Micro-Raman investigations of the formaldehyde-ice system

被引:16
作者
Chazallon, B [1 ]
Lebrun, N
Dhamlincourt, P
Toubin, C
Focsa, C
机构
[1] Univ Sci & Technol Lille, CERLA, Lab Phys Lasers Atomes & Mol, UMR 8523, F-59655 Villeneuve Dascq, France
[2] Univ Sci & Technol Lille, UMR 8024, Lab Dynam & Struct Mat Mol, F-59655 Villeneuve Dascq, France
[3] Univ Lille 1, CERLA, Lab Spectrochim Infrarouge & Ramon, F-59655 Villeneuve Dascq, France
关键词
D O I
10.1021/jp040244w
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Rapidly frozen aqueous solutions containing variable amounts of dissolved formaldehyde (0.1, 5, 7, 10, 15, and 20 mol %) have been analyzed by micro-Raman spectroscopy at ambient pressure and low temperature. The importance of the formladehyde-ice system has been repeatedly quoted in various contexts, such as atmospheric and snowpack chemistry and interstellar and cometary ices. Understanding and characterizing the effects of freezing and the interactions of formaldehyde with ice are therefore of relevant interest. In this study, the distinct vibrational signatures of the oligomers present in the solution and in the frozen ice mixtures have been identified in the 120-4000 cm(-1) spectral range. From the subtle changes of the bands assigned to the CO and CH group frequencies, at least two distinct crystalline phases (pI and pII) are found to coexist with ice at different temperatures. Depending on the cooling-rewarming protocol, pI is found to crystallize in the 163-213 K temperature range. Above similar to213 K, pI gets transformed irreversibly into pII which is stable up to similar to234 K. pII is found to interact more strongly with ice than pI, as revealed, for example, by the drop in frequency of the bands assigned to the O-H stretching as pI transforms into pII. It is suggested that pII consists of a hydrogen-bonded network of oligomers and water molecules. On the other hand, it is suggested that the oligomers mainly present in pI interact through weak forces with the surrounding water molecules.
引用
收藏
页码:432 / 439
页数:8
相关论文
共 43 条
[1]   PHOTOCHEMICAL AND THERMAL EVOLUTION OF INTERSTELLAR PRECOMETARY ICE ANALOGS [J].
ALLAMANDOLA, LJ ;
SANDFORD, SA ;
VALERO, GJ .
ICARUS, 1988, 76 (02) :225-252
[2]   ABSORPTIVITY OF ICE I IN RANGE 4000-30 CM-1 [J].
BERTIE, JE ;
LABBE, HJ ;
WHALLY, E .
JOURNAL OF CHEMICAL PHYSICS, 1969, 50 (10) :4501-&
[3]   INFRARED SPECTRA OF ICES 2 3 + V IN RANGE 4000 TO 350 CM MINUS 1 [J].
BERTIE, JE ;
WHALLEY, E .
JOURNAL OF CHEMICAL PHYSICS, 1964, 40 (06) :1646-+
[4]  
BERTIE JE, 1973, PHYS CHEM ICE
[5]   CRYSTAL STRUCTURE OF A NEW FORM OF POLYOXYMETHYLENE [J].
CARAZZOLO, GA ;
MAMMI, M .
JOURNAL OF POLYMER SCIENCE PART A-GENERAL PAPERS, 1963, 1 (03) :965-&
[6]  
Colthup N.B., 1990, INTRO INFRARED RAMAN
[7]   AVERAGE CONCENTRATIONS OF OH IN TROPOSPHERE, AND BUDGETS OF CH4 CO H-2 + CH3CCL3 [J].
CRUTZEN, PJ ;
FISHMAN, J .
GEOPHYSICAL RESEARCH LETTERS, 1977, 4 (08) :321-324
[8]   Air-snow interactions and atmospheric chemistry [J].
Dominé, F ;
Shepson, PB .
SCIENCE, 2002, 297 (5586) :1506-1510
[9]   CONTINUOUS AUTOMATED-DETERMINATION OF ATMOSPHERIC FORMALDEHYDE AT THE PARTS-PER-TRILLION LEVEL [J].
FAN, Q ;
DASGUPTA, PK .
ANALYTICAL CHEMISTRY, 1994, 66 (04) :551-556
[10]  
Faure P., 1978, J GLACIOL, V21, P65