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Publications

2018

  • Reply to Comment on `The case for in situ resource utilisation for oxygen production on Mars by non-equilibrium plasmas
    • Guerra Vasco
    • Silva Tiago
    • Ogloblina Polina
    • Grofulovic Marija
    • Terraz Loann
    • Lino da Silva Mário
    • Pintassilgo Carlos D.
    • Alves Luís L.
    • Guaitella Olivier
    Plasma Sources Science and Technology, IOP Publishing, 2018, 27. Not Available (10.1088/1361-6595/aaa570)
    DOI : 10.1088/1361-6595/aaa570
  • Study of Ionospheric Variability Using GNSS Observations
    • Jouan Taoufiq
    • Bouziani Mourad
    • Azzouzi Rachid
    • Amory-Mazaudier Christine
    Positioning, SCIRP, 2018 (9), pp.79-96. With the increasing number of applications of Global navigation satellite system, the modeling of the ionosphere is a crucial element for precise positioning. Indeed, the ionosphere delays the electromagnetic waves which pass through it and induces a delay of propagation related to the electronic density (TEC) Total Electronic Content and to the frequency of the wave. The impact of this ionospheric error often results in a poor determination of the stations position, particularly in strong solar activity. The first part of this paper focuses on a bibliographic study oriented first of all on the study of the ionosphere in relation to solar activity and secondly on the determination of the total electron content using GNSS measurements from the IGS network reference stations. Measurements were made on two permanent stations RABT, TETN. We selected years of GNSS measurements to evaluate the geomagnetic impact on the ionosphere, 2001, 2009 and 2013. A description of the ionospheric disturbances and geomagnetic storms was analyzed by determination of TEC, especially in high solar activity. The results show a strong dependence of the ionospheric activity with the geomagnetic activity. (10.4236/pos.2018.94006)
    DOI : 10.4236/pos.2018.94006
  • Analyzing the Magnetopause Internal Structure: New Possibilities Offered by MMS Tested in a Case Study
    • Rezeau Laurence
    • Belmont Gérard
    • Manuzzo Roberto
    • Aunai Nicolas
    • Dargent Jérémy
    Journal of Geophysical Research Space Physics, American Geophysical Union/Wiley, 2018, 123 (1), pp.227-241. We explore the structure of the magnetopause using a crossing observed by the Magnetospheric Multiscale (MMS) spacecraft on 16 October 2015. Several methods (minimum variance analysis, BV method, and constant velocity analysis) are first applied to compute the normal to the magnetopause considered as a whole. The different results obtained are not identical, and we show that the whole boundary is not stationary and not planar, so that basic assumptions of these methods are not well satisfied. We then analyze more finely the internal structure for investigating the departures from planarity. Using the basic mathematical definition of what is a one‐dimensional physical problem, we introduce a new single spacecraft method, called LNA (local normal analysis) for determining the varying normal, and we compare the results so obtained with those coming from the multispacecraft minimum directional derivative (MDD) tool developed by Shi et al. (2005). This last method gives the dimensionality of the magnetic variations from multipoint measurements and also allows estimating the direction of the local normal when the variations are locally 1‐D. This study shows that the magnetopause does include approximate one‐dimensional substructures but also two‐ and three‐dimensional structures. It also shows that the dimensionality of the magnetic variations can differ from the variations of other fields so that, at some places, the magnetic field can have a 1‐D structure although all the plasma variations do not verify the properties of a global one‐dimensional problem. A generalization of the MDD tool is proposed. (10.1002/2017JA024526)
    DOI : 10.1002/2017JA024526
  • Magnetic depression and electron transport in an ion-scale flux rope associated with Kelvin–Helmholtz waves
    • Tang Binbin
    • Li Wenya
    • Wang Chi
    • Dai Lei
    • Khotyaintsev Yuri
    • Lindqvist Per-Arne
    • Ergun Robert
    • Le Contel Olivier
    • Pollock Craig
    • Russell Christopher
    • Burch James
