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The IUPAC Critical Evaluation of theThe IUPAC Critical Evaluation of the
Ro-vibrational Spectra of Water Vapor:Ro-vibrational Spectra of Water Vapor:
Results for HResults for H221818O, HO, H22
1717O, and HDO, and HD1616OO
Jonathan TennysonUniversity College London
Attila G. Császár, Tibor FurtenbacherLoránd Eötvös University
Alexander Z. FazlievInstitute of Atmospheric Optics
Laurence S. Rothman, Iouli E. GordonHarvard-Smithsonian Center for Astrophysics
Ohio State University, June 2008
OutlineOutline
► IUPAC (International Union of Pure and Applied Chemistry)Water Vapor Task Group
- Goals
► Results
► Database and Access Issues
A Database of Water Transitions from A Database of Water Transitions from Experiment and TheoryExperiment and Theory
Members:Jonathan Tennyson (chair), P.F. Bernath, A. Campargue,M.R. Carleer, A.G. Császár, R.R. Gamache, J. Hodges,A. Jenouvrier, O. Naumenko, O. Polyansky, L.S. Rothman,R.A. Toth, A.C. Vandaele, N. Zobov
Objective:Develop a compilation of experimental and theoretical line
positions, energy levels, intensities, and line-shape parameters for water vapor and all of its major isotopologues
Establish a database structure that retains and enables access to all critically evaluated data
Spectroscopic Spectroscopic NNetworks of etworks of WWaterater
Water (except for HDO) has two main SNs:
(Ka + Kc + 3) is even (Ka + Kc + 3) is odd (para) (ortho)
1. Collect, validate, and compile all available measured transitions, including their systematic and unique assignments and uncertainties, into a single database.
2. Based on the given database of assigned transitions, determine those energy levels of the given species which belong to a particular spectroscopic network (SN).
3. Cleansing of the database (misassignments, mislabelings).4. Within a given SN, set up a vector containing all the experimentally
measured transitions selected, another one comprising the requested measured energy levels, and a design matrix which describes the relation between the transitions and the energy levels.
5. Solve the resulting set of linear equations corresponding to the chosen set of vectors and the inversion matrix many times (robust reweighting). During solution of the set of linear equations uncertainties in the measured transitions can be incorporated which result in uncertainties of the energy levels determined.
MARVEL MARVEL SStepsteps
123 MARVEL No. of rotational levels
000 0.000000 194
010 1591.325708(48) 153
020 3144.980414(31) 63
100 3653.142263 (21) 106
001 3748.318070(11) 143
030 [4657.123] 22
110 5227.705603 (46) 68
011 5320.260507(3) 148
040 [6121.552] 21
120 6764.725603(547) 63
021 6857.272709(32) 89
200 7193.246623(20) 83
101 7238.713600(185) 102
002 7431.076115(1449) 28
050 1
130 3
031 10
210 34
111 8792.544310(925) 108
060 1
012 8982.869215(966) 55
041 13
220 12
121 10311.202510(926) 75
022 1
300 65
201 10598.475610(926) 102
102 10853.505315(966) 53
003 46
131 11792.827010(6018) 31
310 28
211 12132.992610(926) 87
112 25
013 12541.225510(926) 39
141 1
042 1
320 3
221 13631.499810(1019) 53
400 29
071 13808.273310(926) 2
301 13812.158110(926) 75
202 14
103 14296.279510(370) 37
340 13
241 6
HH221717O vibrational energy levelsO vibrational energy levels
IUPAC vs HITRANRo-vibrational levels
for H217O
Bending Fundamental: 1250 – 1750 cm-1
Interval (cm-1) References
1. 0 - 170 J. Steenbeckeliers, CRAS Paris B273 (1971) 471
2. 0 - 170 F.C. De Lucia, J. Mol. Spectrosc. 56 (1975) 138 - 145
3. 0 - 177F. Matsushima, H. Nagase, T. Nakauchi, H. Odashima, and K. Takagi,
J. Mol. Spectrosc. 193 (1999) 217 – 223
4. 177 - 600 J. Kauppinen and E. Kyro, J. Mol. Spectrosc. 84 (1980) 405 - 423
5. 1315 - 1986 G. Guelachvili, J. Opt. Soc. Am. 73 (1983) 137 - 150
6. 500 - 7782 SISAM database: http://mark4sun.jpl.nasa.gov/
7. 8564 - 9332A.-W. Liu, S.-M. Hu, C. Camy-Peyret, J.-Y. Mandin, O. Naumenko, and
B. Voronin, J. Mol. Spectrosc. 237 (2006) 53 – 62
8. 4206 - 6600A. Jenouvrier, L. Daumont, L. Regalia-Jarlot, V. G. Tyuterev, M. Carleer,
