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A COMPLETE SPECTROSCOPIC CHARACTERIZATION OF SO AND ITS ISOTOPOLOGUES UP TO THE TERAHERTZ DOMAIN

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Published 2015 January 21 © 2015. The American Astronomical Society. All rights reserved.
, , Citation M. A. Martin-Drumel et al 2015 ApJ 799 115 DOI 10.1088/0004-637X/799/2/115

0004-637X/799/2/115

ABSTRACT

In order to obtain accurate terahertz center frequencies for SO and its isotopologues, we have studied the absorption spectrum of SO, 34SO, and 33SO up to 2.5 THz using continuous-wave terahertz photomixing based on a frequency comb providing an accuracy down to 10 kHz. Sulfur monoxide was produced in a radio frequency discharge of air in a cell containing pure sulfur. Together with the strong absorption signal of the main isotopologue, transitions of 34SO (34S: 4.21%) and 33SO (33S: 0.75%) were observed in natural abundance. The newly observed transitions constitute an extension of the observed rotational quantum numbers of the molecule toward higher N values, allowing an improvement of the molecular parameters for the three species. An isotopically invariant fit has been performed based on pure rotational and ro-vibrational transitions of all SO isotopologues, enabling their accurate line position prediction at higher frequencies. Thanks to this new set of parameters, it is now possible to predict with very high accuracy the frequencies of the ro-vibrational lines. This should enable the research of SO in the mid-IR using ground-based IR telescopes, space-based telescope archives (Infrared Space Observatory, Spitzer), and future space missions such as the James Webb Space Telescope. This set of parameters is particularly well adapted for the detection of SO lines in O-rich evolved stars or in molecular clouds in absorption against bright IR sources.

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1. INTRODUCTION

Since its first detection in the interstellar medium by means of rotational spectroscopy (Gottlieb & Ball 1973), sulfur monoxide, SO, has been observed in a wide variety of astrophysical environments (see Klaus et al. 1994, and references therein). This transient species is particularly abundant in star-forming regions characterized by high temperature and gas concentrations (Blake et al. 1987). It has been detected in the atmosphere of Venus (Na et al. 1990) and in Io, one of Jupiter's moons, where it is thought to be produced by volcanic and photochemical pathways (Lellouch 1996). In planetary atmospheres, the presence of the SO radical results from the photodecomposition of sulfur dioxide (Krasnopolsky 2012). SO is also an important reaction intermediate in combustion and Earth atmospheric chemistry due to its high reactivity and its role in reactions involving molecules containing nitrogen and oxygen (see Burkholder et al. 1987, and references therein).

SO was first identified in the laboratory in 1932 through the observation of its electronic transitions (Martin 1932). Since then, numerous electronic (Colin 1968), ro-vibrational (Kanamori et al. 1985; Burkholder et al. 1987), as well as pure rotational studies have been dedicated to this radical. The electric dipole moment of SO has also been determined by Stark measurements (1.55 D; Powell & Lide 1964). Pure rotational transitions of SO have been observed in the microwave (Lovas et al. 1992), the terahertz (THz), (Cazzoli et al. 1994), and far infrared (FIR) regions (Cheung et al. 1991; Martin-Drumel et al. 2013) in numerous vibrational states of the ground electronic state (Bogey et al. 1982). SO is also the first molecule for which pure rotational transitions have been detected in several excited electronic states (Saito 1970; Clark & De Lucia 1976; Endo et al. 1987; Bogey et al. 1997; Sanz et al. 2003). Since the sulfur atom possesses three relatively abundant isotopes (32S: 95.02%, 34S: 4.21%, 33S: 0.75%), several studies have also been dedicated to the SO isotopologues (e.g., Tiemann 1982; Klaus et al. 1996; Sanz et al. 2003). Isotopically invariant parameters have been derived from combined fits of all isotopic species (Klaus et al. 1996) and Dunham coefficients have also been determined (Sanz et al. 2003).

Recently, pure rotational transitions of SO have been observed by means of synchrotron-based Fourier-transform FIR (FT-FIR) spectroscopy (Martin-Drumel et al. 2013). In this study, 102 transitions were recorded in the spectral range 1.3–2.8 THz with a frequency accuracy limited to 2 MHz. In the present study, we have re-investigated this range of the spectrum using a photomixing technique allowing a higher accuracy to be achieved (down to 10 kHz). We also have extended the observed transitions of both 34SO and 33SO (detected in natural abundance) toward higher frequencies. Improved effective molecular constants and isotopically invariant parameters have been derived from these new results. Frequency predictions obtained from this new isotopically invariant fit are accurate in the THz region and will permit further exploration of the SO (and its rare isotopologues) spectra in astronomical sources observed with the HIFI instrument (De Graauw et al. 2010) on board the Herschel satellite (Pilbratt et al. 2010; see HEXOS and CHESS Herschel guaranteed programs; Wang et al. 2011; Ceccarelli et al. 2010).

2. EXPERIMENTAL METHOD

The continuous-wave terahertz (cw-THz) photomixing spectrometer used in this study has been described in detail elsewhere (Eliet et al. 2011; Hindle et al. 2011; Mouret et al. 2009). Briefly, the operation of the photomixing source is based on the spatial superposition of two extended cavity diode lasers (ECDLs; emitting around 780 nm) creating an optical beatnote, which is converted to free space THz radiation by a photomixer (ultrafast LTG-GaAs device). This spectrometer is tunable between 0.3 and 3.3 THz. A frequency comb (FC) generated by a frequency doubled erbium doped femtosecond fiber laser enables the achievement of the ECDLs' frequency stability of 1 MHz or better. The FC repetition rate, which separates each mode of the FC, is locked to a low phase-noise oven-controlled crystal oscillator, which is itself locked to the GPS timing signal (Spectracom, EC20S). This reference frequency provides an accuracy of 2 × 10−12 over a period of 24 hr. Two phase-locked loops are used to lock the two ECDLs to the FC, accurately fixing the difference frequency; the accuracy in line frequency is thus only limited by the line profile. The use of a third ECDL ensures a continuous tunability up to 500 MHz, illustrated in the study of the SO radical, wherein a 510 MHz continuous portion of the 32SO spectrum was recorded around 1 THz (Figure 1). This spectrum, showing a rotational triplet, has been recorded in about ten minutes using frequency steps of 400 kHz and a time constant of 100 ms. The periodic variations observed in the baseline of the recordings are caused by a weak Fabry–Perot effect established between the photomixer and the bolometer, here separated by 1.87 m. The photomixing technique has the greatest tuning range of any known coherent source in the THz region, and has a spectral purity smaller than the Doppler limit at room temperature.