    Annales Geophysicae, European Geosciences Union, 2018, 36 (3), pp.879-889. We report an ion-scale magnetic flux rope (the size of the flux rope is ∼ 8.5 ion inertial lengths) at the trailing edge of Kelvin–Helmholtz (KH) waves observed by the Magnetospheric Multiscale (MMS) mission on 27 Septem-ber 2016, which is likely generated by multiple X-line re-connection. The currents of this flux rope are highly filamen-tary: in the central flux rope, the current flows are mainly parallel to the magnetic field, supporting a local magnetic field increase at about 7 nT, while at the edges the current filaments are predominantly along the antiparallel direction, which induce an opposing field that causes a significant magnetic depression along the axis direction (> 20 nT), meaning the overall magnetic field of this flux rope is depressed compared to the ambient magnetic field. Thus, this flux rope, accompanied by the plasma thermal pressure enhancement in the center, is referred to as a crater type. Intense lower hybrid drift waves (LHDWs) are found at the magnetospheric edge of the flux rope, and the wave potential is estimated to be ∼ 17 % of the electron temperature. Though LHDWs may be stabilized by the mechanism of electron resonance broadening , these waves could still effectively enable diffusive electron transports in the cross-field direction, corresponding to a local density dip. This indicates LHDWs could play important roles in the evolution of crater flux ropes. (10.5194/angeo-36-879-2018)
    DOI : 10.5194/angeo-36-879-2018
  • Plasma-activation of tap water using DBD for agronomy applications: Identification and quantification of long lifetime chemical species and production/consumption mechanisms
    • Judée Florian
    • Simon Stéphane
    • Bailly Christophe
    • Dufour Thierry
    Water Research, IWA Publishing/Elsevier, 2018, 133, pp.47-59. Cold atmospheric plasmas are weakly ionized gases that can be generated in ambient air. They produce energetic species (e.g. electrons, metastables) as well as reactive oxygen species, reactive nitrogen species, UV radiations and local electric field. Their interaction with a liquid such as tap water can hence change its chemical composition. The resulting " plasma-activated liquid " can meet many applications, including medicine and agriculture. Consequently, a complete experimental set of analytical techniques dedicated to the characterization of long lifetime chemical species has been implemented to characterize tap water treated using cold atmospheric plasma process and intended to agronomy applications. For that purpose, colorimetry and acid titrations are performed, considering acid-base equilibria, pH and temperature variations induced during plasma activation. 16 species are quantified and monitored: hydroxide and hydronium ions, ammonia and ammonium ions, orthophosphates, carbonate ions, nitrite and nitrate ions and hydrogen peroxide. The related consumption/production mechanisms are discussed. In parallel, a chemical model of electrical conductivity based on Kohlrausch's law has been developed to simulate the electrical conductivity of the plasma-activated tap water (PATW). Comparing its predictions with experimental measurements leads to a narrow fitting, hence supporting the self-sufficiency of the experimental set, i.e. the fact that all long lifetime radicals of interest present in PATW are characterized. Finally, to evaluate the potential of cold atmospheric plasmas for agriculture applications, tap water has been daily plasma-treated to irrigate lentils seeds. Then, seedlings lengths have been measured and compared with untreated tap water, showing an increase as high as 34.0% and 128.4% after 3 days and 6 days of activation respectively. The interaction mechanisms between plasma and tap water are discussed as well as their positive synergy on agronomic results. (10.1016/j.watres.2017.12.035)
    DOI : 10.1016/j.watres.2017.12.035
  • A turbulent cascade model of bounce averaged gyrokinetics
    • Xu S.
    • Morel Pierre
    • Gürcan Özgür D.
    Physics of Plasmas, American Institute of Physics, 2018, 25 (2), pp.022304. A shell model is derived for the description of nonlinear bounce averaged gyrokinetics, which is one of the simplest kinetic descriptions in magnetized plasmas. In order to validate the numerical implementation, detailed linear evolution of the system is compared with a linear benchmark based on solving the linear dispersion relation numerically. The resulting wave number spectrum, which extends over 34 decades, is shown to have a robust general structure to model parameters, such as dissipation or the ratio of linear energy injection to nonlinear transfer. In a range of wave numbers where the nonlinear transfer term is dominant, a power law spectrum, roughly of the form k−4 , is observed for the spectral electrostatic potential energy density. The model, being fully kinetic, can be used to obtain the free energy spectra for ion and electron distribution functions as functions of E. This model constitutes the first numerical implementation of a kinetic shell model. (10.1063/1.5020145)
    DOI : 10.1063/1.5020145
  • Experimental benchmark of kinetic simulations of capacitively coupled plasmas in molecular gases
    • Donkó Z.
    • Derzsi A.
    • Korolov Ihor
    • Hartmann P.
    • Brandt S.
    • Schulze J.
    • Berger B.
    • Koepke M.
    • Bruneau Bastien
    • Johnson Erik
    • Lafleur Trevor
    • Booth Jean-Paul
    • Gibson Andrew
    • O'Connell D.
    • Gans T.
