AQUIFER_DATA
Defines an analytical aquifer, which can be modelled by either Carter-Tracy [CT+60]. or Fetkovich [Fet71]. The Carter-Tracy is the default model, which can be used to either describe a radial or linear aquifer.
AQUIFER_DATA must be followed by a name for the aquifer. For example:
AQUIFER_DATA A1
BACKFLOW
DEPTH 2550.0 m
THICKNESS 100 m
RADIUS 507.8 m
PERM 500 mD
COMPRESSIBILITY 2.0E-9 1/Pa
POROSITY 0.1
VISCOSITY 1 cP
CONN_D 1 1 1 9 1 1 X- 3.0
CONN_D 1 9 1 1 1 1 Y- 3.0
END
It is possible to connect the same aquifer to more grid blocks; connections can be added by multiple lines within the definition of one aquifer (see the multiple CONN_D lines above).
The options supported by AQUIFER_DATA are:
BACKFLOW
Specifies that fluids are allowed to migrate from the reservoir to the aquifer.
This option should be used with caution, as it can result in unwanted fluid re-circulations between grid blocks connected to the same aquifer. As a general rule an aquifer should be far away from the main injection/production regions. See example above for a reference on how to use it.
DEPTH
Specify aquifer depth. Units are required. See example above for a reference on how to use it.
ZAQUIFER
Specify aquifer elevation. For example if the aquifer depth is 2500 m, ZAQUIFER will be -2500 m. Units are required.
THETA_FRACTION, THETA
Specify the aquifer angle (for a radial aquifer). Defaulted to a THETA_FRACTION of 1.0.
THETA allows the same data to be added as an angle in degrees - .e.g. THETA 145.
So THETA_FRACTION = THETA/360.0.
See example below:
AQUIFER_DATA north
BACKFLOW
THETA 45
DEPTH 1225.0 m
THICKNESS 50 m
RADIUS 3000.0 m
PERM 300 mD
TEMPERATURE 53.0 C
COMPRESSIBILITY 2.0E-9 1/Pa
POROSITY 0.3
VISCOSITY 1 cP
CONN_D 1 20 20 20 4 13 Y+
END
THICKNESS
Aquifer thickness. Required. Units must be specified. See example above for a reference on how to use it.
WIDTH
Aquifer width, required for linear aquifer. Units must be specified. Example:
AQUIFER_DATA A1
BACKFLOW
DEPTH 2600.0 m
WIDTH 1500.0 m
THICKNESS 1500.0 m
PERM 10 mD
TEMPERATURE 75 C
COMPRESSIBILITY 2.0E-9 1/Pa
POROSITY 0.2
VISCOSITY 1 cP
CONN_D 1 30 1 30 10 10 Z+
END
RADIUS
Aquifer inner radius. Required for radial aquifer. Units must be specified. See example above for a reference on how to use it.
PORO, POROSITY
PORO or POROSITY defines the aquifer porosity. Required. See example above for a reference on how to use it.
PERM, PERMEABILITY
PERM or PERMEABILITY defines the aquifer permeability. Units must be specified. Required. See example above for a reference on how to use it.
VISC, VISCOSITY
VISC or VISCOSITY defines the aquifer viscosity. Units must be specified. Required. See example above for a reference on how to use it.
CMPR, COMPRESSIBILITY
CMPR or COMPRESSIBILITY defines the aquifer compressibility (rock + water): required. See example above for a reference on how to use it.
PINIT, PRESSURE
PINIT or PRESSURE defines the aquifer pressure. Pressure units must be specified. Not required, if not entered the aquifer pressure will be set in equilibrium with reservoir.
See example below:
AQUIFER_DATA north
BACKFLOW
DEPTH 1225.0 m
THICKNESS 50 m
RADIUS 3000.0 m
PERM 300 mD
PINIT 125 Bar
TEMPERATURE 53.0 C
COMPRESSIBILITY 2.0E-9 1/Pa
POROSITY 0.3
VISCOSITY 1 cP
CONN_D 1 20 20 20 4 13 Y+
END
TINIT, TEMPERATURE
TINIT or TEMPERATURE defines the aquifer temperature. Temperature units must be specified.
