Abstract
By analyzing large quantities of discharges in the unfavorable ion drift direction, I-mode operation has been confirmed in the Experimental Advanced Superconducting Tokamak. During the L-mode to I-mode transition, the energy confinement is improvement substantially by the formation of a high-temperature edge pedestal, while the particle confinement remains almost identical to that in the L-mode. Similar with I-mode observations on other devices, the Er profiles obtained by the eight-channel Doppler backscattering system (DBS8) (Hu et al 2017 Rev. Sci. Instrum. 88 073504) show a deeper edge Er well in the I-mode than that in the L-mode. Additionally a weak coherent mode (WCM) with the frequency range of 40–150 kHz is observed at the edge plasma with the radial extent of about 2–3 cm. WCM could be observed in both density fluctuation and radial electric field fluctuation, and the bicoherence analyses showed significant couplings between WCM and high frequency turbulence, implying that the Er fluctuation and the caused flow shear from WCM should play an important role during I-mode operation. In addition, a low-frequency oscillation with a frequency range of 5–10 kHz is always accompanied with WCM, where the geodesic acoustic model intensity decreases or disappears. The evidence shows that the a low-frequency oscillation may be a novel kind of limited cycle oscillation but further investigation is needed to explain the new properties such as the harmonics and obvious magnetic perturbations.
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1. Introduction
As the H-mode with type-I edge localized modes (ELM) can generate unacceptable heat loads to the divertor and plasma-facing components, the I-mode is being explored as an alternative operating mode for future devices. The I-mode simultaneously features high-energy confinement similar to the H-mode, and low particle confinement as with the L-mode without ELMs, and this type of quiet pedestal can protect the divertor target from ELM heat flux with acceptable plasma energy confinement.
The I-mode was originally observed as an energy confinement improved mode in the 1990s [2]; currently, it has been widely investigated in the Alcator C-Mod [3–10], AUG [11–16] and DIII-D [17]. In unfavorable configurations [18], the L-mode to I-mode transition occurs when the heating power exceeds a certain threshold [19], and an edge energy transport barrier [7] is constructed accompanied by the weak coherent mode (WCM) [8–10, 13, 17] at the steepest temperature gradient region. In I-mode operation, an Er well [5, 6, 12, 17] forms at the edge of the plasma, and a stable temperature pedestal is simultaneously established [20, 21]. The poor particle confinement in the I-mode also contributes to a low core impurity level and sustains the operation performance [22, 23].
In this paper, the typical I-mode investigation in the Experimental Advanced Superconducting Tokamak (EAST) is presented for the first time. In 2014, the upper divertor was upgraded to full tungsten, while the lower divertor remained in carbon [24]. Consequently, all high- performance discharges were in the upper single null shape in order to reduce carbon impurities entering the main plasma [25]. Thus, operations most frequently have a clockwise toroidal field, such that the ion drift is directed away from the active X point, which provides a large amount of discharges for I-mode investigation. After numerous equilibrium parameters and fluctuation signals have been analyzed, the I-mode operation in EAST is confirmed. L-mode to I-mode transition can be triggered by all types of heating methods, and no heating preference is observed, which is consistent with the results in other tokamaks [11, 18]. In EAST, the WCM with the frequency of 40–150 kHz is observed in both density fluctuation and Er fluctuation at the plasma edge using the eight-channel Doppler backscattering system (DBS8) in I-mode operation, and a low frequency oscillation (5–10 kHz) is also observed when the WCM is present. The geodesic acoustic model (GAM) may disappear at the location where the WCM is most significant, while it can still exist at other locations in the I-mode on EAST.
The paper is organized as follows. In section 2, the experimental conditions and eight-channel Doppler backscattering system for the fluctuation investigation are presented. The identification of the main features of the I-mode, including the density, temperature and radial electric field profiles, and the WCM are shown in section 3. The nonlinear interaction among the WCM, the low-frequency oscillation and background turbulence by a bicoherence analysis is also included in section 3. The last section is the summary.
2. Experimental conditions and diagnostics
All experiments were performed in EAST [26–29], which is the first full superconducting divertor tokamak with m, m, MA, T. The ITER-like configuration of EAST makes this work more meaningful. EAST features complete RF wave heating, including lower hybrid wave heating (LHW), ion cyclotron resonance heating (ICRF), electron cyclotron resonance heating (ECRH), and two neutral beam injection (NBI) systems, one in the co-current direction while the other is in the counter.