    Plasma Physics and Controlled Fusion, IOP Publishing, 2018, 60 (1), pp.014010. We discuss the origin of uncertainties in the results of numerical simulations of low-temperature plasma sources, focusing on capacitively coupled plasmas. These sources can be operated in various gases/gas mixtures, over a wide domain of excitation frequency, voltage, and gas pressure. At low pressures, the non-equilibrium character of the charged particle transport prevails and particle-based simulations become the primary tools for their numerical description. The particle-in-cell method, complemented with Monte Carlo type description of collision processes, is a well-established approach for this purpose. Codes based on this technique have been developed by several authors/groups, and have been benchmarked with each other in some cases. Such benchmarking demonstrates the correctness of the codes, but the underlying physical model remains unvalidated. This is a key point, as this model should ideally account for all important plasma chemical reactions as well as for the plasma-surface interaction via including specific surface reaction coefficients (electron yields, sticking coefficients, etc). In order to test the models rigorously, comparison with experimental ?benchmark data? is necessary. Examples will be given regarding the studies of electron power absorption modes in O 2 , and CF 4 ?Ar discharges, as well as on the effect of modifications of the parameters of certain elementary processes on the computed discharge characteristics in O 2 capacitively coupled plasmas. (10.1088/1361-6587/aa8378)
    DOI : 10.1088/1361-6587/aa8378
  • Electron bulk acceleration and thermalization at Earth's quasi-perpendicular bow shock
    • Chen L.-J.
    • Wang S.
    • Wilson Iii L. B.
    • Schwartz S. J.
    • Bessho N.
    • Moore T. E.
    • Gershman D. J.
    • Giles B. L.
    • Malaspina D. M.
    • Wilder F. D.
    • Ergun R. E.
    • Hesse Michael
    • Lai H.
    • Russell C. T.
    • Strangeway R. J.
    • Torbert R. B.
    • Viñas A.-F.
    • Burch J. L.
    • Lee S.
    • Pollock C.
    • Dorelli J. C.
    • Paterson W. R.
    • Ahmadi N.
    • Goodrich K. A.
    • Lavraud B.
    • Le Contel Olivier
    • Khotyaintsev Y. V.
    • Lindqvist P.-A.
    • Boardsen S.
    • Wei H.
    • Le A.
    • Avanov L. A.
    Physical Review Letters, American Physical Society, 2018, 120, pp.225101. Electron heating at Earth's quasiperpendicular bow shock has been surmised to be due to the combined effects of a quasistatic electric potential and scattering through wave-particle interaction. Here we report the observation of electron distribution functions indicating a new electron heating process occurring at the leading edge of the shock front. Incident solar wind electrons are accelerated parallel to the magnetic field toward downstream, reaching an electron-ion relative drift speed exceeding the electron thermal speed. The bulk acceleration is associated with an electric field pulse embedded in a whistler-mode wave. The high electron-ion relative drift is relaxed primarily through a nonlinear current-driven instability. The relaxed distributions contain a beam traveling toward the shock as a remnant of the accelerated electrons. Similar distribution functions prevail throughout the shock transition layer, suggesting that the observed acceleration and thermalization is essential to the cross-shock electron heating. (10.1103/PhysRevLett.120.225101)
    DOI : 10.1103/PhysRevLett.120.225101
  • SMILEI : A collaborative, open-source, multi-purpose particle-in-cell code for plasma simulation
    • Derouillat J.
    • Beck A.
    • Pérez F.
    • Vinci T.
    • Chiaramello M.
    • Grassi A.
    • Flé M.
    • Bouchard G.
    • Plotnikov I.
    • Aunai Nicolas
    • Dargent Jérémy
    • Riconda C.
    • Grech M.
    Computer Physics Communications, Elsevier, 2018, 222, pp.351-373. SMILEI is a collaborative, open-source, object-oriented (C ) particle-in-cell code. To benefit from the latest advances in high-performance computing (HPC), SMILEI is co-developed by both physicists and HPC experts. The code's structures, capabilities, parallelization strategy and performances are discussed. Additional modules (e.g. to treat ionization or collisions), benchmarks and physics highlights are also presented. Multi-purpose and evolutive, SMILEI is applied today to a wide range of physics studies, from relativistic laser-plasma interaction to astrophysical plasmas. (10.1016/j.cpc.2017.09.024)
    DOI : 10.1016/j.cpc.2017.09.024
  • Wave Phenomena and Beam-Plasma Interactions at the Magnetopause Reconnection Region
    • Burch J. L.
    • Webster J. M.
    • Genestreti K. J.
    • Torbert R. B.
    • Giles B. L.
    • Fuselier S. A.
    • Dorelli J. C.
    • Rager A. C.
    • Phan T. D.
    • Allen R. C.
    • Chen L.-J.
    • Wang S.
    • Le Contel Olivier
    • Russell C. T.
    • Strangeway R. J.
    • Ergun R. E.
    • Jaynes A. N.
    • Lindqvist P.-A.
    • Graham D. B.
    • Wilder F. D.
    • Hwang K.-J.
    • Goldstein J.
