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Copyright by Athena Ranice Stacy 2011 - The University of Texas at ...

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6.3.3 Local CR Feedback<br />

Our study thus far has assumed th<strong>at</strong> the CRs possibly cre<strong>at</strong>ed in the<br />

early Universe all become part <strong>of</strong> a homogeneous and isotropic background.<br />

However, if a particular minihalo is within sufficiently close range to a CR-<br />

acceler<strong>at</strong>ing PISN, the flux <strong>of</strong> CRs from the near<strong>by</strong> PISN may have a gre<strong>at</strong>er<br />

effect on the evolution <strong>of</strong> the minihalo than th<strong>at</strong> from the CR background.<br />

<strong>The</strong> average CR luminosity associ<strong>at</strong>ed with the PISN is given <strong>by</strong><br />

LCR = 2 × 10 38 erg s −1<br />

<br />

pCR<br />

<br />

0.1<br />

<br />

ESN<br />

×<br />

1052 <br />

∆tSN<br />

erg 2 × 105 yr<br />

−1<br />

, (6.32)<br />

where ∆tSN is the time over which the PISN emits CRs, here assumed to be<br />

approxim<strong>at</strong>ely the time th<strong>at</strong> passes from the beginning <strong>of</strong> the PISN to the end<br />

<strong>of</strong> its Sedov-Taylor phase <strong>of</strong> expansion (see Lagage and Cesarsky 1983). We<br />

can then estim<strong>at</strong>e the CR flux, fCR, and energy density, UCR, emitted <strong>by</strong> the<br />

PISN using<br />

fCR = LCR<br />

, (6.33)<br />

4πd2 where d is the distance between the CR source and the minihalo. This can<br />

also be expressed as<br />

fCR 10 −4 erg cm −2 s −1<br />

<br />

pCR<br />

×<br />

<br />

0.1<br />

<br />

ESN<br />

1052 <br />

∆tSN<br />

erg 2 × 105 −1 −2 d<br />

. (6.34)<br />

yr 100 pc<br />

168

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