Cosmic Ray Connement and Transport Models for Probing their Putative Sources Mikhail Malkov UCSD Partially Supported by NASA and DoE Ackn: R. Sagdeev, P. Diamond, I. Moskalenko, F. Aharonian 1 / 28 Outline 1 Two regimes of CR transport along magnetic eld: -collectively self-impeded -test particle transport in background-turbulence 2 CR self-connement and escape Equation for CR Self-Connement Self-Similar Solution γ -ray Spectra From CR-Illuminated Molecular Clouds Environmental vs Transport-Induced Spectral Breaks Summary and Conclusions 3 CR transport in background wave eld Equation for Transport Driven by Pitch-Angle Scattering CR Transport Equation and its Asymptotic Reduction Chapman-Enskog expansion conclusions (CR test particle transport) 2 / 28 Why need two dierent approaches to CR transport? simple facts about CRs in SNR and in ISM Dk ' DBohm (B/δB)2 →Dk varies between ∼ DB 5 SNR) and DISM ∼ 10 DBohm (quiet ISM). (in CR source, e.g. Away from the sources (SNR), CR energy is comparable to magnetic energy, thermal plasma & star light and CMB all ∼ eV /cc Therefore, in and around a CR source (SNR) PCR B 2 /8π Therefore, CRs cannot escape the source without driving strong MHD waves, so need to evolve CR from strong self-connement regime D ∼ DBohm in and around the source to their dissolution into the ambient ISM, D ∼ DISM DBohm →Interface Problem 3 / 28 Problems addressed under self-connement/free diusion regime Self-connement Free propagation acceleration (Bell CR background spectra 77) CR chemical composition, spectral propagation anomalies (Voelk, Wentzel, p/He Pamela (Adriani 2011) rev. ca 73-74) illumination of adjacent MC (e.g., Aharonian, Drury, Voelk) source morphology Explanations: Drury; Ohira; Blasi; Ptuskin; MM, Diamond, Sagdeev 2012 CR anisotropy, particularly sharp ∼ 10◦ Milagro (Abdo 2008) Interpretations: Drury&Aharonian; Desiati&Lazarian; MM, Diamond, Drury source and Sagdeev (ApJ 2010), Giacinti, Ahlers calorimetry... (coh. turb. realization, statistical eects), (MM, PoP 2015) 4 / 28 CR escape from SNR/Problem setting/geometry CR diuse along MF (⊥propagation may be important, but too many issues, e.g. Kirk, Duy and Gallant 96) generate Alfvén waves that suppress diusion CR escape along MF from two polar cusps of SNR to obtain CR distribution both processes are to be treated self-consistently result will determine MC emissivity 5 / 28 Equations CR propagation in self-excited waves ∂ κB ∂PCR d PCR (p) = dt ∂z I ∂z PCR (p) -partial pressure, I (p) -wave energy, resonance kp = eB0 /c , d/dt = [∂/∂t + (U + CA ) ∂/∂z] , κB ∼ crg (p) Wave generation by ∇PCR associated with the CR pitch-angle anisotropy ∂PCR d I = −CA − ΓI dt ∂z QL integral (Sagdeev et al '61) κB ∂ I (z, t) ln PCR (z, t) = PCR0 z 0 − CA ∂z I0 (z 0 ) z 0 = z − (U + CA ) t 6 / 28 Equations CR/Alfven wave coupling ∂W ∂ 1 ∂W ∂ − = − P0 (z) ∂t ∂z W ∂z ∂z W = CκABa(p) I (p) |z/a| < 1 d/dt ≈ ∂/∂t , P0 -initial -dimensionless wave energy, Self-similar solution in variable |z| > a, CR distribution, √ ζ = z/ t , W (z, t) = w (ζ) for outside initial CR cloud d 1 dw ζ dw + =0 dζ w dζ 2 dζ solution