The turbulence measurements are achieved by the DBS8 system [1], and it can simultaneously launch eight different frequencies (55, 57.5, 60, 62.5, 67.5, 70, 72.5 and 75 GHz) into the plasma. Because the probing beam is obliquely launched to the cutoff layer, the Doppler shift caused by the movement of the turbulence at the cutoff layer fd can be written as , where is the perpendicular velocity, and is the perpendicular wavenumber at the cutoff layer. In the laboratory frame, the perpendicular velocity is the sum of the turbulence phase velocity and background velocity, which is expressed as . In many cases, at the plasma edge, is much smaller than , and we can calculate the radial electric field as [30, 31].
The backscattered signal is obtained as the in-phase () and quadrature () of the I/Q mixer; this complex signal is written as . Then, the phase can be calculated as , and the signal amplitude is , where A corresponds to the density fluctuation level and the phase change rate corresponds to the perpendicular velocity of the cutoff layer (also to the radial electric field with the relationship of ) [31]. Two different methods are commonly used to extract the Doppler shift from the DBS signal: the center of gravity of the complex amplitude signal and the phase derivative method. In this study, we choose the phase derivative method to directly obtain the Doppler shift from the change in phase signal: [31], since it is the simplest method with the best time resolution.
DBS has been widely used for turbulence measurements with specific wavenumbers (4–15 for the system in this article). For the WCM, which is a type of larger-scale fluctuation that cannot be directly observed in the backscattered signal because its wavenumber is too small (less than )). However, the WCM can modulate the cutoff layer [13], and the DBS signal is sensitive to the oscillation caused by this modulation. Thus, WCM features such as the frequency can also be observed in DBS signals.
3. Experimental results and analysis
3.1. Identification of the I-mode
Currently, the I-mode in EAST can be achieved under parameter space with plasma currents of MA and toroidal magnetic field T under upper-single null (USN) geometries with an 'unfavorable' ion directed away from the active X-point [4]. In particular, in discharges with heating-powers above 1.8 MW and line-averaged electron densities above m−3, the features of the I-mode become quite distinct. No heating method preference is observed, and the L-mode to I-mode transition can be triggered by various heating methods. A typical example of the I-mode discharge 69327 is shown in figure 1. This discharge is accompanied with sawtooth instability. The main heating methods are NBI and ECRH, and the power of NBI is constant at 3 MW, while ECRH turns on at 2.58 s with the power of 0.3 MW, as exhibited in figure 1(b). The plasma current is approximately 500 kA, and the line-averaged density from the far infrared interferometer remains almost unchanged in the entire period as shown in figure 1(a). However, the core and edge electron temperature Te from electron cyclotron emissions (ECE) in figure 1(c) with stored energy in figure 1(e) increase to a new plateau approximately 2.6 s after the ECRH is turned on, which indicates the improvement of energy confinement. No density increase and no change in this transition were observed, which proves that the particle confinement remains similar to the L-mode. In the Er fluctuation, the WCM is observed at the edge of the plasma after this transition as shown in figure 1(f), which further identifies the I-mode operation. Clearer exhibitions of fluctuation modes have been shown in panels (g) for L-mode, (h) for the transition state, and (i) for I-mode. One notes that in this channel of the DBS8 system () the GAM disappears gradually during the transition from L-mode to I-mode, while a low-frequency oscillation (LFO) and the WCM develop out. Using the energy confinement calculation formula , a simple calculation shows that during this transition, the energy confinement time has a 7% increase from 36.1 to 38.6 ms.
To further confirm the I-mode, the density and temperature profiles were analyzed. The density profile from the reflectometer and electron temperature profile from Thomson scattering (TS) are shown in figure 2 at the plasma edge, where the L-mode is shown in blue and I-mode in red. Details on this discharge is shown in figure 3. It shows clearly that there is no significant difference in the density profile between the L-mode and I-mode as shown in figure 2(a). In the temperature profile, the electron temperature grows a lot and a clear temperature pedestal forms at the edge in the I-mode region, where the data used here are time-averaged to improve the signal-to-noise ratio of TS data.
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Standard image High-resolution image3.2. Features of the WCM
In EAST, the L-mode to I-mode transition is always accompanied by WCM with the frequency of 40–150 kHz, similar to the results from other devices. Specifically, the WCM in EAST exists in both density fluctuation and Er perturbation by modulating the perpendicular flow. Furthermore, the WCM is more prominent in the Er fluctuation with a wider radial range without the disturbance from background turbulence. But although the WCM is difficult to see in the density perturbation, it still shows up clearly outside of noise in the power spectrum. However, the WCM is quite weak in the magnetic fluctuation in EAST and because of the low sampling rate of the toroidal magnetic probe, the modulus analysis is currently difficult in EAST.
