Method for exploiting a hydrocarbon deposit by history matching of production as a function of diagenesis

US10794155B2 · US · B2

Patent metadata
FieldValue
Publication numberUS-10794155-B2
Application numberUS-201715826459-A
CountryUS
Kind codeB2
Filing dateNov 29, 2017
Priority dateNov 29, 2016
Publication dateOct 6, 2020
Grant dateOct 6, 2020

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  1. Title

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  5. First independent claim

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Abstract

Official abstract text for this publication.

The invention is a method for exploiting a subterranean formation including hydrocarbons with at least one lithologic facies of the formation having undergone at least one diagenetic phase over geological times. From at least one sample of rock obtained from the formation, from measured production data relating to the formation and from a meshed representation representative of the formation, each mesh of the meshed representation is determined including at least one indicator relating to the distribution of the facies present in the mesh. The method comprises a step of history matching in which at least one of the adjustment parameters is the diagenetic state of the identified facies.

First claim

Opening claim text (preview).

The invention claimed is: 1. A method for exploiting a subterranean formation including hydrocarbons, the formation including at least one facies which has undergone at least one diagenetic phase over geological time, from at least one sample of rock obtained from the formation, from measured production data relating to the formation and from a meshed representation representative of the formation with the meshed representation having been formed by meshes, each of the meshes of the meshed representation including at least one indicator relating to distribution of the at least one facies present in the mesh, comprising steps of: A. determining from at least measurements performed on the at least one sample of rock, for at least one of the facies of the formation and for each of the meshes of the meshed representation, a value of at least one parameter of a diagenetic state of the at least one facies of the formation; and B. updating at least values of the parameters of the diagenetic state of at least one of the facies of the formation from the measured production data, for at least one mesh of the meshes of the meshed representation, according to the following steps: i. determining at least one petrophysical property relating to flow in the formation for each of the meshes of the meshed representation, from the values of the parameters of the diagenetic state of the at least one facies of the formation; ii. using a flow simulator and the meshed representation filled with petrophysical properties relating to the flow to simulate production data relating to production of the formation; iii. determining an objective function measuring at least one difference between the measured production data and the simulated production data; and iv. modifying at least the value of the parameters of the diagenetic state of the at least one facies of the formation from the objective function for at least one of the meshes of the meshed representation; and reiterating steps i) to iv) until a predetermined stop criterion is reached; and determining a scheme for exploiting the hydrocarbons of the formation and exploiting the hydrocarbons of the formation with at least the determined scheme for exploiting the hydrocarbons of the formation. 2. The method as claimed in claim 1 , wherein the at least one parameter representative of the diagenetic state of the at least one facies of the formation corresponds to a spatial variability of at least one diagenetic degree of at least one of the diagenetic phases undergone by the facies. 3. The method as claimed in claim 2 , wherein in step B), at least one parameter representative of at least one of a distribution of the facies in the formation and petrophysical properties relating to flow in the formation are also updated. 4. The method as claimed in claim 3 , wherein step B), ii) is performed by a bi-plurigaussian simulation. 5. The method as claimed in claim 2 , wherein step B), ii) is performed by a bi-plurigaussian simulation. 6. The method as claimed claim 2 , in wherein the predetermined stop criterion corresponds to a minimum of the objective function, to a maximum number of iterations of step B), or to a maximum difference between the measured production data and the simulated production data. 7. The method as claimed in claim 2 , wherein the spatial variability is parameterized by a range of a variogram relating to a distribution of the at least one diagenetic degree of the at least one diagenetic phase. 8. The method as claimed in claim 7 , wherein in step B), at least one parameter representative of at least one of a distribution of the facies in the formation and petrophysical properties relating to flow in the formation are also updated. 9. The method as claimed in claim 7 , wherein step B), ii) is performed by a bi-plurigaussian simulation. 10. The method as claimed in claim 7 , wherein the predetermined stop criterion corresponds to a minimum of the objective function, to a maximum number of iterations of step B), or to a maximum difference between the measured production data and the simulated production data. 11. The method as claimed in claim 1 , wherein the at least one parameter representative of the diagenetic state of the at least one facies of the formation corresponds to a proportion of at least one diagenetic degree of at least one of the diagenetic phases undergone by the facies. 12. The method as claimed in claim 11 , wherein the at least one parameter corresponds to a proportion of at least one of the diagenetic degrees in proportion to other diagenetic degrees which remain constant. 13. The method as claimed in claim 11 , wherein in step B), at least one parameter representative of at least one of a distribution of the facies in the formation and petrophysical properties relating to flow in the formation are also updated. 14. The method as claimed in claim 11 , wherein step B), ii) is performed by a bi-plurigaussian simulation. 15. The method as claimed in claim 11 , wherein the predetermined stop criterion corresponds to a minimum of the objective function, to a maximum number of iterations of step B), or to a maximum difference between the measured production data and the simulated production data. 16. The method as claimed in claim 12 , wherein in step B), at least one parameter representative of at least one of a distribution of the facies in the formation and petrophysical properties relating to flow in the formation are also updated. 17. The method as claimed in claim 12 , wherein step B), ii) is performed by a bi-plurigaussian simulation. 18. The method as claimed in claim 12 , wherein the predetermined stop criterion corresponds to a minimum of the objective function, to a maximum number of iterations of step B), or to a maximum difference between the measured production data and the simulated production data. 19. The method as claimed in claim 1 , wherein in step B), at least one parameter representative of at least one of a distribution of the facies in the formation and petrophysical properties relating to flow in the formation are also updated. 20. The method as claimed in claim 19 , wherein the predetermined stop criterion corresponds to a minimum of the objective function, to a maximum number of iterations of step B), or to a maximum difference between the measured production data and the simulated production data. 21. The method as claimed in claim 1 , wherein step B), ii) is performed by a bi-plurigaussian simulation. 22. The method as claimed in claim 21 , wherein the predetermined stop criterion corresponds to a minimum of the objective function, to a maximum number of iterations of step B), or to a maximum difference between the measured production data and the simulated production data. 23. The method as claimed in claim 1 , wherein the predetermined stop criterion corresponds to a minimum of the objective function, a maximum number of iterations of step B), and a maximum difference between the measured production data and the simulated production data. 24. The method as claimed in claim 1 , wherein the determination of the exploitation scheme comprises determination of a position and at least one geometry of injection and production wells, and a determination of a type of assisted recovery. 25. A computer program product which is downloadable from a communication network and stored on a non-transitory storage medium for execution by a processor, comprisi

Assignees

Inventors

Classifications

  • by mechanically taking samples of the soil · CPC title

  • Design optimisation, verification or simulation (optimisation, verification or simulation of circuit designs G06F30/30) · CPC title

  • Numerical modelling · CPC title

  • Subject matter not provided for in other groups of this subclass · CPC title

  • Displacing by water · CPC title

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What does patent US10794155B2 cover?
The invention is a method for exploiting a subterranean formation including hydrocarbons with at least one lithologic facies of the formation having undergone at least one diagenetic phase over geological times. From at least one sample of rock obtained from the formation, from measured production data relating to the formation and from a meshed representation representative of the formation, e…
Who is the assignee on this patent?
Ifp Energies Now, Repsol Sa
What technology area does this patent fall under?
Primary CPC classification E21B41/0092. Mapped technology areas include Fixed Constructions.
When was this patent published?
Publication date Tue Oct 06 2020 00:00:00 GMT+0000 (Coordinated Universal Time) (B2). Legal status and post-grant events are not shown on this page.
What related patents are in patentsdb?
We list 8 related publications on this page (citations in our corpus or others sharing the same primary CPC).