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2.2 MARCO TEORICO

2.1.2 CLIMA ORGANIZACIONAL

2.1.2.2 TIPOS DE CLIMA ORGANIZACIONAL

We model the plasma using the gyro-kinetic formalism (see chapter 2) and include a background radial electric field. This appears in the equations of motion as an

E×B flow[68]. For a particle of mass m, electric charge q, parallel velocity vk,

magnetic momentµand real-space coordinatesR we have: dR dt = vk Bk∗B ∗ + v 2 ⊥ 2ΩiBB∗k B× ∇B+(E0+hE1i)×B BB∗k (5.1) dvk dt = B∗ mBk∗ ·[q∇(φ0+hφ1i) + mv2 ⊥ 2B ∇B] (5.2)

where Bk∗ = b ·B∗ is the parallel component of the generalised magnetic field,

B∗ =B+ (mvke )∇ ×b,bis the unit vector in the direction of the magnetic field,φ0

is the equilibrium electrostatic potential, and hφ1i is the gyro-averaged perturbed electrostatic potential. The equilibrium electrostatic potential does not appear in its gyro-averaged form as it does not vary on the length scale of the gyroradius. Thereforehφ0i=φ0. This formalism is valid in the “low-flow” regime, which holds when the equilibriumE×B speed is smaller than the thermal speed,uEvth.

For the linear simulations, we select a single toroidal mode in each simulation, using a surface-dependent filter (the “diagonal” filter[55]) which suppresses highkk

modes and keeps only poloidal modes with m = [−nq(s)±∆m], where ∆m = 5. The poloidal wavenumber spectra are then constructed by performing a scan in n

and converting tokθρi with the following equation:

kθρi=nq(s0)

r(s0)

where s0 is the location of the peak temperature gradient (i.e. the location of the

strongest drive).

We look at three different profiles of the background electrostatic potential: 1. an analytic profile that gives roughly constant flow shear across the domain

in anad-hoc equilibrium - concentric circular flux surfaces 2. the same profile in a true MHD equilibrium from MAST

3. an electrostatic potential that corresponds to an experimental profile of toroidal angular frequency in MAST

In the third case, we use the toroidal angular frequency profile (fig. 5.13) from transp, a transport analysis code1 , and the radial force balance equation[34]:

ER= (Zen)−1∇p−v×B, (5.4)

neglecting the pressure gradient term, to calculate the equilibrium electrostatic po- tential, φ0. φ0 supports the perpendicular part of the toroidal rotation with the usual E×B drift. The parallel part is provided by a canonical Maxwellian[70] of the form: f0 = n0(ψcorr) (2πT(ψcorr)/m)3/2 exp −−qφ0(ψc) T(ψcorr) (5.5) where m, q, T, n0 and ψ are the mass, charge, temperature, density and poloidal

magnetic flux, the energy is= 12mv2+qφ0(ψ), and ψc=ψ+mvkRBϕ/qB is the

canonical momentum. ψcorr is the “corrected” canonical momentum[71], ψcorr≡ −sign(vk)

q

mR0

p

2(−µB0)H(−µB0), (5.6)

which is used as a radial coordinate designed to reduce spurious parallel flows. Becauseψ−ψc is proportional tovk, parallel flows arise from theφ0(ψ)−φ0(ψc)∝

ERvk term in the exponent of f0. The poloidal part of this parallel flow almost

entirely cancels the poloidal part of theE×B flow fromφ0(there is a small residual poloidal flow from the temperature and density gradients), and the toroidal parts sum up to give the specified rotation profile. Because the parallel flow is provided by the Maxwellian, no new terms appear in the equations of motion; instead, new terms from the modification of the distribution function appear in ddδft [70].

1

transpis a time-dependent tokamak transport data analysis code, comprising numerous mod-

els for various transport and equilibrium process, including NBI heating, MHD equilibrium, neutral transport and angular momentum balance (which is used here to determine the angular frequency

profile). While there is no single reference for the code, thetranspweb page has collated references

Figure 5.1: Typical plots of growth-rates. Left: Field energy in a single toroidal mode; Right: time-evolution of the growth rate. The red dashed lines in both figures indicate the time range over which the growth rate is calculated in the left- hand case, and over which it is averaged, in the right-hand case.

While the toroidal angular frequency is a flux function, it is not true that all other quantities are, for example, the density[72]. Becausenemorbis not currently able to handle poloidal variation of all these equilibrium quantities, and because we restrict ourselves to the low-flow regime, we perform the calculation of φ0 on the outboard midplane and take this as a flux-surface function.

The growth rates are calculated from the field-energy, usingmatlabto per- form the data analysis. nemorboutputs the field-energy on anm, n, tgrid in Fourier space for each time slice. This grid is summed over them-modes to give the toroidal mode energy spectrum as a function of time and toroidal mode number. The energy for each mode is then logged (base-10) and a straight line fitted, the gradient of which is twice the growth-rate. The reason for doing it this way, as opposed to fitting an exponential straight away, is that the noise also grows exponentially. This can be very taxing for the fitting algorithms and often results in a poor fit com- pared with the former method. Another method is also used - the instantaneous growth-rate is found as a function of time by calculating the growth-rate for short time-periods and then averaging over some suitable period. The standard deviation of this average then gives us a better estimate of the uncertainty in the growth-rate compared to the first method, which often grossly over-estimates the error.

By looking atad-hocand MHD equilibria as well as analytic and experimen- tal rotation profiles, we shall study flow shear stabilisation with a broad range of profiles. Thead-hoc case uses thede facto standard gyrokinetic case, thecyclone base case. The cyclone case is a set of standard parameters used to compare gyrokinetic codes and has been well studied. Using this scenario acts firstly as a

“sanity-check”, ensuring that we can reproduce well-established results. Secondly, it allows a degree of comparison between circular and shaped plasmas. The constant shear profile used in the first two cases is the simplest sheared flow profile but is not, however, a physical profile. This is because a flow driven solely by a radial elec- tric field is necessarily mostly poloidal (due to the flow being perpendicular to the magnetic field), and poloidal flows are neoclassically damped in tokamaks. The last case uses a toroidal flow profile, computed using experimental data, allowing us to investigate the effects of a non-constant shear profile. This will also lay the ground- work necessary to perform nonlinear simulations, which permit direct comparison with experiment (see chapter 6).

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