| Optical
sensors
Optical sensors are designed in many ways to detect light
scattering and attenuation in order to measure sediment and
turbidity in water samples. Some of them are shown on the
sketch below, but despite their diversity, they all work in
the same basic way. A water sample, the red-shaded region,
is illuminated by a light source, shown by the red light bulb,
and one or more photodetectors convert the light radiated
from the sample to photocurrent. The amount of photocurrent
depends mainly on the area of the illuminated particles but
also on particle size, shape and reflectivity. Since the area
of the illuminated particles is directly proportional to the
suspended-sediment concentration, SSC, measurements of light
scattering provide a way to estimate SSC. Certain conditions,
explained in the answers to other FAQs (size,
color, disaggregation
effects), must be met to do this accurately. Light absorption
by the sample will also affect the photodetectors and the
indicated turbidity of the water. While laboratory turbidity
meters can have several photodetectors, submersible sensors
usually have only one. This is because it is difficult to
design submersible sensors with multiple detectors. OBS sensors
detect light scattered over a range of angles that depends
on the model and particle concentration in the sample. The
OBS-3 detects light scattered between 140 and 160°, the
OBS-4 sensor (70-160°), the OBS-5 (88-170°); see sketch.

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Conversions of detector
signals
Conversions of detector signals to engineering values, such
as mg l-1 or NTUs is done by a sensors’ signal processor
or by an operator using Excel. A sensor must be calibrated with
sediment or turbidity standards before it can make such conversions.
Sediment calibration is the process by which OBS signals are
related by a mathematical formula to standard SSC values for
suspensions of sediment from the measurement site. OBS sensors
can be calibrated with any natural sediment or man-made particles,
such as wastes from oil shale, coal, glass, and ceramic production.
While several issues demand caution; see
disaggregation effects, a meter calibrated in this way can
be used to estimate rapidly and continuously the SSC in lakes,
rivers, reservoirs, settling ponds and process tanks.
SSC
SSC is a physical quantity with units mass per unit volume
(mg l-1, kgm-3). So knowing its value
at a particular time and location enables calculations of
such things as sediment loads of streams, background SSC levels
for managing waterside construction, dredging, and logging
to minimize adverse impact, and operations complying with
NPDES permits. Calibration for turbidity measurements establishes
a numerical relationship between OBS signals and corresponding
standard NTU values. The resulting mathematical formula is
used for assigning NTU values to water samples from OBS signals.
Unlike SSC, turbidity values are relative units that have
no direct physical significance. |
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Reference:
OBS-3 Suspended Solids & Turbidity Monitor
Instruction Manual, 1991. D & A Instrument
Co.
OBS-3A Recording Suspended Solids Monitor Instruction
Manual, 2001. D & A Instrument Co.
OBS-5 High-level Suspended Solids Monitor Instruction
Manual, 2002. D & A Instrument Co.
John Downing. 2005. Turbidity Monitoring.
Chapter 24 in: Environmental Instrumentation and Analysis
Handbook. John Wiley & Sons, Pages: 511-546. 2005.
John Downing. 1989. Optical Backscatter Turbidimeter
Sensor. U.S. Patent Number 4,841,157.
John Downing. 1998. Suspended particle concentration
monitor. U.S. Patent Number 5,796,481.
John Downing, R.W Sternberg, & C.R.B Lister. 1981. New
Instrumentation for Investigation of Sediment Suspension in
the Shallow Marine Environment. Marine Geology,
Vol. 42, pp. 19-34.
John Downing. 1983. An Optical Instrument for
Monitoring Suspended Pareticles in Ocean and Laboratory.
Proceedings of Oceans ’83, IEEE Publication 83CH 1972-9.
4 pages.
American Public Health Association (AWWA). 1998. Standard
Methods for the Examination of Water and Wastewater.
19th Edition, Method 2130 Turbidity, pp. 2-8 to 2-9.
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