1 parameter 1: sdm address, 2 parameter 2: output option, 1 enter 0: measure la/l – Campbell Scientific TDR100 Time Domain Reflectometry Systems User Manual

Page 27

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TDR100

Waveform

Averaging 4: FP 1

-

128

Number of reflections averaged by the TDR100.

V

p

5:

FP

.1 - 1

relative propagation velocity

Points

6: FP 20-

2048

number of points in waveform

Cable length (meters)

7:

FP

0 -

2100

distance for TDR100 corresponding with

beginning of waveform

Window Length

(meters) 8:

FP .1

-

700

length of reflection waveform

Probe length

9:

4

Physical length of the exposed portion of the

metal rods

Probe

offset

10: FP 0

-

1.0

Accounts for portion of rods not exposed to soil.

See Section 6.2.10.

Input location

11:

4

Input storage location for measurement result. If

waveforms are chosen for output, this location is

occupied by the first data point.

Multiplier

12:

FP

Multiplication factor applied to La/L and stored

in input location specified in parameter 11.

Set to 1 when parameter 2 is 1 or 2.

For electrical conductivity, can be used for probe

constant value.

Offset

13:

FP

Offset value added to La/L and stored in input

location specified in parameter 11. Set to 0 when

parameter 2 is 1 or 2.

6.3 Discussion of TDR Instruction Parameters (Instruction 119)

6.3.1 Parameter 1: SDM Address

The SDM address of the TDR100 is set by selecting hexadecimal values with
the thumbwheel switch on the TDR100 front panel. Instruction 119 requires a
2 digit integer that is the base 4 value of the TDR100 address. See Table 5-1

6.3.2 Parameter 2: Output Option

6.3.2.1 Enter 0: Measure La/L

In the section on TDR Principles, the equation

K

L

L

a

a

=

is presented. The terms of this equality can be related to volumetric water
content using empirical relationships such as equations [3] and [4] shown in
Section 7. The apparent length of the probe rods, L

a

, changes with water

content. Dividing L

a

by the real rod length, L, gives the square root of

dielectric constant. The L

a

/L value is empirically related to volumetric water

content using calibration functions of the form

θ

v

= f(L

a

/L). See Section 7 for

commonly used calibration functions.

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