Derivations and technical details
JINR
2026-06-01
All analytic formulas use natural units, \(\hbar=c=1\). Practical table units are stated explicitly where they are used.
The average power density over the whole solar volume is small: \[ \frac{L_\odot}{(4\pi/3)R_\odot^3} \simeq 0.27~\mathrm{W\,m^{-3}}. \]
The core value is much larger, of order \[ 10^2~\mathrm{W\,m^{-3}}, \]
but still not large by terrestrial engineering standards. The Sun is bright because it is enormous and long-lived.
V. A. Naumov, Solar Neutrinos. Astrophysical Aspects, Phys. Part. Nucl. Lett. 8, 1141-1170 (2011).
The numerical reference curves used in the masterclass may be generated with PEANUTS:
Use deliberately generous core numbers:
proton density: \(n_p\sim 10^{32}~\mathrm{m}^{-3}\);
effective core volume: \(V_{\rm core}\sim 10^{25}~\mathrm{m}^{3}\);
geometric nuclear area: \(\sigma_{\rm geom}\sim\pi(1~\mathrm{fm})^2\sim 10^{-30}~\mathrm{m}^{2}\);
relative velocity: \(v\sim 8\times 10^5~\mathrm{m\,s^{-1}}\).
\[ \dot N_{\rm geom} = \mathcal{L}_{pp}\sigma_{\rm geom} \sim 4\times 10^{64}~\mathrm{s^{-1}}. \]
\[ U(r)=\frac{A}{r}, \qquad A=Z_aZ_b\alpha, \qquad r_C=\frac{Z_aZ_b\alpha}{E}. \]
\[ I(E) = \int_{r_N}^{r_C} \sqrt{2\mu\left(\frac{A}{r}-E\right)}\,dr . \]
\[ I(E) = \sqrt{2\mu E}\,r_C \int_{x_N}^{1} \sqrt{\frac{1}{x}-1}\,dx, \qquad x=\frac{r}{r_C}. \]
\[ dx=2\sin\theta\cos\theta\,d\theta, \qquad \sqrt{\frac{1}{x}-1}=\cot\theta . \]
\[ \int\sqrt{\frac{1}{x}-1}\,dx = \int 2\cos^2\theta\,d\theta = \theta+\frac{1}{2}\sin 2\theta . \]
\[ \int_{x_N}^{1} \sqrt{\frac{1}{x}-1}\,dx = \frac{\pi}{2} -\theta_N -\frac{1}{2}\sin 2\theta_N . \]
\[ \sigma(E) = \frac{S(E)}{E} \exp\!\left[-\sqrt{\frac{E_G}{E}}\right]. \]
\(S(E)\) is the astrophysical \(S\)-factor: the slowly varying nuclear-physics part.
The fast energy dependence is mostly the tunneling factor.
\[ R_{ab} = \frac{n_an_b}{1+\delta_{ab}} \langle\sigma v\rangle . \]
The factor \(1+\delta_{ab}\) avoids double counting identical pairs, for example \(p+p\).
The thermal average is
\[ \langle\sigma v\rangle = \left(\frac{8}{\pi\mu}\right)^{1/2} \frac{1}{(kT)^{3/2}} \int_0^\infty \sigma(E)\,E\,e^{-E/kT}\,dE. \]
\[ \sigma(E) = \frac{S(E)}{E} \exp\!\left[-\sqrt{\frac{E_G}{E}}\right]. \]
\[ S(E) \exp\!\left[ -\frac{E}{kT} -\sqrt{\frac{E_G}{E}} \right]. \]
\[ \Phi(E) = \frac{E}{kT} + \sqrt{\frac{E_G}{E}}. \]
The integrand is proportional to \(\exp[-\Phi(E)]\).
The maximum occurs near
\[ E_0 = \left( \frac{E_G(kT)^2}{4} \right)^{1/3}. \]
The reaction does not occur at one energy.
The useful energy range is the Gamow window around \(E_0\).
A standard estimate of its width is
\[ \Delta \simeq 4\sqrt{\frac{E_0 kT}{3}}. \]
The energy released per complete pp-chain cycle is fixed mainly by nuclear masses.
