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5 ir reflectivity—sediment color, Ir reflectivity—sediment color – Campbell Scientific OBS500 Smart Turbidity Meter with ClearSensor Technology User Manual

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OBS500 Smart Turbidity Meter with ClearSensor™ Technology

FIGURE 8-4. Response of an OBS sensor to a wide range of SSC

8.5 IR Reflectivity—Sediment Color

Infrared reflectivity, indicated by sediment color, has a major effect on

sensitivity because with other factors remaining constant, it changes the

intensity of light scattering. Although turbidity sensors are color blind, tests

have shown that “whiteness”, color, and IR reflectivity are correlated. Calcite,

which is highly reflective and white in color, will produce a much stronger

turbidity 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 8-5. 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.

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