The disclosed embodiments relate generally to systems and methods for storing a fluid, and particularly to systems and methods for storing compressed gas, such as air or natural gas.
Subsurface storage structures may be employed for the storage of fluids, e.g., natural gas, hydrocarbons liquids, air, carbon dioxide and/or other gases. Conventional subsurface storage may include depleted hydrocarbon-bearing reservoirs which exhibit suitable permeability and porosity, and which exhibit suitable pressure retention characteristics (e.g., provided by a shale cap or other geologic features) to retain the stored fluid for later retrieval. However, the use of depleted hydrocarbon reservoirs may be limited for some storage applications. For example, the use of depleted hydrocarbon bearing zones is limited by the location of such formations, which may be in remote areas and distant from sites where storage is desired. Furthermore, the use of depleted hydrocarbon formations may be limited by the dynamic characteristics of the formation. For example, certain fluid storage applications may require relatively rapid injection and/or removal of the stored fluid. Accordingly, such applications may not be compatible with formations wherein the permeability and porosity characteristics of the formation do not permit sufficient injection and/or withdrawal rates. Thus, suitably located depleted hydrocarbon formations, having appropriate permeability, porosity, and flow characteristics may be unavailable for a given storage application. Furthermore, the storage capacity of the formation is fixed and is contingent on the size of the formation employed.
Porous geologic formations that are positioned with respect to relatively non-porous formations in a manner that provides containment of a fluid are used for storage of air, hydrocarbons, and other fluids. Examples of embodiments of this include depleted hydrocarbon reservoirs and confined aquifers. In a general sense, any combination of geologic phenomena that creates a low permeability trap for fluids have the potential for storage of air, hydrocarbon, or other fluids. The broad geologic characteristics of traps are classified as structural traps, stratigraphic traps, and hydrodynamic traps. The trapping mechanisms for a storage volume may be achieved with one or any combination of these mechanisms. The pressurization of these storage volumes is primarily achieved from the in-situ hydrostatic pressure of the volume and contribution from the in-situ lithostatic pressure of the overburden.
Another type of conventional underground structure for fluid storage structure is a salt cavern. Salt caverns may be formed in subterranean salt layers by, e.g., drilling into the salt layer using conventional rotary drilling techniques, then solution mining the salt by introduction of fresh water to the salt formation. The saturated brine produced by dissolution of the salt is then removed and the process is repeated. The solution mining is performed continuously (i.e., fresh water is injected at the same time saturated brine is being removed) until the salt cavern reaches the desired size. Solution mining of salt beds and domes may be a time consuming process, and typically produces large quantities of brine which must be treated and/or disposed of. In addition, the use of salt caverns for fluid storage, like depleted hydrocarbon formations, is limited by the geographical location of salt formations, which may not be convenient or appropriate for a desired fluid storage need or application. Further, like depleted hydrocarbon reservoirs, salt caverns are constrained in size, and accordingly, storage volume, by the corresponding size of a salt formation from which the salt cavern is mined.
Another alternative for underground storage of fluids is excavated caverns formed by blasting. Such excavated caverns may include depleted mines or similar cavern-like structures formed using traditional blasting techniques. However, blasting employed in the formation of such structures typically produces fractures of the surrounding rock formations, and may also weaken the surrounding rock. Accordingly, the fractures may result in structures which are not suitable to contain stored fluids under pressure. For example, a blasted cavern may have lateral, vertical, or angular fissures that allow stored fluids to escape or migrate out of the storage cavern. Such losses are generally unacceptable, particularly in fluid storage applications where pressurized fluids are retained (e.g., compressed gas storage). Furthermore, blasting may damage the integrity of the overburden rock, requiring extensive bracing and/or shoring to keep the resultant cavern open. In addition, blasting may produce large, irregular debris which may require grinding or other size reduction prior to removal. Further, blasting to form caverns may not be suitable for certain locations (e.g., densely populated areas), and thus the location of blasted caverns may be limited.
Accordingly, there exists a need for underground fluid storage facilities which can be constructed in a cost effective fashion, are scalable in size, and can be located conveniently for a given application.
