2012MNRAS.424..532O


Query : 2012MNRAS.424..532O

2012MNRAS.424..532O - Mon. Not. R. Astron. Soc., 424, 532-544 (2012/July-3)

Parsec-scale morphology and spectral-index distribution in faint high-frequency peakers.

ORIENTI M. and DALLACASA D.

Abstract (from CDS):

We investigate the parsec-scale structure of 17 high-frequency peaking radio sources from the faint high-frequency peaker sample. Very Long Baseline Array (VLBA) observations were carried out at two adjacent frequencies, 8.4 and 15.3 GHz, both in the optically thin part of the spectrum, to obtain the spectral-index information. We found that 64 per cent of the sources are resolved into subcomponents, while 36 per cent are unresolved even at the highest frequency. Among the resolved sources, seven have a morphology and a spectral-index distribution typical of young radio sources, while in other four sources, all optically associated with quasars, the radio properties resemble those of the blazar population. The equipartition magnetic field of the single components are a few tens milliGauss, similar to the values found in the hotspots of young sources with larger sizes. Such high magnetic fields cause severe radiative losses, precluding the formation of extended lobe structures emitted at centimetre wavelengths. The magnetic fields derived in the various components of individual source are usually very different, indicating a non-self-similar source evolution, at least during the very first stages of the source growth.

Abstract Copyright: 2012 The Authors Monthly Notices of the Royal Astronomical Society2012 RAS

Journal keyword(s): radiation mechanisms: non-thermal - galaxies: active - radio continuum: general

Simbad objects: 28

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Number of rows : 28
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2026
#notes
1 7C 055201.39+394824.00 Bla 05 55 30.80561419 +39 48 49.1649683     18.30 17.5   ~ 527 2
2 QSO B0646+600 Bla 06 50 31.25435548 +60 01 44.5549353   18.9 18.6 19.65   ~ 125 1
3 GB6 B0732+4751 Rad 07 36 01.4 +47 44 25           ~ 1 0
4 QSO B0738+491 Bla 07 42 02.74895098 +49 00 15.6089311   22.33 21.75 21.33   ~ 62 1
5 NVSS J080459+543157 rG 08 04 59.20968 +54 31 57.4860           ~ 4 1
6 87GB 081544.8+383340 AG? 08 19 00.95619 +38 23 59.8104           ~ 5 0
7 87GB 090216.7+375448 AG? 09 05 27.4406 +37 42 52.723           ~ 6 1
8 6C 091739+622838 Bla 09 21 36.23107643 +62 15 52.1803510   19.76 19.26 18.96   ~ 394 1
9 4C 39.25 Bla 09 27 03.01394144 +39 02 20.8518067   17.17 17.00 16.486   ~ 1036 1
10 6C 092554+502611 BLL 09 29 15.4401569832 +50 13 35.990913000   17.18 16.80 15.94   ~ 159 2
11 NVSS J094351+511321 rG 09 43 51.81887 +51 13 22.4676           ~ 5 1
12 NVSS J095111+345131 Rad 09 51 11.39 +34 51 31.5           ~ 2 0
13 Ton 1125 QSO 09 55 37.9390883544 +33 35 03.940465164     17 16.72   ~ 67 1
14 NVSS J100241+570111 Rad 10 02 41.66625 +57 01 11.4833           ~ 4 0
15 SDSS J100820.75+253339.5 QSO 10 08 20.7541706136 +25 33 39.557482092   19.34 18.96     ~ 22 1
16 7C 112812.59+383153.00 Bla 11 30 53.28261620 +38 15 18.5469361   19.11 18.80 19.42   ~ 233 1
17 FIRST J113552.2+362422 Rad 11 35 52.285 +36 24 21.99           ~ 1 0
18 SDSS J124143.13+384404.3 QSO 12 41 43.134 +38 44 04.30           ~ 3 0
19 6C 124026+380741 Bla 12 42 51.36906848 +37 51 00.0252818   18.86 18.46 18.79   ~ 99 1
20 [VV2006] J130941.5+404757 QSO 13 09 41.5089517896 +40 47 57.233876136   19.67 19.43     ~ 34 0
21 SDSS J131930.29+485103.1 Bla 13 19 30.2945755272 +48 51 03.197155824       18.9   ~ 21 1
22 6C 132700+502509 QSO 13 29 05.80271152 +50 09 26.4008812     18.10     ~ 49 1
23 4C 58.26 Bz? 13 35 25.92853561 +58 44 00.2912887       21.91   ~ 60 1
24 Mrk 668 BLL 14 07 00.39441712 +28 27 14.6901341   16.13 15.35 10.29   ~ 826 3
25 NVSS J143618+482039 Rad 14 36 18.9082 +48 20 41.139           ~ 4 1
26 JVAS B1611+425 Bz? 16 13 04.80334 +42 23 18.8930       19.40   ~ 12 0
27 NVSS J173549+504911 rG 17 35 49.00517 +50 49 11.5659       22.40   ~ 57 1
28 QSO B2134+0028 Bla 21 36 38.58632232 +00 41 54.2128562   17.30 17.08 17.02   ~ 580 2

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