Figure 1.

Figure 1. Observation of a fine structure triplet of 32SO over a continuous range of about 500 MHz. This spectrum required about 10 minutes of acquisition time.

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The THz beam is collimated through the cell and focused onto a silicon liquid-helium cooled detector by means of two off-axis parabolic mirrors. In this study, both amplitude modulation (AM) and frequency modulation (FM) modes of operation have been used. ΔJ = 1 transitions of 32SO have been recorded in AM using a 263 Hz modulation frequency (Figure 1). ΔJ = 0 transitions of 32SO (100 times weaker than ΔJ = 1) as well as lines of 34SO and 33SO have been recorded in FM with a modulation depth of 120 kHz and a rate of 273 Hz (Figure 2). A second harmonic scheme is employed in order to optimize the signal-to-noise ratio (S/N). Despite this rather slow modulation frequency, which was necessary due to the use of a "slow" Si-bolometer, an improvement in S/N by more than a factor 10 has been observed using the FM instead of the AM configuration.

Figure 2.

Figure 2. Fine structure triplet of 34SO (upper trace) and 33SO (lower trace) observed in the frequency modulation.

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The SO radical was produced by a 50 W radiofrequency discharge using air in a cell containing a pure sulfur deposit. The air flow was ensured by a roughing pump. Absorption levels of up to 80% were obtained for the main isotopologue in its vibrational ground state. 34SO and 33SO isotopologues were observed in natural abundance. A discharge in a flow air and H2S mixture yielded a lower SO concentration. SO2 transitions in the ground and first excited vibrational state have been identified in the spectrum (Figures 1 and 2). Experimental conditions were adjusted for each transition in order to achieve the highest S/N possible in a reasonable acquisition time (pressure: 20–500 μbar; time constant: 0.5–2 s; steps: 100–600 kHz.) S/Ns up to 260, 70, and 40 have been obtained for 32SO, 34SO, and 33SO, respectively.

3. RESULTS AND DISCUSSION

In its fundamental X3Σ electronic state, SO is an intermediate between Hund's coupling schemes (a) and (b). However, by convention the rotational structure of the radical is described in the (b) formalism using the rotational quantum number N. The coupling between the electronic spin and the rotation of the molecule, by means of spin–spin (interaction between the magnetic moments associated with the two unpaired electrons under the effect of the rotation) and spin–rotation (interaction with Π excited electronic states) coupling, leads to a rotational fine structure of three components (for N > 0) associated with the quantum number J ($\boldsymbol{J}=\boldsymbol{N+S}$, S = 1) and separated by a few hundred GHz (a few wavenumbers).

Due to the wide range of observed frequencies (and thus of FWHMs) and S/Ns, we performed a line profile fit on all transitions to determine their center frequency and estimate their accuracy. Only lines presenting no more than 60% to 70% of absorption (when recorded in AM) were considered in the process to prevent saturating line shapes. Rotational transitions were fitted with a pseudo-Voigt profile of type (1 − s)G + sL (with G and L a Gaussian and Lorentzian function, respectively, and s the "shape" of the line):

Equation (1)

where A is the height of the line, B is the center frequency, and C is the FWHM. Compared to a classical Voigt profile, the second derivative of this analytical formula can be easily calculated in order to fit the transitions recorded in FM (second derivative shape). The accuracy of each line position δ(ν) was then estimated from the formula (Landman et al. 1982):

Equation (2)

where Δν is the frequency step and S/N is the signal-to-noise ratio.

One-hundred five transitions of 32SO in its vibrational ground state (16 ⩽ N'' ⩽ 58) have been recorded in the spectral region 0.731–2.511 THz with frequency accuracies Δ(ν) ranging from 10 to 800 kHz. 48 (17 ⩽ N'' ⩽ 32) and twenty-one (16 ⩽ N'' ⩽ 22) transitions of the 34SO and 33SO isotopologues in v = 0 have also been observed in natural abundance up to 1.388 THz and 978 GHz, respectively. The observed transitions are presented with their calculated uncertainty in Tables 13.

Table 1. Observed Transitions of the 32SO Radical, Uncertainties, and Obs.−Calc. of the Effective Fit (in MHz)