The present application describes underground storage caverns that may be formed by mechanical excavation of a subsurface formation in a controlled fashion. In some embodiments, the present application provides storage caverns formed by employing tunnel boring techniques, which may be substantially horizontal or slightly inclined. The caverns may be formed in a controlled fashion, are scalable, and may employ geometries to maximize storage volumes while minimizing the surface area of land associated with the storage facility. In addition, the caverns may be formed in a wide array of geologic formations and they may be located essentially anywhere a suitable geologic formation is located regardless of, for example, population density. Storage caverns as described herein may further employ hydraulic pressure compensation to manage wide pressure variations in the storage caverns, and to provide relatively constant injection and discharge pressures when introducing or releasing stored fluids. In some embodiments, the caverns may be employed in a compressed air energy storage (CAES) system for storing energy in the form of compressed air. Alternatively, the present caverns may be employed for the storage of natural gas and hydrocarbon liquids. These embodiments are described herein.
Accordingly, in one aspect, a large-scale, excavated, underground storage system includes at least one substantially vertical borehole and a plurality of lateral caverns extending from the vertical borehole. The lateral caverns are adapted for substantially sealed storage of a fluid and are excavated by a tunnel boring machine. The diameter of each lateral cavern is less than or substantially equal to the diameter of the vertical borehole. Further, the lateral caverns are formed to substantially maximize the volume of the lateral caverns while substantially minimizing the total surface area of the storage subsystem.
In one embodiment, the storage system is fluidically coupled to a compressed air energy storage system. The diameter of the vertical borehole may be sized to receive the tunnel boring machine. Each lateral cavern may be either substantially horizontal or inclined. At least one of the lateral caverns may be fluidically isolated from at least one of the other lateral caverns. At least one of the lateral caverns may be fluidically coupled to a substantially vertical terminal borehole disposed at a terminal end of that lateral cavern.
In another embodiment, each lateral cavern includes a geometry selected from the group consisting of a line, a curve, a circle, a spiral, and combinations of the foregoing. Each lateral cavern may have a substantially similar geometry. At least one of the lateral caverns may have a circular cross-section. The lateral caverns may be arranged in a two-dimensional array and/or a three-dimensional array.
In a further implementation, the fluid is a liquid, a gas, a vapor, a suspension, an aerosol, or a combination of the foregoing. The depth of at least one of the lateral caverns may be selected based at least in part on a lithostatic pressure acting on that lateral cavern. The storage system may further include a pressure compensation system adapted to maintain a substantially constant working pressure in at least one of the lateral caverns, and the pressure compensation system may include a liquid displaceable by a gas stored in that lateral cavern.
In another aspect, a method for constructing a large-scale, excavated, underground storage system includes forming at least one substantially vertical borehole and excavating, by a tunnel boring machine, a plurality of lateral caverns extending from the vertical borehole. The lateral caverns are adapted for substantially sealed storage of a fluid, with each lateral cavern having a diameter less than or substantially equal to the diameter of the substantially vertical borehole. The lateral caverns are formed to substantially maximize the volume of the lateral caverns while substantially minimizing the total surface area of the storage subsystem.
In one embodiment, the method further includes fluidically coupling the storage system to a compressed air energy storage system. The diameter of the vertical borehole may be sized to receive the tunnel boring machine. Each lateral cavern may be either substantially horizontal or inclined. The method may further include fluidically isolating at least one of the lateral caverns from at least one of the other lateral caverns. The method may further include fluidically coupling at least one of the lateral caverns to a substantially vertical terminal borehole disposed at a terminal end of that lateral cavern.
In another embodiment, each lateral cavern includes a geometry selected from the group consisting of a line, a curve, a circle, a spiral, and combinations of the foregoing. Each lateral cavern may have a substantially similar geometry. At least one of the lateral caverns may have a circular cross-section. The method may further include arranging the lateral caverns in a two-dimensional array and/or a three-dimensional array.
In a further implementation, the fluid is a liquid, a gas, a vapor, a suspension, an aerosol, or a combination of the foregoing. The method may further include selecting the depth of at least one of the lateral caverns based at least in part on the lithostatic pressure acting on that lateral cavern. The method may further include maintaining a substantially constant working pressure in at least one of the lateral caverns, which may include displacing a liquid by storing a gas in that lateral cavern.
Other aspects and advantages of the invention will become apparent from the following drawings, detailed description, and claims, all of which illustrate the principles of the invention, by way of example only.
