A MODELING INVESTIGATION OF SUDDEN SODIUM LAYERS

被引:35
作者
COX, RM
PLANE, JMC
GREEN, JSA
机构
[1] School of Environmental Sciences, University of East Anglia
关键词
D O I
10.1029/93GL03002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A time-resolved model, incorporating both vertical diffusion and chemistry, indicates that the minimum source strength required to produce a typical sudden sodium layer (SSL) is about 3 Na atoms cm-3 s-1. However, many of the mechanisms proposed to explain the formation of SSLs are not able realistically to provide this source strength, or the source strength of about 1 Na atom cm-3 s-1 that is required to maintain an SSL over several hours. Furthermore, the sodium reservoirs do not appear to contain sufficient sodium to produce an SSL, although sodium ions (Na+), and meteoric dust coated with sodium compounds, cannot be ruled out. An additional mechanism is proposed, namely, the release of atomic Na by dissociative electron attachment to sodium-containing silicate molecules (e.g. Na2SiO3 or NaAlSiO4) that are produced by meteoric ablation.
引用
收藏
页码:2841 / 2844
页数:4
相关论文
共 28 条
[1]   RATE COEFFICIENT FOR THE GAS-PHASE REACTION OF NAOH WITH CO2 [J].
AGER, JW ;
HOWARD, CJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1987, 92 (D6) :6675-6678
[2]   CHARACTERISTICS OF THE SPORADIC SODIUM LAYERS OBSERVED AT 23-DEGREES-S [J].
BATISTA, PP ;
CLEMESHA, BR ;
BATISTA, IS ;
SIMONICH, DM .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1989, 94 (A11) :15349-15358
[3]   HORIZONTAL STRUCTURES IN SPORADIC SODIUM LAYERS AT 23-DEGREES-S [J].
BATISTA, PP ;
CLEMESHA, BR ;
SIMONICH, DM .
GEOPHYSICAL RESEARCH LETTERS, 1991, 18 (06) :1027-1030
[4]   SIMULTANEOUS RADAR AND LIDAR OBSERVATIONS OF SPORADIC-E AND NA LAYERS AT ARECIBO [J].
BEATTY, TJ ;
COLLINS, RL ;
GARDNER, CS ;
HOSTETLER, CA ;
SECHRIST, CF ;
TEPLEY, CA .
GEOPHYSICAL RESEARCH LETTERS, 1989, 16 (09) :1019-1022
[5]   SPACED LIDAR AND NIGHTGLOW OBSERVATIONS OF AN ATMOSPHERIC SODIUM ENHANCEMENT [J].
CLEMESHA, BR ;
KIRCHHOFF, VWJH ;
SIMONICH, DM ;
TAKAHASHI, H ;
BATISTA, PP .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1980, 85 (NA7) :3480-3484
[6]   CONCERNING THE ORIGIN OF ENHANCED SODIUM LAYERS [J].
CLEMESHA, BR ;
BATISTA, PP ;
SIMONICH, DM .
GEOPHYSICAL RESEARCH LETTERS, 1988, 15 (11) :1267-1270
[7]   THE HEIGHT DISTRIBUTION OF RADIO METEORS - OBSERVATIONS AT 6-MHZ [J].
ELFORD, WG ;
OLSSONSTEEL, D .
JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS, 1988, 50 (09) :811-818
[8]   A VAPORIZATION MODEL FOR IRON SILICATE FRACTIONATION IN THE MERCURY PROTOPLANET [J].
FEGLEY, B ;
CAMERON, AGW .
EARTH AND PLANETARY SCIENCE LETTERS, 1987, 82 (3-4) :207-222
[9]   SOME ASPECTS OF METAL ION CHEMISTRY OF EARTHS ATMOSPHERE [J].
FERGUSON, EE ;
FEHSENFELD, FC .
JOURNAL OF GEOPHYSICAL RESEARCH, 1968, 73 (19) :6215-+
[10]  
GRANIER C, 1985, GEOPHYS RES LETT, V12, P655, DOI 10.1029/GL012i010p00655