Patent Grant
11454097
This disclosure relates to recovering fluids, for example, hydrocarbons, entrapped in subsurface reservoirs.
Hydrocarbons residing in subsurface reservoirs can be raised to the surface of the Earth, that is, produced, by forming wells from the surface of the Earth through the subterranean zone (for example, a formation, a portion of a formation, or multiple formations) to the subsurface reservoirs. In primary hydrocarbon recovery applications, the formation pressure exerted by the subterranean zone on the hydrocarbons causes the hydrocarbons to flow into the well (called a producing well). Over time, the formation pressure decreases, and secondary recovery applications are implemented to recover the hydrocarbons from the reservoirs. Use of electrical submersible pumps (ESPs) disposed in the producing well to pump the hydrocarbons from downhole locations to the surface is an example of a secondary recovery application. Injecting fluids, for example, water, in injection wells surrounding the producing well to force the hydrocarbons in portions of the surrounding subterranean zone towards the producing well is another example of a secondary recovery application. The choice of fluid injected into the injection wells affects recovery of the hydrocarbons through the producing well.
This specification describes technologies relating to artificial rain to enhance hydrocarbon recovery. Implementations of the present disclosure include a method for hydrocarbon recovery method. The hydrocarbon recovery method includes generating artificial, fresh rain water. The method includes mixing a volume of the generated artificial, fresh rain water with a volume of brine water obtained from a brine water source to form a mixture having a water salinity that satisfies a threshold water salinity. The method includes injecting the mixture in an injection well formed in a subterranean zone. The injection well is fluidically coupled to a producing well formed in the subterranean zone to produce hydrocarbons residing in the subterranean zone. The mixture flows the hydrocarbons in the subterranean zone surrounding the producing well toward the producing well. The method includes producing the hydrocarbons in response to injecting the mixture in the injection well.
In some implementations, generating the artificial, fresh rain water further includes seeding clouds above the fresh water reservoir with salt configured to draw water vapor in the atmosphere and condense the drawn water vapor into water droplets that combine to form the artificial, fresh rain water.
In some implementations, the seeding the clouds further includes dropping a quantity of the salt sufficient to draw the water vapor by an airplane.
In some implementations, the salt further includes silver iodide.
In some implementations, the method further includes storing the generated artificial, fresh rain water in a fresh water reservoir positioned below a surface of the Earth in the subterranean zone adjacent the injection well. The method can further include obtaining the brine water from the brine water source, storing the obtained brine water in a brine water reservoir positioned adjacent the fresh water reservoir, and fluidically coupling the fresh water reservoir and the brine water reservoir. In some implementations, the brine water source is a sea. In some implementations, installing the brine water reservoir directly vertically below the fresh water reservoir. In some implementations, obtaining the brine water from the brine water source can further include drawing the brine water through a pipeline that fluidically couples the sea and the brine water reservoir. The method can include, where the clouds are directly above the fresh water reservoir, the method further includes installing a plurality of rain water collectors on the surface of the Earth directly below the clouds and fluidically coupling the plurality of rain water collectors to the fresh water reservoir.
In some implementations, where the artificial, fresh rain water has a lower water salinity compared to the brine water, the method further includes controlling the water salinity of the mixture. Controlling the water salinity of the mixture can further include measuring the water salinity of the mixture before injecting the mixture in the injection well, determining that the measured water salinity is different from the threshold water salinity, and modifying the volume of the artificial, fresh rain water flowed from the fresh water reservoir into the mixing reservoir to mix with the volume of the brine water until the measured water salinity of the mixture matches the threshold water salinity.
Further implementations of the present disclosure include a hydrocarbon recovery method including mixing artificially generated fresh rain water with sea water obtained from a sea to form a mixture, controlling a water salinity of the mixture to satisfy a threshold water salinity, injecting the mixture having the water salinity that satisfies the threshold water salinity in an injection well formed in a subterranean zone, and producing the hydrocarbons in response to injecting the mixture in the injection well. The injection well surrounding a producing well is formed in the subterranean zone to produce hydrocarbons residing in the subterranean zone. The mixture flows the hydrocarbons in the subterranean zone surrounding the producing well toward the producing well. The method can further include installing a plurality of rain water collectors on the surface of the Earth directly below the clouds and fluidically coupling the plurality of rain water collectors to the fresh water reservoir.