    Journal of Geophysical Research Space Physics, American Geophysical Union/Wiley, 2018, 123 (2), pp.1118-1133. This paper reports on Magnetospheric Multiscale observations of whistler mode chorus and higher-frequency electrostatic waves near and within a reconnection diffusion region on 23 November 2016. The diffusion region is bounded by crescent-shaped electron distributions and associated dissipation just upstream of the X-line and by magnetic field-aligned currents and electric fields leading to dissipation near the electron stagnation point. Measurements were made southward of the X-line as determined by southward directed ion and electron jets. We show that electrostatic wave generation is due to magnetosheath electron beams formed by the electron jets as they interact with a cold background plasma and more energetic population of magnetospheric electrons. On the magnetosphere side of the X-line the electron beams are accompanied by a strong perpendicular electron temperature anisotropy, which is shown to be the source of an observed rising-tone whistler mode chorus event. We show that the apex of the chorus event and the onset of electrostatic waves coincide with the opening of magnetic field lines at the electron stagnation point. (10.1002/2017JA024789)
    DOI : 10.1002/2017JA024789
  • Multi-variable comprehensive analysis of two great geomagnetic storms of 2015
    • Kashcheyey Anton
    • Migoya-Orué Yenca
    • Amory-Mazaudier Christine
    • Fleury Rolland
    • Nava B.
    • Alazo-Cuartas K.
    • Radicella S.
    Journal of Geophysical Research Space Physics, American Geophysical Union/Wiley, 2018. During the year 2015 two great geomagnetic storms (Dst<-200nT) occurred on 17 March and 22 June. These two geomagnetic storms have similarities. They occurred during the same decreasing phase of the sunspot cycle 24. The interplanetary and magnetospheric environments were calm before the beginning of the storms. Both events were due to Coronal Mass Ejections (CME)and High Speed Solar Wind (HSSW). Variations of the solar wind velocity and the Bz component of the interplanetary magnetic field (IMF) were also similar. Two key features that are different for these storms are UT time of the beginning(04:45UT for 17March and 18:33UT for 22June) and season (equinox and solstice). The comparison of the impact of the storms on the Earth ionosphere and magnetosphere have been performed using diverse parameters including global ionospheric maps (GIMs) of vertical total electron content (VTEC), data from individual GNSS receivers, ionosondes, magnetometers and instruments from different space missions. Visualizing GIM data as the difference of VTEC between consecutive days allowed understanding better the effect of the storms as a function of time of the beginning of the storm and of the season. It is shown that the presence or absence of scintillations in GNSS signals during these 2 storms in African longitude sector is clearly related to the local time at a given station at the beginning of the storm. (10.1029/2017JA024900)
    DOI : 10.1029/2017JA024900
  • Fast gas heating and radial distribution of active species in nanosecond capillary discharge in pure nitrogen and N<SUB>2</SUB>:O<SUB>2</SUB> mixtures
    • Lepikhin N D
    • Popov N.A.
    • Starikovskaia Svetlana
    Plasma Sources Science and Technology, IOP Publishing, 2018, 27, pp.055005. Fast gas heating is studied experimentally and numerically using pulsed nanosecond capillary discharge in pure nitrogen and N2:O2 mixtures under the conditions of high specific deposited energy (up to 1 eV/molecule) and high reduced electric fields (100300 Td). Deposited energy, electric field and gas temperature are measured as functions of time. The radial distribution of active species is analyzed experimentally. The roles of processes involving excited N2 molecules and ions and N(2D) excited nitrogen species leading to heat release are analyzed using numerical modeling in the framework of 1D axial approximation. (10.1088/1361-6595/aab74e)
    DOI : 10.1088/1361-6595/aab74e
  • Poloidal asymmetries of flows in the Tore Supra tokamak
    • Vermare Laure
    • Hennequin Pascale
    • Gürcan Özgür D.
    • Garbet X.
    • Honoré Cyrille
    • Clairet F.
    • Giacalone J-C.
    • Morel Pierre
    • Storelli A.
    • Team Tore Supra
    Physics of Plasmas, American Institute of Physics, 2018, 25 (2), pp.020704. Simultaneous measurements of binormal velocity of density fluctuations using two separate Doppler backscattering systems at the low field side and at the top of the plasma show significant poloidal asymmetry. The measurements are performed in the core region between the radii 0.7&#8201;<&#8201;&#961;&#8201; < &#8201;0.95, over a limited number of L-mode discharges covering a wide range of plasma conditions in the Tore Supra tokamak. A possible generation mechanism by the ballooned structure of the underlying turbulence, in the form of convective cells, is proposed for explaining the observation of these poloidally asymmetric mean flows. (10.1063/1.5022122)
    DOI : 10.1063/1.5022122
  • Kinetic study of CO<SUB>2</SUB> plasmas under non-equilibrium conditions. II. Input of vibrational energy
    • Grofulovic Marija
    • Silva Tiago
    • Klarenaar Bart
    • Morillo-Candas Ana-Sofia
    • Guaitella Olivier
    • Engeln Richard
    • Pintassilgo C.D.
    • Guerra V.
