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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,

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