N' J' N'' J'' νobs Unc.   Obs.−Calc. N' J' N'' J'' νobs Unc. Obs.−Calc.
17 16 16 15 730500.794 0.006 0.003 35 36 34 35 1500812.597 0.052 0.011
17 17 16 16 731141.318 0.010 0.014 35 35 34 34 1500844.634 0.070 0.005
17 18 16 17 731596.448 0.020 −0.023 36 37 35 36 1543337.554 0.033 0.018
13 13 12 13 735235.258 0.443 −0.134 36 35 35 34 1543358.014 0.030 −0.015
18 17 17 16 773512.352 0.030 0.031 36 36 35 35 1543378.858 0.035 −0.030
18 18 17 17 774064.140 0.008 0.006 37 38 36 37 1585833.824 0.040 0.020
18 19 17 18 774454.646 0.020 −0.021 37 36 36 35 1585871.743 0.039 −0.015
14 14 13 14 777349.654 0.168 −0.116 37 37 36 36 1585883.825 0.043 0.019
19 18 18 17 816495.167 0.005 0.006 38 39 37 38 1628300.550 0.033 0.043
19 19 18 18 816972.307 0.008 −0.001 38 37 37 36 1628354.537 0.030 −0.054
19 20 18 19 817307.322 0.010 −0.013 38 38 37 37 1628358.632 0.040 0.068
15 15 14 15 819582.919 0.123 −0.141 41 42 40 41 1755514.487 0.012 −0.007
20 19 19 18 859451.295 0.020 0.020 41 41 40 40 1755593.648 0.060 −0.063
20 20 19 19 859864.990 0.020 −0.021 41 40 40 39 1755610.234 0.013 −0.020
20 21 19 20 860152.012 0.002 0.003 42 43 41 42 1797854.326 0.050 0.088
16 16 15 16 861911.759 0.233 −0.018 42 42 41 41 1797939.761 0.111 0.104
21 20 20 19 902381.990 0.015 0.016 42 41 41 40 1797962.050 0.089 0.051
21 21 20 20 902741.427 0.005 −0.001 43 44 42 43 1840160.085 0.014 −0.010
21 22 20 21 902986.581 0.005 0.001 43 43 42 42 1840251.568 0.210 0.213
22 21 21 20 945288.113 0.015 0.018 43 42 42 41 1840279.079 0.021 0.022
22 22 21 21 945600.753 0.010 0.009 44 45 43 44 1882431.282 0.070 0.067
22 23 21 22 945809.191 0.010 −0.012 44 44 43 43 1882528.012 0.030 0.025
23 22 22 21 988170.122 0.010 0.005 44 43 43 42 1882560.712 0.050 0.061
23 23 22 22 988442.140 0.009 −0.005 45 46 44 45 1924666.702 0.060 −0.048
23 24 22 23 988618.234 0.005 −0.008 45 45 44 44 1924768.576 0.124 −0.156
24 23 23 22 1031028.243 0.007 −0.010 45 44 44 43 1924805.836 0.150 −0.160
24 24 23 23 1031264.791 0.030 −0.023 46 47 45 46 1966865.938 0.080 0.081
24 25 23 24 1031412.184 0.015 −0.029 46 46 45 45 1966972.835 0.037 0.061
25 24 24 23 1073862.505 0.009 −0.006 46 45 45 44 1967014.346 0.033 0.040
25 25 24 24 1074067.930 0.008 −0.006 47 48 46 47 2009027.719 0.014 0.026
25 26 24 25 1074189.757 0.005 −0.002 47 47 46 46 2009139.291 0.057 −0.001
26 25 25 24 1116672.751 0.039 0.009 47 46 46 45 2009184.768 0.060 −0.022
26 26 25 25 1116850.689 0.017 −0.007 48 49 47 48 2051151.445 0.032 0.027
26 27 25 26 1116949.615 0.010 −0.001 48 48 47 47 2051267.430 0.085 −0.036
28 27 27 26 1202220.034 0.080 0.095 48 47 47 46 2051316.478 0.095 −0.177
28 28 27 27 1202351.851 0.029 −0.017 49 50 48 49 2093236.218 0.047 0.024
28 29 27 28 1202411.573 0.026 −0.016 49 49 48 48 2093356.472 0.038 −0.006
29 28 28 27 1244956.091 0.010 0.003 49 48 48 47 2093409.097 0.076 −0.006
29 29 28 28 1245068.634 0.013 −0.015 50 51 49 50 2135281.061 0.089 −0.123
29 30 28 29 1245111.501 0.011 −0.003 50 50 49 49 2135405.481 0.114 −0.027
30 29 29 28 1287666.615 0.010 −0.001 50 49 49 48 2135461.388 0.103 0.053
30 30 29 29 1287761.799 0.023 −0.005 51 52 50 51 2177285.828 0.300 0.275
30 31 29 30 1287789.321 0.024 0.007 51 51 50 50 2177413.796 0.084 0.061
31 30 30 29 1330351.049 0.049 0.085 51 50 50 49 2177472.782 0.151 0.231
31 31 30 30 1330430.582 0.041 0.065 54 55 53 54 2303046.535 0.035 −0.061
31 32 30 31 1330444.057 0.038 0.040 54 54 53 53 2303185.285 0.063 −0.111
32 31 31 30 1373008.620 0.080 0.085 54 53 53 52 2303252.063 0.061 0.014
32 32 31 31 1373074.332 0.015 0.359 59 60 58 59 2511758.120 0.199 −0.103
32 33 31 32 1373074.332 0.015 −0.306 59 59 58 58 2511912.066 0.165 −0.094
33 32 32 31 1415638.720 0.022 0.024 59 58 58 57 2511988.643 0.385 −0.234
33 34 32 33 1415680.221 0.019 −0.005              
33 33 32 32 1415691.347 0.022 −0.008              
34 33 33 32 1458240.783 0.013 −0.007              
34 35 33 34 1458259.812 0.030 −0.036              
34 34 33 33 1458281.850 0.014 0.004              

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Table 2. Observed Transitions of the 33SO Radical, Uncertainties, and Obs−Calc. of the Effective Fit (in MHz)

N' J' N'' J'' νobs Unc. Obs.−Calc.
17 16 16 15 723120.527 0.100 −0.096
17 17 16 16 723773.541 0.060 0.030
17 18 16 17 724239.271 0.100 0.115
18 17 17 16 765701.564 0.060 −0.034
18 18 17 17 766264.657 0.070 −0.004
18 19 17 18 766664.898 0.050 0.029
19 18 18 17 808253.989 0.060 −0.020
19 19 18 18 808741.466 0.060 0.013
19 20 18 19 809085.500 0.030 0.036
20 19 19 18 850779.866 0.050 −0.005
20 20 19 19 851203.133 0.070 0.045
20 21 19 20 851498.467 0.050 −0.008
21 20 20 19 893280.267 0.300 −0.270
21 21 20 20 893648.772 0.060 0.004
21 22 20 21 893901.769 0.070 −0.024
22 21 21 20 935756.929 0.050 0.051
22 22 21 21 936077.704 0.080 0.008
22 23 21 22 936293.460 0.100 −0.120
23 22 22 21 978209.472 0.060 0.065
23 23 22 22 978489.047 0.060 −0.027
23 24 22 23 978672.033 0.130 −0.171

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Table 3. Observed Transitions of the 34SO Radical, Uncertainties, and Obs.−Calc. of the Effective Fit (in MHz)

N' J' N'' J'' νobs Unc.   Obs.−Calc. N' J' N'' J'' νobs Unc. Obs.−Calc.
17 16 16 15 716194.548 0.011 −0.006 25 24 24 23 1052890.648 0.016 −0.002
17 17 16 16 716859.006 0.010 −0.002 25 25 24 24 1053108.760 0.010 0.000
17 18 16 17 717334.413 0.019 −0.005 25 26 24 25 1053242.510 0.009 0.006
18 17 17 16 758371.481 0.005 −0.009 27 26 26 25 1136826.278 0.017 0.003
18 18 17 17 758945.041 0.010 0.024 27 27 26 26 1136991.152 0.010 0.001
18 19 17 18 759354.202 0.005 0.013 27 28 26 27 1137080.312 0.013 −0.007
19 18 18 17 800519.976 0.005 0.001 28 27 27 26 1178758.414 0.019 −0.018
19 19 18 18 801016.965 0.030 0.026 28 28 27 27 1178901.035 0.030 0.006
19 20 18 19 801369.207 0.006 −0.012 28 29 27 28 1178971.123 0.038 −0.016
20 19 19 18 842642.090 0.012 0.023 29 28 28 27 1220666.290 0.032 0.001
20 20 19 19 843073.978 0.012 −0.011 29 29 28 28 1220788.999 0.032 0.015
20 21 19 20 843377.019 0.013 −0.021 29 30 28 29 1220841.829 0.031 0.010
21 20 20 19 884739.175 0.011 0.019 30 29 29 28 1262549.397 0.023 0.001
21 21 20 20 885115.381 0.014 −0.004 30 30 29 29 1262654.233 0.025 0.002
21 22 20 21 885375.605 0.060 0.064 30 31 29 30 1262691.360 0.032 0.010
22 21 21 20 926812.158 0.010 0.010 31 30 30 29 1304407.197 0.024 −0.031
22 22 21 21 927140.334 0.008 −0.010 31 31 30 30 1304495.994 0.041 0.009
22 23 21 22 927362.870 0.015 −0.018 31 32 30 31 1304518.775 0.027 0.016
23 22 22 21 968861.590 0.011 0.007 32 31 31 30 1346239.181 0.055 −0.043
23 23 22 22 969148.079 0.008 −0.002 32 32 31 31 1346313.464 0.040 0.001
23 24 22 23 969337.459 0.009 0.005 32 33 31 32 1346323.072 0.063 −0.027
24 23 23 22 1010887.730 0.007 −0.000 33 32 32 31 1388044.783 0.056 −0.006
24 24 23 23 1011137.816 0.008 0.001 33 34 32 33 1388103.506 0.062 0.059
24 25 23 24 1011297.769 0.006 −0.003 33 33 32 32 1388105.958 0.067 0.078

