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References

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  1. R. G. Pinnick, G. Fernandez, B. D. Hinds, Appl. Opt. 22, 95 (1983).
    [CrossRef] [PubMed]
  2. D. F. Flanigan, H. P. DeLong, Appl. Opt. 10, 51 (1971).
    [CrossRef] [PubMed]
  3. R. V. Jolliffe, “Evaluation of a Computerized Technique for Determining Particle Distribution Parameters from Aerosol Mass Decay Data,” Edgewood Arsenal Technical Report EATR 4509 (1972).
  4. M. R. Querry, Missouri-Kansas City; private communication.
  5. T. Hatch, S. Choate, J. Franklin Inst. 207, 369 (1929).
    [CrossRef]

1983 (1)

1971 (1)

1929 (1)

T. Hatch, S. Choate, J. Franklin Inst. 207, 369 (1929).
[CrossRef]

Choate, S.

T. Hatch, S. Choate, J. Franklin Inst. 207, 369 (1929).
[CrossRef]

DeLong, H. P.

Fernandez, G.

Flanigan, D. F.

Hatch, T.

T. Hatch, S. Choate, J. Franklin Inst. 207, 369 (1929).
[CrossRef]

Hinds, B. D.

Jolliffe, R. V.

R. V. Jolliffe, “Evaluation of a Computerized Technique for Determining Particle Distribution Parameters from Aerosol Mass Decay Data,” Edgewood Arsenal Technical Report EATR 4509 (1972).

Pinnick, R. G.

Querry, M. R.

M. R. Querry, Missouri-Kansas City; private communication.

Appl. Opt. (2)

J. Franklin Inst. (1)

T. Hatch, S. Choate, J. Franklin Inst. 207, 369 (1929).
[CrossRef]

Other (2)

R. V. Jolliffe, “Evaluation of a Computerized Technique for Determining Particle Distribution Parameters from Aerosol Mass Decay Data,” Edgewood Arsenal Technical Report EATR 4509 (1972).

M. R. Querry, Missouri-Kansas City; private communication.

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Figures (4)

Fig. 1
Fig. 1

Spectral dependence of the extinction coefficient ratio α(λ)/α(0.63) for explosively dispersed EA-soil. The extinction coefficient at 0.63 μm is 0.46 m2 g−1.

Fig. 2
Fig. 2

Imaginary part of the IR complex refractive index for clay minerals commonly found in soils.

Fig. 3
Fig. 3

Extinction spectra computed from Lorenz-Mie theory for kaolinite dusts with σg = 1.78 and mass median diameters between 3.0 and 20.0 μm.

Fig. 4
Fig. 4

Fraction of the total extinction contributed by the small particle mode when Dm = 146.0 μm, σg = 1.87, ρ = 2.5 g cm−3, and fm varies from 0.01 to 0.99.

Equations (3)

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α ( λ ) = 3 2 ρ l f m l Q e ( x , Ñ ) D d m l ,
α ( λ ) = f m α s ( λ ) + ( 1 f m ) α n .
α n = 3 ρ D m exp ( ½ ln 2 σ g ) .

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