The photon luminosity is powered by the part that remains in the plasma:
\[ Q_\gamma \simeq 26.73~\mathrm{MeV} - \langle E_{\nu_1}+E_{\nu_2}\rangle . \]
The neutrino subtraction depends on the branch: pp, pep, \(^7\mathrm{Be}\), \(^8\mathrm{B}\), or hep.
This is why solar luminosity and solar neutrino fluxes are tightly linked but not identical observables.
\[ \frac{L_\odot}{(4\pi/3)R_\odot^3} \simeq 0.27~\mathrm{W\,m^{-3}}. \]
The core value is larger, but still modest on human engineering scales.
The Sun shines because it contains an enormous number of particles, not because each cubic meter is a powerful reactor.
The pp chain is the main hydrogen-burning cycle in the present Sun.
The pp chain begins with
\[ p+p\to d+e^+ + \nu_e. \]
The emitted neutrino has a continuous spectrum with endpoint about
\[ E_\nu^{\max}\simeq 0.42~\mathrm{MeV}. \]
This is the largest solar-neutrino flux, but not the easiest component for water Cherenkov detectors.
The related three-body reaction is
\[ p+e^-+p\to d+\nu_e. \]
It produces an almost monoenergetic neutrino:
\[ E_\nu \simeq 1.44~\mathrm{MeV}. \]
The pep flux is much smaller than pp, but the line is physically clean.
After deuterium is produced,
\[ p+d\to {}^3\mathrm{He}+\gamma, \]
and the pp I branch ends through
\[ {}^3\mathrm{He}+{}^3\mathrm{He} \to {}^4\mathrm{He}+2p. \]
This branch produces pp neutrinos but no high-energy \(^8\mathrm{B}\) neutrinos.
The chain can proceed through beryllium:
\[ {}^3\mathrm{He}+{}^4\mathrm{He}\to{}^7\mathrm{Be}+\gamma, \]
followed by electron capture:
\[ {}^7\mathrm{Be}+e^- \to {}^7\mathrm{Li}+\nu_e. \]
The main neutrino lines are approximately
\[ 0.862~\mathrm{MeV}, \qquad 0.384~\mathrm{MeV}. \]
The high-energy branch is rare:
\[ {}^7\mathrm{Be}+p\to{}^8\mathrm{B}+\gamma, \]
then
\[ {}^8\mathrm{B}\to{}^8\mathrm{Be}^{*}+e^+ + \nu_e. \]
The \(^8\mathrm{B}\) flux is small, but its spectrum extends to high energy. This is why it is central for Super-Kamiokande-like measurements.
The rare reaction
\[ {}^3\mathrm{He}+p\to{}^4\mathrm{He}+e^+ + \nu_e \]
produces the highest-energy solar neutrinos.
The flux is tiny. The importance is not total rate, but the far high-energy tail.
CNO catalytic loop and the smaller NO side branch.
In the CNO cycle, carbon, nitrogen, and oxygen nuclei catalyze hydrogen burning.
The neutrino-producing beta decays are
\[ {}^{13}\mathrm{N}\to{}^{13}\mathrm{C}+e^+ + \nu_e, \]
\[ {}^{15}\mathrm{O}\to{}^{15}\mathrm{N}+e^+ + \nu_e, \]
\[ {}^{17}\mathrm{F}\to{}^{17}\mathrm{O}+e^+ + \nu_e. \]
In Naumov’s notation, the stellar-structure equations are
\[ \frac{dM}{dR}=4\pi R^2\rho, \qquad \frac{dP}{dR}=-\frac{GM\rho}{R^2}, \]
\[ \frac{dL}{dR} = 4\pi R^2 \left[ \epsilon\rho -\rho\frac{d}{dt}\left(\frac{u}{\rho}\right) +\frac{P}{\rho}\frac{d\rho}{dt} \right], \qquad \frac{dT}{dR} = \nabla\frac{T}{P}\frac{dP}{dR}. \]
Here \(M(R)\) is the shell mass, \(L(R)\) is the energy flow through radius \(R\), \(u\) is the internal energy per unit volume, and
\[ \nabla=\frac{d\ln T}{d\ln P}. \]
The four differential equations are not closed until the microphysics is specified:
\[ \rho=\rho(P,T,\{X_a\}), \qquad \kappa=\kappa(P,T,\{X_a\}), \qquad \epsilon=\epsilon(P,T,\{X_a\}). \]
They provide the equation of state, opacity, and nuclear energy-generation rate. The pressure is, in general,
\[ P=P_{\rm gas}+P_{\rm rad}+\frac{B^2}{8\pi}, \]
with the magnetic term usually neglected in standard solar models.