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The following sections detail the two fitting processes performed in this work. We first performed an effective fit for each of the three isotopologues observed in this study. These fits provide the most accurate rotational parameters for the three molecules. However, due to the lack of predictive reliability of such effective fits (see an example in the next paragraph) we performed a global fit of all the data available on SO (all isotopologues and all vibrational states).

3.1. Effective Fit of 32SO, 34SO, and 33SO

The effective Hamiltonian for SO in its X3Σ electronic ground state is:

Equation (3)

Equation (4)

where B is the rotational constant, λ the spin–spin coupling constant, and γ the spin–rotation coupling constant, neglecting the centrifugal distortion. In the case of 33SO, the non-null nuclear spin of the 33S (I = 3/2) leads to a hyperfine structure of four components separated by a few tens of MHz. This effect could not be resolved in the present study.

The newly recorded transitions have been fitted using the SPFIT/SPCAT software (Pickett 1991) together with previously available data reported in the literature for 32SO, 33SO and 34SO (see references in Table 4). Multiple experimental values for one transition were kept in the fit (weighted according to their respective accuracy) since they were all obtained by independent measurements. Reduced standard deviations (dimensionless) of 0.88, 0.82, and 0.85 have been obtained for the three fits. Results are compared with Ref. Martin-Drumel et al. (2013) in the case of 32SO, and to a refit of previously available data for the two other isotopologues (Table 5). For each isotopologue, fitting the newly recorded transitions (only), with parameters fixed at their final values, resulted in rms values lower than 100 kHz, and a reduced standard deviation of 0.99, 0.75, and 0.84. This reflects the quality of our measurements and uncertainty estimation.

Table 4. References Used in the Effective and Isotopically Invariant Fits

Isotopologue References
Effective fit
32S16O Powell & Lide (1964); Winnewisser et al. (1964); Amano et al. (1967); Tiemann (1974); Clark & De Lucia (1976); Bogey et al. (1982);
  Tiemann (1982); Lovas et al. (1992); Cazzoli et al. (1994); Klaus et al. (1996); Bogey et al. (1997); Hansen et al. (1998);
  Martin-Drumel et al. (2013); Sanz et al. (2003)
33S16O Amano et al. (1967); Klaus et al. (1996); Sanz et al. (2003)
34S16O Amano et al. (1967); Tiemann (1974); Bogey et al. (1982); Tiemann (1982); Lovas et al. (1992); Klaus et al. (1996); Sanz et al. (2003)
Isotopically invariant fit (additional references)
32S16O Kawaguchi et al. (1979); Wong et al. (1982); Kanamori et al. (1985); Burkholder et al. (1987)
34S16O Burkholder et al. (1987); Hansen et al. (1998)
36S16O Klaus et al. (1996)
32S17O Klaus et al. (1996)
32S18O Lovas et al. (1992); Tiemann (1974); Bogey et al. (1982); Tiemann (1982); Klaus et al. (1994, 1996); Burkholder et al. (1987)

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Table 5. Ground State Molecular Constants (in MHz) of 32SO, 33SO, and 34SO, and Comparison with Previous Values

  32SO 33SO 34SO
  This Work Previous Valuesa This Work Previous Valuesb This Work Previous Valuesc
B 21 523.555 878 (79) 21 523.556 16 (37) 21 306.465 38 (86) 21 306.465 23 (97) 21 102.732 28 (31) 21 102.733 14 (82)
D × 103 33.915 261 (85) 33.915 56 (70) 33.238 7 (11) 33.239 6 (14) 32.600 73 (55) 32 606 4 (13)
H × 109 −6.974 (22) −7.09 (17)     −6.06 (31)  
λ 158 254.392 (09) 158 254.387 (13) 158 252.22 (14) 158 252.28 (15) 158 249.807 (24) 158 249.816 (27)
λD 0.306 259 (72) 0.306 53 (20) 0.303 65 (62) 0.303 9 (12) 0.300 63 (08) 0.300 28 (79)
λH × 106 0.478 (47)          
γ −168.304 3 (15) −168.304 1 (40) −166.622 (20) −166.630 (21) −164.994 8 (36) −164.992 9 (65)
γD × 103 −0.525 45 (97) −0.523 1 (85) −0.358 (20) −0.344 (35) −0.511 6 (27) −0.515 (22)
b     18.883 (19) 18.883 (19)    
c     −96.34 (11) −96.34 (11)    
eQq     −15.453 1 (71) −15.453 1 (71)    
CI     0.015 1 (73) 0.014 8 (74)    
Fitted lines 329 184 100 79 95 48
σd 0.88 0.64 0.82 0.82 0.85 0.95

Notes. Errors (1σ) are reported in parentheses in the unit of the last digit. aPrevious values from Martin-Drumel et al. (2013). bObtained by refitting data from Amano et al. (1967), Klaus et al. (1996), and Sanz et al. (2003). cObtained by refitting data from Amano et al. (1967), Tiemann (1974), Tiemann (1982), Bogey et al. (1982), Lovas et al. (1992), and Klaus et al. (1996). dReduced standard deviation (dimensionless).