Required for thermal runs.
For an example including TINIT, see above.
GAS_IN_LIQUID_MOLE_FRACTION
Gas in liquid mole fraction in brine. Defaults to 0.0. Only used in GW mode. Example:
AQUIFER_DATA A1
BACK
FET
PV 10000000 m^3
PI 1000 m^3/d/bar
DEPTH 2560.32 m
COMPRESSIBILITY 1.0E-9 1/Pa
GAS_IN_LIQUID_MOLE_FRACTION 0.5D-3
CONN_D 1 1 1 1 1 1 X-
CONN_D 1 1 1 1 2 2 X- 3.0
END
IFT
Influence function table. Not required. If omitted, defaults to infinite aquifer.
Example:
IFT
0.01 0.112
0.05 0.229
0.10 0.315
0.15 0.376
0.20 0.424
0.25 0.469
0.30 0.503
0.40 0.564
0.50 0.616
0.60 0.659
0.70 0.702
0.80 0.735
0.90 0.772
1.00 0.802
1.50 0.927
2.0 1.020
2.5 1.101
3.0 1.169
4.0 1.275
5.0 1.362
6.0 1.436
7.0 1.500
8.0 1.556
9.0 1.604
10.0 1.651
15.0 1.829
20.0 1.960
25.0 2.067
30.0 2.147
40.0 2.282
50.0 2.388
60.0 2.476
70.0 2.550
80.0 2.615
90.0 2.672
100.0 2.723
150.0 2.921
200.0 3.064
250.0 3.173
300.0 3.263
400.0 3.406
500.0 3.516
600.0 3.608
700.0 3.684
800.0 3.750
900.0 3.809
1000.0 3.860
END IFT
CONN_D
Specifies blocks of connections to attach aquifer to reservoir cell faces. Follows the ECLIPSE grdecl convention (K index is counted downwards from the top layer).
See example above.
An example is:
CONN_D 1 9 9 9 1 1 Y+ 3.0
Note that the connection box argument order is:
CONN_D IL IU JL JU KL KU CMF
Where:
IL and IU are a range of cell indices in the I-direction
JL and JU are a range of cell indices in the J-direction
KL and KU are a range of cell indices in the K-direction
CMF: connection multiplier factor (optional)
Connections will be made to cells with I-indices such that \(I \geq IL\) and \(I \leq IU\), etc.
The cell faces to attach the aquifer are specified by one of the following options:
X+ or I+, faces connecting cells with I-indices to cells with (I+1)-indices
Y+ or J+, faces connecting cells with J-indices to cells with (J+1)-indices
Z+ or K+, faces connecting cells with K-indices to cells with (K+1)-indices
The pairs (X- or I-), (Y- or I-) and (Z- or K-) follow the same logic, and are used to connect to cells with (I-1)-indices, (J-1)-indices and (K-1)-indices.
A number of CONN_D sub-keywords may be entered to build up the full connection. If the same face of the same cell is included more than once, only one connection will be generated.
CONN_Z
Warning: keyword to be used only by proficient Cirrus users. Unless there is some specific reason, consider using CONN_D instead.
Specifies blocks of connections to attach aquifer to reservoir cell faces.
CONN_Z use the convention that the K index is counted upwards from the bottom layer. For example:
CONN_Z 1 9 9 9 1 1 Y+ 3.0
Note that the connection box argument order is:
CONN_Z IL IU JL JU KL KU CMF
Where:
IL and IU are a range of cell indices in the I-direction
JL and JU are a range of cell indices in the J-direction
KL and KU are a range of cell indices in the K-direction
CMF: connection multiplier factor (optional)
Connections will be made to cells with I-indices such that \(I \geq IL\) and \(I \leq IU\), etc.
