Issue |
A&A
Volume 520, September-October 2010
|
|
---|---|---|
Article Number | A19 | |
Number of page(s) | 4 | |
Section | Atomic, molecular, and nuclear data | |
DOI | https://doi.org/10.1051/0004-6361/201013998 | |
Published online | 23 September 2010 |
Absorption cross section of molecular oxygen in the transition
at 38 K
H.-C. Lu1 - H.-K. Chen1 - H.-F. Chen1 - B.-M. Cheng1 - J. F. Ogilvie2
1 - National Synchrotron Radiation Research Center, No. 101, Hsin-Ann Road, Hsinchu Science Park, Hsinchu 30076, Taiwan
2
- Escuela de Quimica y CELEQ, Universidad de Costa Rica, Ciudad
Universitaria Rodrigo Facio, San Pedro de Montes de Oca, San Jose 2060,
Costa Rica
Received 6 January 2010 / Accepted 20 April 2010
Abstract
Aims. This investigation was undertaken to determine the
absorption cross sections of oxygen in the VUV region at temperatures
<50 K.
Methods. The absorption spectra of gaseous samples cooled with a
slit jet and near 300 K were measured with the same absorption
system coupled to the VUV beam line of a synchrotron.
Results. The maximum absorption cross section for the transition from X
v = 0 to state E
v = 0 for 16O2 at 38 K was determined to be 98.7 Mb (or
cm2). The value of this maximum absorption cross section at 38 K is 1.7 times the value at 303.7 K.
Key words: astronomical databases: miscellaneous - molecular data - techniques: spectroscopic - ultraviolet: general
1 Introduction
To assess photochemically induced changes in stellar media, one
must have quantitative information about the absorption cross
sections of pertinent molecular species in the vacuum-ultraviolet
(VUV) range (Miller & Yung 2000). We determined the absorption
cross sections of several interstellar molecular species in this
range (H2O, Cheng et al. 1999, 2004; HCl, Bahou et al. 2001; CH4, Lee et al. 2001; CH3OH, Cheng et al. 2002; NH3, Cheng et al. 2006; and Liang et al. 2007), but most
measurements were made near 300 K. One problem in the application
of these data to the photochemical model is that in outer space
the temperature is much less than 300 K: for example, the relevant
atmospheric temperature is 170 K for Jupiter,
140 K
for Saturn,
120 K for Titan,
50 K for Triton, and even
lower for Neptune and Uranus (Yung
DeMore 1999).
Molecular absorption cross sections measured near 300 K are
generally inadequate to explain the observed spectral features and
to allow an accurate determination of the abundance of atmospheric
constituents in outer space. It is thus preferable to measure
directly the absorption cross sections at temperatures <50 K.
Another problem is that thermal motion and the population of
energetic states blur many pertinent features of VUV spectra of
samples near 300 K. If we can obtain spectra of these species
<50 K, we can provide information to define an accurate
potential-energy surface for theoretical consideration and the
dissociation dynamics of interstellar molecules.
To measure the absorption spectra in the VUV region of planetary molecules at temperatures <50 K, we constructed a slit-jet absorption system that is connected to a VUV beamline of a synchrotron at National Synchrotron Radiation Research Center (NSRRC) in Taiwan. Using this setup we have measured the absorption spectra of several molecules of interest; we discuss here the results for O2.
Oxygen not only is a highly important gas on Earth but also has been detected in cold, outer planetary systems and in deep space. Although VUV absorption cross sections of O2 have been extensively investigated (Gibson et al. 1983; Hudson et al. 1966; Huffman 1969; Kanik et al. 1997; Metzger & Cook 1964; Ogawa 1975; Wang et al. 1987; Yoshino et al. 2005, and references therein), the least temperature of a recording was 79 K, which is still not low enough for an understanding of the astrophysical spectral properties of O2. For this reason accurate measurement of data of O2 for temperatures below 79 K is important.