In some implementations, the artificial, fresh rain water is generated by seeding clouds with salt configured to draw water vapor in the atmosphere and condense the drawn water vapor into water droplets that combine to form the artificial, fresh rain water and storing the generated artificial, fresh rain water in a fresh water reservoir positioned below a surface of the Earth in the subterranean zone adjacent the injection well. Seeding the clouds can further include dropping a quantity of the salt sufficient to draw the water vapor by an airplane. The method can further include obtaining the sea water from the sea, storing the obtained brine water in a sea water reservoir positioned directly, vertically below the fresh water reservoir, and fluidically coupling the fresh water reservoir and the sea water reservoir. Controlling the water salinity of the mixture can further include measuring the water salinity of the mixture before injecting the mixture in the injection well, determining that the measured water salinity is different from the threshold water salinity, and modifying a quantity of the artificial, fresh rain water flowed from the fresh water reservoir into the mixing reservoir until the measured water salinity of the mixture matches the threshold water salinity.
In some implementations, the fresh water reservoir is directly, vertically below the clouds.
Implementations of the present disclosure realize one or more of the following advantages. The quantity of oil recovered from a subterranean zone is increased. For example, reducing the salinity of the water injected into the subterranean zone using artificial rain can change the wettability (that is, the measure of a liquid's ability to maintain contact with the reservoir), increasing the quantity of oil recovered per recovery operation. Reducing the injection water salinity can enhance the chemical interactions with rock minerals and its adsorbed oil components. As a result, the rock wettability altered from oil-wet towards water-wet. Oil droplets will be subsequently released from the rock surfaces in a process called oil recovery enhancement. Also, waterflooding operations can be used in geographic regions where natural rainfall can be scarce. The cost of fresh water may be reduced. Current methods for providing fresh water for enhanced oil recovery in many regions of the world include large, complex desalination plants. Artificial rain water can be generated and collected at the reservoir location.
The details of one or more implementations of the subject matter described in this specification are set forth in the accompanying drawings and the description below. Other features, aspects, and advantages of the subject matter will become apparent from the description, the drawings, and the claims.
Like reference numbers and designations in the various drawings indicate like elements.
The present disclosure relates to a method of hydrocarbon recovery using artificial rain. Fresh rain water is artificially generated. A volume of brine water is obtained from a brine water source. The volume of the generated artificial fresh rain water is mixed with the volume of brine water to form a mixture having a water salinity that satisfies a threshold water salinity. The resulting mixture is injected in an injection well formed in a subterranean zone. The injection well is fluidically connected to a producing well by the subterranean zone. The subterranean zone contains hydrocarbons. The mixture flows from the injection well into the subterranean zone and forces the hydrocarbons from the subterranean formation toward the producing well. The producing well produces the hydrocarbons in response to injecting the mixture in the injection well.
As shown in
In some implementations, clouds 106 can be seeded with a salt. Seeding the clouds 106 with salt draws water vapor in the atmosphere 108 into the clouds 106. The drawn water vapor can condense into water droplets that combine to form the artificial fresh rain water 110, similar to the process by which natural rain water is formed. The salt can be silver iodide. In some implementations, a quantity of the salt can be dispersed or dropped into the cloud in a sufficient quantity to draw the water vapor in the atmosphere 108 into the clouds 106. The quantity of the salt sufficient to draw the water vapor can be dropped by an airplane. Silver iodide (AgI) may be released by a generator that vaporizes an acetone-silver iodide solution containing 1-2% AgI and produces aerosols with particles of 0.1 to 0.01 μm diameter. The relative amounts of AgI and other solubilizing agents are usually adjusted based on the yield, nucleation mechanism, and ice crystal production rates.
