m i+ | amu | 109 |
Negative ion mass | m i‒ | amu | 95 |
Positive ion mobility | k i+ | m2/(V s) | 1.33 × 10−4 |
Negative ion mobility | k i‒ | m2/(V s) | 1.85 × 10−4 |
Ionic density ratio | γ | / | 1∼+∞ |
Define dimensionless time τ and dimensionless charge ν as follows
Let γ varies from 1 to 106 and calculate the particle charges. The results are shown in Figure 1. It can be seen from Figure 1 that there are huge differences between the results predicted by EUCM and BCM. Firstly, when γ = 1, EUCM predicts νD = 0 and νE = 0 for the positive and negative ion densities cancelled each other and the net charge density n 0 = 0. However, BCM predicts νD = ‒0.24 and νE = ‒0.20 by τ = 100. Secondly, comparing to the case where γ = 1, the charging dynamics predicted by EUCM changes by a greater extent than that by BCM when γ = 3. Thirdly, equilibrium states can be clearly seen in BCM under the conditions γ = 3 and 10, while they do not appear in EUCM. And the time duration for reaching equilibrium state depends on γ. The larger the γ is, the longer time it takes for reaching the equilibrium state. Lastly, when γ ≥ 10, EUCM predicts that γ impacts the charging dynamics insignificantly, while BCM predicts that γ affects it appreciably.
[IMAGE OMITTED. SEE PDF]
In the following part, both EUCM and BCM are compared with experimental data to check their validities. References [33, 35] reported the bipolar charging characteristics of particles. Figure 2 plots the experimental results for particles of radius a = 0.15 μm and γ = 4.17, 13.91 and +∞. In this case, particles are mainly charged by diffusion. The predicted results given by EUCM and BCM are presented in Figure 2. Note field charging is omitted. It can be seen from Figure 2 that although there are deviations from the experimental data when γ = 13.91 and +∞, the predicted numerical results given by BCM agree well with them qualitatively for all γs. Especially, experimental results show that γ impacts the charging dynamics and equilibrium states exist, which are in good consistency with the predictions by BCM. On the contrary, it appears that γ has an insignificant effect on the charging and no equilibrium states occur.
[IMAGE OMITTED. SEE PDF]
Figure 3 plots the experimental results for particles of radius a = 5.5 μm and γ = 4.17, 13.91 and +∞. In this case, particles are mainly charged by electric field. The predicted results given by EUCM and BCM are presented in Figure 3. Note diffusion charging is omitted. It can be seen from Figure 3 that although there are appreciable deviations from the experimental data, the predicted numerical results given by BCM agree well with them qualitatively for all γs. Especially, experimental results show that γ impacts the charging dynamics and equilibrium states exist, which are in good consistency with the predictions by BCM. On the contrary, it appears that γ has an insignificant effect on the charging and no equilibrium states take place.
[IMAGE OMITTED. SEE PDF]
From the experimental results in Figures 2 and 3, it can be seen that there are two prominent features with regard to the charging behaviours of particles in bipolar ion environment. When γ ≥ 1,
-
the ion density ratio γ is a key parameter controlling the acquired charge of particles. Under given conditions, the particle charge goes up with increasing γ starting from 1;
-
as long as the charging time t pc is large enough, the particle charge can reach steady values, and the time duration for reaching the steady values are dependent on γ. The larger the γ is, the more time it costs.
When γ < 1, after replacing the γ with 1/γ in the two points above, they remain correct.
BCM is able to explain these features. It claims that the physical mechanism behind them is that positive and negative ion charging currents flow into the particle simultaneously. In the following, this point is illustrated in detail. Due to the fact that the positive ion mobility k i+ is a bit smaller than negative ion mobility k i‒, the ratio k i+/k i‒ is a bit less than 1. If the ratio γ is sufficiently large to ensure the conductivity ratio Γ > 1, at the very beginning of the charging process, the positive ionic charging current is larger than the negative ionic charging current, and consequently the particle is positively charged. As time goes by, the more positive charge the particle has, the greater repulsion on positive ions and larger attraction on negative ions it enforces, and thus the positive ion charging current goes down and negative ion charging current goes up. At some time constant, the two charging currents cancel each other, leading to the total charging current being zero, and thus an equilibrium state is reached and a steady charge is obtained. The bigger the γ is, the larger the ratio of the positive ion charging current to the negative one. As a consequence, the more time it takes in reaching an equilibrium state.
