When using the time domain reflectometry (TDR) technique in laboratory
experiments, e.g., with packed soils columns, it is often of great im
portance to obtain high depth resolution with minimal disturbance of t
he soil and to be able to measure close to the soil surface. This requ
ires the use of fairly small TDR probes that can be placed near each o
ther. In laboratory experiments on packed soil, we have examined the i
mportance of relations between the probe-rod diameter, probe-rod lengt
h, distance between probe rods, and distance from the probe to the soi
l surface for accurate determination of volumetric water content. The
experiments were conducted on a coarse sand with three different rod d
iameters (1, 2, and 3 mm), three different rod spacings (10, 20, and 5
0 mm), two rod lengths (50 and 150 mm), and at distances to the soil s
urface varying from 5 to 50 mm. Theoretical work by Knight et al. (199
4, Symposium and workshop on time domain reflectometry in environmenta
l, infrastructure and mining applications, Northwestern Univ., Evansto
n, Illinois, Sept 7-9, 1994, pp. 93-104) has been used to evaluate the
results. In general, theory and measurements agreed very well. Both m
easurements and theory showed that the volume of soil contributing to
the measurement is highly dependent on the spacing of the rods and, to
a lesser degree, on the rod diameter. For rod spacings of 10, 20, and
50 mm, measurements were accurately made as close to the soil surface
as 10, 15, and 20 mm, respectively.