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soil between the lower depth of a mobile NAPLand groundwater,
it may also be reasonable to account for potential NAPL redis-
tribution in the unsaturated soil layer. This redistribution would
decrease the concentrations of mobile NAPL to concentrations
in soil equivalent. to S
r
. After this redistribution, an acceptable
distance between the deepest expected NAPL penetration and
the historical top boundary of the water table capillary fringe
must still remain.
These screening values, as already discussed, are intended for
use in estimating conservative limits of NAPL mobility. The
data of Table 2 may be used for other purposes, such as relating
a known released volume of NAPL to an equivalent soil volume
at the residual concentration level. While it is not the purpose of
this paper to detail this type of calculation, the variability of an
estimated residual concentration level, as illustrated in Figure 3,
clearly needed to be considered.
SUMMARY AND CONCLUSIONS
Screening values describing residual saturation of NAPLs in
unconsolidated vadose zone soils have been tabulated. These
values are proposed for use in estimating concentrations of
immobile NAPL in soil. The values, in Tables 3 and 4, are based
on measured, published values for residual NAPL concentra-
tions in soil, C
res,soil
, in the unsaturated soil zone.
Another value, the soil saturation limit, C
sat,soil
, has already found
use as a screening level for NAPL mobility. C
sat,soil
is a calculat-
ed value estimating the presence of a residual NAPL. Data in
this paper shows C
sat,soil
, is a factor up to 50,000 times less than
the residual NAPL concentration in soil, C
res,soil
. For screening
immobile NAPL concentrations the soil saturation limit is
exceptionally conservative. We would instead recommend use
of the values in Tables 3 and 4.
A complete site assessment, in addition, would also include
evaluation of other potential transport mechanisms, including
soluble dissolution into mobile soil pore water, and volatiliza-
tion into soil pore air. These transport mechanisms, as noted
previously, are discussed elsewhere.
Use of residual NAPL concentration in soil values for screening
immobile NAPL presumes homogenous soils and soil properties.
Consolidated soil matrices, macropores, and fractures will
greatly affect the flow and movement of NAPL and must be
recognized when these screening values are applied. Further, we
note that the values have been developed using a limited data
set, from multiple authors, and no attempt has been made to
judge bias or error in the individual measurement techniques.
ACKNOWLEDGEMENT
Support for preparing this document from American Petroleum
and GRI (formerly the Gas Research Instutite) under GRI
Contract No. 5097-210-3874 is gratefully acknowledged.
REFERENCES
API, 1996. A guide to the Assessment and Remediation of
Underground Petroleum Releases, American Petroleum
Institute, Publication No. 1628, third edition, Washington,
D.C., July 1996.