A. C. Vandaele, S. Mikhailenko, and S. Fally,J. Quant. Spectrosc. Rad. Transfer 105 (2007) 326 – 355
9. 6170 - 6747P. Macko, D. Romanini, S. N. Mikhailenko, O. V. Naumenko, S. Kassi,
A. Jenouvrier, Vl. G. Tyuterev, and A. Campargue,J. Mol. Spectrosc. 227 (2004) 90 – 108
10. 9711 - 10883C. Camy-Peyret, J.-M. Flaud, J.-Y. Mandin, A. Bykov, O. Naumenko,
L. Sinitsa,and B. Voronin, J. Quant. Spectrosc. Rad. Transfer 61 (1999) 795 – 812
11 11365 - 14377M. Tanaka, O. Naumenko, J. W. Brault, and J. Tennyson, J. Mol. Spectrosc. 234
(2005) 1 - 9
12. 16570 - 17125O. Naumenko, M. Sneep, M. Tanaka, S.V. Shirin, W. Ubachs, and J. Tennyson, J. Mol.
Spectrosc. 237 (2006) 63-69
Observed Transitions of HObserved Transitions of H221717O O
Basic requirement► System has mainly valid data. Data are valid if they are experimentally verified. A user can easily check which data are experimental, which are calculated and which
are of indefinite status. Requirements for sorts of data► System has to have primary (data and knowledge)
► System has to have expert (data and knowledge) based on formal and informal constraints. These constraints have to be explicitly formulated.
Requirements for embedded applications► Applications have to provide collective work with data and knowledge
manipulation (upload primary data and download primary and expert data and metadata, check information on formal constrains (selection rules, process types, …), decompose expert data on primary data sources, compare data, construct composite information sources)
Technical requirements► Short time of information actualization► Access (in any time and from practically any place)► Additional services for information processing
Requirements forRequirements for Information System on Spectroscopy (W@DIS) Information System on Spectroscopy (W@DIS)
Alexander FazlievAlexander Fazliev
We use term primary information sourceprimary information source to define the data and metadata which are the result of solution (measurement) of one of the above mentioned spectroscopy problems, related to one molecule and published as a definite resource (in a journal or via the web).
The composite information sourcescomposite information sources (for instance, HITRAN) are the sets of the primary information sources. But it’s rather difficult to check this composition consistence. One of the goals of W@DIS is to make the process of decomposition of the composite information sources on primary information sources automatic.
Information SourceInformation Source
14
W@DIS Information System W@DIS Information System State of the ArtState of the Art
Upload and download of line profile parameters Generation of semantic metadata
Data sources search, tabular and graphical data comparison, root mean square deviation
Line profilesDatabaseKnowledgebaseInterfaces
Upload and download of transitionsGeneration of semantic metadata
Data sources search, tabular and graphical data comparison, root mean square deviation
TransitionsDatabaseKnowledgebaseInterfaces
Upload and download of energy levels Generation of semantic metadata
Data sources search, tabular and graphical data comparison, root mean square deviation
Energy levelsDatabase
KnowledgebaseInterfaces
Data manipulation (upload, storage, presentation, download)
Primary data sourcesReferences
Database
Interfaces
ProblemsEntitiesPart of IS
Line Profile Line Profile Root mean square deviations
► A full set of original experimental and calculation data on water
molecules has been gathered in W@DIS. Number of primary data sources ~ 580
► A knowledgebase of water molecule information sources has been created. One contains more than 40000 facts.
► Informational model of molecular spectroscopy has been developed on
the example of C2v and Cs symmetry molecules. In W@DIS one can
work with the following molecules: H2O, O3, SO2, H2S
► W@DIS has facilities for pairwise comparison of data sets and
calculations of root-mean-square deviations, sets upload and download,…
► IS W@DIS – http://wadis.saga.iao.ru
Summary of Database Delivery SystemSummary of Database Delivery System