    Plasma Sources Science and Technology, IOP Publishing, 2018. This is the second of two papers presenting the study of vibrational energy exchanges in non-equilibrium CO<sub>2</sub> plasmas in low-excitation conditions. The companion paper addresses a theoretical and experimental investigation of the time relaxation of ~70 individual vibrational levels of ground-state CO<sub>2</sub>(X<sup>1</sup>&#931;<sup> </sup>) molecules during the afterglow of a pulsed DC glow discharge, operating at pressures of a few Torr and discharge currents around 50 mA, where the rate coefficients for vibration-translation (V-T) and vibration-vibration (V-V) energy transfers among these levels are validated. Herein the investigation focus the active discharge, by extending the model with the inclusion of electron impact processes for vibrational excitation and de-excitation (e-V). The time-dependent calculated densities of the different vibrational levels are compared with experimental data obtained from time-resolved in situ Fourier Transform Infrared spectroscopy. It is shown that the vibrational temperature of the asymmetric stretching mode is always larger than the vibrational temperatures of the bending and symmetric stretching modes along the discharge pulse, the latter two remaining very nearly the same and close to the gas temperature. The general good agreement between the model predictions and the experimental results validates the e-V rate coefficients used and gives confidence that the proposed kinetic scheme provides a solid basis to understand the vibrational energy exchanges occurring in CO<sub>2</sub> plasmas. (10.1088/1361-6595/aadb60)
    DOI : 10.1088/1361-6595/aadb60
  • Electron Power-Law Spectra in Solar and Space Plasmas
    • Oka Mitsuo
    • Birn J.
    • Battaglia Marina
    • Chaston C. C.
    • Hatch S. M.
    • Livadiotis G.
    • Imada S.
    • Miyoshi Y.
    • Kuhar M.
    • Effenberger F.
    • Eriksson E.
    • Khotyaintsev Yu. V.
    • Retinò Alessandro
    Space Science Reviews, Springer Verlag, 2018, 214. Particles are accelerated to very high, non-thermal energies in solar and space plasma environments. While energy spectra of accelerated electrons often exhibit a power law, it remains unclear how electrons are accelerated to high energies and what processes determine the power-law index delta . Here, we review previous observations of the power-law index delta in a variety of different plasma environments with a particular focus on sub-relativistic electrons. It appears that in regions more closely related to magnetic reconnection (such as the `above-the-looptop' solar hard X-ray source and the plasma sheet in Earth's magnetotail), the spectra are typically soft (delta &gsim;4). This is in contrast to the typically hard spectra (delta &lsim;4) that are observed in coincidence with shocks. The difference implies that shocks are more efficient in producing a larger non-thermal fraction of electron energies when compared to magnetic reconnection. A caveat is that during active times in Earth's magnetotail, delta values seem spatially uniform in the plasma sheet, while power-law distributions still exist even in quiet times. The role of magnetotail reconnection in the electron power-law formation could therefore be confounded with these background conditions. Because different regions have been studied with different instrumentations and methodologies, we point out a need for more systematic and coordinated studies of power-law distributions for a better understanding of possible scaling laws in particle acceleration as well as their universality. (10.1007/s11214-018-0515-4)
    DOI : 10.1007/s11214-018-0515-4
  • Cometary plasma response to interplanetary corotating interaction regions during 2016 June–September: a quantitative study by the Rosetta Plasma Consortium
    • Hajra Rajkumar
    • Henri Pierre
    • Myllys Minna
    • Héritier Kevin
    • Galand Marina
    • Simon wedlund Cyril
    • Breuillard Hugo
    • Behar Etienne
    • Edberg Niklas
    • Goetz Charlotte
    • Nilsson Hans
    • Eriksson Anders I.