A more complete appreciation of the invention and many attendant advantages thereof will be readily obtained as the same becomes better understood by reference to the following detailed description when considered in connection with the accompanying drawings. In the drawings, like reference characters generally refer to the same parts throughout the different views. Further, the drawings are not necessarily to scale, emphasis instead generally being placed upon illustrating the principles of the invention.
Systems and methods for the storage of a compressed gas (such as air, natural gas, hydrogen (H2), helium (He) or argon (Ar)), or a liquid, in underground storage caverns are described herein. The underground storage caverns can be used, for example, to store hydrocarbons such as natural gas, natural gas liquids (NGL) or liquefied petroleum gases (LPG) for later recovery and use. The underground storage caverns can also be used, for example, to store energy in the form of compressed gas, such as air, in a compressed air energy storage (CAES) system. The caverns can have efficient/optimal operating ranges that can vary as a function of, for example, flow rate and pressure, among other parameters. Systems and methods of operating the storage caverns are provided to allow them to function at optimal performance throughout the energy storage cycle of the compressed gas energy storage system.
Throughout the present specification, the words “a” or “an” are understood to mean “one or more” unless explicitly stated otherwise. Further, the words “a” or “an” and the phrase “one or more” may be used interchangeably.
As used herein, “fluid” can mean a liquid, gas, vapor, suspension, aerosol, or any combination thereof. As used herein, “liquid” can include any suitable liquid fluid including, for example, water and/or brine (e.g. water substantially partially or completely saturated with salt), and “gas” can include any suitable gaseous fluid including, for example, air, natural gas, hydrogen (H2), helium (He) or argon (Ar). A power grid can be any local, regional, national, and/or international power grid, grids, or combination of grids. A power source can include any source of power independent of fuel or production method, e.g., solar, wind, fossil fuel, nuclear, geothermal, hydroelectric, etc.
As described herein, in some embodiments, systems and methods can be used for manufacturing underground storage structures (also referred to herein as “underground storage caverns” or “caverns”). In some underground storage structures, a plurality of individual caverns can be constructed to optimize the installed storage capacity per surface area of land (i.e., storage density). In some embodiments, a tunnel boring machine (TBM) can be used to construct caverns for the underground storage structure.
In some embodiments, TBMs may be employed to construct underground storage structures. For example, a vertical boring having a diameter sufficient to introduce a TBM may be formed by, e.g., rotary drilling or excavation, to a desired depth. The TBM can then be lowered into the vertical boring, and a horizontal or substantially horizontal cavern can then be excavated from the base of the vertical borehole by boring with the TBM. TBM boring methods are known in the art, and typically employ a rotary cutting assembly which removes material at a cutting face. Debris cut away from the rock face is continuously transported from the cutting face to the vertical boring, where it is removed to the surface and disposed of Caverns as described may be bored at a slight incline (e.g., 0.1° to 3°) to aid in debris removal, to allow any fluids released during excavation to flow away from the cutting face, and to manage air and/or water traps when a compensating liquid is used for gas storage as described herein. In other embodiments, a vertical bored TBM or SRM tunnel of significant diameter and depth may be utilized directly as the fluidic storage vessel. The density could be further enhanced over traditional and alternative pumped hydro variations by employing gas as the compressible in unison with “pumped, controlled pressure operation of the storage cavity.” The gas can provide an energy density benefit up to six fold over these pumped hydro variations.
In some embodiments, drilling and blasting may be used to construct underground storage structures. For example, in certain types of rock (e.g., hard igneous rock, abrasive rock, silica-containing rock, etc.), modern drilling and blasting machines can be used to cost-effectively construct storage caverns. Such drilling and blasting machines typically use safer, more environmentally friendly explosives relative to traditional explosives. In drill-and-blast operations, a machine with a boom-mounted array of drill heads can be used to drill a predetermined pattern of holes in a rock formation to be excavated. The drills are then removed, explosives are inserted into the drilled holes, and then the explosives are detonated. The resultant explosion fragments the rock in the blast region of the rock face where the explosive were inserted, and those fragments can then be removed. The drill-and-blast machine can then be advance for additional material removal. Alternatively, a combination of drilling/blasting and boring excavation methods may be employed. For example, a drill-and-blast operation may be used to provide an initial excavation, or pilot hole, which may then be expanded or continued with a TBM to form a cavern structure as described herein.
