Campbell 21X Instrukcja Operatora Strona 73

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sEcTtoN
7.
MEASUREMENT
PROGRAMMING
EXAMPLES
are that it requires
an
extra differentialchannel
and
the added expense
of
a 6
wire
cable. In
this
case,
the benefits are worth
the
exp€nse.
The
load
cell
has
a nominalfull
scale
output
of
3
millivolts
per
volt
excitation.
lf the excitation
is
5
volts,
the fullscale
output is
15
millivolts;thus,
the
t15
millivolt range
is selected. The
calibrated
output of the load
cell
is
3.106mV/V1
at a load
of 250
pounds.
Output is desired
in
millimeters
of
water
with
respect to a fixed
point.
The
calibration in
mVA/1/mm
is:
3.1
06mVA/1 l250lb x 2.2lblkg x
3.1416k9/mm/4
=
0.02147mYNylmm
The
reciprocal of
this
gives
the
multiplier
to
convert
mVA/1
into
millimeters.
(The
result
of
Instruction
9 is the ratio of
the
output voltage
to
the actualexcitation
voltage multiplied
by
1000,
which is
mVA/1):
1
/0.021 47 mVA/, /mm
=
46.583mm
I
mY
N
.,
The
output from the load
cell is
connected
so
that
the voltage
increases
as the
mass
of the
lysimeter
increases.
(lf
the actual
mechanical
linkage
was
as
diagrammed
in
Figure
7.13-1,
the
output voltage would
be
positive
when
the
load
cell was
under
tension.)
When
the experiment is
started,
the water
content
of the soil in the lysimeter is
approximately 25o/o
on a volume basis. lt
is
decided to
use
this
as the
reference,
(i.e.,
O.25 x
15O0mm
=
375
mm).
The
experiment is started
at
the beginning of what is
expected to be a
period
during
which
evapotranspiration
exceeds
precipitation.
Instruction
9 is
programmed
with
the
correct multiplier
and
no
offset. After
hooking
everything up,
the counterbalance is
adjusted
so that the load
cell is
near
the top
of
its range;
this
will
allow
a
longer
period
before
readjustment
is
necessary.
The result
of
Instruction
9
(monitored
with
the "6
Mode)
is
109. The
offset
needed
to
give
the desired
initial
value
of 375mm is 266. However, it
is decided
to
add this
offset
in a
separate instruction
so
that
the result of lnstruction
9 can be used
as a
ready
reminder
of the strain
on
the load
cell
(range
=
t140mm).
When
the strain
on the
load
cell nears its rated
limits.
the
counterbalance
recalculated
to
;
the water budoe
CONNE
The
p
10
se
is
out
every
samp
wind
I
01
02:
7.14
227 G',
BLOCK
Soilmoistt
by relating
in resistan,
(lnstructior
resistance
of
the exci'
the sensor
output
output
ounterbalance is readjusted
and the
offset
:calculated to
provide
a
continuous
record of
re water budget.
'he
program
table has
an
execution
intervalof
0
seconds.
The
average value in millimeters
i output to Final
Storage
(not
shown in Table)
very
hour.
The
average
is
used, instead of a
ample,
in
order to cancel out
the effects of
dnd loading on the lysimeter.
ONNECTIONS
EX1
Ht 1
LO1
Ht2
2\X
LO2
+
VX
LYSIMETER
4
rr
J.
n
le
n1
rck
rng(
e
rsal
of
the
-he
ut
227
LOC
rilmoi
relati
resist
rstrucl
sistan
the e:
01:
02:
03:
FI,
:
01:
02:
03:
04:
05:
06:
07:
08:
09:
) sen(
tput s
tDut c
GURE
7.13-2.
6 Wire
Full Bridge
Gonnection for
Load
Cell
PROGRAM
P9
Full BR w/Compensatio
1
Rep
5 5000
mV
slow EX Rang
2 15
mV
slow BR Range
1 lN
Chan
1
Excite all
reps
w/EXcha
;000
mV Excitation
1
Loc
[:RAW
MEAS.]
46.583
Mult
0
Offset
P34 Z=X+F
1
X Loc RAW MEAS.
266 F
2
Z Loc
[:MEAS+OFFS]
GYPSUM SOIL
MOISTURE
K
sture
is measured with
a
gypsum
blr
ng the change in moisture to the chr
ance
of the block. An AC Half Bridg
ion
5) is
used to determine the
ce
of the
gypsum
block. Rapid reve
<citation
voltage
inhibits
polarization
ior.
Polarization
creates an error in
o
the fast integration time is
used.
'l
f
Instruction
5 is
the
ratio
of the outp
7-10
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