    • Goldstein Raymond
    • Tsurutani Bruce T
    • Moré Jérome
    • Vallières Xavier
    • Wattieaux Gaëtan
    Monthly Notices of the Royal Astronomical Society, Oxford University Press (OUP): Policy P - Oxford Open Option A, 2018, 480 (4), pp.4544-4556. Four interplanetary corotating interaction regions (CIRs) were identified during 2016 June–September by the Rosetta Plasma Consortium (RPC) monitoring in situ the plasma environment of the comet 67P/Churyumov–Gerasimenko (67P) at heliocentric distances of ∼3–3.8 au. The CIRs, formed in the interface region between low- and high-speed solar wind streams with speeds of ∼320–400 km s−1 and ∼580–640 km s−1, respectively, are characterized by relative increases in solar wind proton density by factors of ∼13–29, in proton temperature by ∼7–29, and in magnetic field by ∼1–4 with respect to the pre-CIR values. The CIR boundaries are well defined with interplanetary discontinuities. Out of 10 discontinuities, four are determined to be forward waves and five are reverse waves, propagating at ∼5–92 per cent of the magnetosonic speed at angles of ∼20°–87° relative to ambient magnetic field. Only one is identified to be a quasi-parallel forward shock with magnetosonic Mach number of ∼1.48 and shock normal angle of ∼41°. The cometary ionosphere response was monitored by Rosetta from cometocentric distances of ∼4–30 km. A quiet time plasma density map was developed by considering dependences on cometary latitude, longitude, and cometocentric distance of Rosetta observations before and after each of the CIR intervals. The CIRs lead to plasma density enhancements of ∼500–1000 per cent with respect to the quiet time reference level. Ionospheric modelling shows that increased ionization rate due to enhanced ionizing (>12–200 eV) electron impact is the prime cause of the large cometary plasma density enhancements during the CIRs. Plausible origin mechanisms of the cometary ionizing electron enhancements are discussed. (10.1093/mnras/sty2166)
    DOI : 10.1093/mnras/sty2166
  • The effects of secondary electron emission on plasma sheath characteristics and electron transport in an ExB discharge via kinetic simulations
    • Tavant Antoine
    • Croes Vivien
    • Lucken Romain
    • Lafleur Trevor
    • Bourdon Anne
    • Chabert Pascal
    Plasma Sources Science and Technology, IOP Publishing, 2018, 27 (12), pp.124001. Hall-effect thrusters, which are electrostatic devices based on an E B ´ plasma discharge, have successfully been used as satellite propulsion systems for the last few decades. However, the presence of anomalous electron cross-field transport is still poorly understood, and involves complex and strongly coupled mechanisms such as azimuthal electron drift instabilities and intense secondary electron emission (SEE) from the thruster walls. The present work focuses on the relative importance of these two phenomena. We use a 2D particle-in-cell/Monte Carlo collision model configured to simulate the radial-azimuthal directions near the thruster exit plane. A constant radial magnetic field and axial electric field are imposed, and electron drift instabilities are observed in the azimuthal (E B ´) direction. A simplified SEE model is implemented and an extensive parametric study is performed to directly determine the effect on electron transport. It is found that, for the operating conditions used in our simulations, SEE enhances the near-wall electron mobility by a factor 2, while reducing the bulk plasma mobility by about 20% (due to electron cooling). However, the dominant contribution to anomalous electron transport is still observed to be caused by electron drift instabilities driven by the E B ´ discharge configuration. SEE modifies the electron mobility profile, but the spatially-averaged value remains relatively constant. Three different operating regimes are identified depending on the SEE rate value: two that are stable, and a third which shows an oscillatory behaviour. In addition to electron transport, the kinetic simulations give new insight into the plasma sheath formation at the radial walls, and comparison with typical analytical sheath models demonstrate important differences. (10.1088/1361-6595/aaeccd)
    DOI : 10.1088/1361-6595/aaeccd
  • Solar Wind Turbulence Studies Using MMS Fast Plasma Investigation Data
    • Bandyopadhyay Riddhi
    • Chasapis A.
    • Chhiber R.
    • Parashar T. N.
    • Maruca B. A.
    • Matthaeus W. H.
    • Schwartz S. J.
    • Eriksson S.
    • Le Contel Olivier
    • Breuillard Hugo
    • Burch J. L.
    • Moore T. E.
    • Pollock C. J.
    • Giles B. L.
    • Paterson W. R.
    • Dorelli J. C.
    • Gershman D. J.
    • Torbert R. B.
    • Russell C. T.
    • Strangeway R. J.
    The Astrophysical Journal, American Astronomical Society, 2018, 866 (2), pp.81. Studies of solar wind turbulence traditionally employ high-resolution magnetic field data, but high-resolution measurements of ion and electron moments have been possible only recently. We report the first turbulence studies of ion and electron velocity moments accumulated in pristine solar wind by the Fast Plasma Investigation (FPI) instrument on board the Magnetospheric Multiscale Mission. Use of these data is made possible by a novel implementation of a frequency domain Hampel filter, described herein. After presenting procedures for processing of the data, we discuss statistical properties of solar wind turbulence extending into the kinetic range. Magnetic field fluctuations dominate electron and ion-velocity fluctuation spectra throughout the energy-containing and inertial ranges. However, a multispacecraft analysis indicates that at scales shorter than the ion inertial length, electron velocity fluctuations become larger than ion-velocity and magnetic field fluctuations. The kurtosis of ion-velocity peaks around a few ion inertial lengths and returns to a near Gaussian value at sub-ion scales. (10.3847/1538-4357/aade93)
    DOI : 10.3847/1538-4357/aade93
  • 3D Anisotropy of Solar Wind Turbulence, Tubes, or Ribbons?