A typical example of a perturbation spectrum is shown in figure 3, and all the perturbation data here are from channel 67.5 GHz of the DBS8 at . From the ray tracing calculation, the perpendicular wavenumber is approximately 4–6 cm−1. As mentioned above, the low-wavenumber WCM can modulate the cutoff layer; then, it can be observed by the DBS system even at a higher perpendicular wavenumber. In this shot, a clear transition appears at approximately 3.6 s, and the discharge enters a strong I-mode after 3.7 s. Panel (a) shows the time evolution of LHW heating and stored energy . The evolutions of the density perturbation and radial electric field perturbation spectra are shown in panels (b) and (c), and the evolutions of the intensity of the density fluctuations and the radial electric field (Er) shear measured by DBS8 are exhibited in panel (d). Here the intensity of the density fluctuations is the integration of the frequency range 200–700 kHz to avoid the influence of the WCM (the frequency range is about 40–150 kHz). At 3.0 s, along with the increase of the LHW heating power from 300 kW to 1 MW the edge Er shear increases dramatically, and the density fluctuation level decreases slightly, but no obvious changes in the density fluctuation spectrum and the Er perturbation spectrum are observed. At 3.4 s, the increase of LHW heating power to 2.1 MW increases the edge Er shear further, and the density fluctuation level shows a dramatical decrease, then the WCM forms in both density fluctuations and Er perturbations, indicating the L-mode to I-mode transition. In the transition process, along with the development of the WCM, the GAM still exists in the Er fluctuation, and the frequency increases from 13 to 16 kHz with the increase of the edge temperature. It should be mentioned that the GAM is not always observed at the location where the WCM is most significant in I-mode operation, and it may disappear in nearly 60% of I-mode discharges at this location as shown in figure 1(f) and series (b)–(d) of figure 7, but it may still exist at other radial locations. Simultaneously, the WCM is more clear in the power spectrum as shown in figure 3(e) and (f), in which the comparison between L-mode (2.6–3 s) and I-mode (3.8–4.2 s) is exhibited and the peak at approximately 30–90 kHz is distinct both in the density and Er fluctuations in the I-mode.
The comparison of Er profiles in the L-mode and I-mode and the radial distribution of the WCM amplitude are shown in figure 4. For the typical I-mode parameter with T and the line-averaged density m−3, only four high-frequency channels of the DBS8 system inside the separatrix are shown here. In the I-mode, the edge Er well is much deeper than that in the L-mode at approximately , which is consistent with the reports in Alcator C-Mod [5, 6] and AUG [11, 12]. The red line in figure 4 is the radial distribution of the WCM amplitude. The WCM could only be distinctly observed in the 70 GHz and 72.5 GHz channels and be reluctantly found in the 75 GHz channel, suggesting that WCM locally exists inside the Er well and only covers several centimeters (2–3 cm) of the edge plasmas.
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Standard image High-resolution imageSpecifically, a low-frequency oscillation (LFO) with a frequency range of 5–10 kHz always accompanies the WCM in the EAST I-mode operation as shown in figure 1(f) (approximately 7 kHz) and in figures 3(a) and (b) (approximately 9 kHz). Many observations show that the LFO is another character of the I-mode operation beside the WCM in EAST, and it seems that LFO is always present instead of GAM at the position where WCM is generated. Unlike the GAM, the density perturbation and electron temperature perturbation of LFO are both distinct as well as the Er perturbation. Actually, the oscillation could be detected by nearly all diagnostics at the plasma edge, such as the magnetic pick-up coils, filterscopes, divertor probes, edge (ECE) channel, absolute extreme ultra violet diodes (AXUV), soft-X rays and even loop voltage coils. The power spectra of some signals during the I-mode in shot 75280 are shown in figure 5, and these distinct peaks suggest that the LFO has a large influence on the plasma edge region although its radial extent range is similar to the WCM. It should be noted that the second harmonic of LFO could also sometimes be seen, as shown in figures 5(a), (b) and (e). The toroidal symmetry feature of LFO could be easily confirmed from the magnetic coils (not shown), together with the fact that LFO is always present instead of GAM at the position where WCM is generated, implying that LFO is a novel kind of zonal flow during I-mode operation. However, there are several significant differences between LFO here and the quasiperiodic Er oscillation (also called limited-cycle oscillation, LCO, or dithering sometimes) appearing during L-H transition in EAST and other devices [32–35]. Firstly, LFO seems to not be purely electrostatic, as shown in figures 5(a) and (b); secondly, the typical LFO frequency is about 3 times larger than the LCO in EAST L-H transitions (2–3 kHz) [32] against the ion-ion collisional damping process of zonal flows; thirdly, the harmonics of zonal flow have never been reported before and is difficult to explain theoretically [36]. There must be some other process, such as coupling between the LFO and WCM that needs to be considered in the predator-prey model [37, 38] to explain these differences. More investigation is needed to draw definitive statements on the nature of LFO.