2 Experiments
We measured the absorption spectra of gaseous samples cooled with
a slit jet and near 300 K at the same end station coupled to the
VUV beam line of a synchrotron, for which a systematic layout is
displayed in Fig. 1. In brief, the gaseous stream from
the jet intersected, in the absorption chamber, the beam of VUV
radiation from a beam line of the synchrotron; the VUV light was
dispersed with a high-flux cylindrical-grating monochromator
(focal length 6 m). The intensity of VUV light was monitored
through light reflected from a LiF beamsplitter placed before the
absorption chamber and at 45
from the beam line. A small
fraction of the reflected light passed one additional LiF plate
and impinged on a glass window coated with sodium salicylate. The
luminescent signal subsequently detected with a photomultiplier
tube (Hamamatsu R943-02) in a photon-counting mode was employed
for normalization.
The light transmitted through the LiF beam splitter crossed the
cooled gaseous stream expanded from the slit jet (
mm) in
its absorption chamber, which was sealed with two LiF windows; the
distance between these two windows was 0.050 m. The light
transmitted through that absorption chamber irradiated a glass
window coated with sodium salicylate. In the same way, the
fluorescence was detected with a photomultiplier in a
photon-counting mode. That absorption chamber was connected to
three turbomolecular pumps (TG 2813 EMCA-03, Osaka Vacuum Ltd.)
each having a pumping speed 2.8 m3 s-1. One pump was
connected to a dry pump (Alcatel ADS 501, pumping speed 510 m3/h) and the other two were connected to a dry pumping
system (Edwards iQMB1200, pumping speed 940 m3/h). Before
measuring the absorption spectrum of a supersonically expanded
sample, we evacuated the cell to 1 mPa with the turbomolecular
pumping system.
![]() |
Figure 1: Schematic diagram of the experiment. |
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The absorption spectrum of a gaseous sample near 300 K was also measured with this end station. The tube
between the LiF exit window of the slit-jet absorption chamber and
the phosphor-coated glass window served as a gaseous absorption
cell near 300 K. While we recorded the absorption spectra of
gaseous samples near 300 K, we charged this tube cell with a
gaseous sample and stopped the flow of the jet. The density of gas
in the cell was determined from the gaseous pressure monitored
with a capacitance manometer (MKS-Baratron); the temperature was
measured with a thermocouple. The absorption cross section,
,
is determined from the absorbance A according to
A = ln(I0/I) = n
l +
, in which I0 and I are incident and
transmitted light intensities, respectively; n is the
number density of the gas, and l (=8.47 cm) is the length
of the path of gaseous absorption. The offset,
,
was
determined at n = 0, when the gas cell was pumped below 1
mPa. At each wavelength, a value of
was obtained from a
linear fit of 4-6 absorbances measured at varied gaseous
pressures.
Oxygen (purity 99.999,
Matheson) was used without further
purification. The wavelength was calibrated with absorption lines of Xe (Yoshino & Freeman
2005), CO (Tilford et al. 1965; Simmons et al. 1969)
and H2O (Wang et al. 1977); the accuracy of a measured wavelength is limited by the scan step.
3 Results and discussion
With the VUV absorption system we measured samples of the same gas
in two modes - for the static gas near 300 K and for the gas
flowing through the slit jet. Absolute cross sections for the
absorption of O2 at 303.7 K appear in Fig. 2A
for spectral regions 115-180 nm. Considering all possible
systematic errors, we estimate experimental uncertainties of cross
sections to be within 10 per cent of our reported values. The
absorption of O2
in the spectral range 130-175 nm belongs to the Schumann-Runge
continuum, for which we measured the cross sections at intervals
0.05 nm. Comparison of these cross sections with those of previous
measurements near 300 K indicates that our data agree
satisfactorily within the experimental uncertainty. For instance,
Yoshino et al. (2005) reported the cross section
at 143.26 nm and 295 K to be 14.2 Mb (1 Mb = 10-18 cm2); our value is 15.4 Mb, 8 per cent larger than theirs. In the same region,
Ogawa & Ogawa (1975)
specified the cross section at 143.0 nm and 298 K to be
15.3 Mb, similar to our value 15.1 Mb. In other regions, we
recorded the data at interval 0.02 nm; the maximum values are
57.6 Mb for state E
at 124.44 nm, and 18.4 Mb for state a
at 120.54 nm . That these values agree satisfactorily with 57.6 and 16.2 Mb, reported by Ogawa & Ogawa (1975), demonstrates that our experimental system operates effectively.
