3D Fluid Modeling of Positive Streamer Discharges in Air with Stochastic

3D Fluid Modeling of Positive Streamer Discharges in Air with Stochastic

3D fluid modeling of positive streamer discharges in air with stochastic photoionization Robert Marskar SINTEF Energy Research, Sem Sælands vei 11, 7034 Trondheim, Norway. E-mail: [email protected] Abstract. Streamer discharges are thin plasma channels that precede lightning and sparks. They usually evolve in bundles as stochastic tree-like structures and are inherently difficult to model due to their multiscale nature. In this paper, we perform a computer investigation of positive streamer discharges in air using contemporary photoionization models. We report on three-dimensional computer simulations under conditions that are available in laboratory spark-gap experiments. The solutions demonstrate a multiscale morphology consisting of streamer fluctuations, branching, and the formation of a discharge tree. Some branches are comparatively thick and noisy, while others are thin, smooth, and carry electric fields exceeding 250 kV/cm at their tips. Our results are consistent with past experiments and clarify the puzzling branching dynamics and stochastic morphology of positive streamer discharges. arXiv:2001.02072v2 [physics.plasm-ph] 9 Apr 2020 3D fluid modeling of positive streamer discharges in air with stochastic photoionization 2 1. Introduction has been shown that the TGFs precede the lightning stroke, i.e. TGFs are associated with the lightning Streamer discharges are fast, filamentary plasma leader or streamer corona, and not the stroke [42]. Var- discharges. They evolve from electron avalanches, ious branching mechanisms based on hydrodynamic in- are driven by local field enhancement at their tips, stabilities [43, 44], gas impurities [45{47], and stochas- and can propagate with or against the electric field. tic fluctuations [33, 35, 48{50] have also been proposed Streamers that propagate with the electric field are and investigated by the gas discharge community. called positive streamers and the ones that propagate Positive streamers (the type that propagates from against the electric field are called negative streamers. the anode to the cathode) also require a source of Streamers are the natural precursor of lightning and electrons in front of them. In air, which we study sparks, are used in a variety of industrial applications in this paper, the free electrons are supplied by [1{14], and also exist naturally as sprite discharges photoionization of molecular oxygen. For streamer in the upper atmosphere [15]. They usually do not discharges, photoionization can be modeled with appear in isolation but evolve inherently as three- continuum models [51{54] or discrete models [21, dimensional structures that often branch or form 23, 49, 50]. Beyond selecting discrete or continuum irregular tree structures [16{19]. The morphology of a photons, it is not clear which photoionization model streamer discharge is rich, and their structure is often one should use. In air, the classical Zheleznyak model reminiscent of the fractal-like structure of lightning, [55, 56] has been highly enabling for the streamer but the two are not the same nor do they share the discharge community, but it is derived under stationary same spatial and temporal scales. A review of streamer conditions which are not met for streamer discharges. discharges can be found in Ebert et al. [20]. More recently, Stephens et al. [24] has compiled a The three-dimensional multiscale structure of minimum model for photoionization in air. We remark streamer discharges restricts analytical treatment and that in fluid models the Zheleznyak model is often also makes them complicated to model. Streamer computed using a Helmholtz-based approach [51{54]. discharges are important in many aspects of plasma However, if the number of ionizing photons is not physics, but advanced computer modeling is required sufficiently high, continuum models lead to artificial in order to probe even elementary features. Streamer smoothing of the photoionization profile ahead of modeling mostly fits in two categories: Kinetic and the streamer. Recently, Bagheri and Teunissen fluid. Kinetic models evolve electrons as computational [50] compared the Zheleznyak model using discrete (super-)particles and contain all the ingredients for photons and continuum models. Although good describing streamer discharges. Various papers report agreement between the two approaches was found, the on particle modeling of streamer discharges, but results showed a strong sensitivity on the selection of all of these are limited to fairly short propagation photoionization parameters. The authors considered a lengths [21{25]. Fluid models, on the other hand, comparatively high and uniform background field and evolve truncated moments of the electron distribution did not include a