Soil water storage over a 2.85-m soil depth was measured from 200 alum
inum access pipes, separated by 0.3 m in both directions, in a 1.2 x 1
5.0-m plot in dry and wet periods during 1988 and 1989 The objective w
as to determine the minimum plot size and number of soil water content
measurements if measured with a neutron probe for small field trials.
The minimum plot size representing the 15-m plot was found to be depe
ndent on water storage variance and on the distance over which soil wa
ter storage measurements were spatially correlated. We concluded that
a plot length of 5 m was needed to represent the mean and variance of
the 15-m plot. Bootstrapping and temporal stability analysis were used
to estimate the minimum number of observation tubes required to estim
ate the mean and variance of 1.2 x 5.0-m plots. Bootstrapping showed t
hat at least 10 soil water storage measurements were required in the 5
-m plot. Soil water storage distribution within the plot was found to
be highly stable in time, especially for individual soil layers. Using
temporal stability analysis, the number of required access pipes need
ed to estimate a plot-average soil water storage was further reduced t
o three. However, the variance of soil water storage was not conserved
while reducing the number of measurement locations. We propose that a
field study with small field trials should start with the maximum fea
sible plot size and number of measurement locations. In this initial p
hase, statistical techniques as proposed in this study can then be app
lied to reduce the required number of observations, using predetermine
d error limits.