
Citation: | Donggui WU, Guanghai HU, S ZOLETNIK, Guosheng XU, Siye DING, Jianbin LIU, Linming SHAO, Yifeng WANG, Ran CHEN, Ning YAN, Yan CHAO, Ping WANG, D DUNAI, G ANDA, Liang CHEN, Liang WANG. Plasma edge density fluctuation measurements via lithium beam emission spectroscopy on EAST[J]. Plasma Science and Technology, 2022, 24(5): 055102. DOI: 10.1088/2058-6272/ac4d1e |
Accurate and stable measurements of edge density fluctuation with high spatio-temporal resolution have been achieved by the lithium beam emission spectroscopy (Li-BES) diagnostic on experimental and advanced superconducting tokamak (EAST). The new narrower band interference filter exhibits good ability to suppress background emission signal even under strong lithium coating of the tokamak. The raw data measured by channels at different spatial locations in avalanche photo diode camera with high chopping frequency show good consistency. Based on the detected experimental data, detailed information of density profile and fluctuation structures is obtained. A clear edge coherent mode in the auto-power spectrum is observed in pedestal region, which is regarded as the dominant factor for the strong pedestal density fluctuation amplitude. The cross-power spectrum analysis further excludes the additional effects of common-mode noises and non-local perturbation, demonstrating that the detected fluctuation is only caused by local density fluctuation. The normalized radial and poloidal wave-number spectra can specify the quantitative changes of radial wavenumber (kr) and poloidal wavenumber (kθ) during the pedestal density fluctuation phase. This new Li-BES system, which can provide more accurate experimental data, allows further studies of edge density fluctuation and complex transport process on EAST.
Water-electrode discharges can normally operate at atmospheric pressure and at a glow discharge mode [1], because the water electrode limits discharge current, and water evaporation has a cooling effect [2]. They are attracting more and more attentions due to abundance in reactive oxygen and nitrogen species [2, 3]. Accordingly, water-electrode glow discharges at atmospheric pressure have broad potentials in diversified application fields, including water purification and activation [4–8], nanomaterials synthesis [9, 10], catalysis [11, 12], and medicine [13, 14].
The plasma attachment to a water electrode is apt to be uniform, presenting a disk shape in the interface between the glow plasma and the water electrode [15]. Other than the uniform disk, some discrete spots can also be formed above a water electrode [16]. Under proper conditions, some self-organized patterns appear, especially above a water anode [17, 18]. A single ring is formed if the electrical conductivity of water anode is higher than 17.3 μS·cm-1 [19, 20]. The single ring is attributed to the distinctive rotating motion of a micro-discharge channel, resulting from the generated electronegative species during the discharge that poison the discharge [21]. Diameter of the single ring increases until reaching a maximum, and then decreases with the increase of discharge current [18]. Besides, the single-ring pattern varies and may transit to other discharge patterns with adjusting gas flow rate, discharge current, and gap width [22]. Although various parameters can affect pattern transitions, the determining factor is related to electrode and gas temperatures [22]. In fact, the formation mechanism of pattern is still not understood very well [23]. With a reaction–diffusion mechanism, patterns above a water anode are initiated with an autocatalytic reaction of electrons, which is dictated by discharge current and ionic strength [24].
More complex ring patterns have been observed above a water anode. For example, a double-ring pattern is formed with 1.0% NaCl solution used as a water anode [25]. Excited by an alternating-current (AC) sinusoidal voltage, the double-ring pattern has also been found under a low conductivity of 55 nS·cm-1 [26]. Compared to the double ring, a triple-ring pattern is only formed with a conductivity higher than several hundred μS·cm-1, which can be excited by a direct-current (DC) voltage [27], an asymmetric sine [28], or a square wave [29]. Up to now, concentric-ring patterns more than quadruple rings have not been reported in the literature.
In this work, concentric-ring patterns up to five rings are formed in the interface between the water anode and the glow discharge plasma. The ring number of the concentric-ring patterns increases with increasing ionic strength (electrical conductivity) and discharge current. These concentric-ring patterns are numerically reproduced based on the model of the autocatalytic reaction.
