Method for modelling the formation of a sedimentary area by simulating current-induced particle transport
A method for modelling the formation of a sedimentary area is disclosed, comprising: •—a setup step comprising defining a geological gridded model of the area comprising a plurality of cells, and setting a reference water level, •—a step of simulating the evolution of the model over a period of time, comprising: •a. assigning a water depth to each cell, •b. determining, for each cell, a direction and velocity of a water current, •c. introducing at least one particle in at least one cell of the model, •d. transporting each introduced particle in the model, based on the computed direction and velocity of the water current, comprising displacing the particle to a neighboring cell or depositing the particle in the cell, and the determination whether the particle is displaced or deposited depends on a particle granulometric class and the velocity of the water current applied to the particle, •e. updating the geological gridded model of the area according to the transport of each introduced particle.
1. A computer implemented method for modelling a formation of a sedimentary area, the method comprising:
a setup comprising defining a geological gridded model of the sedimentary area, said geological gridded model comprising a plurality of cells, and setting a reference water level, at least one supply process of particles to be introduced within the model, and at least one current to be modelled, and
simulating an evolution of the geological gridded model over a predetermined period of time T, comprising:
assigning a water depth to each cell of the geological gridded model,
determining, for each cell of the geological gridded model, a direction and velocity of a water current,
introducing at least one particle in at least one cell of the geological gridded model, and
transporting each introduced particle in the geological gridded model, based on the determined direction and velocity of the water current,
wherein the transport of a particle comprises displacing the particle to a neighboring cell of the model or depositing the particle in the cell, said transporting comprising determining if the particle is displaced or if it is deposited, depending on a particle granulometric class and the velocity of the water current applied to the particle, and
updating the geological gridded model of the area according to the transport of each introduced particle.
2. The method according to claim 1 , wherein updating the geological gridded model of the area comprises updating a height of each cell according to at least one of the amount of deposited particles, eustatism and subsidence.
3. The method according to claim 1 , wherein transporting each introduced particle is repeated until all introduced particles are deposited or have exited the geological gridded model.
4. The method according to claim 1 , wherein the at least one current to be modelled is chosen among a group consisting of:
a river mouth current,
a wind-induced current,
a tidal current, and
a surface ocean current, and
the determination of a direction and velocity of a water current comprises, for each cell:
determining a direction and energy of each modelled current, and
determining a direction and energy of a global water current resulting from a sum of each modelled current.
5. The method according to claim 1 , wherein each water current is decomposed into a plurality of sub-currents comprising at least:
a plume current, located at a water surface, and
a bottom current, located at a water bottom, and
wherein determining the velocity of the water current comprises determining a velocity of each sub-current into which the water current is decomposed.
6. The method according to claim 5 , wherein each particle is introduced at a depth determining a sub-current among the plurality of sub-currents applied to the particle.
7. The method according to claim 6 , wherein the introducing at least one particle and transporting each introduced particle comprise:
introducing at least one particle based on a clastic supply process,
transporting each particle introduced based on a clastic supply process,
introducing at least one particle based on a carbonates supply process, and
transporting each particle introduced based on a carbonates supply process.
8. The method according to claim 1 , wherein each supply process is chosen among at least one of:
clastic supply processes, comprising at least a river mouth supply and a mineral spring causing travertine deposition, and
carbonates supply processes, comprising at least in situ carbonates production and remobilization of in-situ carbonates.
9. The method according to claim 7 , wherein a depth at which the particle is introduced is determined based on a type of supply process of the particle.
10. The method according to claim 1 , wherein the transporting a particle comprises displacing at least one particle to a neighboring cell, and displacing a particle comprises:
determining an advective movement of the particle and displacing the particle according to the determined advective movement, and
determining a dispersive movement of the particle displaced according to the determined advective movement and displacing the particle according to the determined dispersive movement.
11. The method according to claim 1 , wherein the setup comprises setting a supply process of particles as in situ carbonates production, or comprises setting a water current to be modelled as a tidal current, and the simulating step is performed by iterating the assigning of the water depth, the determining of the direction and velocity of the water current, the introducing of at least one particle in at least one cell of the geological gridded model, and the transporting of each introduced particle in the geological gridded model a number N of times, each iteration allowing for simulating the evolution of the geological gridded model after a period of time of a duration T/N, and the number N of times being determined during the setup.
