5TE Operator's Manual
3.Theory
soil matrix and that water was collected and tested for EC.
Solution EC is the electrical conductivity of pore water
removed from a saturated paste. In this case, the soil is wet-
ted with distilled water until the soil saturates, then the soil
is placed on filter paper in a vacuum funnel and suction is
applied. An electrical conductivity measurement on the
water removed from the sample will give the solution elec-
trical conductivity. Theoretically, the two are related by the
bulk density. An example calculation will illustrate this rela-
tionship: A soil is at 0.1 m
of 0.7 dS/m, and a bulk density of 1.5 Mg/m
culate the solution EC as follows.
ρ
φ
=
−
=
b
1
1
ρ
s
Solution
EC
In this example, ø is the porosity,
density of the minerals (assumed to be 2.65 Mg/m
script d is distilled water, and θ is volumetric water content.
We assume that the EC of the distilled water is 0 dS/m. In
practice, solution EC calculated from this method and solu-
tion EC taken from a laboratory soil test may not agree well
because wetting soil to a saturated paste is very imprecise.
Reference
Hilhorst, M.A. 2000. A pore water conductivity sensor.
Soil Science Society of America Journal 64:6 1922-
1925
1
5 .
−
=
. 0
43
. 2
65
(
σ
θ
σ
φ
+
=
p
d
φ
3
3
/m
VWC, has a pore water EC
)
( )
θ
−
0
7 .
0
1 .
=
0.43
ρ
is bulk density,
b
10
3
. We can cal-
+
0
=
. 0
162
dS/m
3
), sub-
ρ
is
s
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