Environmental Engineering Reference
In-Depth Information
Surface change
Net negative
Matrix grain
Bound layer
HC
HC
HC
Pore Throat
Electro-Osmotic
HC
HC
HC
HC
HC
HC
Matrix grain
EXPLANATION
H 2 O molecule
Hydrocarbon
Cl -
Bound layer
Na +
Figure 3.14 Pore throat schematic showing electrokinetic transport of the outer
Helmholtz layer, modifying the effective pore throat size for fluid flow (after Hill, 1999)
1997,1997, Tchillingarian, 1952) showed up to forty-fold volumetric
fluid flow increases in cores containing clays, compared to only 2 - 3 fold
increases in pure silica cores, as shown in figure 3.15. Chilingar, et. al. (1970)
speculated that this latter (silica core) fluid flow might be due to a thermal
effect. Mitchell (1993) maintained that all silica minerals show increased
flow, under DC fields, but that those with high cation exchange capacity
(CEC) exhibit the greatest flow increases. The results in figure 3.15 agree
with Mitchell's (1993) argument.
For those pore throats completely filled with the Helmholtz double layer,
the application of current will develop salinity gradients across the cation
selective membranes, which will store energy. Any fluctuation in the local
electric fields will result in discharge of this stored energy, similar to dis-
charging a super capacitor (Conway, 1999), potentially inducing a break-
down of complex hydrocarbon molecules, resulting in simpler daughter
product molecules.
3.9
DCEOR Field Operations
Figure 3.16 illustrates one possible DCEOR field implementation, where
anode(s) are placed near the ground surface and cathode(s) are placed
in, or near, producing well(s). An alternative configuration utilizes both
 
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