The cavern may be constructed to any desired length (e.g., about 100 m to about 1 km or more) and cross-sectional area (e.g., an effective diameter from about 1 m to about 10 m or more) suitable for a particular storage application. Typically the caverns are elongated, with a relatively high length/diameter ratio. The horizontal cavern formed by the TBM typically has a circular cross-section, which may provide structural integrity and relative ease of excavation. Caverns formed by a TBM may have essentially any geometry, and are typically constrained only by the maneuvering capabilities of the TBM (e.g., minimum turning radius). For example, caverns formed by a TBM may be linear, curved (e.g., spirals, circles), or variations and combinations thereof (e.g., linear and curved portions may be combined in a single cavern structure).
The location and geometry of caverns as described herein may be determined by the extent of available surface real estate available for constructing such storage structures. Geometry for caverns may be selected in view of, or determined by, the geologic characteristics of a given rock formation where the caverns are to be constructed. For example, geometry for the present caverns may be selected to avoid geologic faults, which may compromise pressure and/or structural integrity of the cavern. In addition, it may be desirable to avoid certain rock formations (e.g., acidic rock formations), as disposal of debris from excavation of certain rock types may require special handling and disposal, which may be costly. Further, the location, depth and/or shape of caverns may be selected so that they are constructed in rock which displays desirable mechanical (e.g., rock strength) or fluid characteristics (e.g., permeability, porosity), or avoids those with unsuitable mechanical or fluid characteristics. For example, the location, depth and/or shape of caverns may be selected to avoid karst-prone geologic formations, as these may lack suitable mechanical and/or fluid integrity for construction of the present cavern structures. Location and construction of storage caverns may also be selected because of geologic formations due to ease of excavation of those formations. For example, a site may be selected where the rock is relatively easily removed (i.e., can be excavated at higher rates due to the mechanical characteristics of the rock), as rapid removal of rock may reduce the overall cost of cavern construction, for example, by reducing the operating and maintenance cost of the TBM. Accordingly, in certain embodiments, relatively soft geologic formations may be selected. In certain cases, TBMs may be employed to form the caverns in salt formations, as an alternative to solution mining of such formations.
In some embodiments, multiple caverns (e.g., two or more) can be constructed off a single vertical borehole to provide a series of caverns which can be interconnected via the central borehole. The two or more caverns can have the same geometry, or may have different geometries. In some embodiments, multiple caverns can be constructed with geometries to maximize cavern volumes while minimizing the total surface area of land used for the storage facility. For example, several caverns can be formed in nested spirals, as concentric circles, as parallel lines, etc. This can provide a cost effective method of creating large volumes of storage via the construction of multiple caverns off a single central vertical borehole while maximizing storage volume for a given area. In certain embodiments, two or more TBMs may be introduced into a single vertical borehole, and may be employed to simultaneously construct multiple caverns off a single central vertical borehole. In embodiments where two or more caverns are constructed from a central vertical borehole, the individual caverns may be fluidically isolated. Alternatively, each of the caverns may be connected to other caverns, or the caverns may be connected in subgroups which are fluidically isolated from other subgroups of caverns off a central borehole.
The caverns may also be constructed in a vertical array. For example, one or more caverns may be constructed at a selected depth, and then one or more caverns can subsequently be constructed at another depth either above or below the depth of the first array of caverns. Thus, in some embodiments, the geometries of an array of caverns at one depth may be selected to provide maximum storage density at a given depth, then one or more similar arrays may be constructed to provide additional storage density for a given area, as described above with respect to fluidic isolation of horizontal arrays of caverns.
Embodiments of the caverns may have depths from about 400 m to about 2,000 m, although the specific depth of the storage caverns can be selected in view of the required operational characteristics of the caverns for a given application. For example, the depth of the caverns can be selected in view of the desired working or operating pressures for a selected storage application. In certain embodiments, the depth of a cavern can be selected such that the lithostatic pressure is approximately equivalent to a desired operating pressure of the storage structure. Thus, for high pressure applications (e.g., storage of compressed gases) a deeper cavern may be constructed to provide sufficient lithostatic pressure from the overburden to provide a storage cavern which will withstand high storage pressures. Alternatively, where lower working pressures may be employed, e.g., for the storage of liquids, shallower caverns may be employed.
