The reaction rate density between species
A and
B, having number densities
nA,
B, is given by:r=n_A\,n_B\,k_r where
kr is the
reaction rate constant of each single elementary binary reaction composing the
nuclear fusion process;k_r=\langle\sigma(v)\,v\ranglewhere
σ(
v) is the
cross-section at relative velocity
v, and averaging is performed over all velocities. Semi-classically, the cross section is proportional to \pi\,\lambda^2, where \lambda =h/p is the
de Broglie wavelength. Thus semi-classically the cross section is proportional to \frac{E}{m} =c^{2}. However, since the reaction involves
quantum tunneling, there is an exponential damping at low energies that depends on
Gamow factor EG, given by an
Arrhenius-type equation:\sigma(E) = \frac{S(E)}{E} e^{-\sqrt{\frac{E_\text{G}}{E}}}.Here astrophysical
S-factor S(
E) depends on the details of the nuclear interaction, and has the dimension of an energy multiplied by a cross section. One then integrates over all energies to get the total reaction rate, using the
Maxwell–Boltzmann distribution and the relation:\frac{r}{V}=n_A n_B \int_0^{\infty}\Bigl(\frac{S(E)}{E}\, e^{-\sqrt{\frac{E_\text{G}}{E}}} \cdot2\sqrt{\frac{E}{\pi(kT)^3}}\, e^{-\frac{E}{kT}} \,\cdot\sqrt{\frac{2E}{m_\text{R}}}\Bigr)dEwhere
k = 86,17 μeV/K, m_\text{R} =\frac{m_Am_B}{m_A+m_B} is the
reduced mass. The integrand equals S(E)\,e^{-\sqrt{\frac{E_\text{G}}{E}}}\cdot2\sqrt{2/\pi}(kT)^{-3/2}\, e^{-\frac{E}{kT}}\,/\sqrt{{m_\text{R}}}. Since this integration of
f(
E, constant
T) has an exponential damping at high energies of the form \sim e^{-\frac{E}{kT}} and at low energies from the Gamow factor, the integral almost vanishes everywhere except around the peak at E0, called
Gamow peak. There:-\frac{\partial}{\partial E} \left(\sqrt{\frac{E_\text{G}}{E}}+\frac{E}{kT}\right)\,=\, 0 Thus: E_0 = \left(\frac{1}{2}kT \sqrt{E_\text{G}}\right)^\frac{2}{3} and \sqrt{E_\text{G}}=E_0^\frac{3}{2}/\frac{1}{2}kT The exponent can then be approximated around
E0 as:e^{-(\frac{E}{kT}+\sqrt{\frac{E_\text{G}}{E}})}\approx e^{-\frac{3E_0}{kT}}e^{\bigl(-\frac{3(E-E_0)^2}{4E_0kT}\bigr)}=e^{-\frac{3E_0}{kT}\bigl(1+(\frac{E-E_0}{2E_0})^2\bigr)}=e^{-\frac{3E_0}{kT}\bigl(1+(E/E_0-1)^2/4\bigr)} And the reaction rate is approximated as:\frac{r}{V} \approx n_A \,n_B \,\frac{4\sqrt(2/3)}{ \sqrt{m_\text{R}}} \,\sqrt{E_0}\frac{S(E_0)}{kT} \, e^{-\frac{3E_0}{kT}} Values of
S(
E0) are typically , but are damped by a huge factor when involving a
beta decay, due to the relation between the intermediate bound state (e.g.
diproton)
half-life and the beta decay half-life, as in the
proton–proton chain reaction. Note that typical core temperatures in
main-sequence stars (the Sun) give
kT of the order of 1 keV: \log_{10}kT=-16+\log_{10}2.17. Thus, the limiting reaction in the
CNO cycle, proton capture by , has
S(
E0) ~
S(0) = 3.5keV·b, while the limiting reaction in the
proton–proton chain reaction, the creation of
deuterium from two protons, has a much lower
S(
E0) ~
S(0) = 4×10−22keV·b. Incidentally, since the former reaction has a much higher Gamow factor, and due to the relative
abundance of elements in typical stars, the two reaction rates are equal at a temperature value that is within the core temperature ranges of main-sequence stars. ==References==