depends on a background turbulence level W 0 1, and integrated CR pressure in the cloud: Z Π= 0 1 P0 dz 1 7 / 28 CR self-similar distribution Comparing and Contrasting with conventional TP predictions: Π'3 CA a (p) P̄CR (p) 1 c rg (p) B02 /8π considerable delay of CR escape narrower spatial distribution of CR cloud extended self-similar, √ Self-connement vs test-particle escape, tPCR vs √ z/ t for dierent values of CR pressure Π (from MM, P. Diamond, R. Sagdeev, F. Aharonian and I. Moskalenko ApJ 2013) P ∝ 1/z region 8 / 28 Results/CR pressure distribution CR partial pressure (found in closed but implicit form) is well approximated by: √ h i−3/5 2 tP = 2 ζ 5/3 + (DNL )5/6 e −W0 ζ /4 , particle diusivity is strongly suppressed by √ ζ = z/ t self-connement eect: DNL ∼ DISM e −Π , integrated CR pressure parameter is typically large: Π'3 CA a (p) P̄CR (p) 1 c rg (p) B02 /8π 9 / 28 Breaks in Spectra of Escaping CRs normalized partial pressure P (p) approximation n o−3/5 P ≈ 2 z 5/3 + [DNL (p) t]5/6 for at DNL (p) < z 2 /t DNL (pbr ) = z 2 /t , p = pbr , δ from if exp (−Π) ∝ P DISM (p) is at at if δ < 0, P p > pbr momentum independent (DSA TP DNL ∝ p δ , and CR pressure p −σ and p < pbr for raises with DISM ∝ δ>0 p f ∼ p −4 ) break index = δ/2 Π (p) p λ at p ∼ pbr , so δ = λ − σ, −δ/2 at and steepens to p −δ/2 at as p p < pbr then p = pbr . and it levels o at 10 / 28 Morphological Signatures of CR Self-Connement central source (magenta radio image) emission is masked bi-polar morphology of escaping CR is clearly seen not everywhere correlated with the dense gas (green contours) distribution: strong γ -ux is expected from overlapping regions of CR and gas density Fermi-LAT W44, γ -image of SNR Uchiyama et al 2012 strong indication of eld aligned propagation CR diusivity is suppressed by up to a e.g. Uchiyama et al 2012) factor of ten ( 11 / 28 Spectral Signatures of the DSA and subsequent escape from W 44 presumably from dense MC illuminated by CR best t is given by a TP source spectrum E −q , q = 2, no cut-o required within CR subjected to propagation in evanescent Alfven waves inside MC wave evanescence and damping are due to ion-neutral collisions in MC γ -emission from MC near SNR W44 →break in the CR spectrum of index unity E −q → E −q−1 12 / 28 Escape Summary and Conclusions escape of CR from accelerator is treated self-consistently with self-generated Alfven waves resulting CR distribution is obtained in a closed form strong self-connement of CR is demonstrated for PCR B 2 /8π results are consistent with recent observations of W44 by Fermi-LAT escape spectra are roughly DSA-like power laws with breaks (not peaked at Emax ) environment (target for pp reactions) is equally important to interpret observed emission from adjacent MC 13 / 28 Test Particle Transport: Basic Equation CR transport driven by pitch-angle scattering, gyro-phase averaged z -along B; ∂f ∂f ∂ ∂f + vµ = 1 − µ2 D (µ) ∂t ∂z ∂µ ∂µ µ -cosine of CR pitch angle need evolution equation for 1 f0 (t, z) ≡ hf i (t, z) ≡ 2 Z1 f (µ, t, z) dµ. −1 Answer deems well known (e.g., Parker 65, Jokipii 66): average and expand