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Table 4:

HCO+ and H13CO+ results.
Source HCO+ 4-3 H13CO+ 4-3 $V_{\rm LSR}^a$
  $\int T_{\rm MB} {\rm d} V^b$ $T_{\rm MB}$ $\int T_{\rm MB} {\rm d} V^b$ $T_{\rm MB}$  
  (K km s-1) (K) (K km s-1) (K) (km s-1)
Chamaeleon  
Ced 110 IRS 4 4.0 3.1 0.38 0.25 4.3
Ced 110 IRS 6 0.5 0.4 <0.06 - 4.8
Cha IRS 6a <0.2 - <0.06 - 4.6
Cha IRN 0.87 0.95 <0.06 - 4.5
Cha INa 2 <0.2 - <0.06 - 4.8
Corona australis  
CrA IRAS 32 4.1 2.9 0.72 0.53 5.6
HH 100-off 4.8 3.2 <0.06 - 5.9
RCrA IRS 5 14.2 7.0 0.96 0.86 5.7
RCrA IRS 7A 63.7 17.4 3.8 1.6 5.5
RCrA IRS 7B 49.0 18.7 3.8 2.2 5.7
RCrA TS 3.5 <0.2 - <0.06 - 5.9
Isolated  
HH 46 8.4 5.4 1.1 1.0 5.3
IRAS 07178-4429 1.0 0.6 <0.08 - 3.4
IRAS 12496-7650 1.9 1.5 <0.06 - 1.9
IRAS 13546-3941 <0.12 - <0.06 - -5.7
IRAS 15398-3359c 5.9 4.6 - - 5.2

a The rest velocity $V_{\rm {LSR}}$ was determined by fitting Gaussians to either the H13CO+ 4-3 (preferred) or C18O 3-2 lines (see Table 3); b calibration uncertainties estimated at 20$\%$ dominate the uncertainty of the integrated intensity; c data from HARP-B map.


Source LaTeX | All tables | In the text

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