Clouds seeding with silver iodide can be only effective if the cloud is super-cooled and the proper ratio of cloud droplets to ice crystals exists. Silver iodide acts as an effective ice nucleus at temperature of 25° F. (−4° C.) and lower. Several factors can impact artificial rain processes such as the type of cloud, its temperature, moisture content, droplet size distribution, and updraft velocities in the cloud. Additional steps that can increase the likelihood of rain is the methodology of the cloud seeding operations which includes identification the suitable situation based on the previously mentioned factors, arrangement of an appropriate seeding agent, and successful transport and diffusion or direct placement of the seeding agent to the super-cooled liquid and vapor must be available to provide precipitation. Using numerical models can be important to evaluate seeding potential and its efficiency.
Alternatively, a laser pulse may be able to produce condensation in the atmosphere 108. Firing a laser beam made up of short pulses into the air ionizes nitrogen and oxygen molecules around the beam to create a plasma, resulting in a ‘plasma channel’ of ionized molecules. These ionized molecules could act as natural condensation nuclei.
The clouds 106 that are selectively seeded by the salt are situated over multiple rain water collectors (for example, rain water collectors 116a, 116b, and 116c). The multiple rain water collectors 116a, 116b, and 116c are directly below the clouds 106. By directly below the clouds 106, it is meant that at least some, a substantial portion, or all of the artificial fresh rain water 110 falling from the clouds 106 can be collected in the rain water collectors 116a, 116b, and 116c as the artificial fresh rain water 110 lands on the surface 104 of the Earth. The rain water collectors are stationary and adjacent to the injection well site. Alternatively, movable or transportable rain water collectors can be used.
The rain water collectors 116a, 116b, and 116c can be surface reservoirs. The surface reservoirs can be constructed from Earth materials, for example, rocks, dirt, soil, and sand positioned to retain water. The surface 104 of the Earth in the rain water collectors 116a, 116b, and 116c can be lined to prevent the artificial fresh rain water 110 from absorbing into the Earth. For example, a plastic liner can be placed in the rain water collectors 116a, 116b, and 116c. Alternatively, or in addition, the rain water collectors 116a, 116b, and 116c can be constructed from a plastic or metal. For example, the rain water collectors 116a, 116b, and 116c can be tanks. In some implementations, the rain water collectors 116a, 116b, and 116c can be partially covered by a cover (not shown) to reduce artificial fresh rain water 110 losses to the atmosphere 108 by evaporation. The cover can collect the artificial fresh rain water 110 falling from the clouds 106 and direct the artificial fresh rain water 110 to the rain water collectors 116a, 116b, and 116c.
The rain water collectors 116a, 116b, and 116c are fluidically connected to a water reservoir 120 by flow conduits (for example, flow conduits 118a, 118b, and 118c fluidically connected to rain water collectors 116a, 116b, and 116c, respectively). The flow conduits 118a, 118b, and 118c allow flow from the rain water collectors 116a, 116b, and 116c to the water reservoir 120.
A valve 128 can be positioned in each of the flow conduits 118a, 118b, and 118c to control flow from the rain water collectors 116a, 116b, and 116c to the water reservoir 120. For example, valve 128a, valve 128b, and valve 128c can be positioned in flow conduits 118a, 118b, and 118c, respectively, to control the flow the artificial fresh rain water 110 from the rain water collectors 116a, 116b, and 116c, respectively, to the water reservoir 120. For example, valve 128a can open to allow artificial fresh rain water 110 to flow from rain water collector 116a through flow conduit 118a to the water reservoir 120. For example, valve 128a can shut to stop artificial fresh rain water 110 from flowing from rain water collector 116a through flow conduit 118a to the water reservoir 120. For example, valve 128a can partially open or partially shut to increase or decrease, respectively, the quantity of artificial fresh rain water 110 flowed from rain water collector 116a through flow conduit 118a to the water reservoir 120.