Based on the forgoing comparisons and analysis, it can be concluded that EUCM is not applicable to model the particle charging in mediums full of bipolar ions, such as particles suspended around HVDC lines, while BCM has the ability to do so.
Applications of the bipolar charging models
China Electric Power Research Institute has conducted a large number of experiments on the effects of airborne suspended particles on the GTEF under UHVDC lines. In hazy days, the GTEF could increase quite a lot and this increase depends heavily on the RH. As RH goes up, the increased GTEF goes down. Figures 4 and 5 display two typical results. They are obtained under the full-scale UHVDC test line at Beijing by using a GTEF measurement system. The detailed descriptions of this line and the GTEF measurement system can be found in References [36, 37]. In Figure 4a,b the GTEF distributions under RH = 80% in a heavily hazy day and RH = 40% in a lightly hazy day are presented, respectively. In Figure 5 the time series data of GTEF varying with RH in a hazy day are shown.
[IMAGE OMITTED. SEE PDF]
[IMAGE OMITTED. SEE PDF]
It can be seen from Figure 4a that in a heavily hazy day, the GTEF distribution is slightly symmetric under RH = 80%, but as can be seen from Figure 4b that it becomes extremely asymmetric under RH = 40% in the other slightly hazy day and both the maximum absolute negative GTEF and the one at ‒60 m increase appreciably. Besides, the electric field at ‒60 m is greater than that at ‒50 m, which rarely occurs in clear days. In a word, comparing with that in highly humid and heavily hazy days, particles affect the GTEF in a greater extent in dry and lightly hazy days. It can be seen from Figure 5 that the maximum absolute GTEF at the negative side reduces from 30 to 15 kV/m as RH increases from 35% to 65% in a hazy day. All these experimental results indicate that airborne suspended particles have an impact on GTEF and humidity can control this influence. To the authors' knowledge, this phenomenon has never been identified and reported in the literature. In the following part, a qualitative explanation is given by using BCM.
A number of experimental results obtained under the full-scale UHVDC test line in Beijing by China Electric Power Research Institute show that the GTEF distribution is nearly symmetric when RH = 60∼70% in clear summer days and the lower the RH is, the higher the asymmetry and the absolute GTEF at the negative side will be. It can be inferred from these observations that on the whole the ion density ratio γ in symmetric case is closer to one comparing to the asymmetric case, and the higher the asymmetry is, the more γ deviates from 1. One can deduce based on this inference and the forgoing analysis on BCM that as a whole, particles surrounding HVDC lines are charged at a lower level in symmetric case comparing to the asymmetric case, and the higher the asymmetry is, the higher level of charge the particles will have. Hence, at low RH, for example RH = 40%, particles tend to have more charges than that at high RH, for example RH = 80%. In addition, particle charge can be lowered by reducing the ion density γ on the whole as RH increases from 35% to 65%. As stated before, the physical mechanism behind this charge reduction is the adjustment of positive and negative ion charging current to the particles.
HYBRID CHARGING MODELS FOR PARTICLES SUSPENDED AROUND HVDC LINES
Normally, HVDC lines are in bipolar operation, and thus airborne suspended particles are charged by bipolar ions. Both diffusion charging and field charging mechanisms are existent for these particles around HVDC lines. In this section, an empirical field-diffusion charging model combining these two mechanisms is proposed, in which the Maxwell-Wagner relaxation model is adopted for field charging, Fuchs' model is used for diffusion charging, and charges obtained by these two models are summed:
This model is to be verified in the following part. Predictions of charging dynamics for particle radii of 0.15 and 5.5 μm given by our proposed field-diffusion charging model is presented and compared with experimental data in Figure 6.
[IMAGE OMITTED. SEE PDF]
In Figure 6a the data are extracted from Reference [33] and parameters for calculation are the same as those for Figure 2; in Figure 6b the data are extracted from Reference [35] and parameters for calculation are the same as those for Figure 3. Note that dimensionless electric field defined in Fjeld et al. 1990 differs between Figure 6a,b since electric field strength is held constant for different particle diameters. As can be seen from Figure 6 that the theoretical values of particle charging dynamics given by this model are in good agreement with the experimental data. Therefore, the proposed field-diffusion charging model is preliminarily validated. Its effectiveness in a wide range of parameters will be systematically investigated in a work in the near future.