As shown in figure 1, a 3.0 mm diameter rod is made from tungsten, which has a flat end. The rod electrode is placed above a glass reservoir, which has a diameter (inner diameter) of about 75 mm. The reservoir with a depth of 75 mm is full of water, whose initial electrical conductivity is 330 μS·cm-1. The electrical conductivity of the water anode is measured by a conductivity tester (Inesa DDSJ-308F). The water reservoir is cooled by being placed in a water tank at a constant temperature of about 25 ℃. Water in the reservoir serves as the anode through electrical ground via an immersed metal mesh, and the rod acts as the cathode through being connected to a DC power source (Glassman EK15R40). In the circuit, a ballast resistor (R=50 kΩ) is used to restrict the discharge current. The gap width (d) is 5.0 mm. The gas discharge in the gap is carried out in atmospheric environment. Hence, the working gas is room air at a pressure of 1.013×105 Pa, with a temperature of 300 K and a humidity of 35%. A single-lens-reflex camera (Canon EOS 5D Mark IV) with variable exposure time (texp) is used to obtain water-anode discharge patterns at an oblique angle (45°). After being focused by a lens, light emission is transmitted by an optical fiber into the entrance slit of a spectrometer (PI ACTON SP2750) with a grating of 2400 grooves mm-1, thus optical emission spectrum can be collected. A voltage probe (Tektronix P6015A) is used to detect applied voltage (Va), and a current coil (Pearson 8600) is employed to measure discharge current (I). Waveforms of Va and I are monitored by a digital oscilloscope (Tektronix DPO4104). Typical waveforms of Va and I are presented in figure 1(b). It can be seen that no pulse can be found in Va and I, which means that the discharge operates in a continuous mode.
After atmospheric pressure glow discharge is initiated in the air gap, a radial-stripe pattern is formed at once above the water anode with I of 30.0 mA, as illustrated in figure 2. The radial-stripe pattern is surrounded by a ring as time elapses, leading to a single-ring pattern at 10 min. The ring number continuously increases from 15 to 25 min. That is to say, the concentric-ring pattern undergoes a scenario from a double ring (15 min), a triple ring (20 min), to a quadruple ring (25 min). For these concentric-ring patterns, the center is luminous. At last (30 min), a quintuple ring is time-invariantly stabilized above the water anode. Different to other concentric-ring patterns, the quintuple-ring pattern has a dark center. In a word, the ring number of the concentric-ring patterns increases with time elapsing, and up to five rings have been observed under the constant current of 30.0 mA. It is the first time that the quadruple-ring and the quintuple-ring patterns are observed in atmospheric pressure water-anode glow discharge.
As mentioned above, pattern becomes time-invariant after about half an hour operation of the discharge. However, the final time-invariant pattern evolves with varying discharge current, as presented in figure 3. At a low discharge current (5.0 mA), the pattern seems like a diffuse spot. Its diameter slightly increases with increasing discharge current. With a current of 10.0 mA, the diffuse-spot pattern transits to a single ring (the center is dark), which is similar to that reported by Shirai et al [30, 31]. When discharge current is increased to 14.0 mA, a diffuse spot appears in the center of the single-ring pattern. The diameter of the single ring increases and the central spot grows as discharge current is further elevated (16.0 mA). When discharge current reaches 20.0 mA, the central spot evolves into a new ring, resulting in a double-ring pattern. In a word, it seems that as discharge current increases, newcomer tends to appear in the center, which then transits to a new ring under a proper current. Interestingly, the pattern obeys this rule with further increasing discharge current, as can be seen for the transitions from the double-ring pattern (20.0 mA) to the triple ring (24.0 mA), from the triple-ring pattern (25.0 mA) to the quadruple ring (27.0 mA), and from the quadruple ring (28.0 mA) to the quintuple ring (30.0 mA). During these transitions, the ring number increases with increasing discharge current. Up to five concentric rings have been formed, and there is a central spot in the center of the quintuple ring at 31.0 mA. With further increasing discharge current, the concentric-ring patterns cannot be sustained above the water surface, and some discrete spots can be seen above the water anode (32.0 mA).
Electronegative species generated in the discharge, such as O, O3, H, OH, NO, NO2, NO3, NH, and NH2, can attach free electrons [21]. Resultantly, negative ions, mainly O-, H-, OH-, NO-, etc, will be deposited on the water surface [15, 32]. The deposited negative ions enhance the electric field in the interface between the bulk plasma and the water anode, resulting in a layer near the water surface, which is brighter than the plasma above it [15, 33]. When these negative ions are distributed nonuniformly, the region with more negative ions is brighter due to a higher enhanced field. In the bulk plasma, electrons are mainly produced near the axis of the discharge due to the high α (the first Townsend ionization coefficient) resulting from the maximal electric field in the center. In turn, more electrons will generate more electronegative species near the discharge axis. After generation, electrons and electronegative species near the axis diffuse to the rim. Hence, compared with the discharge rim, more electrons and electronegative species are abundant in the center. As a result, more negative ions tend to be deposited above the central region of the pattern. Therefore, newcomer is inclined to appear in the center of the concentric-ring patterns with increasing current.
As pointed out by Rumbach P et al [24], ionic strength (IS) and discharge current (I) mutually dictate the autocatalytic reaction of electrons. Hence, IS and I should be responsible for the pattern evolution mentioned before. Between them, IS is positively related with electrical conductivity. Hence, the electrical conductivity of the water anode is studied, as indicated in figure 4. Resulting from the generation of HNO3 and HNO2 [34, 35], the conductivity of the water anode increases with time, which reaches saturation after about 30 min operation. Moreover, the conductivity increases with increasing discharge current. In combination with figures 2 and 3, it can be deduced from figure 4 that pattern type varies with the variation of electrical conductivity (related with IS).