    • Verdini Andrea
    • Grappin Roland
    • Alexandrova Olga
    • Lion Sonny
    The Astrophysical Journal, American Astronomical Society, 2018, 853 (1), pp.85. We study the anisotropy with respect to the local magnetic field of turbulent magnetic fluctuations at magnetofluid scales in the solar wind. Previous measurements in the fast solar wind obtained axisymmetric anisotropy, despite that the analysis method allows nonaxisymmetric structures. These results are probably contaminated by the wind expansion that introduces another symmetry axis, namely, the radial direction, as indicated by recent numerical simulations. These simulations also show that while the expansion is strong, the principal fluctuations are in the plane perpendicular to the radial direction. Using this property, we separate 11 yr of Wind spacecraft data into two subsets characterized by strong and weak expansion and determine the corresponding turbulence anisotropy. Under strong expansion, the small-scale anisotropy is consistent with the Goldreich & Sridhar critical balance. As in previous works, when the radial symmetry axis is not eliminated, the turbulent structures are field-aligned tubes. Under weak expansion, we find 3D anisotropy predicted by the Boldyrev model, that is, turbulent structures are ribbons and not tubes. However, the very basis of the Boldyrev phenomenology, namely, a cross-helicity increasing at small scales, is not observed in the solar wind: the origin of the ribbon formation is unknown. (10.3847/1538-4357/aaa433)
    DOI : 10.3847/1538-4357/aaa433
  • Compressible Magnetohydrodynamic Turbulence in the Earth’s Magnetosheath: Estimation of the Energy Cascade Rate Using in situ Spacecraft Data
    • Hadid Lina
    • Sahraoui Fouad
    • Galtier Sébastien
    • Huang S.Y.
    Physical Review Letters, American Physical Society, 2018, 120 (5), pp.055102. The first estimation of the energy cascade rate |εC| of magnetosheath turbulence is obtained using the CLUSTER and THEMIS spacecraft data and an exact law of compressible isothermal magnetohydrodynamics turbulence. |εC | is found to be of the order of 10−13J.m−3.s−1, at least two orders of magnitude larger than its value in the solar wind (order of 10−16 J.m−3.s−1 in the fast wind). Two types of turbulence are evidenced and shown to be dominated either by incompressible Alfénic or compressible magnetosonic-like fluctuations. Density fluctuations are shown to amplify the cascade rate and its spatial anisotropy in comparison with incompressible Alfv´enic turbulence. Furthermore, for compressible magnetosonic fluctuations, large cascade rates are found to lie mostly near the linear kinetic instability of the mirror mode. New empirical power-laws relating |C | to the turbulent Mach number and to the internal energy are evidenced. These new finding have potential applications in distant astrophysical plasmas that are not accessible to in situ measurements. (10.1103/PhysRevLett.120.055102)
    DOI : 10.1103/PhysRevLett.120.055102
  • Multi frequency matching for voltage waveform tailoring
    • Schmidt Frederik
    • Schulze J.
    • Johnson Erik
    • Booth Jean-Paul
    • Keil D.
    • French David M
    • Trieschmann Jan
    • Mussenbrock Thomas
    Plasma Sources Science and Technology, IOP Publishing, 2018, 27 (9), pp.095012. Customized voltage waveforms composed of a number of frequencies and used as the excitation of radio-frequency plasmas can control various plasma parameters such as energy distribution functions, homogeneity of the ion flux, or ionization dynamics. So far this technology, while being extensively studied in academia, has yet to be established in applications. One reason for this is the lack of a suitable multi frequency matching network that allows for maximum power absorption for each excitation frequency that is generated and transmitted via a single broadband amplifier. In this work, a method is introduced for designing such a network based on network theory and synthesis. Using this method, a circuit simulation is established that connects an exemplary matching network to an equivalent circuit plasma model of a capacitive radio-frequency discharge. It is found that for a range of gas pressures and number of excitation frequencies the matching conditions can be satisfied, which proves the functionality and feasibility of the proposed concept. Based on the proposed multi frequency impedance matching, tailored voltage waveforms can be used at an industrial level. (10.1088/1361-6595/aad2cd)
    DOI : 10.1088/1361-6595/aad2cd
  • How dielectric, metallic and liquid targets influence the evolution of electron properties in a pulsed He jet measured by Thomson and Raman scattering
    • Klarenaar Bart
    • Guaitella Olivier
    • Engeln Richard
    • Sobota Ana
    Plasma Sources Science and Technology, IOP Publishing, 2018, 27 (8), pp.085004. Thomson scattering using a Bragg grating notch filter is used to determine the electron properties of a pulsed, kHz-driven, non-thermal atmospheric pressure plasma jet in helium expanding in air. The plasma jet is allowed to freely expand or interact with targets with different electrical properties, i.e. glass, copper and water. With the same setup, Raman scattering is used to determine spatially- and time-resolved the densities and rotational temperatures of oxygen and nitrogen molecules entrained into the jet. Fast imaging is used to determine the development of the discharge in the plasma jet as well as its behavior in the plasma-target interaction zone. As the discharge approaches the target, the rise of electron density was followed by the fall of electron temperature. The discharge is influenced only over a few millimeters before it hits the target. The electron density and temperature during the spreading of the discharge on the low-permittivity target are measured to be resp. 2 × 1019 m&#8722;3 and &#8776;1 eV. During the return stroke on the high-permittivity and the metallic target the densities rise with a factor 1.5 resp. 2.2, and the temperature with a factor 2.5 for both cases. The discharges on the high- and low-permittivity targets extinguished soon after the initial impact of the ionization front, while the diffuse discharge on the metallic target extinguished only after the end of the voltage pulse (with a duration of 1 &#956;s). In the diffuse discharge the electron temperature reaches 3.4 eV, the gas temperature increases by approximately 100 K and the electron density increases by approximately a factor three with respect to before its formation. (10.1088/1361-6595/aad4d7)
    DOI : 10.1088/1361-6595/aad4d7
  • Low-Altitude Observations of Recurrent Short-Lived keV Ion Micro-Injections Inside the Diffuse Auroral Zone
    • Sauvaud J.-A.
