Pm. Jardine et al., UNSATURATED TRANSPORT PROCESSES IN UNDISTURBED HETEROGENEOUS POROUS-MEDIA .1. INORGANIC CONTAMINANTS, Soil Science Society of America journal, 57(4), 1993, pp. 945-953
Prolonged disposal of organic and inorganic waste in shallow land buri
al sites throughout the USA has prompted detailed investigations of su
bsurface contaminant transport processes. The fate and transport of co
ntaminant leakage from pits, trenches, and cribs into the vadose zone
via storm events is not well understood. The objective of this study w
as to investigate the thermodynamic and kinetic processes controlling
the transport of inorganic contaminants in unsaturated, heterogeneous
subsurface media. Large undisturbed columns were isolated from a propo
sed waste site consisting of fractured saprolite (weathered interbedde
d shale and limestone), and steady-state nonreactive and reactive solu
te transport experiments were performed at a variety of pressure heads
. Observed breakthrough curves (BTC) for binary and ternary mixtures i
n the Co-Sr-Ca system were delayed relative to nonreactive Br BTC, ind
icating that the former tracers were adsorbed by the solid phase. Tran
sport of the binary mixtures Co-Ca and Sr-Ca was predicted reasonably
well with the equilibrium convective-dispersive (CD) equation using in
dependent measurements of all model parameters. However, application o
f the nonequilibrium or kinetic CD model to the observed Sr and Co bin
ary data resulted in an improved description of contaminant transport.
Cation-exchange equilibria relationships on homogenized subsurface ma
terial, using both shake batch and miscible displacement methods, adeq
uately described the thermodynamic processes that were prevalent durin
g contaminant transport. These results suggest that preferential trans
port of reactive contaminants is negligible for the unsaturated condit
ions used in this study, and that the structured saprolite within the
subsurface media is a chemically active constituent during reactive so
lute transport. Although the transport of contaminants in the ternary
Co-Sr-Ca system tem exhibited many of the same features as the binary
transport studies, an attempt to simulate the transport of contaminant
s in the ternary system as independent species was less than adequate.