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

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Figure 6.1: Penetr<strong>at</strong>ion depth as a function <strong>of</strong> CR energy. We here assume<br />

a neutral hydrogen number density <strong>of</strong> nH = 1 cm −3 . Only clouds with radii<br />

larger than about a few hundred pc will entirely <strong>at</strong>tenu<strong>at</strong>e the lowest-energy<br />

CRs through ioniz<strong>at</strong>ion losses. This also implies th<strong>at</strong> low-energy CRs are<br />

necessary to contribute significant ioniz<strong>at</strong>ion and he<strong>at</strong>ing, as those are the<br />

ones th<strong>at</strong> will release most <strong>of</strong> their energy into gas clouds <strong>of</strong> size ∼ 0.1−1 kpc.<br />

their energy into the gas. In contrast, higher energy CRs will quickly travel<br />

through a minihalo without transferring much <strong>of</strong> their energy into the gas.<br />

<strong>The</strong>y instead lose energy more slowly over much longer distances. Accounting<br />

for the <strong>at</strong>tenu<strong>at</strong>ion yields CR ioniz<strong>at</strong>ion and he<strong>at</strong>ing r<strong>at</strong>es <strong>of</strong><br />

and<br />

ΓCR(D) = Ehe<strong>at</strong><br />

ɛmax<br />

50 eV ɛmin<br />

<strong>The</strong>se r<strong>at</strong>es can also be written as<br />

ζCR(D) = ΓCR<br />

160<br />

<br />

dɛ dnCR<br />

dt ion dɛ e−D/Dpdɛ (6.25)<br />

nH 0Ehe<strong>at</strong><br />

. (6.26)

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