METAL FLUX IN NEAR SHORE CAPPING SITES UNDER CONDITIONS
OF SUBMARINE GROUNDWATER DISCHARGE
Individuals
-
Timothy E. Ford, Ph.D. Research Interests:
transport and transformations of contaminants in aquatic
systems, survival of pathogens in the environment, biofilms
in water distribution systems.
-
James P. Shine, Ph.D. Assistant Professor
of Environmental Chemistry, Harvard School of Public Health.
Research Interests: Fate of contaminants in aquatic environments,
metal speciation and bioavailability.
-
Raveendra V. Ika, Research Specialist,
Harvard School of Public Health.
-
Chunhua Liu, Ph.D., Harvard School of
Public Health.
Objective
Theoretical simulations suggest that capping
is very efficient in preventing contaminant transport to the
overlying water. For example, published calculations based
on molecular diffusion alone suggest that it would take more
than 900 years for trichlorophenol to break through a 45 cm
cap. However, there have been few detailed investigations
of capping efficiency under conditions of advective flux,
with past research focusing on diffusive fluxes. This study
is designed to investigate the efficiency of capping under
conditions of both advective and diffusive fluxes. Advective
fluxes are a function of submarine groundwater discharge (SGD),
tidal effects and changing chemistries from interactions of
groundwater, pore water and seawater.
|
Approach and Preliminary Findings
|
In laboratory studies, we have shown that over a six month
period no metal (Ag, Cd, Cr, Cu, Ni, Mo, Pb, Zn) transport occurs
into capping material in simulator cells under undisturbed conditions.
Hence, it is reasonable to assume that sedimentation rates in
depositional areas may be sufficient to prevent contaminant
breakthrough by molecular diffusion. In order to evaluate advective
transport of metals through capping material, we have established
a series of capping simulator cells with different groundwater
chemistries and flow rates. Our data suggested that advective
transport of sediment pore water may potentially lead to a very
high flux of metals to the overlying water after capping. The
time to reach this breakthrough depended on the depth of capping,
property of capping material and flow rate of SGD. When coming
to the steady-state stage, advective transport of metals is
highly significant under conditions of SGD compared with diffusion
process. Results also suggested that sorption capacity of metals
by capping material sand may be very small. In general, results
from first set of lab experiment suggest that SGD may significantly
effect capping efficiency and, therefore, greater emphasis on
groundwater hydrology is critical before selection of near-shore
capping sites for disposal of contaminated sediment. The second
set of lab experiment was conducted to study mechanism of metal
transport under conditions of SGD and influence of metal transport
by different factors such as depth of sediment, SGD flow rate,
acidity of SGD, and Dissolved Oxygen (DO) in SGD. A mathematical
model was set up to model metal transport through capping material
under conditions of SGD considering physi-chemistry, hydrology
factors.
|
|