Figure 5 presents 300–800 nm scanned optical spectrum emitted from the discharge above the water anode. Besides the second positive system of N2(C3Πu→B3Πg) [32], spectral lines of Ar I (4p→4s) [36], and O I (3p3P→3s3S) at 844 nm [37], the first negative system of
The aforementioned concentric-ring patterns are simulated by the same method explored by Rumbach P et al [24]. From the Turing reaction–diffusion mechanism [43], it is believed that electrons are used as activators. Through the collision ionization of electrons, the autocatalytic reaction is realized, which is dictated by discharge current (I) and ionic strength (IS). With this model, the discharge patterns are given by the eigenfunctions (harmonics) of the cylindrical Laplacian (
Ylmn(r,z,θ)=Jm(κmlr)[Amlcos(mθ)+Bmlsin(mθ)]sin(knz), | (1) |
where Jm(kmlr) corresponds to the mth Bessel function of the first kind. (r, z, θ) are cylindrical coordinates.
The relationship between the l value and discharge current is listed in table 1. From table 1, one can see that the integer (l) increases with increasing discharge current. However, discharge current has a small variation range for a specific l value. Hence, all of the concentric-ring patterns formed in experiments have been numerically reproduced in simulations. However, at most five rings have been observed in experiments, which transit to discrete spots with current higher than 32 mA. This can be explained from the criteria for stability, which is related with the first Townsend ionization coefficient (α) [24]. α in the interfacial layer between the bulk plasma and the water anode is influenced by Tg. With a current higher than 32 mA, Tg is so high that stability criteria cannot be satisfied any more, resulting in the disappearance of the concentric-ring patterns. As a result, at most five concentric rings have been observed in our experiment. However, the maximal number of concentric rings is not limited according to formula (1). Hence, we believe that more rings could be obtained if the onset of thermal instability are restrained. Therefore, we will try our best to reduce the gas temperature in our future work through the usage of liquid nitrogen as a refrigerant, similar to that reported in the [44–46].
l | I (mA) | Pattern type |
l=2 | 10≤I < 14 | Single ring |
l=3 | 14≤I < 20 | Single ring with a central spot |
l=4 | 20≤I < 22 | Double ring |
l=5 | 22≤I < 24 | Double ring with a central spot |
l=6 | 24≤I < 25 | Triple ring |
l=7 | 25≤I < 27 | Triple ring with a central spot |
l=8 | 27≤I < 28 | Quadruple ring |
l=9 | 28≤I < 30 | Quadruple ring with a central spot |
l=10 | 30≤I < 31 | Quintuple ring |
l=11 | 31≤I < 32 | Quintuple ring with a central spot |
In summary, various concentric-ring patterns have been formed above the water anode of a glow discharge operated in atmospheric pressure air. The results reveal that the ring number of the patterns increases with time elapsing. Moreover, it increases with increasing discharge current. Among these concentric-ring patterns, it is the first time that the quadruple-ring and the quintuple-ring patterns are observed in water-anode glow discharge operated in atmospheric pressure air. For both the quadruple ring and the quintuple ring, the center is either luminous or dark, depending on the discharge current. It has been found that the electrical conductivity of the water anode, electron temperature, electron density, and gas temperature vary as a function of time elapses and increasing discharge current. At last, the various concentric-ring patterns are reproduced in simulations based on the autocatalytic reaction model dictated by ionic strength and discharge current.
The authors would like to acknowledge the support and contributions of the EAST team. The work is supported by the National Key R & D Program of China (Nos. 2017YFA0301300, 2019YFE03030000), National Natural Science Foundation of China (Nos. 11805238, 11775264, 11922513, U19A20113, 11905255, 12005004), Anhui Provincial Natural Science Foundation (No. 2008085QA38), Institute of Energy, Hefei Comprehensive National Science Center (No. GXXT-2020-004).
Data availability statement
The data that support the findings of this study are available from the corresponding authors upon reasonable request.
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l | I (mA) | Pattern type |
l=2 | 10≤I < 14 | Single ring |
l=3 | 14≤I < 20 | Single ring with a central spot |
l=4 | 20≤I < 22 | Double ring |
l=5 | 22≤I < 24 | Double ring with a central spot |
l=6 | 24≤I < 25 | Triple ring |
l=7 | 25≤I < 27 | Triple ring with a central spot |
l=8 | 27≤I < 28 | Quadruple ring |
l=9 | 28≤I < 30 | Quadruple ring with a central spot |
l=10 | 30≤I < 31 | Quintuple ring |
l=11 | 31≤I < 32 | Quintuple ring with a central spot |