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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