The cell faces to attach the aquifer are specified by one of the following options:
X+ or I+, faces connecting cells with I-indices to cells with (I+1)-indices (GRDECL grid format).
Y+ or J+, faces connecting cells with J-indices to cells with (J+1)-indices (GRDECL grid format).
Z+ or K+, faces connecting cells with K-indices to cells with (K+1)-indices (K index counted upwards from the bottom layer).
The pairs (X- or I-), (Y- or I-) and (Z- or K-) follow the same logic, and are used to connect to cells with (I-1)-indices, (J-1)-indices and (K-1)-indices.
When using CONN_Z, the top faces of a reservoir with 100 layers are defined with Z+. See the following example:
CONN_Z 1 50 1 50 100 100 Z+
FET
Selects a Fetkovich analytical aquifer [Fet71], instead of the Carter-Tracy, which is the default model otherwise. A FET aquifer requires the user to specify the aquifer pore volume (PV), and the aquifer productivity index (PI), both referring to surface volumes. See example below:
AQUIFER_DATA AQ1
BACK
FET
PV 10000000 m^3
PI 1000 m^3/d/bar
DEPTH 2500 m
COMPRESSIBILITY 1.0E-4 1/Bar
CONN_D 1 20 1 10 1 20 X-
END
Note that the aquifer porosity, permeability, viscosity, internal radius/thickness and angle (theta) are not required.
PV
Specifies the aquifer pore volume at surface conditions, required only by the Fetkovich aquifer (see FET for an example).
PI
Specifies the aquifer productivity index in terms of surface volumes. This is required only by the Fetkovich aquifer (see FET for an example).
AQCON_AREA/AQCON_AREA_PERM
These are options for controlling the manner in which the total aquifer-resevoir flow is divided between all the cells connected to the aquifer.
If AQCON_AREA is used the flow is divided on the basis of the area of the cell face connected to the aquifer
If AQCON_AREA_PERM is used the flow is divided on the basis of the product of the area of the cell face and the permeability of the the cell in the direction of the face.
The default is AQCON_AREA.
These keywords have no arguments.
Note that these two keywords can be used in both the AQUIFER_DATA and AQNUM_DATA blocks.
See example below:
AQUIFER_DATA north
BACKFLOW
AQCON_AREA_PERM
DEPTH 1225.0 m
THICKNESS 50 m
RADIUS 3000.0 m
PERM 300 mD
TEMPERATURE 53.0 C
COMPRESSIBILITY 2.0E-9 1/Pa
POROSITY 0.3
VISCOSITY 1 cP
CONN_D 1 20 20 20 4 13 Y+
END
ALLOW_ACTIVE_NEIGHBOUR
Alias: ALLOW_ACTIVE_NEIGHBOR.
The default rule for creating aquifer connections matches Eclipse, but is different from Intersect ©, which allows connections to cell faces which have an active neighbour on that face.
When this keyword is used, a connection is made to the specified face irrespective of whether it has an active neighbour on that face. This matches the Intersect © methodolgy.
(Intersect © of the Schlumberger Corporation).
Examples of the use of this keyword may be found in the repository in the folder:
cirrus_1.9/regression_tests/towg/bo/
aquifer_linear_ac_allow.in:
AQUIFER_DATA A1
DEPTH 2550.0 m
THICKNESS 100 m
WIDTH 100 m
PERM 500 mD
COMPRESSIBILITY 2.0E-9 1/Pa
POROSITY 0.2
VISCOSITY 1 cP
CONN_D 19 19 1 1 1 1 X+
ALLOW_ACTIVE_NEIGHBOUR
END
And in acnum_ac__allow.in:
AQNUM_DATA A1
RPV 200000000 m^3
RPI 2.13175 m^3/d/bar
CONN_D 9 9 1 1 1 1 X+
VISC 2 cp
REP_CELL_D 12 1 1
ALLOW_ACTIVE_NEIGHBOUR
END