CONCLUSION
The aim of this paper is to develop charging models for airborne suspended particles around HVDC lines.
Firstly, Equivalent unipolar charging models (EUCMs) and bipolar charging models (BCMs) for describing field and diffusion charging mechanisms in bipolar ion environment are introduced and the Maxwell-Wagner relaxation is proposed to be incorporated into the EUCM and BCM for field charging.
Secondly, the EUCMs and BCMs are analysed and validated by comparing them with experimental data reported in the literature. It is found that in BCMs, the ion density ratio γ is a key parameter in controlling the particle charge and as long as the charging time t pc is incomparable to the Maxwell-Wagner relaxation time τ MW, the particle charge can reach steady values, and the time duration for reaching the steady values is dependent on γ. The larger the γ is, the more time it costs to reach a steady value. While EUCM does not have these features. The results also show that BCMs are applicable to modelling the particle charging in bipolar ion environment, while EUCMs are not. The predictions made by BCM that takes into account the Maxwell-Wagner relaxation are in good agreement with experimental results.
Thirdly, the BCM is proposed to analyse the experimental results that the GTEF could increase quite a lot and this increase depends heavily on the RH. As RH goes up, the increased GTEF goes down. These are not understood before. It is demonstrated that the BCMs is able to qualitatively explain these experimental results with the help of the fact that the ion density ratio γ decides the particle charge in bipolar ion environment. The ion density ratio γ at medium RH is much closer to 1 than that at low RH on the whole. As RH goes up, γ reduces and so does the particle charge. Hence, GTEF declines and compared with that in highly humid and heavily hazy days, particles affect the GTEF by a greater extent in dry and slightly hazy days.
Finally yet importantly, a new charging model combining field and diffusion charging mechanism is proposed for airborne particles suspended around HVDC lines and preliminarily validated by experimental results.
Further researches can be conducted in lots of aspects, for instance the systematic investigation on the effectiveness of the new field-diffusion charging model in a wide range of parameters, the coupling of the new model with the corona ion flow field model of HVDC lines and predicting the GTEF under the lines.
ACKNOWLEDGEMENTS
This work was supported by the State Grid Corporation of China (52,010,118,001P).
The authors would like to express their gratitude to the referees for their precious advices.
Bian, X.M. , et al.: The role of low air pressure in the variation of negative corona‐generated space charge in a rod to plane electrode. High Vol. 3(2), 126–132 (2018)
Guo, J. , et al.: Experimental research on the total electric field and ion current density under level bipolar ±800 kV DC transmission lines. China Electric Power Research Institute (2009). Technical‐Report
Ju, Y. , He, K. : Experimental study on the impacts of airborne suspended particles on the ground total electric field under HVDC lines. China Electric Power Research Institute (2017). Technical‐Report
Ma, X.Q. , et al.: Research on 3‐D total electric field of crossing high voltage direct current transmission lines based on upstream finite element method. High Vol. 1–11 (2020). [DOI: https://dx.doi.org/10.1049/hve2.12025]
Zhu, J. , et al.: Experimental studies on effects of surface morphologies on corona characteristics of conductors subjected to positive DC voltages. High Vol. 5(4), 489–497 (2020)
Li, X.B. , et al.: Experimental investigation on correlation of corona‐induced vibration and audible noise from DC conductor. High Vol. 1(3), 115–121 (2016)
Oglesby, S. , Nichols, G. : Electrostatic Precipitation. Marcel Dekker, Inc., New York (1978)
Biskos, G. , Reavell, K. , Collings, N. : Description and theoretical analysis of a differential mobility spectrometer. Aerosol Sci. Tech. 39(6), 527–541 (2005)
Hinds, W. : Aerosol Technology: Properties, Behavior and Measurement of Airborne Particles,
