05.06.2013 Views

PNNL-13501 - Pacific Northwest National Laboratory

PNNL-13501 - Pacific Northwest National Laboratory

PNNL-13501 - Pacific Northwest National Laboratory

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Study Control Number: PN00057/1464<br />

Infrared Polarization Signatures<br />

Thomas A. Blake, John F. Schultz<br />

This project will produce a laboratory database of infrared reflectance and polarization spectra of liquid phase chemical<br />

compounds coated onto terrestrial surfaces such as rocks, minerals, sands, clays, etc. The database will be indispensable<br />

in understanding remote sensing data of the terrain surrounding suspected weapons of mass destruction proliferation sites.<br />

Such a database could also be extended to detecting changes in soil salinity and moisture as well as surface pollution such<br />

as petroleum spills.<br />

Project Description<br />

The purpose of this project is to set up a Fourier transform<br />

infrared spectrometer that can then be used to record<br />

reflectance spectra of low volatility organic and<br />

organophosphorous compounds coated onto terrestrial<br />

surfaces. In the second year, the spectrometer will be<br />

modified to include an ellipsometry capability, so that<br />

changes in the state of polarization as light reflects off<br />

these coated surfaces can be measured. The database of<br />

infrared reflectance and polarization spectra of a select<br />

group of compounds on a select group of surfaces will be<br />

invaluable in interpreting remote sensing data of soils<br />

surrounding suspected proliferation sites. To date, we<br />

have set up the Fourier transform spectrometer, and a<br />

reflectance accessory for holding our samples and<br />

recording spectra at variable reflectance and detection<br />

angles. We have begun recording reflectance spectra of<br />

several surfaces such as rough cut quartz crystal, and<br />

quartz and feldspar sands. The spectra agree nicely with<br />

reflectance spectra recorded for geological spectral<br />

databases, and we are now coating quartz and feldspar<br />

sands with dimethyl methylphosphonate, which is a<br />

benign simulant of the G class of chemical weapon<br />

compounds, and recording reflectance spectra of these<br />

coated surfaces. The spectra show that there is a<br />

significant change in the spectra in going from the<br />

uncoated to coated surface. Such changes will provide a<br />

“smoking gun” signature of the presence of this<br />

compound. This work is now expanding to other<br />

compounds and other surfaces.<br />

Introduction<br />

The objective of this project is to explore unpolarized and<br />

polarization-resolved reflectance spectra for detecting the<br />

presence of liquids and particulates related to the<br />

production of weapons of mass destruction on surfaces<br />

around suspected facilities. It will be possible to detect<br />

changes in the reflectance spectra as a surface is coated<br />

with liquids, thus providing information about the<br />

operational status of a facility and likely locations for<br />

physical sampling. By comparing how the reflectance<br />

spectra change as a compound accumulates and ages on a<br />

surface, it may also be possible to identify classes of<br />

compounds, and perhaps even specific chemicals. We<br />

will determine whether such spectral features can be<br />

found for each compound-substrate combination and if<br />

the signatures will be pronounced enough to detect from a<br />

remote sensing platform. If this work indicates that the<br />

polarization-resolved reflectance spectra can be used to<br />

detect weapons-related compounds on surfaces, we see<br />

immediate extension to a number of important battlefield<br />

chemical warfare and environmental applications.<br />

Field data will be collected using multispectral passive<br />

remote sensing systems similar to NASA’s Airborne<br />

Visible and InfraRed Image Spectrometer (wavelength<br />

coverage 0.4 to 2.45 µm) or Thermal Infrared<br />

Multispectral Scanner (wavelength coverage 8 to 12 µm).<br />

These instruments operate from NASA’s ER-2 and Lear<br />

Jet aircraft, respectively, and have instantaneous ground<br />

fields of view of about 10 meters. As an example of<br />

sensitivity, the Thermal Infrared Multispectral Scanner<br />

uses liquid nitrogen cooled HgCdTe detectors and has a<br />

noise equivalent temperature difference of 0.1 K at 300 K.<br />

This figure of merit can be related to a noise equivalent<br />

reflectance difference of 0.002 at a wavelength of 8 µm.<br />

Since most terrestrial materials have a reflectance<br />

between 0.2 and 0 the instruments are sensitive to<br />

reflectance changes of 1 part in 100. The laboratory<br />

measurements will allow us to quantify reflectance<br />

changes with amounts of coverage of our target<br />

compounds (Asrar 1989; Wolfe and Zissis 1985).<br />

Tailings and effluents pumped from mines (Barettino et<br />

al. 1999), petroleum ground spills (Brodskii and Savchuk<br />

Sensors and Electronics 401

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!