The temperature gradient is decomposed as
\[ \nabla = \nabla_{\rm rad} +\nabla_{\rm cond} +\nabla_{\rm conv}. \]
For radiative transfer in local thermodynamic equilibrium, in natural units,
\[ \nabla_{\rm rad} = \frac{3}{16\pi aG} \frac{\kappa P}{T^4} \frac{L}{M}. \]
Convection starts when the radiative gradient exceeds the adiabatic one:
\[ \nabla_{\rm rad}> \nabla_{\rm ad}, \qquad \nabla_{\rm ad} = \left(\frac{\partial\ln T}{\partial\ln P}\right)_s. \]
This is why opacity, composition, and the treatment of convection enter solar-neutrino predictions.
For the masterclass we take as input:
We do not solve the solar model. We use its output.
\[ |\nu(0)\rangle = \cos\theta\,|\nu_1\rangle + \sin\theta\,|\nu_2\rangle. \]
\[ |\nu(t)\rangle = \cos\theta\,e^{-iE_1t}|\nu_1\rangle + \sin\theta\,e^{-iE_2t}|\nu_2\rangle. \]
\[ A_{ee}(t) = \langle\nu_e|\nu(t)\rangle = \cos^2\theta\,e^{-iE_1t} + \sin^2\theta\,e^{-iE_2t}. \]
\[ A_{e\mu}(t) = \langle\nu_\mu|\nu(t)\rangle = \sin\theta\cos\theta \left(e^{-iE_2t}-e^{-iE_1t}\right). \]
\[ |\nu_\alpha\rangle = \sum_{i=1}^3 U_{\alpha i}^{*}|\nu_i\rangle, \qquad \alpha=e,\mu,\tau. \]
\[ U_{\rm PMNS} = R_{23}(\theta_{23})\, U_{13}(\theta_{13},\delta_{\rm CP})\, R_{12}(\theta_{12}). \]
\[ P_{ee}^{3\nu} \simeq \cos^4\theta_{13}\,P_{ee}^{2\nu} + \sin^4\theta_{13}. \]
With \(c_{ij}\equiv\cos\theta_{ij}\) and \(s_{ij}\equiv\sin\theta_{ij}\),
\[ \small U_{\rm PMNS} = \begin{pmatrix} 1&0&0\\ 0&c_{23}&s_{23}\\ 0&-s_{23}&c_{23} \end{pmatrix} \begin{pmatrix} c_{13}&0&s_{13}e^{-i\delta_{\rm CP}}\\ 0&1&0\\ -s_{13}e^{i\delta_{\rm CP}}&0&c_{13} \end{pmatrix} \begin{pmatrix} c_{12}&s_{12}&0\\ -s_{12}&c_{12}&0\\ 0&0&1 \end{pmatrix}. \]
Vacuum mixing in matrix form
\[ \nu_f= \begin{pmatrix} \nu_e\\ \nu_x \end{pmatrix}, \qquad \nu_f=U(\theta)\nu_m. \]
\[ U(\theta) = \begin{pmatrix} \cos\theta & \sin\theta\\ -\sin\theta & \cos\theta \end{pmatrix}. \]
Hamiltonian
\[ i\frac{d}{dt}\nu_f = H_{\rm vac}\nu_f, \qquad H_{\rm vac} = U \begin{pmatrix} \frac{m_1^2}{2E} & 0\\ 0 & \frac{m_2^2}{2E} \end{pmatrix} U^\dagger. \]
After subtracting an irrelevant trace
\[ H_{\rm vac} = \frac{\Delta m^2}{4E} \begin{pmatrix} -\cos2\theta & \sin2\theta\\ \sin2\theta & \cos2\theta \end{pmatrix}. \]
\[ |\nu_e\rangle = \cos\theta_m|\nu_1^m\rangle + \sin\theta_m|\nu_2^m\rangle. \]
\[ \tan2\theta_m = \frac{\Delta m^2\sin2\theta} {\Delta m^2\cos2\theta-2EV_e}. \]
\[ \Delta m_m^2 = \Delta m^2 \sqrt{ \left(\cos2\theta-\frac{2EV_e}{\Delta m^2}\right)^2 + \sin^2 2\theta }. \]
\[ \lambda_\pm = \pm\frac{\Delta m_m^2}{4E}. \]
\[ P_{ee}^{\rm matter} = 1-\sin^2 2\theta_m\, \sin^2\!\left( \frac{\Delta m_m^2 L}{4E} \right). \]
\[ P_{ex}^{\rm matter} = 1-P_{ee}^{\rm matter}. \]
