A reanalysis of the 1978 tracer experiment at Borden, Ontario, is perf
ormed using spatial moments. The tracer experiment involved the unifor
m injection of chloride ions into an aquifer, and the resulting plume
was allowed to migrate under natural gradient conditions. Detailed mon
itoring of the evolving plume was then performed in three dimensions.
The work of Sudicky et al. (1983) showed that the solute cloud evolved
as two plumes owing to variations in hydraulic conductivity at the si
te. In this paper we compute the zeroth through the fourth spatial mom
ents of the plume in the lower hydraulic conductivity zone. From these
moments the solute mass of the plume, the velocity of the center of m
ass, the dispersion, the skew, and the kurtosis of the plume are calcu
lated. These results are compared with the results of Sudicky et al. a
s well as with the theoretical results of Gelhar et al. (1979) and Naf
f (1990). Our computed plume velocity and apparent horizontal transver
se macrodispersivity are in agreement with the estimates of Sudicky et
al.; however, our apparent longitudinal macrodispersivity estimate ex
ceeds that of Sudicky et al. by a factor of 2. The apparent horizontal
transverse macrodispersivity obtained is also quite similar to that o
f Freyberg (1986). At early times, the plume is found to be positively
skewed as well as platykurtic. This supports the findings of Gelhar e
t al. and contradicts those of Naff.