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STREAMER INITIATION AND PROPAGATION IN WATER WITH THE ASSISTANCE OF BUBBLES AND ELECTRIC FIELD INITIATED RAREFACTION Wei Tiana) and Mark J. Kushnerb) a)Department of Nuclear Engineering and Radiological Sciences University of Michigan, Ann Arbor, MI 48109, USA [email protected] b)Department of Electrical Engineering and Computer Science University of Michigan, Ann Arbor, MI 48109, USA [email protected] November 2011 GEC * Work supported by Department of Energy Office of Fusion Energy Science AGENDA Introduction to plasma discharges in liquids Breakdown mechanism: Initiation and propagation Initiation: avalanche inside the bubble Propagation: electric field rarefaction Electric field emission Dielectric constant reduction Description of the model Concluding Remarks GEC2011 University of Michigan Institute for Plasma Science & Engr. DISCHARGES IN LIQUIDS Plasmas sustained in liquids and bubbles in liquids are efficient sources of chemically reactive radicals, such as O, H, OH and H2O2. Applications include pollution removal, sterilization and medical treatment. The mechanisms for initiation of plasmas in liquids are poorly known. K. Schoenbach et al, Plasma Sources Sci. Technol. 17 (2008) 024010 GEC2011 K. Shih et al, Plasma Process. Polym. 6 (2009), 729 University of Michigan Institute for Plasma Science & Engr. BREAKDOWN MECHANISM Two competing theories of liquid breakdown Electronic impact-ionization process within the bulk liquid Breakdown process inside gas phase Because of high molecular density in water, electronic impact-ionization should be virtually absent in bulk water in absence of E > many MV/cm Electrons are known to be solvated in water very rapidly – must ionize very efficiently before solvation GEC2011 Local, low-density regions are likely required for breakdown University of Michigan Institute for Plasma Science & Engr. BREAKDOWN MECHANISM Increasing static pressure reduces likelihood for bubble formation. Breakdown voltage increases due to lack of bubbles. 40-100 m bubbles B. Locke et al, Trans. Ind. Appl. 45, 630 (2009). “The electric field increases the instability increment for the stratification along the field.” “A strong electric field (1~100 MV/cm) can induce anisotropic decay into liquid and vapor phases for a fluid. ” GEC2011 A. L. Kupershtokh et al, Tech. Phys. Lett. 32, 634 (2006). Evidence that large electric fields produce regions of lower density in liquids due to polarization forces. University of Michigan Institute for Plasma Science & Engr. MODELING PLATFORM: nonPDPSIM Poisson’s equation: ( q j N j s ) j Transport of charged and neutral species: N j t j S j Electron Temperature (transport coefficient obtained from Boltzmann’s equation): ne 5 j E ne i K i N i e Te Te t 2 i GEC2011 University of Michigan Institute for Plasma Science & Engr. MODELING PLATFORM: nonPDPSIM Radiation transport and photoionization: S m (ri ) N m (ri ) 3 A N r ' G r ' , r d mk k k j k j i rj ' k Electric field emission 1 3 2 q E 0 work 0 J e ATk2 exp k T B k GEC2011 ri exp lk N l rj 'drj ' l r ' j G rj ' , ri 2 4 rj 'ri The field emission occurs at the gas-liquid interface The gas-liquid interface is treated as a solid surface Field enhanced thermionic emission University of Michigan Institute for Plasma Science & Engr. CONFIGURATION A “generic” point-to-plane, cylindrically symmetric geometry used for study. Powered electrode radius: 100 m Bubble in contact with electrode radius: 50 m. Outside boundaries grounded. Inside the bubble, H2O at 1 atm; Outside the bubble, H2OL at liquid density. Gas dielectric constant ε/ε0 ~ 1; Liquid dielectric constant ε/ε0 ~ 80. GEC2011 University of Michigan Institute for Plasma Science & Engr. REPRESENTATIVE REACTIONS Reactions in Liquid Water e + H 2 OL Liquid Water (H2OL) e ↔ e L + H 2 OL e L + H 2 OL ↔ H 2 OL Reactions in Water Vapor e e Field Emission Electric Field Rarefaction e + H2O → e + e + H2O+ e + H2O+ → H + OH e+H → e + H* H* → H + hn Water Vapor (H2O) hn + H2O → H2O+ + e Field Emission H 2 OL → e + H 2 OL + GEC2011 University of Michigan Institute