\[ H_f(R) = H_{\rm vac} + \begin{pmatrix} V_e(R)&0\\ 0&0 \end{pmatrix}. \]
\[ H_f(R)|\nu_i^m(R)\rangle = \lambda_i(R)|\nu_i^m(R)\rangle. \]
\[ \left|\frac{d\theta_m}{dR}\right| \ll |\lambda_2-\lambda_1| = \frac{\Delta m_m^2(R)}{2E}. \]
The masterclass table
stores the PEANUTS daytime result for \(^8\mathrm{B}\) neutrinos:
\[ P_{ee}^{day} = P_{ee}^{day} \left(E_\nu;\sin^2\theta_{12},\Delta m^2_{21}\right). \]
PEANUTS computes this from the solar model, the \(^8\mathrm{B}\) production profile, and adiabatic solar propagation.
During the day, solar neutrinos reach the detector without crossing the Earth.
At night they can propagate through Earth matter before detection.
This modifies the mass-state mixture projected onto \(\nu_e\):
\[ P_{ee}^{\mathrm{night}}(E,\eta) \ne P_{ee}^{\mathrm{day}}(E). \]
\(\eta\) denotes the nadir angle.
The Earth matter correction is usually small:
\[ \Delta P_{ee}^{\oplus} = P_{ee}^{\mathrm{night}}-P_{ee}^{\mathrm{day}}. \]
It is nevertheless coherent and measurable statistically in large detectors.
The optional masterclass table
stores this quantity computed with PEANUTS Earth propagation for several nadir angles \(\eta\).
The table
uses the same PEANUTS calculation at selected \(E_\nu\) and \(\eta\) values while scanning \((\sin^2\theta_{12},\Delta m^2_{21})\).

A common observable is
\[ A_{\mathrm{DN}} = 2\frac{N_{\mathrm{night}}-N_{\mathrm{day}}} {N_{\mathrm{night}}+N_{\mathrm{day}}}. \]
For neutrino-electron scattering, neglecting radiative corrections, the differential cross section has the structure
\[ \frac{d\sigma}{dT} = \frac{2G_F^2m_e}{\pi} \left[ g_L^2 +g_R^2\left(1-\frac{T}{E_\nu}\right)^2 -g_Lg_R\frac{m_eT}{E_\nu^2} \right]. \]
The coupling constants differ between \(\nu_e e\) and \(\nu_{\mu,\tau}e\) scattering.
Using \(s_W^2=\sin^2\theta_W\simeq0.231\):
| channel | \(g_L\) | value | \(g_R\) | value |
|---|---|---|---|---|
| \(\nu_e e\to\nu_e e\) | \(\frac{1}{2}+s_W^2\) | \(0.731\) | \(s_W^2\) | \(0.231\) |
| \(\nu_{\mu,\tau}e\to\nu_{\mu,\tau}e\) | \(-\frac{1}{2}+s_W^2\) | \(-0.269\) | \(s_W^2\) | \(0.231\) |
For antineutrinos the roles of \(g_L\) and \(g_R\) are interchanged in the recoil-energy dependence.

Linear high-energy approximations in cm\(^2\) for solar-neutrino energies. The full recoil spectrum is used only in precision analyses.
For binned expected counts \(\mu_i\),
\[ n_i \sim \mathrm{Poisson}(\mu_i). \]
A fixed random seed gives a reproducible pseudoexperiment for all students.
The point is to separate the true model from one possible observed dataset.
For counting data use
\[ \chi^2 = 2\sum_i \left[ \mu_i-n_i+n_i\ln\frac{n_i}{\mu_i} \right]. \]
For \(n_i=0\), the logarithmic term is defined as zero.