![]() |
Figure 2: Absorption spectra of O2 in the wavelength range 115-180 nm: A) absorption cross section at 303.7 K; B) absorption spectrum of O2 through the slit jet at stagnation pressure 26.7 kPa. Inset: expanded absorption spectra about 124.4 nm recorded with resolution 0.01 nm at 303.7 K (dashed line) and with the jet (solid line). |
Open with DEXTER |
For the gas flowing through the slit jet, the corresponding absorption
spectrum of oxygen recorded in spectral range 115-180 nm at
stagnation pressure 26.7 kPa is displayed in Fig. 2B. Although at first glance the shape of the spectrum for the jet-expanded
carrier resembles that for 300 K, scrutiny reveals significant differences. The inset in Fig. 2 compares the absorption into
state E
v = 0 in wavelength range 124-125 nm for the static gas at
temperature 303.7 K and for the jet-expanded gas; the profiles of
the absorption depend strongly on temperature. For absorption near
300 K, although the overlapping lines are not entirely resolved,
two branches are discernible with branch P more intense than branch R;
the half width of the resultant band is about 0.15 nm. For the
carrier gas subjected to jet expansion, we observed only one main
feature with half width 0.07 nm.
Using published parameters for widths of lines (Lewis et al. 1988) and for wavenumbers of states X
v = 0 and E
v = 0 of 16O2 (Welch & Mizushima 1972), we simulated the absorption attributed to the transition E
v = 0, using a Fano line shape (Lewis et al. 1988) for each individual contributing line in a region 80 200-80 500 cm-1
as a function of temperature. Although more accurate expressions for
the rotational terms of states X and E are available (Steinbach &
Gordy 1973), so as to ensure
an accurate and consistent simulation we employed directly the
expressions reportedly used to evaluate the specified parameters (Ogawa
& Ogawa 1975). Our derived spectra reproduce faithfully both the reported spectra (Lewis et al. 1988) at 79 K and 295 K and our own spectrum of gaseous O2 at 303.7 K. To derive the temperature of the jet-expanded gas, we then simulated the absorption spectra of O2 from 15 K to 50 K and compared them with the experimental spectrum. By this means, we
conclude that the temperature of the jet-expanded beam of O2 at stagnation pressure 26.7 kPa is
K; the absorption spectrum about 124 nm as simulated at 38 K and convoluted with resolution 7 cm-1 and as measured experimentally appear in Fig. 3. In the corresponding simulated spectrum of O2
in thermal equilibrium at 38 K, the total absorption contains all
six branches - three P branches and three R branches, but the R
branches contribute most intensity; P and R branches are thus congested
in a band with full width 45 cm-1 (0.07 nm) at half maximum.
![]() |
Figure 3: Comparison of absorption spectra about 124.4 nm for jet-expanded O2 (solid line) and simulation at 38 K (dashed line). |
Open with DEXTER |
As these absorption spectra have discrete structure, the measured
absorption cross sections depend on the spectral slit width of the
monochromator: the greater is the resolution, the larger is the
apparent cross section at a maximum of absorption. For this reason, a
comparison of absorption cross sections from separate authors is
difficult, but integration of absorption cross sections over a spectral
range yields an oscillator strength (f value) that is
formally independent of monochromator slit width and is thus comparable for various experiments. The f value is calculated according to
d
,
with absorption coefficient
/ Mb and wavenumber
/ cm-1. Our f value
for the transition E
v = 0 of O2 in the spectral range 124-125 nm at
303.7 K is 0.00665, which is near the value 0.00625 reported by
(Lewis et al. 1988).
