Appendix D. SDI-12 Sensor Support
E-3
It is also essential that particle shape remains constant during the monitoring
period.
0
20
40
60
80
100
120
140
160
180
Scat t ering Angle
0.01
0.1
1
R
e
la
ti
v
e
S
c
a
tt
e
ri
n
g
I
n
te
n
s
it
y
Cubes
Plates
Spheres
OBS-3+
FIGURE E-3. Relative scattering intensities of grain shapes
E.4 High Sediment Concentrations
At high sediment concentrations, particularly in suspensions of clay and silt,
the infrared radiation from the emitter can be so strongly attenuated along the
path connecting the emitter, the particle, and the detector, that backscatter
decreases exponentially with increasing sediment concentration. For mud, this
occurs at concentrations greater than about 5,000 mg/l. FIGURE
calibration in which sediment concentrations exceeding 6,000 mg/l
cause the
output signal to decrease. It is recommended not to exceed the specified
turbidity or suspended-sediment ranges, otherwise the interpretation of the
signal can be ambiguous. For example, a signal level of 2,000 mV (FIGURE
) could be interpreted to indicate SSC values of either 3,000 or 33,000 mg/l.
Factory calibrations are performed in the linear region designated ‘A’ on the
graph.