In some implementations, the valve 128a, valve 128b, and valve 128c can be operated manually. In some implementations, the valve 128a, valve 128b, and valve 128c can be operated remotely by the controller 134. For example, the controller 134 may generate a signal to energize the valve 128a open to flow a quantity of artificial fresh rain water 110 from the rain water collector 116a to the water reservoir 120.
A pump (for example, pump 130a, pump 130b, and pump 130c) can be positioned in each of the flow conduits 118a, 118b, and 118c to move the artificial fresh rain water 110 from the rain water collectors 116a, 116b, and 116c to the water reservoir 120. For example, pump 130a, pump 130b, and pump 130c can positioned in flow conduits 118a, 118b, and 118c, respectively, to flow the artificial rain water 110 to the water reservoir 120. In some implementations, the pump 130a, pump 130b, and pump 130c can be operated manually. In other implementations, the pump 130a, pump 130b, and pump 130c can be operated remotely by the controller 134. For example, the controller 134 may generate a signal to energize the pump 130a to flow a quantity of artificial fresh rain water 110 from the rain water collector 116a to the water reservoir 120.
The flow conduits 116a, 116b, and 116c can include various sensors 132d, 132e, and 132f, respectively, configured to sense fluid conditions and transmit the fluid conditions to the controller 134. For example, the sensors 132d, 132e, and 132f, can sense fluid pressure, temperature, flow rate, salinity, or conductivity in flow conduits 116a, 116b, and 116c, respectively.
The water reservoir 120 collects and stores the artificial fresh rain water 110 from the rain water collectors 116a, 116b, and 116c via the flow conduits 118a, 118b, and 118c. The water reservoir 120 can be underground, that is, beneath the surface 104 of the Earth. The water reservoir 120 can be constructed from a plastic or metal. For example, the water reservoir 120 can be a tank. The water reservoir 120 is fluidically connected to a mixing reservoir 122 by a flow conduit 118d, substantially similar to the flow conduits 118a, 118b, and 118c described earlier. A pump 130d may be positioned in flow conduit 118d to flow artificial fresh rain water 110 from the water reservoir 120 to the mixing reservoir 122. A valve 128d can be positioned in flow conduit 118d to control the flow of artificial fresh rain water 110 from the water reservoir 120 to the mixing reservoir 122.
The mixing reservoir 122 receives the artificial fresh rain water 110 from the water reservoir 120 through the flow conduit 118d. The mixing reservoir 122 also receives brine water from a brine water source through another fluid conduit 118e. The brine water source can be a sea 124. The brine water can be sea water 126. Alternatively, the brine water source can be a brine fluid from another subterranean zone. Another potential source for brine water can be an industrial plant, for example, a desalinization plant where brine water is a byproduct of an industrial process. Produced water from other production wells can be reinjected a source for brine water.
The flow conduit 118e is substantially similar to the flow conduits discussed earlier. A pump 130e can be positioned in flow conduit 118e to flow sea water 126 from the sea 124 to the mixing reservoir 122. A valve 128e can be positioned in flow conduit 118e to control the flow of sea water 124 from the sea 126 to the mixing reservoir 122.
In some implementations, the artificial fresh rain water 110 and the sea water 126 mix in the mixing reservoir 122 by the flow of the artificial fresh rain water 110 and the sea water 126 into the mixing reservoir 122. The artificial fresh rain water 110 and the sea water 126 may mix in the mixing reservoir 122 by diffusion. In other implementations, the mixing reservoir 122 has a component to actively mix the artificial fresh rain water 110 and the sea water 126 mix in the mixing reservoir 122. For example, the mixing reservoir can include a pump, a nozzle, an impeller, or an aeration system.
The mixing reservoir 122 includes a flow conduit 118f to flow a mixture of the artificial fresh rain water 110 and the sea water 126 to an injection well 112. The flow conduit 118f is substantially similar to the flow conduits described earlier. A pump 130f may be positioned in flow conduit 118f to flow the mixture from the mixing reservoir 122 to the injection well 112. A valve 128f can be positioned in flow conduit 118f to control the flow of the mixture from the mixing reservoir 122 to the injection well 112.