Harrison, R. , Carslaw, K. : Ion‐aerosol‐cloud processes in the lower atmosphere. Rev. Geophy. 41(3), 1012 (2003)
Hewitt, G. : The charging of small particles for electrostatic precipitation. Trans. Amer. Insti. Electri. Eng. Part I. 76(31), 300–306 (1957)
Kirsch, A. , Zagnit'ko, A. : Field charging of fine aerosol particles by unipolar ions. Aero. Sci. Tech. 12(3), 465–470 (1990)
Smith, W. , et al.: Experimental investigations of fine particle charging by unipolar ions – a review. J. Aerosol. Sci. 9, 101–124 (1978)
He, K. , et al.: Effect of Maxwell–Wagner relaxation on field charging of particles. Aerosol Sci. Tech. 49(12), 1210–1221 (2015)
Fuchs, N. : On the charging of particles in atmospheric aerosols. Izvestiia Akademii Nauk SSSR. Seriia Geograficheskaia i Geofizi‐Cheskaia. 11, 341–348 (1947)
Natanson, G. : On the theory of the charging microscopic aerosol particles as a result of capture of gas ions. Sov. Phys. Tech. Phys. 5, 538–551 (1960)
Hoppel, W. , Frick, G. : Ion—aerosol attachment coefficients and the steady‐state charge distribution on aerosols in a bipolar ion environment. Aerosol Sci. Tech. 5(1), 1–21 (1986)
Hoppel, W. , Frick, G. : Comment on the comparison of measured and calculated values of ion aerosol attachment coefficients. Aerosol Sci. Tech. 11(3), 254–258 (1989)
Stommel, Y. , Riebel, U. : Comment on the calculation of the steady‐state charge distribution on aerosols < 100 nm by three body trapping method in a bipolar ion environment. Aerosol Sci. Tech. 41(9), 840–847 (2007)
Kirsch, A. , Zagnit'ko, A. : Diffusion charging of submicrometer aerosol particles by unipolar ions. J. Coll. Inter. Sci. 80, 111–117 (1981)
Adachi, M. , Kousaka, Y. , Okuyama, K. : Unipolar and bipolar diffusion charging of ultrafine aerosol particles. J Aerosol Sci. 16, 109–123 (1985)
Pui, D. , Fruin, S. , McMurry, P. : Unipolar diffusion charging of ultrafine aerosols. Aerosol Sci. Tech. 8, 173–187 (1988)
Biskos, G. , Reavell, K. , Collings, N. : Unipolar diffusion charging of aerosol particles in the transition regime. J. Aerosol Sci. 36(2), 247–265 (2005)
Gentry, J. , Brock, J. : Unipolar diffusion charging of small aerosol particles. J. Chem. Phys. 47, 64–69 (1967)
Marlow, W. , Brock, J. : Unipolar charging of small aerosol particles. J. Coll. Inter. Sci. 50(1), 32–38 (1975)
Huang, D. , Seinfeld, J. , Marlow, W. : BGK Equation solution of coagulation for large Knudsen number aerosols with a singular attractive contact potential. J. Coll. Inter. Sci. 140, 258–276 (1990)
Hoppel, W. : Study of drifting charged aerosols from HVDC lines. Electric Power Research Institute, California (1980). Technical‐Report
Zaffanella, L. : Field‐effect research at the high voltage transmission research center. Electric Power Research Institute, California (1991). Technical‐Report
Suda, T. , Sunaga, Y. : Calculation of large ion densities under HVDC transmission lines by the finite difference method. IEEE Trans. Pow. Deli. 10(4), 1896–1905 (1995)
Zou, Z. : Impacts of atmospheric particles on the ionised field of high voltage direct current conductor and application research. Ph.D. Thesis, North China Electric Power University, Beijing (2017)
Reischl, G.P. , et al.: Bipolar charging of ultrafine particles in the size range below 10 nm. J. Aerosol. Sci. 27(6), 931–949 (1996)
Nishida, R.T. , et al.: Modelling the effect of aerosol polydispersity on unipolar charging and measurement in low‐cost sensors. J. Aero. Sci. 130, 10–21 (2019)
Gauntt, R. : The continuum regime charging of submicrometer particles by bipolar air ions model and experiments. Ph.D. Thesis, Texas A&M University, USA (1982)
Nishida, R.T. , et al.: A simple method for measuring fine‐to‐ultrafine aerosols using bipolar charge equilibrium. ACS Sens. 5(2), 447–453 (2020)
Fjeld, R. , Wu, D. , McFarland, A. : Evaluation of continuum regime models for bipolar charging of particles in the 0.3‐13 µm diameter size range. IEEE Trans. Indus. Appl. 26(3), 523–528 (1990)
Zhao, L.X. , et al.: Altitude correction of radio interference of HVdc transmission lines part II: measured data analysis and altitude correction. IEEE Trans. Electromag. Compat. 59(1), 284–292 (2016)
