Prime pagine RA2010FUS:Copia di Layout 1 - ENEA - Fusione
Prime pagine RA2010FUS:Copia di Layout 1 - ENEA - Fusione
Prime pagine RA2010FUS:Copia di Layout 1 - ENEA - Fusione
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040<br />
progress report<br />
2010<br />
2<br />
Pulse # 73744<br />
a)<br />
6<br />
S(μW/sr nm) Ipla (MA)<br />
1<br />
0<br />
0.4<br />
0.2<br />
0<br />
0<br />
4<br />
Time (s)<br />
Figure 1.49 – After a <strong>di</strong>sruption, in the absence of plasma, the<br />
extra light seen by the Thomson scattering detectors is thought<br />
to be due to the interaction between the laser pulses and dust<br />
particles later released by the wall. a) plasma current, b)<br />
average dust signal of the 4th spectral channel of every core<br />
spectrometer<br />
b)<br />
8<br />
P thr (MW)<br />
4<br />
2<br />
0<br />
0<br />
H e conc scan shots<br />
P thr, scal 08<br />
D references<br />
40 80<br />
H e concentration (%)<br />
Figure 1.50 – Power threshold (P thr ) obtained with NBI<br />
as function of helium concentration for both He and D<br />
reference <strong>di</strong>scharges at 1.7 MA/1.8 T. All the<br />
configurations had the same low δ≈0.25 shape, and<br />
densities variations 2.3–2.8×10 19 m –3<br />
Dust<br />
Ra<strong>di</strong>ation has been observed by the high resolution Thomson scattering (HRTS) system after plasma<br />
terminations, which reveals the presence of impurities along the beam path released by the wall during the<br />
<strong>di</strong>sruptive power quench, known as dust [1.92]. This ra<strong>di</strong>ation has been carefully analyzed and, due to its<br />
spectral features, seems not to be due to pure scattering but to a more complicated laser–matter interaction.<br />
The intensity is compatible with the expected <strong>di</strong>mension of dust grains and the temporal decay shows two<br />
timescales (fig. 1.49). Averaging the values of the peaks in the signal traces over all spectrometers, one can have<br />
a rough estimate of the dust content. The dust lasts for about 1.5 seconds after the <strong>di</strong>sruption. A preliminary<br />
<strong>di</strong>stribution of the signals has been obtained and compared with a compound Poisson <strong>di</strong>stribution.<br />
L to H mode transition<br />
Data taken during the 2009 JET helium campaign have been fully analyzed and presented at the 2010 EPS<br />
Conference [1.93]. L–H in helium has been observed as a transition to Type III ELMs with a small<br />
confinement improvement associated with a small edge pedestal. Helium concentration varied from 1 to 87%<br />
and was found to have little impact on the power threshold (fig. 1.50). This is in line with recent ASDEX–U<br />
stu<strong>di</strong>es, but in contrast with JET 2001 results, which showed that He plasmas had a 40% higher threshold than<br />
D equivalents. However, it should be noted that the 2001 comparison was performed at lower density<br />
(∼2.0×10 19 m –3 ) than the more recent data base (∼2.3–2.8×10 19 m –3 ). If a slope inversion of the density<br />
dependence were at play, the 2009 and the 2001 results might be reconciled. Unfortunately, helium data at low<br />
density are not available in the 2009 database. Although physics understan<strong>di</strong>ng still remains to be improved<br />
and further experiments will have to be carried out, recent results seem to encourage the helium choice for the<br />
non–nuclear phase of ITER.<br />
Safety factor profile determination<br />
Profiles of the safety factor are determined by the motional stark effect (MSE) <strong>di</strong>agnostic combined with<br />
equilibrium reconstruction. The positions of low–order rational surfaces q=m/n (from 2/1 to 4/3, m and n<br />
being the poloidal and toroidal mode numbers, respectively) have been systematically compared with the ones<br />
inferred from the frequency of MHD modes. The connection between mode frequency and rational surface<br />
location depends on the velocity of the magnetic island produced by the mode at the correspon<strong>di</strong>ng rational<br />
surface. A previous assumption of island propagation at the toroidal velocity of the carbon impurity resulted<br />
to be inconsistent. Much better agreement was found by assuming that the island rotates with the deuterium<br />
ions fluid; the latter was calculated by ra<strong>di</strong>al force balance from carbon toroidal rotation and ion temperature<br />
profiles neglecting poloidal rotation. If neoclassical carbon poloidal rotation is included in the force balance,