    • Delcourt Dominique C.
    • Parrot Michel
    • Payan D.
    • Raita T.
    • Penou E.
    Journal of Geophysical Research Space Physics, American Geophysical Union/Wiley, 2018, 123, pp.2054–2063. The AMBRE experiment onboard the ocean topography mapper JASON‐3 aims at measuring the spacecraft potential as well as auroral particle precipitation using two top‐hat analyzers for electrons and ions in the 20 eV‐28 keV energy range. The JASON‐3 spacecraft has a nearly circular orbit at an altitude of 1336 km with an inclination of 66°, at times probing the equatorward part of the auroral oval in a nearly tangential manner upon leaving the outer radiation belt. In this region of space, during periods of enhanced geomagnetic activity with small or moderate storms, AMBRE detected recurrent “micro‐injections” of ions with energies in the 200 eV‐28 keV range and which exhibit clear time of flight dispersion. Ray tracing using single trajectory computations suggests that these ions are launched from a source located in the 8000‐12000 km altitudinal range and subsequently propagate downward toward the ionosphere. Such observations of quasi‐periodic dispersed downflowing ions are new and we argue that these structures could be produced by ion‐wave interactions at mid‐altitudes. (10.1002/2017JA025075)
    DOI : 10.1002/2017JA025075
  • Geocatalytic uptake of ozone onto natural mineral dust
    • Wang Xianjie
    • Romanias Manolis
    • Thevenet Frederic
    • Rousseau Antoine
    Catalysts, MDPI, 2018, 8 (7), pp.263. Beyond tailored and synthetic catalysts sought out for ozone decomposition, mineral dusts provide naturally mixed metal oxide materials. The steady-state uptake of O3 evidenced across a wide concentration range signifies the catalytic decomposition of O3. The geocatalytic properties of such natural mineral dust open up new perspectives in atmospheric chemistry and catalytic processes. (10.3390/catal8070263)
    DOI : 10.3390/catal8070263
  • The role of instability-enhanced friction on anomalous electron and ion transport in Hall-effect thrusters
    • Lafleur Trevor
    • Chabert Pascal
    Plasma Sources Science and Technology, IOP Publishing, 2018, 27 (1), pp.015003. Using a self-consistent 2D particle-in-cell (PIC) simulation, we investigate the electron transport in Hall-effect thrusters. The PIC simulation is explicit in time and models the axial and azimuthal directions of a thruster without using any artificial parametric or geometric scaling factors. The applied discharge voltage and external magnetic field causes electrons to drift in the azimuthal direction, and this drives an instability in the plasma that produces large amplitude oscillations in both the plasma density and azimuthal electric field. A Fourier transform in time and space shows that the oscillations follow a dispersion relation similiar to that for an ion acoustic instability (in agreement with a recent kinetic theory). Correlated with the presence of this instability is an enhanced electron cross-field transport; even in the absence of electron-wall collisions and secondary electron emission. The amplitude of plasma density oscillations (but not electric field oscillations) is found to decrease significantly in a region just downstream of the thruster exit (before then increasing again), and reaches levels similar to those measured experimentally with collective light scattering techniques. By taking relevant velocity moments of the electron distribution function in the PIC simulations, we reconstruct each term in the electron momentum conservation equation and demonstrate that anomalous electron transport can be explained entirely due to an instability-enhanced friction force between electrons and ions. This friction force acts as an additional momentum loss allowing electrons to cross the magnetic field, and as an accelerating force causing ions to rotate azimuthally in the same direction as the electrons. Clear evidence of ion-wave trapping in the instability electric field is observed. (10.1088/1361-6595/aa9efe)
    DOI : 10.1088/1361-6595/aa9efe