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[tel-00726959, v1] Caractériser le milieu interstellaire ... - HAL - INRIA

[tel-00726959, v1] Caractériser le milieu interstellaire ... - HAL - INRIA

[tel-00726959, v1] Caractériser le milieu interstellaire ... - HAL - INRIA

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A&A 541, A58 (2012)<strong>tel</strong>-<strong>00726959</strong>, version 1 - 31 Aug 2012the rotation ladder is thermalized (Liszt et al. 2010). Of coursethis is of substantial assistance in the present work. Conversely,the high brightness (5−12 K) of many of lines we detectedshould not be taken as discrediting their origin in diffuse gas.Earlier we showed that, in the mean, CO-H 2 conversion factorsare similar in diffuse and dense fully mo<strong>le</strong>cular gas (Lisztet al. 2010), because the small abundance of CO relative to H 2in diffuse gas is compensated by a much higher brightness perCO mo<strong>le</strong>cu<strong>le</strong>. But the proportionality between W CO and N(CO)in diffuse gas, where CO represents such a small fraction of theavailab<strong>le</strong> gas phase carbon, means that the CO map of a diffusecloud is really an image of the CO chemistry. Moreoverthe CO abundance exhibits extreme sensitivities to local conditionsthat are manifested as order of magnitude scatter inN(CO)/N(H 2 ) in optical absorption line studies (Sonnentruckeret al. 2007; Burgh et al. 2007; Sheffer et al. 2007, 2008), evenbeyond the often-rapid variation of N(H 2 ) with E B−V (Savageet al. 1977)(E B−V ≈ A V /3.1). The net result is that the CO emissionmap of a diffuse cloud can only indirectly be interpreted astracing the underlying mass distribution, or even that of the H 2 .Nonethe<strong>le</strong>ss, it should (we hope) provide some impression ofthe nature of the host gas, especially in the absence of any othermeans of ascertaining this.In this paper we present maps of CO J = 1−0 emissionat arcminute resolution over 11 sky fields, typically 30 ′ × 30 ′around the positions of compact extragalactic mm-wave continuumsources that we have long used as targets for absorptionline studies of the chemistry of diffuse clouds. As is thecase for nearly all background sources seen at galactic latitudes|b| < 15−18 ◦ , and for some sources at higher latitudes, the currenttargets were known to show absorption from HCO + andfrom one or more other commonly-detected species (OH, CO,C 2 H, C 3 H 2 ); most but not all directions also were known to showCO emission in at <strong>le</strong>ast some of the kinematic features presentin absorption.This work is organized as follows. The observational materialdiscussed here is summarized in Sect. 2. In Sects. 3−5 wediscuss the new maps with sources grouped in order of kinematiccomp<strong>le</strong>xity. Section 6 is an intermediate summary of the<strong>le</strong>ssons drawn from close scrutiny of the maps. Section 7 brieflydiscusses the influences of galactic and internal cloud kinematicsand Sect. 8 presents a comparison of CO intensity and reddeningwithin a few of the simp<strong>le</strong>r individual fields. Appendix A showsa few position-velocity diagrams that, whi<strong>le</strong> of interest, couldbe considered redundant with those shown in the main text inFigs. 13 and 14. Figures B.1 and B.2 in Appendix B show the targetlines of sight in the context of large-sca<strong>le</strong> galactic kinematicssamp<strong>le</strong>d in H I emission.2. Observational material2.1. CO J = 1–0 emissionOn-the-fly maps of CO J = 1−0 emission were made at theARO 12 m <strong>tel</strong>escope in 2008 December, 2009 January and2009 December in generally poor weather using filter banks with100 kHz or 0.260 km s −1 channel spacing and spectral resolution.System temperatures were typically 450−750 K. The datawere subsequently put onto 20 ′′ pixel grids using the AIPS tasksOTFUV and SDGRD; the final spatial resolution is 1 ′ .Mostmaps are approxima<strong>tel</strong>y 30 ′ × 30 ′ on the sky and were comp<strong>le</strong>tedin 4−5 h total observing time. The new CO emission dataare presented in terms of the TR ∗ sca<strong>le</strong> in use at the 12 m antennaand all velocities are referred to the kinematic Local StandardA58, page 2 of 23of Rest. The typical rms channel-channel noise in these mapsat 1 ′ and 0.26 km s −1 resolution is 0.4−0.5 K; their sensitivity israther moderate and the detectability limit is of order 1 K km s −1for a sing<strong>le</strong> line component.More sensitive CO J = 1−0 line profi<strong>le</strong>s at higher spectralresolution (25 kHz) had been previously observed toward thecontinuum sources as part of our survey efforts, for instance seeLiszt & Lucas (1998). It is these profi<strong>le</strong>s that are displayed inthe figures shown here representing emission in the specific directionof the background target and used to calculate line profi<strong>le</strong>integrals as quoted in Tab<strong>le</strong> 1.Many inters<strong>tel</strong>lar clouds lie at distances of about 150 pc fromthe Sun, just outside the Local Bubb<strong>le</strong>. At this distance the 1 ′ resolutionof our CO mapping corresponds to 0.041 pc.2.2. H I absorption and emission and N(H I)The λ 21 cm H I absorption spectra shown here are largely fromthe work of Dickey et al. (1983) augmented by a few spectrataken at the VLA in 2005 May. The spectral resolution of thisdata is 0.4−1.0 km s −1 .Figures B.1 and B.2 of the Appendix B show latitudevelocitydiagrams of H I emission drawn from the Leiden-Dwingeloo Survey of Hartmann & Burton (1997).The H I column densities quoted in Tab<strong>le</strong> 1 were derived inone of two ways. Where an H I absorption profi<strong>le</strong> exists we appliedthe formula given in footnote 3 to Tab<strong>le</strong> 1, which is an empiricalrelation derived by Liszt et al. (2010) using the AreciboH I emission-absorption survey data of Hei<strong>le</strong>s & Troland (2003).The effective H I spin temperature implied by use of this formulais 143 K. In other cases (see footnote 4 to Tab<strong>le</strong> 1) we apply theoptically-thin limit to the data of Hartmann & Burton (1997).2.3. Mo<strong>le</strong>cular absorptionAlso shown here are spectra of λ18 cm OH absorption fromLiszt & Lucas (1996), λ6cmH 2 CO from Lisztetal.(2006), J =1−0 mm-wave absorption spectra of CO (Liszt & Lucas 1998),HCO + (Lucas & Liszt 1996), HCN and HNC (Liszt & Lucas2001), CS J = 2−1 (Lucas & Liszt 2002) and the 87.32 GHzN = 1−0, J = 3/2−1/2, F = 2−1 transition of C 2 H(Lucas &Liszt 2000).2.4. ReddeningMaps of reddening were constructed from the results of Sch<strong>le</strong>ge<strong>le</strong>t al. (1998). This dataset has 6 ′ spatial resolution on a 2.5 ′ pixelgrid. The stated sing<strong>le</strong>-pixel error is a percentage, 16%, of thepixel value. On average, 1 mag of reddening corresponds to aneutral gas column N(H) = 5.8 × 10 21 cm −2 (Savage et al. 1977).2.5. Target fieldsThe positions and other observational properties are summarizedin Tab<strong>le</strong> 1 where the sources are grouped according to their orderofpresentationinSects.3−5.The groups appear in orderof increasing reddening and gas column density and decreasingdistance from the galactic plane. The line profi<strong>le</strong> integrals W COquoted in Tab<strong>le</strong> 1 result from the more sensitive earlier observationsnoted in Sect. 2.1. The mean values quoted for W CO alongindividual sightlines are averages over the new map data takenfor this work.

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