Experiments on model and real soil blocks designed to assess the feasi
bility of using magnetic resonance imaging for three-dimensional mappi
ng of the time-varying spatial distribution of water in structured soi
ls are reported. The results show that, notwithstanding inherent probl
ems in imaging natural soils with a significant iron content, experime
ntal parameters can be identified which allow satisfactory images to b
e obtained. Magnetic resonance imaging may therefore provide important
information on soil structure and water movement in dual porosity soi
ls, with attendant benefits for the calibration of models of non-Darci
an flow in such soils.