In some embodiments, the geologic characteristics of the rock formation in which the present caverns are constructed may be sufficient to retain the stored fluids at the working pressures employed in the storage facility. For example, certain types of rock (e.g., shale) possess low permeability, low porosity, or both, and the rock formation may provide fluidic isolation of a cavern for the storage of gases. In other embodiments, where liquids are to be stored in the cavern, pressure sealing may be unnecessary as the liquid may not migrate at sufficient rates or in sufficient quantities to warrant the cost of lining the caverns. However, in some embodiments, where the caverns are constructed in rock which is not pressure competent, e.g., the caverns will not retain fluids at the working pressure employed in storage due to rock properties (e.g., permeability, porosity) or naturally occurring fissures and/or fractures, the caverns can be sealed to provide pressure integrity. Sealing methods include linings such as, for example, spraying a suitable lining material on the walls of the cavern (e.g., concrete, “shotcrete”) or by lining the cavern with a pipe. Alternatively, a lining can be created by filling the cavern with a slurry having a sealing material (e.g., cement, bentonite), and “squeezing” the sealing material into the walls of the cavern by pressurizing the cavern filled with the slurry material. The slurry can then be removed, effectively providing a pressure competent seal to the cavern. In other embodiments, a desired shallower depth or sub optimal geologic characteristics may not be sufficient to solely rely on geostatic pressure for containment. An optimized lining or pressure vessel could be utilized to help contain dense fluidic storage while not needing the same mechanical properties or safety margin that would be mandated at the surface.
After formation of a desired number of cavern structures, removal of the excavation debris, and optionally sealing of the caverns, the storage structure can be isolated and connected to the surface to provide for introduction and removal of fluids to be stored. Traditional sealing methods, including lining the central borehole with a liner pipe and cementing the same in place may be employed. However, given the significant diameter of the vertical access boring through which a TBM is lowered, alternative methods may be employed to control the costs associated with lining the vertical boring. For example, a lining (e.g., concrete or “shotcrete”) may be applied. Alternatively, as described above with respect to tunnel sealing, the vertical borehole may be sealed by employing squeeze techniques. In other embodiments, the vertical boring may only be sealed for a fixed depth above the top of the cavern structures, and a mechanical seal (e.g., a concrete barrier) may be affixed above the lined portion, sealing the cavern structures but alleviating the need for lining of the entire vertical borehole. Alternatively, in some embodiments each cavern off a central borehole may be individually sealed by, e.g., installation of a mechanical barrier to provide pressure isolation of individual caverns off a central boring where two or more caverns off the central boring have been constructed, for example, an embodiment may include storage of more than one type of fluid, or different storage pressures of a single fluid.
Fluid communication between the surface and the storage facility may be provided by conventional pipe installation such as that used in production of hydrocarbon fluids (e.g., casing). Such casing can provide a fluid conduit to a storage cavern that may have one or more interconnected caverns. Alternatively, multiple casing strings can be run to individual caverns, to provide compartmentalized storage in each individual cavern, where such fluidic isolation is desired. Such casing strings can be connected to a manifold at the surface to provide controlled isolation of individual caverns, and selective introduction and/or removal of stored fluids. Alternatively, a plurality of interconnected caverns may be connected to the surface via a single casing string. The pressure rating of individual casing strings may be selected in view of the working pressures of the storage system to be employed, and the diameter of casings may be selected in view of the flow rates required for introduction and removal of the stored fluid.
For example, in certain embodiments, the caverns can be used to store compressed air for later energy generation. Turbines, pumps, or other devices employed to harness the energy provided by release and expansion of compressed air may require relatively constant supply pressure for safe and efficient operation. Hydraulic pressure compensation systems may be employed, using a suitable working fluid such as water or brine. Alternatively, pressure compensation systems may be used to aid in removal of, e.g., stored liquids by displacement of the stored liquids. For example, hydrocarbon liquids are less dense than water, and thus the introduction of aqueous pressure compensation fluids such as water or brine into the present storage caverns will displace stored hydrocarbon liquid, maintain the cavern pressure, and aid in removal of the stored liquid. In gas storage applications, a pressure compensation fluid can also aid in production of the stored fluid, and can maintain a desired pressure and temperature in the storage cavern to prevent pressure cycling of the cavern and minimize the rate of strain on the cavern wall faces.
