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TABLE
4-VII
Estimated volume of increased permeability for nuclear explosions in reservoir rock (After Coffer et al.,
1964;
courtesy of USAEC)
Yield (in Kt) at Cavity
Depth of Height
of
Volume of gross
scaled depth
of
radius
burial permeable permeability
burial (ft) (ft)
(ft) zone
increase
(ft) (acre-ft)
Kt
ft
10
800
450
100
800
450
500
800
450
1000
800
450
96
110
167
196
252
290
299
346
1720
970
3720
2100
6350
3600
8000
4500
540
620
940
1110
1420
1640
1690
1950
2.1
x
lo3
3.2
x
lo3
1.1
x
104
1.8
x
104
3.8
x
lo4
5.9
x
104
6.4~10~
1.0~10~
fracture system, the hydraulic fracturing techniques appear to be more advanta-
geous than the nuclear mass rubbling process.
Furthermore, in areas where the effectiveness of hydraulic fracturing has been
well established, nuclear fracturing cannot compete because of its high cost.
Guidelines for reservoir characteristics desired in the case of nuclear fracturing
include low reservoir permeability, massive zones bounded by thick impermeable
formations, gas-bearing reservoirs, and low-viscosity oil deposits.
Basically, a nuclear detonation in a wellbore creates a cavity resulting from the
vaporization of the rock and its saturating fluids. Fracture system radiates from this
cavity into the formation. Rock collapse into the cavity forms a chimney-rubble
zone, with most of the molten material and radioactive fission products con-
centrated in the bottom of these zones (Atkinson,
1964).
A schematic presentation
of
a typical post-shot environment resulting from a contained underground nuclear
explosion is illustrated in Fig.
4-59.
Studies of several contained underground nuclear explosions showed that the
nuclear devices have yielded a rather consistent model
of
the geometric features.
Mathematical relationshps have been developed for calculating specific characteris-
tics of the post-shot geometry as a function
of
the yield of the nuclear device, depth
of burial, and type
of
formation (Boardman et al.,
1964;
Bray et al.,
1965).
Table
4-VII
shows
(1)
the variation in cavity radius,
(2)
the volume of rock (in
acre-feet) in which there is a drastic permeability increase, and
(3)
height of the
created permeable zone as a function of yield at the depth of burial of
450
and
800
ft. Although these data are only qualitative, they do show how these parameters are
expected to vary.
For detailed treatment of fracturing, the reader
is
referred to the classical work of
Howard and Fast
(1970)
and excellent treatment of the subject by Craft et al.
(1962)
and Halliburton Company
(1976).