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Standard image High-resolution imageTo further investigate the interaction among the WCM, LFO and background turbulence, bicoherence analyses are used in this article. The cross-bicoherence of two signals and is defined as:
where is the Fourier transform of . Figure 6 presents the amplitude, amplitude and cross-bicoherence [39] from two channels with and without GAM in the DBS8 during I-mode shot 71078. Panels (a)–(d) are the channel with only LFO and panels (e)–(h) are the adjacent channel with LFO and GAM coexisting. In panel (a) without GAM, two lines are quite bright in figure 6(a): , and , which indicates strong nonlinear interactions among the LFO, WCM and background turbulence. This is the first observation of the coupling between the WCM and background turbulence. Also the enlargement of the low-frequency part in panel (b) shows a strong interaction between the WCM and LFO with a different color bar, which matches well with the report in AUG [13] but substitutes the GAM with the LFO which may strongly indicate that the LFO observed in EAST plays a similar role to the process of I-mode development as the GAM reported in AUG [13]. In the summed bicoherence, the peaks at approximately 9 kHz (LFO) and 35–74 kHz (WCM) are distinct, which strongly exceed the significance level, as shown in figure 6(d). To clearly show the intensity between LFO/WCM and high frequency turbulence (>200 kHz), the summed bicoherence with only high frequency components (f1 > 200 kHz) is also estimated as the red line in panel (d), which is about twice the summed bicoherence with all frequency components, indicating that the averaged coupling intensity between LFO/WCM and high frequency turbulence is actually much larger than that between LFO and WCM. These results imply that although the total density fluctuation level is decreasing during I-mode, the coupling between small scale turbulence and large scale coherence modes such as LFO and WCM still plays an important role, and WCM and LFO may both receive energy from background turbulence. For the channel with both GAM and LFO, two lines are observed in panel (g), referred to as and , respectively. Although WCM still exists in this channel, which could be speculated from the couplings between LFO and WCM in panel (f), no obvious coupling between the WCM and background turbulence is observed (the summed bicoherence at f3 = 30–70 kHz a little above the noise level is due to the contribution from the LFO/GAM and WCM couplings), again implying that the nonlinear three-wave interactions between WCM and turbulence mainly occur at the generation location of WCM.
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Standard image High-resolution image4. Summary
The I-mode operation in EAST has been verified, and it can be maintained for almost the entire flat top in one discharge. The unfavorable ion direction is also a key condition in the I-mode appearance as it is in Alcator C-Mod, AUG and DIII-D. The L-mode to I-mode transition can be triggered by various heating methods such as LHW heating, NBI, ICRF heating and ECRH as shown in figure 7, no heating preference is observed. However, a preference of high plasma currents is found in EAST. Many observations show that the L-mode to I-mode transition mainly occurs in the discharges with heating power >1.8 MW and the density > m−3. Generally, the I-mode has a stored energy improvement of nearly 50% based on the L-mode.
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Standard image High-resolution imageAs a typical characteristic of the I-mode, the WCM is observed in both density perturbation and Er perturbation in EAST. An Er well is observed at the plasma edge in the L-mode and I-mode regions, and it is deeper in the I-mode, as observed in AUG. The WCM is mainly localized inside the position of the Er well, and extends radially by only 2–3 cm, i.e. it could be distinctly observed at one or two channels for DBS diagnostics. Specifically, a low-frequency oscillation with a frequency range of 5–10 kHz is observed to always accompany the WCM in the I-mode operation, Which is regarded as another typical characteristic for the I-mode in EAST. It is possible that this is a novel kind of limited-cycle oscillation, but some unique features like the magnetic components and the harmonics still need more investigation. The GAM which is often observed in the L-mode region is not always observed in I-mode operation, and it may disappear in nearly 60% of I-mode discharges at the location where the WCM is the most significant, but it may still exist at other radial locations. Through the bicoherence analysis, it is found that both WCM and LFO strongly couple to the background turbulence in EAST, and interaction between the WCM and LFO also exists strongly which may indicate that the LFO may play a similar role in the process of I-mode development as the GAM in AUG, where GAM is found to both modulate and broaden the WCM. The bicoherence also implies that the coupling between WCM with turbulence is probably a key factor during the generation and saturation processes of WCM. Considering that the intrinsic instability of WCM is still unknown, the role of small scale turbulence should be paid more attention for future research on WCM.
Acknowledgments
The authors especially thank Dr Jerry Hughes for the helpful discussions and Dr Tianfu Zhou for his kind help in ECE DATA provision. The present work was supported in part by the National MCF Energy R&D Program under Grant No. 2017YFE0301204 and 2018YFE0311200, Natural Science Foundation of China under Grant No. 11635008 and the Anhui Provincial Natural Science Foundation No. 1708085QA23. We also acknowledge the EAST team for the support of these experiments.