Accurate monitoring of flow instabilities, which can occur when nonaqu
eous phase liquids (NAPLs) flow through porous media, is an important
component of predicting the transport and fate of these compounds in t
he subsurface. In particular, flow situations in which three mobile ph
ases (such as water, NAPL, and air) exist in the porous media are inhe
rently complex. Unfortunately, the relatively low source intensities a
nd the nontunable source energies make traditional dual gamma techniqu
es unsuitable to study flow instabilities which can change within seco
nds, We present an alternate technique, which uses synchrotron X rays
from the Cornell High Energy Synchrotron Source (CHESS) to measure thr
ee-phase fluid saturations on the time scale of seconds. Using the har
monic content resulting from X ray diffraction, we obtained a high-int
ensity X ray beam consisting of distinct tunable energies. Three-phase
saturations were measured on 5-s timescales during fingering of light
NAPL into regions of dry and water wet sandy soil. In the water wet s
oil the oil finger was less saturated, slower, and wider than the same
finger in the dry soil. The results yield insights into the nature of
three-phase preferential flow.