12. A non-transitory computer readable storage medium, having stored 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 to claim 1 .
13. A device for modelling the formation of a sedimentary area, the device comprising a processor configured to implement the method according to claim 1 .
14. A computer implemented method for modelling a formation of a sedimentary area, the method comprising:
a setup comprising defining a geological gridded model of the sedimentary area comprising a plurality of cells, and setting a reference water level, at least one supply process of particles to be introduced within the model, and a plurality of modelled individual water currents, and
simulating an evolution of the geological gridded model over a predetermined period of time, comprising:
assigning a water depth to each cell of the geological gridded model,
determining, for each cell of the geological gridded model, a direction and velocity of a water current,
wherein the determination of a direction and velocity of the water current comprises, for each cell, determining a direction and energy of each modelled individual water current, and determining a direction and energy of a global water current resulting from a sum of each modelled individual water current,
introducing at least one particle in at least one cell of the geological gridded model, transporting each introduced particle in the geological gridded model, based on the determined direction and velocity of the water current,
wherein the transport of a particle comprises displacing the particle to a neighboring cell of the model or depositing the particle in the cell, and the transporting step comprises determining if the particle is displaced or if it is deposited, depending on a particle granulometric class and the velocity of the water current applied to the particle, and
updating the geological gridded model of the area according to the transport of each introduced particle.
15. The method according to claim 14 , wherein the plurality of modelled individual water currents are chosen among a group consisting of:
a river mouth current,
a wind-induced current,
a tidal current, and
a surface ocean current.
16. A computer implemented method for modelling a formation of a sedimentary area, the method comprising:
a setup comprising defining a geological gridded model of the sedimentary area comprising a plurality of cells, and setting a reference water level, at least one supply process of particles to be introduced within the model, and at least one current to be modelled, and
simulating an evolution of the geological gridded model over a predetermined period of time, comprising:
assigning a water depth to each cell of the geological gridded model,
determining, for each cell of the geological gridded model, a direction and velocity of a water current,
introducing at least one particle in at least one cell of the geological gridded model, transporting each introduced particle in the geological gridded model, based on the determined direction and velocity of the water current,
wherein each water current is decomposed into a plurality of sub-currents comprising at least:
a plume current, located at water surface, and
a bottom current, located at water bottom,
wherein determining the velocity of the water current comprises determining a velocity of each sub-current into which the water current is decomposed,
wherein the transport of a particle comprises displacing the particle to a neighboring cell of the model or depositing the particle in the cell, and the transporting step comprises determining if the particle is displaced or if it is deposited, depending on a particle granulometric class and the velocity of the water current applied to the particle, and
updating the geological gridded model of the area according to the transport of each introduced particle.
17. The method according to claim 16 , wherein each particle is introduced at a depth determining a sub-current among the plurality of sub-currents applied to the particle.
18. A computer implemented method for modelling a formation of a sedimentary area, the method comprising:
a setup comprising defining a geological gridded model of the sedimentary area comprising a plurality of cells, and setting a reference water level, at least one supply process of particles to be introduced within the model, and at least one current to be modelled, and
simulating the evolution of the geological gridded model over a predetermined period of time, comprising:
assigning a water depth to each cell of the geological gridded model,
determining, for each cell of the geological gridded model, a direction and velocity of a water current,
introducing at least one particle in at least one cell of the geological gridded model,
transporting each introduced particle in the geological gridded model, based on the determined direction and velocity of the water current,
wherein the transport of a particle comprises displacing the particle to a neighboring cell of the model or depositing the particle in the cell, and the transporting step comprises determining if the particle is displaced or if it is deposited, depending on a particle granulometric class and the velocity of the water current applied to the particle,
wherein the transporting a particle comprises displacing at least one particle to a neighboring cell, and displacing a particle comprises:
determining an advective movement of the particle and displacing the particle according to the determined advective movement, and
determining a dispersive movement of the particle displaced according to the determined advective movement and displacing the particle according to the determined dispersive movement, and
updating the geological gridded model of the area according to the transport of each introduced particle.