The Interaction of Atmospheric Pressure Plasma DBDs and Jets with Liquid Covered Tissues: Fluxes of Reactants to Underlying Cells Wei Tian, Seth Norberg, Natalia Yu. Babaeva and Mark J. Kushner University of Michigan, 1301 Beal Ave, Ann Arbor, MI 48109-2122 USA [email protected], [email protected], [email protected], [email protected] Abstract: When treating tissue in biomedical applications, atmospheric pressure plasmas are typically not in direct contact with the tissue. Rather the plasma first contacts an overlying thin layer of liquid, typically water having dissolved gases and organic matter, such as blood-serum. The plasma generated reactivity is filtered by the liquid prior to reaching the tissue. We discuss results from a computational investigation of dielectric barrier discharge and plasma jet treatment of tissue through thin water layers. Keywords: atmospheric plasmas, DBDs, jets, liquids, plasma medicine, modeling 1. Introduction The use of atmospheric pressure plasmas for treating human tissue often involves cells and tissue covered by a hundreds of micron thick layer of liquid. This layer could be, for example, blood serum consisting of water with dissolved proteins and gases. The reactive species produced by the plasma (radicals, ions, photons) must penetrate through the liquid layer or react with the liquid before this reactivity reaches the underlying cells. The liquid has a finite vapor pressure and so evaporates into the adjacent air, which likely saturates the air directly above the liquid with water vapor. The plasma then interacts with this high humidity region prior to reaching the liquid. Biological liquids are not pristine water – they contain organic matter and dissolved gases. The reactivity of plasma produced radicals and ions with the liquid, and the transmission of reactivity to the underlying tissue, can be a sensitive function of these dissolved materials and gases. In this paper, we discuss a computational investigation of the interaction of atmospheric pressure dielectric barrier discharges (DBDs) sustained in air and plasma jets with liquid layers in contact with tissue. The liquid layer is water with dissolved gases (here, O2) and hydrocarbons. We find that liquid layers of only a few hundred microns are sufficient to dramatically change the character of the reactive species produced in the gas phase prior to reaching the underlying tissue. The fluences of the reactive species to the tissue are sensitive functions of the UV/VUV radiation produced by the plasma and which is incident onto the liquid layer, the organic content within the liquid and dissolved gases. 2. Description of the Model. In this investigation, we used the modeling platform nonPDPSIM, which addresses plasma, photon and neutral transport on a 2-dimensional unstructured mesh.[1] Poisson’s equation is solved for the electric potential coincident with the electron energy equation using rate coefficients obtained from stationary solutions of Boltzmann’s equation. Navier-Stokes equations are solved for neutral flow. In this model, the liquid is conceptually treated identically to a gas phase plasma – it merely has a neutral component with a liquid density. The transport of gas phase species into the liquid is governed by Henry’s law that specifies the saturated density of the gas component at the surface of the liquid. We also allow evaporation of liquid vapor into the gas phase. This is accomplished by holding the gas phase density of the evaporating species at the saturated vapor pressure at the surface of the liquid, and allowing diffusion to naturally transport the species into the gas phase. The reaction mechanism in water was developed from many sources, including the environmental chemistry literature.[2] Radiation transport in nonPDPSIM is addressed using a propagator – Green’s function technique. In this technique, the rate of absorption at r for by species j of photons emitted by species i at site r is Rj r Ai N i r e Nj r ji i r r 4 r Nk r k r 2 jk dr d 3r where ij is the photo-absorption cross section and Ai is the Einstein coefficient. The integral along the propaga tion path accounts for absorption prior to reaching r . This technique is directly applied to photons generated in the gas phase incident onto and into the liquid. Photon transport from the gas phase into the liquid is naturally accounted for by the line-of-sight integral for absorption along the mean-free-path. In these results, we do not account for reflection or refraction at the gas-liquid boundary. We are only including deep UV or VUV radiation in our transport model, which has a mean free path for absorption in the water of only a few microns, and so refraction effects will be small. The base case consists of a DBD sustained in atmospheric pressure air which is initially dry having a gap of 1.5 mm between the dielectric covered electrode and the surface of the water. The water layer is 200 m thick on top of a tissue like dielectric. The effective ground plane is 2 mm under the tissue. The water has 3 ppm dissolved O2. The water evaporates into the dry air with a vapor pressure of 27 Torr at the surface of the water. The applied voltage is -18 kV. The water is first allowed to evaporate for 10 ms. Three discharge pulses are then simulated at 100 Hz (10 ms separation) followed by a 1 