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

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Figure 6.5: <strong>The</strong>rmal evolution <strong>of</strong> primordial gas in a minihalo under the effect<br />

<strong>of</strong> a PISN explosion 100 pc away (left column) and 10 pc away (right column).<br />

<strong>The</strong> PISN is assumed to emit CRs for 2×10 5 yr with a minimum CR energy <strong>of</strong><br />

10 6 eV. We assume th<strong>at</strong> the CR flux reaches the cloud during different stages<br />

in its collapse, characterized <strong>by</strong> the corresponding densities: nH = 1 cm −3 (top<br />

row) and nH = 10 2 cm −3 (bottom row). <strong>The</strong> dashed lines show the evolution<br />

without CR flux prsent. <strong>The</strong> dotted lines show the CMB temper<strong>at</strong>ure floor <strong>at</strong><br />

z = 20. Notice th<strong>at</strong> the cloud has to be extremely close to the explosion site<br />

(d ∼ 10 pc) to experience a significant effect. Such close proximity, however, is<br />

very unlikely due to the strong radi<strong>at</strong>ive feedback from the PISN progenitor.<br />

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