Because, in our work, the absorption spectra of O2
near 300 K and for jet-expanded conditions were measured with the
same optical parameters, it is possible to derive the absorption cross
section at the temperature of the jet-expanded sample based on the
oscillator strength obtained at 303.7 K. With this scheme and a
value
f = 0.00665, the absorption cross section of O2 at 38 K in transition E
v = 0 and spectral range 124-125 nm is
derivable, as shown in Fig. 4. The maximum absorption cross section for the transition E
v = 0 of O2 at 124.4 nm is thus calculated to
be 97.8 Mb at 38 K, which is about 1.7 times the value for 303.7 K.
![]() |
Figure 4: Absorption cross sections about 124.4 nm of O2 at 38 K (solid line) and 303.7 K (dashed line). |
Open with DEXTER |
![]() |
Figure 5:
Cross section at the wavelength of maximum absorption in the transition from state X
|
Open with DEXTER |
VUV spectra provide a powerful analytical tool that has been applied
during spacecraft missions. For example, the Cassini Ultraviolet
Imaging Spectrograph (UVIS) included channels for extreme ultraviolet
(EUV) and far ultraviolet (FUV) spectral imaging to record VUV spectra
for targets in outer space at very low temperatures (Ajello 2005; Esposito et al. 2005; Shemansky et al. 2005).
To verify the spectra obtained with these spacecraft and to explain the
photochemical model within the atmospheres of these cold targets, we
require extensive optical data applicable at those temperatures. Our
present values of the absorption cross section of O2
at 38 K are applicable for this purpose and are thus valuable for
astrophysical applications. In our work we obtained the maximum cross
sections of O2 for state E
as 97.8 Mb at 38 K and 57.6 Mb at 303.7 K. Lewis
et al. obtained 92 Mb at 79 K. These three cross
sections exhibit a linear relation with temperature, as displayed in
Fig. 5; by this means one can estimate a rough value for other temperatures.
4 Conclusion
In the spectral range 115-180 nm with a synchrotron as a source of
VUV radiation, we measured absorption cross sections of O2 in
a stagnant sample at 303.7 K and in a flowing gas subjected to
adiabatic expansion. Using published optical parameters, we
simulated the absorption spectra for the transition E
v = 0 in
wavelength range 124-125 nm and concluded that the temperature of
the expanded beam is
K. Based on oscillator strength
0.00665 obtained for 303.7 K, the maximum absorption cross section
of O2 at 38 K for the transition into state E
is derived to be 98.7 Mb, which is 1.7 times
that for 303.7 K.
National Science Council of Republic of China and National Synchrotron Radiation Research Center provided financial support.
References
- Ajello, J. M., Pryor, W., Esposito, L., et al. 2005, Icarus, 178, 327 [NASA ADS] [CrossRef] [Google Scholar]
- Bahou, M., Chung, C.-Y., Lee, Y.-P., et al. 2001, ApJ, 559, L179 [NASA ADS] [CrossRef] [Google Scholar]
- Cheng, B.-M., Chew, E. P., Liu, C.-P., et al. 1999, Geophys. Res. Lett., 26, 3657 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
- Cheng, B.-M., Chung, C.-Y., Bahou, M., Lee, Y.-P., & Lee, L. C. 2002, J. Chem. Phys., 117, 4293 [NASA ADS] [CrossRef] [Google Scholar]
- Cheng, B.-M., Chung, C.-Y., Bahou, M., et al. 2004, J. Chem. Phys., 120, 224 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
- Cheng, B.-M., Lu, H.-C., Chen, H.-K., et al. 2006, ApJ, 647, 1535 [NASA ADS] [CrossRef] [Google Scholar]