s afterglow. In select cases, there is 30 ppm of an alkane-like hydrocarbon, designated as RH. Figure 1 – Positive ion densities during and after the third discharge pulse. (left) Total positive ion density in the gas phase at 6 ns into the pulse. (top enlargement) H2OL+ at 10 ns in the liquid layer. (bottom enlargement) H3OL+ at 40 ms. 3. DBDs Incident onto Liquid Covered Tissue Positive ions during and after the third discharge pulse are shown in Fig. 1. (The enlargements in the figure show the water layer above the tissue.) The total positive ion density in the gas phase is shown near its peak density (5 1014 cm-3) at about 6 ns into the discharge pulse. H2OL+ is shown near the peak of its density (3 1015 cm-3) at 10 ns. (The subscript L denotes a liquid species.) Positive ions which diffuse into the water produce H2OL+ by charge exchange with the equivalent of gas kinetic rate coefficients. This corresponds to a mean free path of at most only a few microns. A major contribution to H2OL+ is photoionization by UV/VUV radiation produced in the gas phase. The cross section for photolysis and photoionization of H2OL is near 10-17 cm2, and so at liquid densities, the photolysis also occurs within microns of the surface. The H2OL+ then quickly reacts with H2OL (again, with nearly the equivalent of gas kinetic rate coefficients) to form hydronium, H3OL+ and OHL. H3OL+ is a relatively stable species which then diffuses through the water layer to the tissue below. Its peak density at 40 ms in the afterglow (2 1015 cm-3) is nearly the same as for H2OL+. Figure 2 – OH, OHL and H2O2L during and after the third discharge pulse. (left) OH density in the gas phase at 10 ns into the pulse. (top) OHL at 10 ns in the liquid layer. (bottom) H2O2L at 70 ms. Hydrogen-peroxide is an important biocidal species in plasma activated water. H2O2L is dominantly a product of reactions between two OHL radicals. The densities of OH, OHL and H2O2L are shown in Fig. 2 during and after the 3rd discharge pulse. The gas phase distribution of OH is quite broad due to the accumulation and transport of unreacted OH from the previous discharge pulses and afterglows. The density of OH increases as the water surface is approached due to the higher density of H2O vapor resulting from evaporation. The density of OHL is maximum at the end of the discharge pulse at the surface of the water. This early peak is due to the photodissociation of H2OL by plasma produced UV/VUV fluxes and the charge exchange of H2OL+ with H2OL which forms H3OL+ and OHL. The lifetime of OHL is relatively short as it is rapidly consumed by formation of H2O2L. Since in the absence of organic matter H2O2L is relatively stable in water, its density accumulates from pulse to pulse as the H2O2L slowly diffuses through the water to the underlying tissue. The possible importance of photolysis in producing reactive species in the water is shown in Fig. 3 where the densities of H2O2L and O3L are plotted as a function of time 25 m below the surface of the water. Values are shown with and without photolysis reactions during the three discharge pulses and up to 0.15 s into the afterglow. The formation of H2O2L is dominated by OHL whose production is in turn significantly enhanced by photolysis. In the absence of photolysis, H2O2L is formed by gas phase OH or H2O2 that diffuses into the water and is 100 times lower in density than with photolysis. This is a general trend for any species whose origin can be traced to either OHL or HL. In contrast, O3L is formed either by diffusion of O3 from the gas phase into the water or reactions of OL with O2L in the water. Since neither of these processes is sensitive to the Figure 3 – Densities H2O2L and O3L during and after the three discharge pulses. Values are shown 25 m below the surface of the water with and without photolysis reactions. The times of the 3 pulses are noted by arrows. production of OHL or HL by photolysis, the density of O3L is essentially the same with or without photolysis. The presence of organic material in the water can significantly alter the reactive species. The reaction of potentially highly oxidizing species such as OH, H2O2 and O3 with organic molecules in the gas phase is nearly gas kinetic. In most cases, the reaction sequence begins by hydrogen abstraction from the organic species by the oxidizing species – for example, OH RH R H 2O . Here, RH represents an alkane-like hydrocarbon and R represents an alkyl-like radical. Note that similar reactions with aromatic or cyclic organic compounds also have nearly gas kinetic rate coefficients. The analogous reactions in water are also the equivalent of being nearly gas kinetic.