Environmental Engineering Reference
In-Depth Information
Fig. 1
Physical model and schematic representation of the well and porous medium discretization
Momentum balance equation
f
m
v
m
ˁ
m
2
d
ti
g
c
dP
dz
=−
ˁ
m
g
cos
ʸ
+
ˁ
m
v
m
g
c
dv
m
dz
−
+
(2)
g
c
Energy balance equation
f
p
ˁ
p
u
p
+
v
p
2
g
c
J
c
Q
loss
∂
∂
t
3600
xA
ti
+
p
h
p
+
(3)
v
p
2
g
c
J
c
ˁ
p
v
sp
g
cos
ʸ
=−
∂
z
ˁ
p
v
sp
+
g
c
J
c
p
p
where the subscripts g,
l
and
m
represent gas, liquid and mixture, respectively,
P
is
pressure (which is the saturation pressure
P
sat
)
,
ˁ
is density,
v
s
is superficial velocity,
g
is the gravity acceleration,
is the local angle between the well and the vertical
direction,
g
c
is the gravitational conversion constant,
d
ti
is the inner diameter of the
tubing,
f
m
is friction factor,
v
is velocity,
Q
loss
is the fluid heat loss,
A
ti
is the inner
tubing area,
p
is the phase index (liquid or gas),
h
is enthalpy,
u
is internal energy,
f
is the gas volume fraction,
J
c
is the mechanical equivalent of heat (788 ft-lbf/Btu),
and 3,600 converts hours to seconds.
The heat losses, from the water-steam mixture to the porous medium, are dimin-
ished by thermal resistances due to the wall well, insulation, annulus, casing and the
cementing wall (see Fig.
1
), then we have that
ʸ
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