Yan, S. , et al.: Research of measuring system for total electric field at ground level in complicated environment. Pow. Sys. Tech. 37(1), 183–189 (2013)
You have requested "on-the-fly" machine translation of selected content from our databases. This functionality is provided solely for your convenience and is in no way intended to replace human translation. Show full disclaimer
Neither ProQuest nor its licensors make any representations or warranties with respect to the translations. The translations are automatically generated "AS IS" and "AS AVAILABLE" and are not retained in our systems. PROQUEST AND ITS LICENSORS SPECIFICALLY DISCLAIM ANY AND ALL EXPRESS OR IMPLIED WARRANTIES, INCLUDING WITHOUT LIMITATION, ANY WARRANTIES FOR AVAILABILITY, ACCURACY, TIMELINESS, COMPLETENESS, NON-INFRINGMENT, MERCHANTABILITY OR FITNESS FOR A PARTICULAR PURPOSE. Your use of the translations is subject to all use restrictions contained in your Electronic Products License Agreement and by using the translation functionality you agree to forgo any and all claims against ProQuest or its licensors for your use of the translation functionality and any output derived there from. Hide full disclaimer
© 2021. This work is published under http://creativecommons.org/licenses/by-nc-nd/4.0/ (the "License"). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.
Abstract
Ground total electric field (GTEF) is a vital parameter in the field of electromagnetic environment of high voltage direct current (HVDC) lines. Some experimental works reported that airborne suspended particles can be charged in the corona ion flow of the lines and thus affect GTEF. This paper aims at studying the charging models for particles. Equivalent unipolar charging models (EUCMs) and bipolar charging models (BCMs) for describing field and diffusion charging mechanisms in bipolar ion environments are introduced and the Maxwell‐Wagner relaxation is proposed to be incorporated. Besides, the EUCMs and BCMs are analysed and validated through comparisons with experimental data. The results show that BCMs are applicable to describing the particle charging in a bipolar ion environment, while EUCMs are not. The predictions made by BCM that takes into account the Maxwell‐Wagner relaxation are in good agreement with experimental results. Moreover, the BCMs are proposed to analyse the experimental results about GTEF in the presence of particles, which are not understood before. It is demonstrated that the BCMs are able to qualitatively explain these results. Finally yet importantly, a new charging model combining field and diffusion charging mechanism is proposed for airborne suspended particles around HVDC lines and validated by experiments. The results show that the proposed hybrid field‐diffusion charging model is able to give predictions consistent with experiments.
You have requested "on-the-fly" machine translation of selected content from our databases. This functionality is provided solely for your convenience and is in no way intended to replace human translation. Show full disclaimer
Neither ProQuest nor its licensors make any representations or warranties with respect to the translations. The translations are automatically generated "AS IS" and "AS AVAILABLE" and are not retained in our systems. PROQUEST AND ITS LICENSORS SPECIFICALLY DISCLAIM ANY AND ALL EXPRESS OR IMPLIED WARRANTIES, INCLUDING WITHOUT LIMITATION, ANY WARRANTIES FOR AVAILABILITY, ACCURACY, TIMELINESS, COMPLETENESS, NON-INFRINGMENT, MERCHANTABILITY OR FITNESS FOR A PARTICULAR PURPOSE. Your use of the translations is subject to all use restrictions contained in your Electronic Products License Agreement and by using the translation functionality you agree to forgo any and all claims against ProQuest or its licensors for your use of the translation functionality and any output derived there from. Hide full disclaimer
Details

1 Department of High Voltage, China Electric Power Research Institute, Beijing, China
2 Department of Electrical Engineering, Tsinghua University, Beijing, China
3 State Grid Corporation of China, Beijing, China