for Plasma Science & Engr. INITIATION INSIDE BUBBLES t (ns) 0.50 1.00 0.0 ~ 1.0 Bubble ~ 50 m [e] Vmax=+10 kV with rise time of 1.0 ns (cm-3 ) Electric field emission occurs when strong electric field reaches the gas-liquid interface. EF The electric field concentrates on the axis and leads the avalanche. (MV/cm) Positive charges outline the discharge and produce the electric field. ρ (cm-3) MIN GEC2011 MAX University of Michigan Institute for Plasma Science & Engr. PROPAGATION: E-FIELD RAREFACTION A streamer can produce its own electric field enhancement at the conductive tip. The enhanced electric field at the tip exceeding a limit produces a phase-like transition, likely on an atomic scale. In the model, densities, compositions and other phase-related properties are changed to produce a low-density volume. The streamer extends itself into the new lowdensity area. The loop continues until the streamer reaches the grounded electrode. GEC2011 E-field Enhancement Phase Transition Low-density Regions Streamer Extension University of Michigan Institute for Plasma Science & Engr. 0.0 ~ 1.7 ns PROPAGATION Threshold ~ 1 MV/cm Vmax=+10 kV with rise time of 1.0 ns Streamer initiates inside the bubble first. The electric field triggers the phase transition, in which the density decreases by about 3 orders. Streamer extends itself into the changed area due to high E/N. The potential is expelled ahead and compressed to produce strong electric field. This mechanism makes the streamer propagating into water by itself. Flood represents the electron density Lines represent the electric potentials GEC2011 MIN University of Michigan Institute for Plasma Science & Engr. PROPAGATION: EFIELD EMISSION Vmax=+10 kV with rise time of 1.0 ns The electric field is produced by positive charges and enhanced by dielectric constant difference. The positive charge density is large due to electronic impact ionization at strong electric field. 0.0 ~ 1.7 ns A strong electric field emission occurs at the top interface because the electric field is strong there. The emitted electrons intensify the electronic impact ionization so that the positive charge density is increased. MIN MAX GEC2011 ρ (cm-3) EF (MV/cm) Se (cm-3s-1) University of Michigan Institute for Plasma Science & Engr. ELECTRIC FIELD EMISSION 1 3 2 q E 0 work 0 2 J e ATk exp k T B k The work function used for liquid water is 1.7 ~ 1.9 eV. Larger emission current results in larger propagation velocity. Work Function Streamer Velocity 1.7 eV 3.82×107 cm/s 1.8 eV 1.44×107 cm/s 1.9 eV 0.37×107 cm/s GEC2011 The field emission current will not affect the streamer propagation until it reaches 0.1 A/cm2. University of Michigan Institute for Plasma Science & Engr. PROPAGATION:SMALLER BUBBLE 0.0 ~ 1.1 ns Bubble ~ 20 um Vmax=+30 kV with rise time of 1 ns The bubble is so small that the electron loss is huge and electron impact ionization cannot help avalanche. Stronger field emission is needed to provide more seed electrons. Flood represents the electron density Lines represent the electric potentials GEC2011 University of Michigan Institute for Plasma Science & Engr. PROPAGATION: DIELECTRIC REDUCTION K. Schoenbach et al, Plasma Sources Sci. Technol. 17 (2008) 024010 0.0 ~ 1.6 ns 0.0 ~ 1.6 ns The dielectric constant is not reduced much until the electric field reaches 5 MV/cm (Emax ~ 1.5 MV/cm in the case). The streamer becomes a little wider due to the dielectric constant reduction but not affected much. Generally, it does not affect much. MIN MAX [e] (cm-3) ε/ε0 University of Michigan Institute for Plasma Science & Engr. CONCLUDING REMARKS The breakdown mechanism consists of two processes, initiation inside the bubble and propagation due to the electric field rarefaction. Electric field rarefaction may contribute to creating a low density channel, in which the streamer can propagate. Field emission contributes to the propagation process and becomes more important for smaller bubbles. The dielectric constant reduction is not important at the electric field ~ 1 MV/cm. GEC2011 University of Michigan Institute for Plasma Science & Engr.