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Section 8. Factors Affecting OBS Response
0510
Sediment Concentration (g/l)
15
0
1
2
3
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5
Signal (V)
A
FIGURE 8.3-1. Response at High Sediment Concentrations
8.4 Sediment Color
Sediment color, after particle size, has a major effect on OBS sensitivity, and if
it changes, it can degrade the accuracy of measurements. Although OBS
sensors are “color blind”, “whiteness”, color, and IR reflectivity (measured by
an OBS sensor) are well correlated. Calcite, which is highly reflective and
white in color, will produce a much stronger OBS signal on a mass-
concentration basis than magnetite, which is black and IR absorbing.
Sensitivity to colored silt particles varies from a low of about one for dark
sediment to a high of about ten for light gray sediment; see FIGURE 8.4-1. In
areas where sediment color is changing with time, a single calibration curve
may not work. Resulting errors will depend on the relative concentrations of
colored sediments.
8-3
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