Preferential flow has been increasingly recognised as a major component of
water movement in many soils, particularly clays. This paper reviews proble
ms in the measurement of solute fluxes in these soils, and discusses the so
lutions that have been adopted in UK studies of cracking clay soils. The es
timation of solute fluxes is subject to many sources of error, which are be
st reduced by replicated measurements, such as those available in multi-plo
t experiments.