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The addition of new transitions with higher N values allows the determination of molecular parameters with higher accuracy. The error of the centrifugal distortion parameters is decreased by up to an order of magnitude. Furthermore, λH for 32SO and H for 34SO have been determined for the first time. In case of 33SO, the hyperfine structure due to the 33S nucleus has not been resolved, hence the hyperfine structure parameters b, c, eQq, and CI are not better determined. The amelioration of the centrifugal distortion parameters is particularly visible when examining the dispersion on the frequency predictions for the 32SO radical in Figure 3. This plot presents the difference between the frequencies of the lines observed in this study (cw-THz) and the calculated frequencies obtained with different parameter sets (obs. − calc.). The experimental uncertainty on the line frequency is plotted as error bars. The calculated frequencies based on the initial set of data (pure rotational data from the literature apart from Martin-Drumel et al. 2013) present the strongest discrepancy with the experimental values. This set of data contains pure rotational transitions up to 1.9 THz and the deviation of the prediction is visible, 2.5 MHz at 2.5 THz, while the error on the frequencies of the lines at 2.5 MHz were estimated to be of only 5 kHz. This illustrates the lack of reliability of effective fits regarding the predictions mentioned above.

Figure 3.

Figure 3. Comparison of the frequency predictions of 32SO obtained using the parameters from the initial pure rotation data, those from Martin-Drumel et al. (2013; synchrotron-based FT-FIR), and the final parameters obtained in this study (cw-THz). Error bars are the uncertainty on the frequency of the experimental transitions.

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We also note that the addition of FT-FIR data in the fit allows a significant improvement of the prediction, despite the fact that these data have a limited frequency accuracy of 2 MHz. This is an illustration of the complementarity of synchrotron-based FT-FIR spectroscopy and cw-THz technique for the study of transient species (see also Martin-Drumel et al. 2012): the former allows a broad survey of the FIR region with a limited resolution (30 MHz), consequently allowing a fast and efficient recording at kHz resolution of the same transitions with the latter technique.

3.2. Isotopically Invariant Fit

In order to provide reliable frequency predictions of SO isotopologues—including rare isotopologues—in the THz range, we performed an isotopically invariant fit. This global fit includes all reported pure rotational and ro-vibrational transitions of SO isotopologues in all observed vibrational states using the fitting programs associated with the MADEX spectroscopic code (Cernicharo 2013). The fitting code was checked against the results of Klaus et al. (1996) and provided the same rotational constants. The Dunham expansions used to determine the matrix elements are those reported in Klaus et al. (1994), although the hyperfine structure has not been considered. For the sake of clarity, energy expressions are summarized below.

The rovibrational energy levels are expressed by an expansion involving the isotopically invariant parameters Uij and the reduced mass μ (in a.u.):

Equation (5)

The spin–rotation (SR) and spin–spin (SS) interactions are expressed using the isotopically invariant parameters γij and λij:

Equation (6)

Equation (7)

The breakdown of the Born–Oppenheimer approximation yields a slight modification of the previous equations. For instance, denoting the isotopes A and B for the two nuclei, the U01 constant is defined as (Tiemann 1982):

Equation (8)

where $X_{01}^A$ and $X_{01}^B$ carry the corrections to the Born–Oppenheimer approximation. MA and MB are the atomic masses of the considered isotopes while $M_A^0$ and $M_B^0$ are the atomic masses of the reference isotopes (here 32S and 16O). Atomic masses used in our fits are taken from the AME2012 (Audi et al. 2012; Wang et al. 2012). Unlike the one used by Klaus et al. (1994), our program did not allow us to include hyperfine interactions. Consequently, for isotopologues containing the nuclei 33S (spin I = 3/2) or 17O (spin I = 5/2), the observed hyperfine components have been averaged with a weight relative to their intensities (taken from the CDMS website; Müller et al. 2001), and the resulting frequencies have been included in the global fit.

Pure rotation and ro-vibration transitions of six isotopologues of SO from this work and the literature have been included in our fit. For the first time rotational and vibrational transitions have been merged in an isotopically invariant fit for the SO radical allowing the determination of the Ui0 constants. In total, 1766 transitions were included (see detailed references in Table 4): 1121 for 32S16O with v = 0–33, 53 for 33S16O with v = 0–8, 296 for 34S16O with v = 0–11, 28 for 36S16O with v = 0, 4 for 32S17O with v = 0, and 264 for 32S18O with v = 0–1.

A fit of all rotational and vibrational data using the uncertainties given by the different authors for the IR transitions produces a result in which the uncertainties for the rotational constants, Uij(j ≠ 0), are slightly degraded. An examination of the different sets of IR lines (by looking at the individual reduced standard deviation of each set of data) suggests that the quoted uncertainties for these data are in some cases optimistic. Hence, we have multiplied these uncertainties by a factor of two and eliminated in the final fit all lines for which the observed minus calculated frequencies exceed 3σ. The complete linelist is presented in the machine-readable table. A short example is shown in Table 6. The resulting 43 isotopically invariant parameters are given in Table 7 (reduced standard deviation of the fit: 0.8997). For the sake of comparison with previous studies and to observe the influence of the newly recorded transitions, a global fit including only pure rotational transitions has also been performed. The results are given in column two and can be compared with the results of Klaus et al. (1996) presented in the third column. The uncertainties of all parameters are improved with our data by a factor of 2–5.

Table 6. Pure Rotation and Ro-vibration Transitions of SO Included in the Isotopically Invariant Fit

Sa Ob N' J' ν' N'' J'' ν'' νobs Unc. Ref.
1 5 2 1 0 1 1 0 13043.8 0.20 1964JCP...41...1413c
1 5 0 1 0 1 0 0 30001.6 0.20 1964JCP...41...1413
1 5 3 2 0 2 2 0 36201.7 0.20 1964JCP...41...1413
1 5 1 2 0 0 1 0 62931.0 0.50 1964JCP...41...1413
1 5 4 3 0 3 3 0 66034.9 0.50 1964JCP...41...1413

Notes. Positive values indicate frequency in MHz, negative in cm−1. a1 = 32S; 2 = 33S; 3 = 34S; 4 = 36S. b5 = 16O; 6 = 17O; 7 = 18O. cPowell & Lide (1964).

Only a portion of this table is shown here to demonstrate its form and content. A machine-readable version of the full table is available.

