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are high viscosity products and may have residual saturation points many times higher than
gasoline. Finer soil textures (such as silt) exhibit higher residual saturation points than coarser
textures (such as sand).
The compiled data from Brost and DeVaull indicate that residual saturation concentrations for
"middle distillates" (i.e., No. 2 fuel oil and diesel) ranged from 2,300-23,000 mg/kg as soil texture
ranged from coarse gravel to silt (data from Fussell et al.). API (1980) reports a value for
residual saturation diesel in "soil" as 34,000 (moisture content unknown). Sand was selected
by the NJDEP as a reasonably conservative soil texture for determination of a default upper limit
concentration for No. 2 fuel oil and diesel based on the residual saturation point. The results of
Fussell et al. indicate that the residual saturation point for "medium sand" ranged from of 8,000-
13,000 mg/kg. The soil moisture in these measurements was approximately 0.04 (v/v), which
is in between median values for the wilt point (~0.02) and the field capacity (~0.06) for
subsurface sand (Carsel et al., 1988). Since infiltrating petroleum would likely displace some of
the soil moisture being held at field capacity, this soil moisture content was felt to be
appropriate. As is discussed in Brost and DeVaull, the residual saturation concentrations from
the study of Fussell et al. tend to be lower than those from other studies. This is illustrated by
comparing the range of residual saturation points of gasoline in medium sand by Fussell et al.
(3,000-6,000 mg/kg), with a range of 20,000-44,000 mg/kg reported for medium sand under
similar moisture contents (Hoag and Marley, 1986). Thus, the residual saturation points of
Fussell et al. appear to be conservative relative to other studies. Based on this assessment,
Brost and DeVaull recommend a residual saturation concentration of 8,000 mg/kg for medium
sand soil and middle distillates (i.e., diesel and No. 2 fuel oil). The NJDEP concurs that this
value appears reasonable as a generic concentration to use as an upper limit for these fuel types
in order to prevent the occurrence of mobile free product.
Using a similar analysis for "fuel oils" (i.e., fuel oils heavier than diesel and No. 2 fuel oil), the
compiled data from Brost and DeVaull indicate that residual saturation concentrations for
heavier fuel oil ranged from 5,000-51,000 mg/kg as soil texture ranged from coarse gravel to silt
(data from Fussell et al.). API (1980) reports a value for residual saturation fuel oil and
lubricating oil in "soil" as 53,000 (moisture content unknown). Again, looking at the results for
medium sand from Fussell et al., where soil moistures were judged to be appropriate, the
residual saturation point was estimated to be in the range of 17,000 to 30,000 mg/kg, and the
recommended value for residual saturation for fuel oils heavier than diesel is 17,000 mg/kg.
The NJDEP concurs with this assessment.
Data for lubricating oils other than mineral oil, as reported in Brost and DeVaull, is scarce.
Furthermore, many of the reported results either do not include soil moisture contents or were
inappropriately run on dry soil. For this reason, Brost and DeVaull do not recommend a residual
saturation concentration for lubricating oils. However, review of the Brost and DeVaull report
yields residual saturation values for mineral oil in glacial till and alluvium with water contents of
0.02 and 0.03, respectively. The reported residual saturation values are 11,000-19,000 mg/kg
for glacial till and 61,000 mg/kg for alluvium. Both of these materials may vary widely in soil
texture, but glacial till is more likely to be similar to sandy soils than alluvial material. Given that
the residual saturation value selected for heavier fuel oils lies within the range reported for
mineral oil in glacial till, it is judged by the NJDEP that the value of 17,000 mg/kg used for
heavier fuel oil is also adequately protective for lubricating oils.