METHOD FOR DETERMINING THE GEOMETRY OF AN AREA OF A RESERVOIR

1 . A computer implemented method for determining a geometry of an investigated area of a reservoir, wherein a volume (V) of the investigated area is known, the method comprising:

receiving a geological model of the soil in which said area is located, the geological model comprising a plurality of adjacent cells each having respective spatial coordinates and respective permeability values, and two wells being simulated in said geological model;

determining a preferred flowing path between the two wells, the preferred flowing path being formed by a series of adjacent cells of the model, and determined based on the respective permeability values of the cells;

evaluating a volume (V p ) of the preferred flowing path; and

if the volume (V p ) of the preferred flowing path is lower than the volume (V) of the investigated area, updating the preferred flowing path until its volume (V p ) is superior or equal to the volume (V) of the investigated area.

2 . A computer implemented method according to claim 1 , wherein the updating of the preferred flowing path comprises adding to the current flowing path at least one cell, each added cell being adjacent to at least one cell of the current flowing path and having a permeability value suitable for increasing the permeability of the current flowing path.

3 . A computer implemented method according to claim 1 , wherein the preferred flowing path is determined by implementing a fast-marching algorithm.

4 . The computer implemented method according to claim 3 , wherein the fast-marching algorithm is configured to maximize the permeability (K p ) of the preferred flowing path.

5 . The computer implemented method according to claim 1 , wherein said method is performed after a well testing preliminary phase during which the volume (V) of the investigated area and an equivalent permeability (K eq ) between two wells drilled in the reservoir are determined, and wherein the two wells of the geological model correspond to said two wells of the well testing preliminary phase.

6 . The computer implemented method according to claim 5 , further comprising a step of defining a search zone of the geological model, comprising:

delimiting a three-dimensional zone in the geological model such that said zone has a volume corresponding to that of the investigated area and the two wells of the geological model are contained within said zone;

establishing two planes within the geological model, each plane extending vertically and orthogonally to a segment linking the two wells; and

defining the search zone as the part of the three dimensional zone contained within the planes,

wherein the search zone defines the cells that may be included in the preferred flowing path.

7 . The computer implemented method according to claim 1 , further comprising, if the volume (V p ) of the preferred flowing path is superior or equal to the volume of the investigated area (V), computing the permeability of the preferred flowing path (K r ) and comparing said permeability to an equivalent permeability (K eq ) between the wells.

8 . The computer implemented method according to claim 7 , wherein each cell of the geological model further comprises at least one local mineralogical composition parameter, and the method further comprises, if the permeability (K r ) of the preferred flowing path is different from the equivalent permeability (K eq ) between the two wells, steps of:

simulating a stochastic movement of a particle in the geological model, said particle having coordinates in said model and having an aggressiveness parameter;

modifying the local mineralogical composition parameter while taking into account at least:

the coordinates of the particle in said model,

the aggressiveness of the particle, and

the local mineralogical composition parameter;

modifying the aggressiveness of the particle while taking into account at least the modification of the local mineralogical composition, and

computing an updated permeability (K p ) of the preferred flowing path taking into account the modification of the local mineralogical composition, and

comparing the updated permeability (K r ) of the preferred flowing path to the equivalent permeability (K eq ).

9 . The computer implemented method according to claim 8 , further comprising a step of terminating the method if the updated permeability reaches the equivalent permeability.

10 . The computer implemented method according to claim 8 , further comprising a step of detecting an error in the geological model if the updated permeability of the preferred flowing path becomes more remote from the equivalent permeability than the initial permeability of the preferred flowing path.

11 . A computer program product, comprising a set of instructions adapted to implement the method according to claim 1 , when it is executed by a processor.

12 . A non-transitory computer readable storage medium, having thereon a computer program comprising program instructions, the computer program being loadable into a processor and adapted to cause the processor to carry out, when the computer program is run by the processor, the method according claim 1 .

13 . A device for determining the geometry of a reservoir, the device comprising a processor configured for implementing the method according to claim 1 .

14 . A reservoir characterization method, comprising:

performing a well test during which a volume of an investigated area of the reservoir and an equivalent permeability between two wells drilled in the reservoir are determined; and

performing the method according to claim 1 .

15 . A reservoir characterization method according to claim 14 , wherein the well test comprises:

causing a pressure disturbance at a first one of the wells drilled in the reservoir;

measuring a radius of investigation; and

inferring from said radius of investigation a volume of the investigated area.

16 . A reservoir characterization method according to claim 15 , wherein the well test further comprises:

measuring at the second of the wells drilled in the reservoir a pressure variation in response to the pressure disturbance; and

inferring from said pressure variation an equivalent permeability value between the two wells.