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Table 7. Isotopically Invariant Parameters for the SO Radical

  Ro-vibrational Rotational (This Work) Rotationala Units
U10 3757.49542(195)  ⋅⋅⋅  ⋅⋅⋅ cm−1
X$^S_{10}$ −0.02551(209)  ⋅⋅⋅  ⋅⋅⋅ cm−1
X$^O_{10}$ −0.017252(516)  ⋅⋅⋅  ⋅⋅⋅ cm−1
U20 −68.32167(622)  ⋅⋅⋅  ⋅⋅⋅ cm−1
U30 0.47556(818)  ⋅⋅⋅  ⋅⋅⋅ cm−1
U40 −0.04041(463)  ⋅⋅⋅  ⋅⋅⋅ cm−1
U50 0.005031(934)  ⋅⋅⋅  ⋅⋅⋅ cm−1
U01 230387.59070(231) 230387.59057(277) 230387.56040(520) MHz amu
X$^S_{01}$ 7.80287(568) 7.80306(679) 7.8170(230) MHz amu
X$^O_{01}$ 21.4882(454) 21.4880(542) 21.5320(270) MHz amu
U11 −6001.6578(164) −6001.6561(197) −6001.4290(360) MHz amu3/2
U21 25.7585(267) 25.7522(321) 25.4620(750) MHz amu2
U31 −0.8254(175) −0.8211(211) −0.5910(560) MHz amu5/2
U41 −0.01197(508) −0.01296(611) −0.1180(140) MHz amu3
U51 −0.022075(633) −0.021972(759)  ⋅⋅⋅ MHz amu7/2
U61 0.0011700(256) 0.0011663(306)  ⋅⋅⋅ MHz amu4
U02 −3.8543097(229) −3.8543191(281) −3.853730(130) MHz amu2
U12 −0.004547(114) −0.004482(144) −0.008590(390) MHz amu5/2
U22 −0.0011636(577) −0.0011953(717)  ⋅⋅⋅ MHz amu3
U03 −0.0000078489(791) −0.0000078478(946) −0.00001260(140) MHz amu3
U13     0.0000299(46) MHz amu7/2
U04 −0.000000001040(146) −0.000000001041(174)  ⋅⋅⋅ MHz amu4
γ00 −1787.4277(276) −1787.4285(332) −1787.4230(370) MHz amu
γ10 −45.508(176) −45.501(212) −45.670(210) MHz amu3/2
γ20 1.871(133) 1.857(160) 2.210(150) MHz amu2
γ30 0.0986(216) 0.0995(260)  ⋅⋅⋅ MHz amu5/2
γ01 −0.060460(184) −0.060481(221) −0.058950(400) MHz amu2
γ11 0.00439(108) 0.00452(130)  ⋅⋅⋅ MHz amu5/2
λ00 157795.4203(201) 157795.4208(241) 157795.5340(680) MHz
X$^S_{00}$ 0.299(229) 0.303(273) −0.570(240) MHz
X$^O_{00}$ −7.722(235) −7.721(280) −7.200(130) MHz
λ10 2979.597(136) 2979.592(164) 2978.670(640) MHz amu1/2
X$^S_{10}$ −2.697(160) −2.702(191)  ⋅⋅⋅ MHz amu1/2
λ20 112.732(159) 112.745(191) 114.50(160) MHz amu
λ30 13.6225(953) 13.619(113) 12.00(130) MHz amu3/2
λ40 −0.1057(327) −0.1054(391) 0.780(310) MHz amu2
λ50 0.22948(606) 0.22949(724)  ⋅⋅⋅ MHz amu5/2
λ60 −0.018122(580) −0.018125(692)  ⋅⋅⋅ MHz amu3
λ70 0.0014205(229) 0.0014203(273)  ⋅⋅⋅ MHz amu7/2
λ01 3.24222(125) 3.24213(151) 3.24430(200) MHz amu
λ11 0.14226(791) 0.14287(954) 0.1490(120) MHz amu3/2
λ21 0.03545(466) 0.03505(561) 0.03140(780) MHz amu2
λ02 0.00005374(357) 0.00005379(426)  ⋅⋅⋅ MHz amu2
σb 0.8997 0.8112 0.70  

Notes. Errors (1σ) are reported in parentheses in the unit of the last digit. aConstants derived by Klaus et al. (1996). bReduced standard deviation.

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Born–Oppenheimer Breakdown (BOB) coefficients have been derived from the isotopically invariant fit following the formula (for an atom A; Watson 1980):

Equation (9)

Table 8 presents these coefficients together with a comparison with Klaus et al. (1996). Δ01 coefficients are slightly better determined while Δ10 are determined for the first time.

Table 8. Born–Oppenheimer Breakdown (BOB) Coefficients Derived from the Isotopically Invariant Fit

Parameter This Work Klaus et al. (1996)
$\Delta _{01}^S$ −1.9725 (14) −1.9772 (58)
$\Delta _{01}^O$ −2.7175 (57) −2.7247 (34)
$\Delta _{10}^S$ 0.395 (32)  ⋅⋅⋅
$\Delta _{10}^O$ 0.1338 (40)  ⋅⋅⋅

Note. Errors (1σ) are reported in parentheses in the unit of the last digit.

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Finally, molecular parameters for 12 isotopologues of SO in v = 0 to 5 (32S16O, 32S17O, 32S18O, 33S16O, 33S17O, 33S18O, 34S16O, 34S17O, 34S18O, 36S16O, 36S17O, 36S18O) have been derived from the isotopically invariant fit using a nonlinear least squares method. The obtained parameters are presented in Tables 912. The quality of the determination of the obtained parameters can be estimated since the error is dominated by the one of the dominant parameters (Y01 for B0, Y02 for D0, Y03 for H0,...). As an example, for 32SO in v = 0 the error on B0 (21 523.556 51 MHz, Table 9) should be of the order of 2 kHz (i.e., the error on Y01; Table 7) for all isotopologues, which is the strength of the isotopically invariant fit. This can be verified by comparison with the B0 value obtained using the effective fit for 32SO (21 523.555 878 (79) MHz; Table 5). The two values differ by 0.6 kHz, attesting to the quality of the derived parameters. However, for 32SO, 33SO, and 34SO in their vibrational ground state, the rotational constants of Table 5 are more accurate. For all other isotopologues and vibrational states, the parameters given in the previous tables will permit the prediction of reliable rotational frequencies in the THz domain.

