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Basic Aerosol Solid
Components Data Files
Complex Refraction Indices: m
= p-iq
|
component identifications- column 1;
number of real and imaginary parts of
complex refractive index - column 2;
temperature (K)- column 3;
available spectral range (micron) - columns
4 to 7;
references - column 8 |
|
Components*
|
#
p/q
refraction
indices
|
Temperature K
|
P
|
q
|
References
|
|
Wavelength (micron)
|
|
min
|
max
|
min
|
max
|
|
Ammonium
Sulfate (Crystalline form)
|
61/61
|
T=293 K
(assumed)
|
0.2
|
40
|
0.2
|
40
|
Toon et al., 1976
|
|
Ash
|
61/61
|
T=293 K
(assumed)
|
0.2
|
40
|
0.2
|
40
|
Volz F., 1972a, 1973; Shettle and Fenn, 1979.
|
|
Carbonaceous
|
61/61
|
T=293 K
(assumed)
|
0.2
|
40
|
0.2
|
40
|
Shettle and Fenn, 1979; Twitty, J. T. and Weinman, 1971
|
|
Dust-Like
|
61/61
|
T=293 K
(assumed)
|
0.2
|
40
|
0.2
|
40
|
Volz F., 1972a, 1973; Shettle and Fenn, 1979.
|
|
Hematite
(Iron Oxide)
|
68/68
|
T=293 K
(assumed)
|
0.2
|
300
|
0.2
|
300
|
Longtin et al., 1988; Galuza et al., 1979; Kerker et al., 1979;
Steyer, 1974; Onari, 1977
|
|
Insoluble
|
61/61
|
T=293 K
(assumed)
|
0.25
|
40
|
0.25
|
40
|
Shettle and Fenn, 1979
|
|
Meteoric
Dust
|
62/62
|
|
0.2
|
50
|
0.2
|
50
|
Fenn et al., 1985; Shettle, and Volz, 1976
|
|
Mineral
(nucleus mode)
|
61/61
|
T=293 K
(assumed)
|
0.25
|
40
|
0.25
|
40
|
Carson and Benjamin, 1980; Sokolik et al., 1993
|
|
Mineral
(accumulation mode)
|
61/61
|
T=293 K
(assumed)
|
0.25
|
40
|
0.25
|
40
|
Carson and Benjamin, 1980; Sokolik et al., 1993
|
|
Mineral
(coarse mode)
|
61/61
|
T=293 K
(assumed)
|
0.25
|
40
|
0.25
|
40
|
Carson and Benjamin, 1980; Sokolik et al., 1993
|
|
Mineral-transported
|
61/61
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T=293 K
(assumed)
|
0.25
|
40
|
0.25
|
40
|
Carson and Benjamin, 1980; Sokolik et al., 1993
|
|
Quartz
|
68/68
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T=293 K
(assumed)
|
0.2
|
300
|
0.2
|
300
|
Gray, 1963; Drummond, 1936; Spitzer, and Kleinman, 1961; Philipp,
1985; Longtin et al., 1988.
|
|
Sand
|
68/68
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T=293 K
(assumed)
|
0.2
|
300
|
0.2
|
300
|
Longtin et al., 1988
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Sea
Salt
(Crystalline form)
|
61/61
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T=293 K
(assumed)
|
0.2
|
40
|
0.2
|
40
|
Dorsey, 1940; Volz, 1972a;
Shettle and Fenn, 1979;
|
|
Sea
salt (accumulation mode)
|
61/61
|
T=293 K
(assumed)
|
0.25
|
40
|
0.25
|
40
|
Shettle and Fenn, 1979
|
|
Sea
salt (coarse mode)
|
61/61
|
T=293 K
(assumed)
|
0.25
|
40
|
0.25
|
40
|
Shettle and Fenn, 1979
|
|
Sodium
Chloride (Crystalline form)
|
90/90
|
T=293 K
(assumed)
|
0.2
|
30000
|
0.2
|
30000
|
Eldridge and Palik, 1985
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|
Soot
|
61/61
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T=293 K
(assumed)
|
0.25
|
40
|
0.25
|
40
|
Shettle and Fenn, 1979
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Volcanic
Dust
|
61/61
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T=293 K
(assumed)
|
0.2
|
40
|
0.2
|
40
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Volz, F. E. , 1973
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