Instrument Measures Fluorescence From Chlorophyll in Plants
Stennis Space Center, Mississippi
Apr 30 2000
Page 2 of 2
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Atmospheric oxygen strongly attenuates incident sunlight in
spectral lines in two groups known as A band (wavelength ≈
760 nm) and B band (wavelength ≈
688 nm). Each of these bands includes about 40 spectral lines with such strong
absorption that the atmosphere can be considered opaque at the middle wavelengths
of these lines. Chlorophyll fluoresces strongly at these wavelengths. Thus,
if light from plants at these wavelengths is measured, one can be assured that
the measurement represents only fluorescence from chlorophyll, without contribution
from scattered sunlight. Of course, the measuring instrument
must be close enough to the plants in question that atmospheric oxygen does
not also appreciably absorb the fluorescence from the chlorophyll, along with
sunlight at the affected wavelengths; the resulting practical limit on the range
of the present instrument or any similar instrument is 100 to 200 meters.
The present sensor (see Figure 2) is based on this
spectral-discrimination principle. Light from sunlit plants is focused by a lens,
then made to pass through a filter that passes wavelengths in a chosen 10-nm-wide
subband of A or B band. The band-pass-filtered light passes through an entrance
chopper, then along a light pipe to a spherical integrating cavity. Centered in
the cavity is a quartz bulb that contains a gaseous mixture of oxygen and argon
at a total pressure of about 100 torr (about 13 kPa).
Figure 2. This Spectral-Line Discriminator measures fluorescence from sunlit plants. Discrimination against scattered sunlight is achieved by a design that utilizes the absorption spectrum of atmospheric oxygen in combination with absorption and fluorescence in a bulb that contains oxygen.
When the entrance-chopper aperture is open, the oxygen in the
bulb is illuminated by plant fluorescence plus scattered sunlight in the chosen
subband of A or B band, but the oxygen absorbs only the light at its characteristic
absorption wavelength in this subband. Because the atmosphere has already filtered
out sunlight at these wavelengths, the light absorbed by the oxygen consists
almost entirely of fluorescence emitted by the plants. While the entrance-chopper
aperture remains open, a silicon photodiode measures the total A- or B-band
radiation received by the cavity.
When the entrance-chopper aperture is closed, the oxygen in
the bulb emits the absorbed light energy as fluorescence in A band (regardless
of whether the illumination is in A band or B band). Because the entrance-chopper
aperture is closed, the remaining light in the cavity consists entirely of this
secondary fluorescence, proportional to the fluorescence from the plants. An
exit chopper synchronized in opposite phase with the entrance chopper opens
to allow this light to pass to a photomultiplier tube cooled to a temperature
40 K below ambient. The output of the photomultiplier tube is processed and
fed to a data-acquisition system.
This work was completed by Paul L. Kebabian, Herman E. Scott,
and Andrew Freedman of Aerodyne Research, Inc., for Stennis
Space Center under 1996 SBIR Phase II: NAS #NAS13-707. For further information,
contact Herman Scott of Aerodyne Research, Inc., at (978) 663-9500 extension
267).
In accordance with Public Law 96-517, the contractor has elected
to retain title to this invention. Inquiries concerning rights for its commercial
use should be addressed to
Laurie S. Dean, Commercialization Manager
Aerodyne Research, Inc.
45 Manning Road
Billerica, MA 01821-3976
Refer to SSC-00037, volume and number of this NASA Tech
Briefs issue, and the page number.
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