Table 9. Derived Parameters (in MHz) for 32SO in the Six Lowest Vibrational Levels of the Electronic Ground State

  v = 0 v = 1 v = 2 v = 3 v = 4 v = 5
Isotopologue 32S16O
B 21523.55651 21351.59505 21180.06610 21008.95451 20838.24344 20667.91389
D × 102 3.39162 3.39304 3.39465 3.39645 3.39845 3.40063
H × 109 −6.47734 −6.47734 −6.47734 −6.47734 −6.47734 −6.47734
L × 1014 −8.04693 −8.04693 −8.04693 −8.04693 −8.04693 −8.04693
γ −168.30517 −169.57865 −170.81684 −172.01815 −173.18097 −174.30370
γD × 104 −5.26007 −5.14161 −5.02315 −4.90469 −4.78623 −4.66777
λ 158254.38332 159189.34399 160148.99572 161135.78421 162152.28832 163201.27051
λD × 101 3.06232 3.10943 3.16278 3.22236 3.28818 3.36023
λH × 107 4.73466 4.73466 4.73466 4.73466 4.73466 4.73466
Isotopologue 32S17O
B 20677.80911 20515.89547 20354.38135 20193.25309 20032.49559 19872.09182
D × 102 3.12977 3.13105 3.13250 3.13412 3.13591 3.13787
H × 109 −5.74192 −5.74192 −5.74192 −5.74192 −5.74192 −5.74192
L × 1014 −6.85242 −6.85242 −6.85242 −6.85242 −6.85242 −6.85242
γ −161.66569 −162.86535 −164.03249 −165.16566 −166.26342 −167.32432
γD × 104 −4.85508 −4.74793 −4.64079 −4.53365 −4.42651 −4.31937
λ 158244.74695 159160.65402 160100.21102 161065.71645 162059.58924 163084.41473
λD × 101 2.94132 2.98556 3.03555 3.09130 3.15281 3.22006
λH × 107 4.36914 4.36914 4.36914 4.36914 4.36914 4.36914
Isotopologue 32S18O
B 19929.27880 19776.08755 19623.26769 19470.80683 19318.69126 19166.90561
D × 102 2.90683 2.90799 2.90930 2.91077 2.91239 2.91416
H × 109 −5.13947 −5.13947 −5.13947 −5.13947 −5.13947 −5.13947
L × 1014 −5.91098 −5.91098 −5.91098 −5.91098 −5.91098 −5.91098
γ −155.79078 −156.92631 −158.03168 −159.10556 −160.14663 −161.15358
γD × 104 −4.51015 −4.41246 −4.31478 −4.21709 −4.11940 −4.02171
λ 158236.06300 159134.79727 160056.26376 161002.63355 161976.18753 162979.35856
λD × 101 2.83426 2.87602 2.92312 2.97556 3.03335 3.09648
λH × 107 4.05792 4.05792 4.05792 4.05792 4.05792 4.05792

Notes. Weighted sigma = 0.6791. Standard deviation = 8.8978 MHz.

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Table 10. Derived Parameters (in MHz) for 33SO in the Six Lowest Vibrational Levels of the Electronic Ground State

  v = 0 v = 1 v = 2 v = 3 v = 4 v = 5
Isotopologue 33S16O
B 21306.46510 21137.10196 20968.16273 20799.63267 20631.49538 20463.73240
D × 102 3.32341 3.32479 3.32635 3.32811 3.33005 3.33217
H × 109 −6.28291 −6.28291 −6.28291 −6.28291 −6.28291 −6.28291
L × 1014 −7.72650 −7.72650 −7.72650 −7.72650 −7.72650 −7.72650
γ −166.60082 −167.85522 −169.07505 −170.25875 −171.40477 −172.51154
γD × 104 −5.15457 −5.03908 −4.92359 −4.80810 −4.69261 −4.57712
λ 158252.04078 159182.12015 160136.62293 161117.95670 162128.65888 163171.44597
λD × 101 3.03126 3.07763 3.13011 3.18869 3.25339 3.32420
λH × 107 4.63944 4.63944 4.63944 4.63944 4.63944 4.63944
Isotopologue 33S17O
B 20460.68961 20301.32252 20142.34669 19983.74883 19825.51426 19667.62643
D × 102 3.06426 3.06550 3.06691 3.06848 3.07022 3.07213
H × 109 −5.56258 −5.56258 −5.56258 −5.56258 −5.56258 −5.56258
L × 1014 −6.56855 −6.56855 −6.56855 −6.56855 −6.56855 −6.56855
γ −159.96154 −161.14248 −162.29159 −163.40747 −164.48870 −165.53387
γD × 104 −4.75372 −4.64938 −4.54503 −4.44069 −4.33634 −4.23199
λ 158242.35753 159153.28989 160087.60564 161047.56603 162035.54963 163054.09712
λD × 101 2.91026 2.95378 3.00293 3.05771 3.11812 3.18417
λH × 107 4.27769 4.27769 4.27769 4.27769 4.27769 4.27769
Isotopologue 33S18O
B 19712.13399 19561.44258 19411.11459 19261.13798 19111.49943 18962.18404
D × 102 2.84370 2.84483 2.84611 2.84753 2.84911 2.85083
H × 109 −4.97297 −4.97297 −4.97297 −4.97297 −4.97297 −4.97297
L × 1014 −5.65704 −5.65704 −5.65704 −5.65704 −5.65704 −5.65704
γ −154.08680 −155.20395 −156.29159 −157.34845 −158.37325 −159.36469
γD × 104 −4.41247 −4.31743 −4.22238 −4.12734 −4.03229 −3.93725
λ 158233.62960 159127.30151 160043.44012 160984.18000 161951.76266 162948.57746
λD × 101 2.80321 2.84426 2.89053 2.94203 2.99876 3.06072
λH × 107 3.96980 3.96980 3.96980 3.96980 3.96980 3.96980

Notes. rms = 8.8978 MHz. Reduced standard deviation = 0.6791.

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Table 11. Derived Parameters (in MHz) for 34SO Isotopologues in the Six Lowest Vibrational Levels of the Electronic Ground State

