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Kt
Sr
4
KK rs
Q
K
H
rK
where z f is the distance between the fracture and the bottom of the aquifer,
and H the aquifer thickness. K r , the permeability along the radial direction
parallel to the fracture, can be interpreted as the permeability increased by
the existence of the horizontal fracture. K z , the vertical permeability,
represents the matrix permeability, S s the specific storage coefficient, t the
time since the pumping started, r f the radius of the horizontal fracture, s the
drawdown and Q the pumping discharge rate.
Adjustment of observed drawdowns by Gringarten theoretical curves
(Fig. 3) leads to high value of H DG , suggesting a high permeability anisotropy.
Difference between observations and theoretical curve at short times is
attributed to well losses in the pumping well. Knowing the geometry of the
case (i.e. the thickness H of the aquifer), supposing the distance z f between
the bottom of the aquifer and the fracture equal to half H and using the
value determined by Maréchal et al. (2005) using Neuman method for S s
(9.7 × 10 -5 at IFP-9), the hydrodynamic properties of the aquifer are evaluated
(Table 2): K r the horizontal permeability, K z the vertical permeability and
the radius r f of the horizontal fracture. It is observed that the anisotropy of
the aquifer is shown in the pumping wells while estimated fracture radius
is coherent with field observations.
r
rzf
r
t DG =
, s DG =
and, H DG =
2
sf
f
z
Table 2: Permeability, anisotropy degree and radius of the horizontal fracture
determined at pumping wells using Gringarten method
Known parameters
Parameters determined by adjustment
z
H
K
K
Pumping
H
Fissure
z f
S s *
H DG
r f
K r
K z
f
r
()
()
Well
(m)
(m)
(1/m)
(-)
(m)
(m/s)
(m/s)
z
IFP-9
7.3
F9/1
4.0
0.55
9.7E-05
5
3.4
2.9E-05
5.2E-06
5.5
* S s is the average of specific storage coefficient determined for each site using
Neuman method at observation wells.
10
Observations
Gringarten model
H DG = 5
1
10
100
1000
Time (min)
Figure 3. Adjustment of drawdown in pumping well IFP-9 using
Gringarten theoretical curves.
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