field-dependent expression for the function. The computational cost of fluid models is emission efficiency [56]. lower than with kinetic models but they are also less Motivated by the broad applicability of streamer accurate, particularly in regions of low electron density. discharges and their inherent multiscale difficulties, we Fluid models for streamers are widely studied, see e.g. present a three-dimensional computer investigation of [26{35], but attempts to directly simulate e.g. spark- positive streamer discharges in atmospheric air using gap experiments in 3D have so far been unsuccessful state-of-the-art photoionization models [24]. Our goal due to the numerical effort involved. is to shed light on the fundamental multiscale structure Although widely studied in two spatial di- of streamer discharges when they are modeled by mensions, streamer discharges are inherently three- a fluid model, i.e. how they emerge, propagate, dimensional and are far from being completely un- and branch. In this paper we use a fluid model derstood. There is, for example, a current discus- for all charged species and include ion chemistry in sion regarding the production of X-rays and terrestrial the channel [57], which is important when modeling gamma-ray flashes (TGFs) in laboratory spark exper- timescales longer than some tens of nanoseconds. iments and lightning discharges [36{41]. Recently, it We also include supplemental results using the 3D fluid modeling of positive streamer discharges in air with stochastic photoionization 3 Zheleznyak photoionization model, and remark on an abundance of literature on the plasma chemistry of + + some modeling uncertainties relating to the use of both air, we remark that ion conversion O2 ! O4 together + photoionization models. Our numerical results are with electron-ion recombination e− + O4 ! O2 + O2 computed for 15 mm pin-plane gaps with an applied is one of the main electron loss mechanism in the voltage of 15 kV, i.e. for an experimentally available channel, and occurs on the timescale of some tens configuration. The results demonstrate streamer of nanoseconds. Some electron loss processes, like morphologies that are consistent with experiments, and dissociative electron attachment, are not included in thus we are able to clarify the role of photoionization the present study. The overall role of incomplete on the evolution and branching of positive streamer reaction sets for streamer evolution in air is not discharges in air. known. We nonetheless remark that Pancheshnyi and Starikovskii [57] have investigated the role of the 2. Physical model electron loss processes summarized in table1. The authors found that although the conditions in the The fluid streamer model is described by a set of drift- channel are influenced by the inclusion or absence diffusion-reaction equations coupled to the Poisson of electron loss processes, the streamer discharge equation for the electric field: dynamics changed insignificantly. @ne 2.1. Photoionization = −∇ · (vene − Derne) + Se; (1) @t In air, ionizing photons are generated through electron @ni impact excitation of molecular nitrogen to energy levels = Si; (2) @t above the ionization threshold of O , followed by ρ 2 r · E = ; (3) spontaneous emission. Photoionization of O2 provides 0 a source of free electron-ion pairs around the streamer where ne is the electron density, ve is the electron drift head. In this model, excited states of nitrogen are velocity, De is the electron diffusion coefficient, Se is first generated through collisions between electrons and the electron source term, and ni is the density of ions molecular nitrogen: of type i. E is the electric field where ρ is the space charge density. The ions are assumed to be immobile. e− + N2 ! e− + N2∗; (4) We consider air at standard atmospheric condi- where N∗ indicates an excited state of molecular tions T = 300 K, N = 2:45 × 1025 m 3 and use 2 − nitrogen. The excited nitrogen molecules then the plasma chemistry as given by Pancheshnyi and terminate through one of three processes: Radiation, Starikovskii [57], which solves for seven species: elec- + + + + + predissociation, or collisional quenching, i.e. trons, N2 ,O2 ,N4 ,O4 ,O2 N2, and O2−. The reac- tions are outlined in table1. In this table, the bottom two reactions denote lumped photoionization reactions N2∗ ! ? + γ; (5) which are discussed in detail in section 2.1. We also N∗ ! ?; (6) adopt the local field approximation and compute ki- 2 N∗ + M ! ; (7) netic coefficients by using BOLSIG+[58{60]. The com- 2 ? puted electron impact and attachment rates are shown where γ indicates an ionizing photon, M denotes either in figure1 as function of the electric field magnitude N2 or O2, and the target states ? are not of interest E = jEj. and are therefore not tracked further. Note that We incorporate

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