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Stars as Laboratories for Fundamental Physics - MPP Theory Group

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The Energy-Loss Argument 11<br />

against the <strong>for</strong>ce of gravity. In Eq. (1.5) c p is the heat capacity at<br />

constant pressure. Further, the quantity ∇ ad ≡ (∂ ln T/∂ ln p) s , taken<br />

at constant entropy density s, is the “adiabatic temperature gradient.”<br />

It is not really a gradient. It is a thermodynamic quantity characteristic<br />

of the medium at the local conditions of ρ, p, T , and the chemical<br />

composition.<br />

The calculation of ϵ x <strong>for</strong> a number of hypotheses concerning the<br />

existence of novel particles or novel properties of neutrinos will be a<br />

major <strong>as</strong>pect of this book. Even <strong>for</strong> a given interaction law between<br />

the particles and the medium constituents this is not always a straight<strong>for</strong>ward<br />

exercise because the presence of the ambient medium can have<br />

a significant impact on the microscopic reactions.<br />

This is equally true <strong>for</strong> the nuclear energy generation rates. Nuclear<br />

reactions are slow in stars because the low temperature allows only few<br />

nuclei to penetrate each other’s Coulomb barriers. There<strong>for</strong>e, screening<br />

effects are important, and the nuclear cross sections need to be known at<br />

energies so low that they cannot be me<strong>as</strong>ured directly in the laboratory.<br />

Much of the debate concerning the solar neutrino problem revolves<br />

around the proper extrapolation of certain nuclear cross sections to<br />

solar thermal energies.<br />

1.2.4 Energy Transfer<br />

The transfer of energy is driven by the radial temperature gradient. In<br />

the absence of convection heat is carried by photons and electrons moving<br />

between regions of different temperature, i.e. by radiative transfer<br />

and by conduction. In this c<strong>as</strong>e the relationship between the energy<br />

flux and the temperature gradient is<br />

L r = − 4πr2<br />

3κρ<br />

d(aT 4 )<br />

, (1.6)<br />

dr<br />

where aT 4 is the energy stored in the radiation field (a = π 2 /15 in<br />

natural units) and κ is the opacity (units cm 2 /g). It is given by a sum<br />

κ −1 = κ −1<br />

γ<br />

+ κ −1<br />

c<br />

+ κ −1<br />

x , (1.7)<br />

where κ γ is the radiative opacity, κ c the contribution from conduction<br />

by electrons, and κ x w<strong>as</strong> included <strong>for</strong> a possible contribution from novel<br />

particles. The quantity (κ γ ρ) −1 = ⟨λ γ ⟩ R is the “Rosseland average”<br />

of the photon mean free path—its precise definition will be given in<br />

Sect. 1.3.4.

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