The different features described here can include sensors that can sense fluid properties and transmit a signal to a controller 134 (described later) to control flow of the mixture based on the sensed value. For example, the rain water collectors 116a, 116b, and 116c, the water reservoir 120, the various flow conduits, and the mixing reservoir 122 can include sensors. Examples of the fluid properties sensed by the sensors include fluid level (in the case of a reservoir), temperature, salinity, pH, flow rate, resistivity, or conductivity. For example, a sensor 132a can be disposed in the water reservoir 120 to sense resistivity of the artificial fresh rain water 110. A signal representing the resistivity of the artificial fresh rain water 110 in the water reservoir 120 can be sent to the controller 134. Based on the resistivity value in the water reservoir 120, the controller 134 can control the flow of the artificial fresh rain water 110 into the mixing reservoir 122. For example, a sensor 132b can be disposed in the sea water 126 flow conduit 132b to sense resistivity of the sea water 126. A signal representing the resistivity of the sea water 126 in the flow conduit 118e can be sent to the controller 134. Based on the resistivity value in the flow conduit 118e, the controller 134 can control the flow of the sea water 126 into the mixing reservoir 122. For example, a sensor 132c can be disposed in the mixture in the mixing reservoir 122 to sense resistivity of the mixture. A signal representing the resistivity of the mixture in the mixing reservoir 122 in can be sent to the controller 134. Based on the resistivity value in the mixing reservoir 122, the controller 134 can control the flow of the sea water 126 or the artificial fresh rain water 110 into the mixing reservoir 122.
The controller 134 can be a non-transitory computer-readable medium storing instructions executable by one or more processors to perform operations described here. In some implementations, the controller 134 includes firmware, software, hardware or combinations of them. The instructions, when executed by the one or more computer processors, cause the one or more computer processors to control the salinity of the mixture in the mixing reservoir 122 when the artificial fresh rain water has a lower water salinity compared to the sea water.
The controller 134 can control the salinity of the mixture by measuring the salinity of the mixture before injecting the mixture in the injection well 112 and flowing a quantity of artificial fresh rain water 110 from the water reservoir 120 or a quantity of sea water 126 from the sea 124 based on the salinity of the mixture. The controller 134 can receive a signal representing the conditions of the artificial fresh rain water 110 in the water reservoir 120 from sensors 132g. For example, the controller 134 receives signals representing the fluid level, temperature, salinity, pH, or conductivity in water reservoir 120. The controller 134 can receive signal representing the conditions of the sea water 126 in the flow conduit 118e from sensors 132j. For example, the controller 134 receives signals representing the fluid flow rate, temperature, salinity, pH, or conductivity in flow conduit 118e. The controller 134 can receive signal representing the conditions of the mixture in the mixing reservoir 122 from sensors 132i. For example, the controller 132 receives signals representing the fluid level, temperature, salinity, pH, or conductivity in mixing reservoir 120.
The controller can determine that the measured salinity of the mixture in the mixing reservoir 122 is different from the threshold water salinity. The controller 134 can modify the volume of the artificial, fresh rain water 110 flowed from the fresh water reservoir 120 into the mixing reservoir 122 to mix with the volume of the sea water until the measured water salinity of the mixture matches the threshold water salinity. The controller 134 can generate signals to operate pump 130d to flow artificial fresh rain water 110 from the water reservoir 120 to the mixing reservoir 122 until the measured water salinity of the mixture matches the threshold water salinity. Alternatively or in addition, the controller 134 can generate signals to operate valve 128d to flow artificial fresh rain water 110 from the water reservoir 120 to the mixing reservoir 122 until the measured water salinity of the mixture matches the threshold water salinity. For example, the controller 134 commands valve 128d open to allow artificial fresh rain water 110 flow from the water reservoir 120 to the mixing reservoir 122. Subsequently, the controller 134 commands valve 128d can shut to stop artificial fresh rain water 110 from the water reservoir 120 to the mixing reservoir 122. Alternatively or in addition, the controller 134 commands valve 128d can partially open or partially shut to increase or decrease, respectively, the quantity of artificial fresh rain water 110 flowed from the water reservoir 120 to the mixing reservoir 122.
