
TDR100
23
6.2.12 Parameter 12: Multiplier
Multiplication factor applied to the value stored in the input location specified
in parameter 11. Set to 1 when parameter 2 is 1 or 2. The multiplier can be
used for the probe constant value when measuring electrical conductivity.
6.2.13 Parameter 13: Offset
Offset value added to the value stored in input location specified in parameter
11. Set to 0 when parameter 2 is 1 or 2.
6.2.13.1 Probe Constant for Electrical Conductivity Measurement
The section, TDR Principles, presents the equation used for soil bulk electrical
conductivity. For convenience, it is repeated here.
σ
ρ
ρ
=
−
+
K
Z
p
c
1
1
A portion of the datalogger algorithm evaluates the reflected waveform to
determine the applied and reflected voltages. From this, the reflection
coefficient, ρ, can be calculated. The term, Z
c
, is the reflectometer impedance
and is a constant 50 ohms.
The electrical conductivity routine in the datalogger returns the value
11
1Z
c
+
ρ
which must be multiplied by the probe constant, K
p
, to get an electrical
conductivity value.
The probe constant (K
p
) is easily determined using PCTDR or can be
determined through calibration. The probe rods are immersed in solutions of
known electrical conductivity and values of
11
1Z
c
−
+
ρ
ρ
collected by the
datalogger. A linear regression of known electrical conductivity to the result
from the datalogger will have a slope equal to the probe constant. When
performing a calibration with independently measured electrical conductivity,
take caution to account for the strong temperature dependence of electrical
conductivity. This calibration is generally recommended if accurate absolute
electrical conductivity values are required.
Laboratory calibrations were performed to determine a K
p
value for the
CS600, CS605 and CS610 probes with the following results.
TABLE 6-2. Probe Constant Values for Campbell Scientific Probes
Probe model probe constant (K
p
)
CS600 3.16
CS605 & CS610 1.74
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