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PNNL-13501 - Pacific Northwest National Laboratory

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Single Channel Signal<br />

0.0025<br />

0.0020<br />

0.0015<br />

0.0010<br />

0.0005<br />

Single Channel Reflectance Spectra vs. Wavenumber (cm -1 )<br />

Single channel spectrum: quartz sand<br />

200 to 290 µm grain size, dry<br />

Single channel spectrum: quartz sand<br />

200 to 290 µm grain size,<br />

coated with dimethyl methylphosphonate<br />

Reflectance spectrum is the ratio of coated<br />

sand to dry sand. Reflectance angle is 63°.<br />

0.0000<br />

4000 3600 3200 2800 2400 2000 1600<br />

Wavenumbers (cm<br />

1200 800 400<br />

-1 )<br />

Figure 3. Infrared spectra of dimethyl methylphosphonate<br />

on quartz sand<br />

Single Channel Signal<br />

Single Channel Signal<br />

0.35<br />

0.30<br />

0.25<br />

0.20<br />

0.15<br />

0.10<br />

0.05<br />

0.00<br />

4000 3600 3200 2800 2400 2000<br />

Wavenumbers (cm<br />

1600 1200 800 400<br />

-1 Comparison of Single Channel Reflectance Signal for Mirror, Sand, and Quartz Crystal<br />

(reflectance angle ca. 45°)<br />

mirror reflectance<br />

quartz slab reflectance<br />

)<br />

0.0020<br />

0.0015<br />

0.0010<br />

0.0005<br />

Ottawa quartz sand (540-840 µm particle size) reflectance<br />

0.0000<br />

4000 3600 3200 2800 2400 2000 1600<br />

Wavenumbers (cm<br />

1200 800 400<br />

-1 )<br />

Figure 4. Comparison of reflectance signal strength for a<br />

flat mirror, a quartz slab, and quartz sand<br />

We found that for the same compound, dimethyl<br />

methylphosphonate for example, its evaporation rate off<br />

of metal surfaces is extremely slow compared to that off<br />

of quartz crystal, and is different than that off the quartz<br />

3.0<br />

2.5<br />

2.0<br />

1.5<br />

1.0<br />

0.5<br />

Ratio Coated Spec./Dry Spec.<br />

sand. Research into this would provide invaluable<br />

information to modelers calculating the accumulation of<br />

effluent compounds on surfaces surrounding proliferation<br />

sites.<br />

Summary and Conclusions<br />

We established a spectroscopic facility for recording<br />

reflectance spectra of chemical compounds coated onto<br />

terrestrial surfaces. Prominent spectral feature changes<br />

take place when these surfaces are coated. The continued<br />

research will provide a database of compounds and<br />

surfaces that should prove valuable to the intelligence<br />

community for evaluating possible weapons of mass<br />

destruction proliferation sites.<br />

References<br />

Asrar G. 1989. Theory and Applications of Optical<br />

Remote Sensing. Chapter 12, John Wiley & Sons, New<br />

York.<br />

Barettino EL-PD, C Anton-Pacheco, G Ortiz, JC Arranz,<br />

JC Gumiel, B Martinez-Pledel, M Aparicio, and<br />

O Montouto. 1999. “The Extent of the Aznalcollar<br />

Pyritic Sludge Spill and its Effects on Soils.” Sci. Tot.<br />

Environ. 242:57-88.<br />

Brodskii ES, SA Savchuk. 1998. “Determination of<br />

Petroleum Products in the Environment.” J. Anal. Chem.<br />

53:1070-1082.<br />

Mikati GOF. 1997. Temporal Analysis of Multispectral<br />

Video/Satellite Imagery for the Detection and Monitoring<br />

of Salinity on Agricultural Lands. Dissertation, Utah<br />

State University, UMI order no. DA9822024.<br />

Wolfe WL, GJ Zissis, eds.. 1985. The Infrared<br />

Handbook. pp 19-10 – 19-17. ERIM, Ann Arbor,<br />

Michigan.<br />

Sensors and Electronics 403

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