Campbell CS616, Instruction Manual

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CS616 and CS625 Water Content Reflectometers
Gravimetric water content is calculated after the container weight is accounted
for.
θ
g
wet dry
dry
m m
m
=
−
For the bulk density,
ρ
bulk
dry
cylinder
m
volume
=
the dry weight of the sample is divided by the sample tube volume.
The volumetric water content is the product of the gravimetric water content
and the bulk density
θ θ ρ
v g bul
=
*
k
The average water content for the replicates and the recorded CS616 period are
one datum pair to be used for the calibration curve fit.
8.5 Calculations
The empty cylinders used for core sampling should be clean and both empty
weight and volume are measured and recorded. For a cylinder, the volume is
volume
d
h
=
⎛
⎝⎜ ⎞
⎠⎟
π
* *
2
2
where d is the inside diameter of the cylinder and h is the height of the
cylinder.
During soil sampling it is important that the cores be completely filled with soil
but not extend beyond the ends of the cylinder.
Once soil core samples are obtained, place the soil-filled cylinder in a small
tray of known empty weight. This tray will hold the core sample during drying
in an oven.
To obtain m
wet
, subtract the cylinder empty weight and the container empty
weight from the weight of the soil filled cylinder in the tray. Remove all the
soil from the cylinder and place this soil in the tray. Dry the samples using
oven or microwave methods as described above.
To obtain m
dry
, weigh the tray containing the soil after drying. Subtract tray
weight for m
dry
. Calculate gravimetric water content,
θ
g
, using
θ
g
wet dry
dry
m m
m
=
−
.
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