Dispersion Relation and Instabilities Using Green's Function ================================================================= .. admonition:: This is a review :class: warning This is my reading notes about the paper: `Capozzi, F., Dasgupta, B., Lisi, E., Marrone, A., & Mirizzi, A. (2017). Fast flavor conversions of supernova neutrinos: Classifying instabilities via dispersion relations, 1–25 `_. A Simple System --------------------------------- For a nonlinear system which has a linearized relation .. math:: \mathscr D S = 0, where :math:`\mathscr D` is a derivative operator that contains terms like :math:`\partial_t` and :math:`\boldsymbol\nabla`. Assuming collective modes :math:`S = Q e^{i(\mathbf k \cdot \mathbf x - \omega t)}`, the equation becomes .. math:: D(\omega, \mathbf k) = 0, which is in fact the dispersion relation. The picture behind these math is that we are treating the field as waves. By "solving" the dispersion relation, we find :math:`\omega(\mathbf k)` or :math:`\mathbf k(\omega)`, which is substituted into the wave form, .. math:: S = Q e^{i(\mathbf k(\omega) \cdot \mathbf x - \omega t)}, or .. math:: S = Q e^{i(\mathbf k \cdot \mathbf x - \omega(\mathbf k) t)}. However, we need to integrate over all Fourier modes in general. So we have the solution of the field .. math:: S = \int d\omega Q_\omega e^{i(\mathbf k(\omega) \cdot \mathbf x - \omega t)}, or .. math:: S = \int d\mathbf k Q_{\mathbf k} e^{i(\mathbf k \cdot \mathbf x - \omega(\mathbf k) t)}. Instability of the system is related the convergence of the integrals. This was done by P. A. Sturrock. [Sturrock1958]_ For the general equation of coherence .. math:: \mathscr D S = f(\mathbf x,t), the authors consider the Green's function of the equations, i.e., .. math:: \mathscr D G = \delta(\mathbf x)\delta(t). Fourier transform of :math:`G` leads to .. math:: D(\omega,\mathbf k) \tilde G = \mathrm{Const}, where the constant is chosen to be 1. The formal solution is .. math:: \tilde G = \frac{1}{D(\omega,\mathbf k)}. Inverse Fourier transform of the solution .. math:: G(t,\mathbf x) = \frac{1}{(2\pi)^2} \iint d\mathbf k d \omega \tilde G e^{i(\mathbf k \cdot \mathbf x - \omega t)} = \frac{1}{(2\pi)^2} \iint d\mathbf k d \omega \frac{1}{D(\omega,\mathbf k)} e^{i(\mathbf k \cdot \mathbf x - \omega t)}. .. admonition:: Choice of Coefficient :class: toggle The Fourier transform is chosen to be .. math:: \tilde g = \frac{1}{(2\pi)^2} \iint d\omega d \mathbf k g e^{i(\mathbf k \cdot \mathbf x - \omega t)}, which has coefficient :math:`1/(2\pi)^2`. The inverse transform would have no coefficient. .. admonition:: Solution to S :class: note The solution for coherence is .. math:: S = \iint G f d\mathbf x dt, which indicates that the Fourier mode .. math:: \tilde S = \tilde G \tilde f. .. [Sturrock1958] Sturrock, P. A. (1958). `Kinematics of Growing Waves. Physical Review, 112(5), 1488–1503. `_ .. admonition:: One Pole Case :class: warning I have no idea how is Eqn. 27 derived. Also have questions about Eqn. 34 for convective instability of 0 group velocity. Neutrinos ----------------------- The off diagonal elements of the density matrix :math:`S` obays the equation of the form .. math:: i(\partial_t + \mathbf v \cdot \nabla) S = f(\mathbf x, t) in linear regime. Gap ------------------------