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People frequently inquire as to the sensitivity of Ocean Optics spectrometers
-- particularly, sensitivity as a function of wavelength. The issue typically
comes up in the context of the user wanting to convert the amplitude of the raw
data spectra -- or the "Scope" mode, as it's denoted in OOIBase32™
Spectrometer Operating Software -- into some meaningful energy spectra.
To understand the answer, be aware that it is not practical to apply
correction factors for the various phenomena that affect the amplitude. We
provide a more useful alternative: a NIST-traceable radiant standard (the LS-1-CAL),
which can be used to normalize the spectra to energy terms. In our OOIBase32
operating software, this normalized data can be processed in the "I"
(Irradiance) mode as relative energy (scaled 0 to 1). In our OOIIrrad Irradiance
Measurement Software, the data can be processed in absolute terms (calculated in
mW/cm2/nm or in lumens or lux per unit
area).
For experiments investigating transmission or reflection, the data are
normalized to the spectra of a physical standard such as transmission in air or
reflection of a diffuse white standard.
These are some of the factors affecting spectrometer system amplitude:
- CCD detector response. A typical response
curve of an unmodified silicon detector is available from our supplier,
although it provides only part of the story. We add a coating to the CCD to
spoil an optical cavity formed by the SiO2 layers in the structure. This
eliminates large oscillations in amplitude that vary with wavelength. For UV
response, we add a phosphor coating. The data in the manufacturer's detector
specifications is at best an approximation of the response you can
anticipate from the detector in your system.
- Fiber attenuation. Attenuation is fairly flat in the Visible but
increases dramatically in the UV region. In the NIR, there are water
absorption bands at 750 nm and 900 nm that affect fiber attenuation, as
shown in these spectral
attenuation curves.
- Grating efficiency. All ruled or holographically etched
gratings optimize first-order spectra at certain wavelength regions,
depending on the blaze wavelength of the grating and other factors. We offer
14 gratings; each has characteristics that define its efficiency. Use these grating
charts to compare grating efficiencies.
- Collection optics. Sampling optics can have spectral signatures
themselves. A good example would be the collimating lenses used in our
cuvette holder assemblies. These are simple lenses with chromatic
aberrations, which vary with their focus. You can see the magnitude of these
chromatic effects in these UV
cuvette holder transmission curves.
- Sources and samples. Light sources and samples also have their own
spectral response. If the light itself is the sample, this spectral response
is what you're trying to measure. If you are using the light to measure a
sample -- such as in transmission and reflection experiments -- then the
spectra of the light source must be considered. An example of such a spectra
is available in the description of our LS-1-Tungsten
Halogen Light Source.
- Other factors. Some characteristics of the design and electronics
of the CCD array also can affect sensitivity. For example, the detector's
voltage signal includes an offset consisting of dark-current signal and an
amplifier zero set point that we call "Dark." This value varies
from pixel to pixel, so it must be subtracted for each CCD element. Also,
there is some variation in responsivity among pixels, so that data
normalization must be done on a pixel-by-pixel basis as well. (This
normalization removes so-called "fixed pattern noise.")
The only practical way to account for all of these factors is to do a
calibration experiment and "normalize" the data by comparing the
sample spectra to a suitable reference spectra:
1. %Transmission(i) or %Reflection(i) = [S(i)-D(i)]/[R(i)-D(i)], where
S is the sample intensity at pixel (i) (CCD pixel number from 0 to 2047), D
is the dark intensity at pixel (i), and R is the reference intensity at
pixel (i);
2. Absorbance(i) = -log[T(i)]; or
3. Energy I(i) = B(i)[T(i)], where B is the spectra of the radiant standard.
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Last Modified: Sunday, April 14, 2002
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