The injection well 112 is positioned in the subterranean zone 102 and extends from the surface 104 of the Earth downward to the subterranean zone 102 of the Earth. The injection well 112 receives the mixture from the mixing reservoir 122. The injection well 112 is fluidically coupled to the subterranean zone 102. The injection well 112 raises the pressure of the mixture to a pressure above a subterranean zone 102 pressure. The injection well 112 injects the pressurized mixture from the mixing reservoir 122 into the subterranean zone 102.
The subterranean zone 102 is the geologic formations of the Earth. The subterranean zone 102 can be contain both liquid and gaseous phases of various fluids and chemicals including water, oils, and hydrocarbon gases. The subterranean zone 102 receives the pressurized mixture from the injection well 112. The pressurized mixture forces a fluid flow, indicated by arrow 138 from the injection well 112 through the subterranean zone 102 to a production well 114.
The production well 114 extends from the surface 104 of the Earth downward to the subterranean zone 102 of the Earth. The production well 114 conducts the fluids and chemicals from the subterranean zone 102 of the Earth to the surface 104 of the Earth. The production well 114 can also be known as the producing well. Once on the surface 104 of the Earth, the fluids and chemicals can be stored or transported for refining into useable products.
In some implementations, an observation well (not shown) can be drilled into the subterranean zone 102. Sensors, substantially similar to the sensors described earlier, can be positioned in the observation well in the subterranean zone to sense fluid properties of the subterranean zone. The sensors in the subterranean zone can transmit a signal representing the fluid conditions in the subterranean formation 102 to the controller 134. The controller 134 can control the flow of the mixture to the subterranean zone 102 based on the sensed values.
At 204, a volume of the generated artificial, fresh rain water is mixed with a volume of brine water obtained from a brine water source to form a mixture having a water salinity that satisfies a threshold water salinity. Obtaining the brine water from the brine water source can include storing the obtained brine water in a brine water reservoir positioned adjacent the fresh water reservoir and fluidically coupling the fresh water reservoir and the brine water reservoir. Where the brine water source is a sea, obtaining the brine water from the brine water source includes drawing the brine water through a pipeline that fluidically couples the sea and the brine water reservoir. The method can include installing the brine water reservoir directly vertically below the fresh water reservoir. Where the artificial, fresh rain water has a lower water salinity compared to the brine water, the method includes controlling the water salinity of the mixture. Controlling the water salinity of the mixture can include measuring the water salinity of the mixture before injecting the mixture in the injection well, determining that the measured water salinity is different from the threshold water salinity, and modifying the volume of the artificial, fresh rain water flowed from the fresh water reservoir into the mixing reservoir to mix with the volume of the brine water until the measured water salinity of the mixture matches the threshold water salinity.
At 206, the mixture is injecting into the injection well formed in a subterranean zone. The injection well is fluidically coupled to a producing well by the subterranean zone. The producing well is formed in the subterranean zone to produce hydrocarbons residing in the subterranean zone. The mixture flows the hydrocarbons in the subterranean zone surrounding the producing well toward the producing well. At 208, the hydrocarbons are produced in response to injecting the mixture in the injection well.
Certain implementations have been described to recover hydrocarbons using artificial, fresh rain water by controlling salinity of the mixture. The techniques described here can alternatively or additionally be implemented to control other fluid properties. For example, total dissolved solids or pH can be controlled.
Thus, particular implementations of the subject matter have been described. Other implementations are within the scope of the following claims.
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| Number | Date | Country | |
|---|---|---|---|
| 20220213769 A1 | Jul 2022 | US |