[2] These reactions are the basis of many water purification systems. The densities of O3L are shown in Fig. 4 as a function of time 25 m below the surface of the water and 25 m above the tissue. Values are shown with and without 30 ppm of RH through the 1 second afterglow. In the absence of RH, O3L is relatively unreactive. After the discharge pulses and the diffusion of O3 into the water from the gas phase, the density of O3L becomes fairly uniform in the water layer. This uniformity is indicated by the densities of O3L at the top and bottom of the liquid layer converging. With RH, the density of O3L at the tissue is significantly reduced due to reactions with RH as the O3L diffuses through the water layer. Note that O3L is relatively slow reacting compared to other reactive oxygen species (ROS). Ultimately, it is the reactants that survive traversing the liquid layer or are produced during the traversal that Figure 4 – Densities O3L during and after the three discharge pulses and 1 s into the afterglow. Values are shown 25 m below the surface of the water and 25 m above the tissue; with and without 30 ppm RH. Figure 5 – Fluences of (top) ions and (bottom) neutrals to the underlying tissue after 1 s exposure following the three discharge pulses. Values are shown for the (blue) base case, (red) without UV/VUV photolysis and (green) with 30 ppm RH. are responsible for treating the underlying tissue. As a measure of this treatment potential, the fluxes of reactants to the tissue and cells underlying the liquid were integrated for 1 s after the discharge pulses. The resulting fluences (cm-2) for the base case, without UV/VUV fluxes and with RH are shown in Fig. 5. The fluences of positive ions to the tissue are dominated by hydronium (H3OL+) in all cases. It is likely that all positive ions striking the surface of the water produce H2OL+ which quickly forms H3OL+ in addition to the photoionization of water. H3OL+ is essentially a terminal species once formed. It is possible that H3OL+ may charge exchange to low ionization potential RH species, a process not included here. The fluences of negative ions are more sensitive to the details of the reaction mechanism than positive ions. For example, in the absence of UV/VUV fluxes the fluence of O3L- decreases by a factor of nearly 300. This decrease is ultimately a consequence of the decrease in the production of OHL in the absence of photolysis. The reaction sequence is: e H 2 OL eL H 2 O2 L OH L OH L OL O2 L O3 L . Here eL is a solvated electron (an electron loosely bound to water molecules). In this particular example, the production of O3L- is facilitated by the presence of dissolved O2L in the water. In the absence of dissolved O2L the fluence of O3L- further diminishes. The fluence of neutral species that trace their origin to production of OHL are generally reduced in the absence of the photolysis of H2OL, the most important of these species being H2O2L. Species that are not sensitive to the production of OH L, including the majority of reactive nitrogen species (RNS), change little in the absence of UV/VUV photolysis. An exception is NO2L- which increases in the absence of OHL production as it charge exchanges with OHL to form OHL-. With 30 ppm of RH, the fluences of ROS to the underlying tissue are significantly changed. Nearly all of the ROS with the exception of O3L and H3OL+ significantly decrease due to the rapid reaction with RH, beginning with simple hydrogen abstraction. The fluence of O3L is less diminished only because it is less reactive with RH however over many seconds its fluence would also decrease relative to non-ROS species. Since O3L is primarily formed by diffusion of O3 from the gas phase, it is naturally less sensitive to the liquid kinetics. The fluences of most RNS species, particularly HNO3L, are nearly insensitive to the presence of RH. The exception is NO2L-. The fluence of O3L- increases due to the reduction in the density of H2O2L, which would otherwise react with OL-, a precursor of O3L-. The lost reactivity to the tissue due to the reduction in the fluence of ROS is replaced by a large fluence of R L. We expect that the initially produced R L by reaction of ROS with RH undergoes a series of quasithermo-neutral reactions with other RH species. These reactions produce other forms of alkyl like radicals or selectively degrade the RH through chain breaking reactions. The terminal reaction of R L is likely with the underlying tissue. 4. Extension to plasma jets The interaction of plasma jets with thin water layers potentially and significantly differs from DBD treatment. The acidification of the liquid is likely dominated by direct injection of positive ions (or production of positive ions by photoionization) in DBDs, and so the acidification likely more rapid in DBDs than in plasma jets. The remote nature of the plasma jets diminishes production of OHL in at least two ways – reduced rates of photolysis and reduced production of H3OL+ through charge exchange of its precursor H2OL+. Reactive species which do not trace their production to OHL will therefore be more important, on a relative basis, in jets compared to DBD treatment. These species include RNS and O3L. The role of OHL is further diminished by the more rapid gas flow in jets which disperses the water vapor evaporated from the liquid surface. These results are sensitive to whether the plasma bullet produced by the jet extends to the surface of the liquid. If that is the case, the differences between DBD and plasma jet treatment of liquid covered tissue diminish. 5. Acknowledgements This work was supported by US Dept. of Energy Office of Fusion Energy Science and the US National Science Foundation. 6. References [1] Z. Xiong, E. Robert, V. Sarron, J.-M. Pouvesle and M. J. Kushner, J. Phys. D: Appl. Phys. 45, 275201 (2012). [2] G. V. Buxton, C. L. Greenstock, W. P. Helman, A. B. Ross, J. Phys. Chem. Ref. Data 17, 512 (1988).
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