- Esposito, L. W., Colwell, J. E., Larsen, K., et al. 2005, Science, 307, 1251 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
- Gibson, S. T., Gies, H. P. F., Blake, A. J., McCoy, D. G., & Rogers, P. J. 1983, J. Quant. Spectrosc. Radiat. Trans., 30, 385 [NASA ADS] [CrossRef] [Google Scholar]
- Hudson, R. D., Carter, V. L., & Stein, J. A. 1966, J. Geophys. Res., 71, 2295 [NASA ADS] [Google Scholar]
- Huffman, R. E. 1969, Can. J. Chem., 47, 1823 [Google Scholar]
- Kanik, I., Beegle, L., Noren, C., Ahmed, S. M., & Link, R. 1997, Chem. Phys. Lett., 759, 297 [CrossRef] [Google Scholar]
- Lee, A. Y. T., Yung, Y. L., Cheng, B. M., et al. 2001, ApJ, 551, L93 [NASA ADS] [CrossRef] [Google Scholar]
- Lewis, B. R., Gibson, S. T., Emami, M., & Carver, J. H. 1988, J. Quant. Spectrosc. Radiat. Trans., 40, 1 [NASA ADS] [CrossRef] [Google Scholar]
- Liang, M.-C., Cheng, B.-M., Lu, H.-C., et al. 2007, ApJ, 657, L117 [NASA ADS] [CrossRef] [Google Scholar]
- Metzger, P. H., & Cook, G. R. 1964, J. Quant. Spectrosc. Radiat. Trans., 4, 107 [NASA ADS] [CrossRef] [Google Scholar]
- Miller, C. E., & Yung, Y. L. 2000, J. Geophys. Res-Atmos., 105, 29039 [NASA ADS] [CrossRef] [Google Scholar]
- Ogawa, M. 1975, Can. J. Phys., 53, 2703 [Google Scholar]
- Ogawa, S., & Ogawa, M. 1975, Can. J. Phys., 53, 1845 [NASA ADS] [CrossRef] [Google Scholar]
- Shemansky, D. E., Stewart, A. I. F., Robert A., et al. 2005, Science, 308, 978 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
- Simmons, J. D., Bass, A. M., & Tilford, S. G. 1969, ApJ, 155, 345 [NASA ADS] [CrossRef] [Google Scholar]
- Steinbach, W., & Gordy, W. 1973, Phys. Rev. A, 8, 1753 [NASA ADS] [CrossRef] [Google Scholar]
- Tilford, S. G., Vanderslice, J. T., & Wilkinson, P. G. 1965, Can. J. Phys., 43, 450 [NASA ADS] [Google Scholar]
- Wang, H. T., Felps, W. S., & McGlynn, S. P. 1977, J. Chem. Phys., 67, 2614 [NASA ADS] [CrossRef] [Google Scholar]
- Wang, J., McCoy, D. G., Blake, A. J., & Torop, L. 1987, J. Quant. Spectrosc. Radiat. Trans., 38, 19 [NASA ADS] [CrossRef] [Google Scholar]
- Welch, W. M., & Mizushima, M. 1972, Phys. Rev. A, 5, 2692 [NASA ADS] [CrossRef] [Google Scholar]
- Yoshino, K., & Freeman, D. E. 2005, J. Opt. Soc. Am. B, 2, 1268 [Google Scholar]
- Yoshino, K., Parkinson, W. H., Ito, K., & Matsui, T. 2005, J. Mol. Spect., 229, 238 [Google Scholar]
- Yung, Y. L., & DeMore, W. B. 1999, Photochemistry of Planetary Atmospheres (New York: Oxford University Press) [Google Scholar]
All Figures
![]() |
Figure 1: Schematic diagram of the experiment. |
Open with DEXTER | |
In the text |
![]() |
Figure 2: Absorption spectra of O2 in the wavelength range 115-180 nm: A) absorption cross section at 303.7 K; B) absorption spectrum of O2 through the slit jet at stagnation pressure 26.7 kPa. Inset: expanded absorption spectra about 124.4 nm recorded with resolution 0.01 nm at 303.7 K (dashed line) and with the jet (solid line). |
Open with DEXTER | |
In the text |
![]() |
Figure 3: Comparison of absorption spectra about 124.4 nm for jet-expanded O2 (solid line) and simulation at 38 K (dashed line). |
Open with DEXTER | |
In the text |
![]() |
Figure 4: Absorption cross sections about 124.4 nm of O2 at 38 K (solid line) and 303.7 K (dashed line). |
Open with DEXTER | |
In the text |
![]() |
Figure 5:
Cross section at the wavelength of maximum absorption in the transition from state X
|
Open with DEXTER | |
In the text |
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