Magnetic resonance imaging (MRI) allows non-destructive and non-invasi
ve measurement and visualisation of both static and dynamic water phen
omena. Flow and transport processes can either be measured by followin
g the local intensity in time-controlled sequential images, by mapping
the effect of contrast agents or labelled molecules, or by mapping th
e (proton) displacement in a well known time interval directly. By a p
roper choice of methods, a time window ranging from milliseconds to we
eks (or even longer) can be covered. Combining transport measurements
with relaxation time information allows the discrimination of transpor
t processes in different environments or of different fluids, even wit
hin a single picture element within an image. Here we present an overv
iew of the principles of NMR imaging techniques to visualise and unrav
el complex, heterogeneous transport processes in porous systems. Appli
cations and limitations will be discussed, based on results obtained i
n model and artificial soil systems. (C) 1997 Elsevier Science B.V.