Temporal moments analysis of solute breakthrough curves is used to investig
ate the preferential leaching of chloride, nitrate and phosphate trough an
Australian soil. Recent studies have shown that current models and methods
do not adequately describe the leaching of nutrients through soil, often un
derestimating the risk of groundwater contamination by surface-applied chem
icals, and overestimating the concentration of resident solutes. This inacc
uracy results primarily from ignoring soil structure and nun-equilibrium be
tween soil constituents, watts and solutes. Therefore simple models are req
uired to accurately characterise solute transport in natural and agricultur
al soils under non-equilibrium conditions. A multiple sample percolation sy
stem, consisting of 25 individual collection wells was constructed to study
. the effects of localised soil heterogeneities on the transport of nutrien
ts (NO3-, Cl-, PO43-) in the vadose zone of an agricultural soil predominan
tly dominated by clay. Using data collected from the multiple sample percol
ation experiments, this paper compares and contrasts the performance of tem
poral moments analysis with two mathematical models for predicting solute t
ransport: the advective-dispersion model with a reaction term (ADR) and a t
wo-region preferential flow model (TRM) suitable for modelling preferential
transport. The values for solute transport parameters predicted by tempora
l moments analysis were in excellent agreement with experimental data and r
esults from ADR and TRM. It is concluded that temporal moments analysis whe
n applied with other physical models such as the ADR and TRM, provide an ex
cellent means of obtaining values for important solute transport parameters
and gaining insight of preferential flow. These results have significant r
amifications for modelling solute transport and predicting nutrient loading
s.