in 1/D : ∂f0 v ∂ =− ∂t 2 ∂z ∂f 1−µ ∂µ 2 , v ∂f0 ∂f '− ∂µ 2D ∂z 14 / 28 Master Equation equation for f0 ∂f0 ∂ ∂f0 v2 = κ κ= ∂t ∂z ∂z 4 Critical step: 1 − µ2 D ∂f /∂t is neglected compared to v ∂f /∂z for Dt & 1 anisotropic part f˜ = f − f0 must Justication: −λ1 Dt decay ∝ e higher orders → suggest retaining ∂f /∂t →∂ 2 f0 /∂t 2 largely and higher derivative terms in master equation, e.g. Earl 1973, Litvinenko & Schlickeiser 2013 arrive at telegrapher's equation: where ∂f0 ∂ ∂f0 ∂ 2 f0 − κ +τ 2 =0 ∂t ∂z ∂z ∂t 2 τ ∼ 1/D , κ ∼ v /D 15 / 28 Pros and Cons of telegraph equation ∂f0 ∂t − ∂ ∂f0 ∂z κ ∂z 2 + τ ∂∂tf20 = 0 Pros ameliorates the major defect of diusive approximation, innite propagation velocity (UHECR: Aloisio $ Berezinsky, 2013) allows for a wave-like transport of CR clouds keeps the transport description simple Cons parabolic equation becomes hyperbolic no longer an evolution equation cannot be solved with no recourse to lower-level equation (needed to compute ∂f0 /∂t at t = 0) n n innite sequence of ∂ f0 /∂t -terms will result from iterations smells of not properly handled (eliminated) secular terms 16 / 28 Looking ahead: Is the telegraph term real? TE: ∂f0 ∂t − ∂ ∂f0 ∂z κ ∂z 2 + τ ∂∂tf20 = 0 In a sense... yes, BUT! coecient τ at ∂ 2 f0 /∂t 2 -term obtained by simple iteration in 1/D , is numerically incorrect neglected ∼ ∼ ∂ 4 f0 /∂z 4 -term contributes to the same order ∂ 3 f0 /∂z 3 contribute to even lower order unless D (µ) is symmetric and the term zeroes out being converted into τ -term ∂ 2 f0 /∂t 2 term the term ∼ ∂ 4 f0 /∂z 4 is subdominant compared to the other two for alters Dt & 1 τ and may largely be ignored altogether in the long time transport 17 / 28 Basic Equation with magnetic focusing gyro-phase averaged equation with magnetic focusing ∂f ∂f ∂f σ ∂ ∂f + vµ +v = νD (µ) 1 − µ2 1 − µ2 ∂t ∂z 2 ∂µ ∂µ ∂µ σ = −B −1 ∂B/∂z - magnetic mirror inverse scale; scattering rate, while ν -pitch angle D (µ) ∼ 1 small parameter ε= λ CR m.f .p. v = = 1 lν l problem scale l - scale of the problem; τ ν → τ ; z/l → z ; σl → σ ∼ 1 ∂f ∂ ∂f σ 2 ∂f 2 ∂f 1−µ − D (µ) 1 − µ = −ε µ + ∂t ∂µ ∂µ ∂z 2 ∂µ 18 / 28 Formal Expansion in ε1 f = f0 + εf1 + ε2 f2 + · · · ≡ f0 + f˜ where hf i = f0 , with 1 h·i = 2 Z1 (·) dµ −1 Master equation D E ∂ ∂f0 µf˜ = −ε +σ ∂t ∂z X ∞ ε2 ∂ n−1 2 ∂fn = +σ ε 1−µ 2 ∂z ∂µ n=1 xed evolutionary structure similarly to Lorenz's gas (Gurevich 61, Kruskal &Bernstein) f0 depends on slow time t2 = ε2 t rather than on t. 19 / 28 Regular Expansion slow time in f0 evolution suggests to attribute time derivative term to higher orders, so term ∝ ∂ 2 f0 /∂t 2 appears, converting the convection - diusion equation into a telegraph equation. However, f˜ does depend on t (as on the fast time) Ordering should be dierent (f = f0 + εf1 + · · · ≡ f0 + f˜): ∂fn ∂fn ∂ − D (µ) 1 − µ2 ∂t ∂µ ∂µ = −µ ∂fn−1 ∂fn−1 σ − 1 − µ2 ≡ Φn−1 (t, µ, z) ∂z 2 ∂µ 20 / 28 Chapman-Enskog analysis Solubility condition for f2 : hΦ1 i = 1 2 (∂/∂z + σ) 1 − µ2 /D ∂f0 /∂z = 0 Too strong restriction... However, f0 depends on slow time t2 suggesting multi-time expansion: CE: ∂/∂t = (∂/∂t)0 + ε (∂/∂t)1 + . . . more customary is a hierarchy of independent variables t → t0 , t1 , . . . ∂ ∂ ∂ ∂ = +ε + ε2 ... ∂t ∂t0 ∂t1 ∂t2 ∂fn ∂fn ∂ − D (µ) 1 − µ2 = Ln−1 [f ] (t0 , . . . , tn ; µ, z) ∂t0 ∂µ ∂µ n ∂fn−1 X ∂fn−k ∂fn−1 σ ≡ −µ − 1 − µ2 − ∂z 2 ∂µ ∂tk k=1 21 / 28 Chapman-Enskog analysis Solution can be written as fn = f n (t2 , . . . ; µ) + f˜n (t0 , . . . ; µ) where f˜n and fn satisfy, respectively, the following equations: h i ∂ f˜n ∂ f˜n ∂ − D (µ) 1 − µ2 = Ln−1 f˜ (t0 , . . . , tn ; µ, z) ∂t0 ∂µ ∂µ and − ∂ f¯n ∂ D (µ) 1 − µ2 = Ln−1 f¯ (t2 , . . . , tn ; µ, z) ∂µ ∂µ The solution for f˜n takes the form 22 / 28 Chapman-Enskog analysis f˜n = ∞ X (n) Ck (t) e −λk t0 ψk (µ) k=1 can be easily found for any − n using eigenfunctions of diusion operator ∂ψk ∂ D (µ) 1 − µ2 = λk ψk , ∂µ ∂µ For D = 1, for example, ψk are λk = k (k + 1), k = 0, 1, . . . . constants (n) Ck the Legendre polynomials with are determined by initial conditions for f˜n all f˜n exponentially decay in time for Starting from t&1 n=0 ∂ f¯0 =0 ∂t0 23 / 28 Chapman-Enskog analysis solubility condition for f¯1 ∂ f¯0 = 0. ∂t1 1 ∂f0 f¯1 = − W 2 ∂z where ∂W 1 = , hW i = 0. ∂µ D solubility condition for f2 yields nontrivial result for master eq., the leading term of the ∂f0 1 = ∂t2 4 ∂f0 /∂t expansion in ε1 * + 1 − µ2 ∂ ∂f0 +σ m , m= . ∂z ∂z D 24 / 28 Chapman-Enskog analysis solubility condition for f3 and f4 , ... ∂f0 ∂t3 ∂f0 ∂t4 ( ∂ σ + ∂z 2 2 ∂f0 1 ∂ ∂ σ = − +σ + µW 2 4 ∂z ∂z 2 ∂z 1 ∂ = +σ × 8 ∂z 2 0 W U −m + ∂ +σ ∂z ∂ ∂z * [m (1 − µ) + U]2 2 D ( 1 − µ2 ) +) ∂f0 ∂z where Zµ U≡ −1 1 − µ2 dµ, D U 0 = ∂U/∂µ 25 / 28 Chapman-Enskog analysis process may be continued 1 − µ2 ∂fn /∂µ ad innitum since terms containing can be expressed through fn−1 , interested in evolving f0 on time scales contributions of f˜n and retain only master equation up to f¯n 's: t2 & 1 or fn−2 , ... t & ε− 2 neglect ε4 : ∂f0 ε2 = ∂z0 m − ε∂z00 µW 2 + ∂t 4 * " +#) 2 0 ε2 [m (1 − µ) + U]2 ∂f0 00 2 0 W U − m + ∂z ∂z ∂z 2 2D (1 − µ2 ) ∂z here ∂z0 = ∂z + σ and ∂z00 = ∂z + σ/2. 26 / 28 Is Telegraph Equation recoverable? The structure of ME (magnetic focusing, asymmetry dropped) ∂t f = ε2 ∂z2 1 − τ ε2 ∂z2 f or, to the leading order in ε, formally ε2 ∂z2 f ≈ ∂t f , ε4 ∂z4 f ≈ ∂t2 f ∂f0 ∂ 2 f0 ∂ 2 f0 − ε2 2 + τ 2 = 0 ∂t ∂z ∂t τ -term belongs to the fast time part of the CE reduction scheme f , ε → 0: (1 + τ ∂t )∂t f = O ε2 associated with the anisotropic part of t&τ f = const for ε = 0 First solution: transient phenomenon, decays at Second solution: long time evolution 27 / 28 Conclusions (Test Particle CR transport) CR transport, constrained by scattering on magnetic irregularities revisited Chapman-Enskog approach revealed convective terms arising from the magnetic focusing eect, only no telegrapher (second order time derivative) term emerges in any order of the proper asymptotic expansion the telegraph ∂ 2 /∂t 2 -term may formally be back-converted from the fourth order of expansion, (usually not entertained in the literature) as well as higher time derivative terms but they do not play any signicant role in the CR transport within the method's validity range 28 / 28