  v = 0 v = 1 v = 2 v = 3 v = 4 v = 5
Isotopologue 34S16O
B 21102.73177 20935.79500 20769.27415 20603.15484 20437.42111 20272.05496
D × 102 3.26002 3.26137 3.26289 3.26460 3.26649 3.26856
H × 109 −6.10403 −6.10403 −6.10403 −6.10403 −6.10403 −6.10403
L × 1014 −7.43459 −7.43459 −7.43459 −7.43459 −7.43459 −7.43459
γ −165.00144 −166.23801 −167.44069 −168.60794 −169.73826 −170.83011
γD × 104 −5.05654 −4.94379 −4.83105 −4.71831 −4.60556 −4.49282
λ 158249.83181 159175.30919 160124.95906 161101.15343 162106.39109 163143.34570
λD × 101 3.00211 3.04778 3.09945 3.15712 3.22077 3.29042
λH × 107 4.55095 4.55095 4.55095 4.55095 4.55095 4.55095
Isotopologue 34S17O
B 20256.92979 20099.94025 19943.33428 19787.09895 19631.21996 19475.68122
D × 102 3.00340 3.00462 3.00599 3.00752 3.00921 3.01107
H × 109 −5.39771 −5.39771 −5.39771 −5.39771 −5.39771 −5.39771
L × 1014 −6.31026 −6.31026 −6.31026 −6.31026 −6.31026 −6.31026
γ −158.36234 −159.52580 −160.65808 −161.75780 −162.82358 −163.85406
γD × 104 −4.65958 −4.55782 −4.45605 −4.35429 −4.25253 −4.15077
λ 158240.10389 159146.34526 160075.72015 161030.45505 162012.89091 163025.52682
λD × 101 2.88112 2.92396 2.97232 3.02620 3.08560 3.15052
λH × 107 4.19274 4.19274 4.19274 4.19274 4.19274 4.19274
Isotopologue 34S18O
B 19508.35030 19359.99236 19211.99045 19064.33282 18917.00655 18769.99714
D × 102 2.78509 2.78619 2.78743 2.78882 2.79035 2.79202
H × 109 −4.82003 −4.82003 −4.82003 −4.82003 −4.82003 −4.82003
L × 1014 −5.42626 −5.42626 −5.42626 −5.42626 −5.42626 −5.42626
γ −152.48777 −153.58775 −154.65885 −155.69981 −156.70939 −157.68634
γD × 104 −4.32177 −4.22917 −4.13657 −4.04397 −3.95136 −3.85876
λ 158231.33403 159120.23139 160031.34651 160966.77998 161928.73653 162919.56506
λD × 101 2.77408 2.81446 2.85996 2.91058 2.96633 3.02719
λH × 107 3.88798 3.88798 3.88798 3.88798 3.88798 3.88798

Notes. rms = 8.8978 MHz. Reduced standard deviation = 0.6791.

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Table 12. Derived Parameters (in MHz) for36SO in the Six Lowest Vibrational Levels of the Electronic Ground State

  v = 0 v = 1 v = 2 v = 3 v = 4 v = 5
Isotopologue 36S16O
B 20727.98664 20565.48218 20403.37916 20241.66385 20080.32103 19919.33356
D × 102 3.14502 3.14631 3.14777 3.14940 3.15120 3.15317
H × 109 −5.78394 −5.78394 −5.78394 −5.78394 −5.78394 −5.78394
L × 1014 −6.91936 −6.91936 −6.91936 −6.91936 −6.91936 −6.91936
γ −162.05980 −163.26380 −164.43512 −165.57230 −166.67389 −167.73844
γD × 104 −4.87867 −4.77087 −4.66308 −4.55528 −4.44749 −4.33969
λ 158245.74142 159162.69970 160103.36959 161070.05823 162065.19394 163091.37241
λD × 101 2.94850 2.99291 3.04310 3.09908 3.16083 3.22837
λH × 107 4.39043 4.39043 4.39043 4.39043 4.39043 4.39043
Isotopologue 36S17O
B 19882.13562 19729.48795 19577.20994 19425.28926 19273.71231 19122.46379
D × 102 2.89307 2.89423 2.89553 2.89699 2.89860 2.90036
H × 109 −5.10303 −5.10303 −5.10303 −5.10303 −5.10303 −5.10303
L × 1014 −5.85516 −5.85516 −5.85516 −5.85516 −5.85516 −5.85516
γ −155.42104 −156.55257 −157.65409 −158.72427 −159.76181 −160.76539
γD × 104 −4.48887 −4.39176 −4.29464 −4.19753 −4.10042 −4.00331
λ 158235.92958 159133.48463 160053.71427 160998.78163 161970.95902 162972.66986
λD × 101 2.82752 2.86913 2.91605 2.96829 3.02584 3.08872
λH × 107 4.03872 4.03872 4.03872 4.03872 4.03872 4.03872
Isotopologue 36S18O
B 19133.51192 18989.41421 18845.65911 18702.23545 18559.13096 18416.33189
D × 102 2.67888 2.67992 2.68111 2.68242 2.68387 2.68546
H × 109 −4.54697 −4.54697 −4.54697 −4.54697 −4.54697 −4.54697
L × 1014 −5.02030 −5.02030 −5.02030 −5.02030 −5.02030 −5.02030
γ −149.54677 −150.61541 −151.65628 −152.66820 −153.64997 −154.60040
γD × 104 −4.15740 −4.06919 −3.98098 −3.89277 −3.80456 −3.71635
λ 158227.08088 159107.13481 160008.94931 160934.56297 161886.11354 162865.87626
λD × 101 2.72049 2.75966 2.80376 2.85279 2.90674 2.96561
λH × 107 3.73972 3.73972 3.73972 3.73972 3.73972 3.73972

Notes. rms = 8.8978 MHz. Reduced standard deviation = 0.6791.

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4. CONCLUSION

New pure rotational transitions of the SO radical and of its two most abundant isotopologues have been measured in the THz spectral region (up to 2.5 THz). The use of the cw-THz photomixing technique based on a FC allowed very high accuracy line frequency measurements. Reliable effective parameters have been obtained for these three isotopologues. We also performed a global mass independent fit including all pure rotational and ro-vibrational transitions reported in the literature on all observed isotopologues of SO.

Thanks to this new set of parameters it is now possible to predict with very high accuracy the frequencies of the ro-vibrational lines. This should enable the research of SO in the mid-IR using ground-based IR telescopes, space-based telescope archives (Infrared Space Observatory, Spitzer), and future space missions such as the James Webb Space Telescope. This set of parameters particularly well-adapted for the detection of SO lines in O-rich evolved stars or in molecular clouds in absorption against bright IR sources.

The authors gratefully acknowledge Caroline C. Womack for her helpful comments on the manuscript. The THz spectrometer was funded by the Communauté urbaine de Dunkerque, the Région Nord-Pas de Calais, the Ministére de l'éducation nationale, de l'enseignement supérieur et de la recherche, and European funds in the context of the IRENI (Institut de Recherche en ENvironnement Industriel) and InterregIVA "Cleantech" programs. J. Cernicharo thanks the Spanish MINECO program for funding support through grants CSD2009-00038 (CONSOLIDER program "ASTROMOL"), AYA2009-07304, and AYA2012-32032, and the European Research Council for funding under the European Union's Seventh Framework Program (FP/2007-2013) / ERC-2013-SyG, Grant Agreement No. 610256 NANOCOSMOS.

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10.1088/0004-637X/799/2/115