In some embodiments, the storage structures can be used to store compressed air in a compressed air energy storage system (CAES). CAES systems are a type of system for storing energy in the form of compressed air. CAES systems can be used to store energy when electricity demand is low, typically during the night, and then to release the energy when demand is high, typically during the day, as described in U.S. Patent Publication. No. 2012/0057997, entitled “Systems and Methods for Optimizing Thermal Efficiency of a Compressed Air Energy Storage System,” the disclosure of which is incorporated herein by reference in its entirety. Thus, in certain embodiments, CAES systems may be coupled to the underground storage caverns provided herein to store compressed air for energy storage and subsequent generation.
CAES systems may be used in conjunction with the present bored cavern structures. For example, while CAES systems may be coupled to conventional underground storage structures (e.g., depleted hydrocarbon reservoirs, salt domes), as described herein, the location of such conventional underground storage structures is limited to where those structures naturally occur. Conversely, bored tunnel storage caverns can be constructed anywhere suitable rock is found, which is generally in most locations. Accordingly, the location of a CAES system is not particularly constrained, and such facilities can be placed where energy storage and delivery is needed (e.g., near power lines, near urban areas, etc.) or where excess power generation is available (e.g., wind turbine farms, nuclear power plants, etc.).
In some embodiments, a pressure compensation system may be employed to maintain relatively constant working pressures in the storage caverns. Pressure cycling, e.g., pressure variations during introduction and discharge of a stored fluid may affect the mechanical properties of the rock in which the caverns are constructed. Further, such pressure cycling may compromise the integrity of cavern linings, where such linings are employed. Thus, in some embodiments, the storage structure may use a pressure compensation system to minimize pressure cycling. Such pressure compensation may provide relatively constant deliver pressures of stored fluids.
For example, an embodiment of the storage structure can include a first storage location disposed at a first elevation, the first storage location configured to contain a liquid and a gas. The first storage location is further configured to receive compressed gas from a compressor and is in fluid communication with a second storage location disposed at a second elevation, the second elevation greater than the first elevation. The second storage location is configured to contain a volume of liquid such that the volume of liquid contained within the second storage location imparts a hydrostatic pressure on the first storage location. The first and second storage locations are configured to allow at least a portion of the liquid contained in the first storage location to flow from the first storage location to the second storage location as compressed gas is moved into the first storage location from the compressor/expander device. The first and second storage locations are further configured to allow at least a portion of the liquid contained in the second storage location to flow from the second storage location to the first storage location as compressed gas is removed from the first storage location.
In some storage systems, the second storage location can be elevated relative to a first storage location, and a liquid contained in the second storage location can maintain a pressure and/or range of pressures within the first storage location. As compressed gas is delivered to the first storage location, a portion of the liquid contained in the first storage location is displaced to the second storage location at a higher elevation than the first storage location. Once a desired amount of the liquid has been displaced from the first storage location to the second storage location, the first storage location can be fluidically isolated from the second storage location with, for example, a valve, thus allowing the first storage location to further be pressurized with compressed gas without inducing additional liquid flow from the first storage location to the second storage location. For example, in some embodiments, in may be desirable to move substantially all of the liquid from the first storage location to the second storage location before closing the valve to fluidically isolate the two storage locations. In other embodiments, it may be desirable to only move a portion of the liquid from the first storage location to the second storage location depending on, for example, the capacity of the second storage location or other operational parameters. As compressed gas is removed from the first storage location, a portion of the liquid contained in the second storage location can flow into the first storage location to occupy a volume in the first storage location previously occupied by the mass of the compressed gas that has been removed. In this manner, substantially all of the compressed gas contained in the first storage location can be released from the first storage location and delivered to a compressor/expander device, thus utilizing the entire volume of the cavern for energy storage in the form of compressed gas while maintaining a desired minimum pressure for the gas contained in the first storage location.
The compressor/expander 104 is in fluid communication with a source of gas such as, for example, a source of ambient air, and fluidly coupled via the gas pathway 112 to the storage cavern 106 to which gas can be transferred after being compressed. Valves can be used to open and close the fluid communication between the compressor/expander 104 and the source of gas and between the compressor/expander 104 and the storage tunnel 106. As the compressor/expander 104 delivers compressed gas to the storage cavern 106, the pressure within the storage cavern 106 increases until the pressure reaches a predetermined level and/or substantially equals the pressure of the compressed gas being delivered from the compressor/expander 104.
In some cavern storage applications such as, for example, described above with reference to
The motor/generator 202 can be operatively coupled to a power supply (not shown in
The compressor/expander 204 can be in fluid communication with a source of gas such as, for example, a source of ambient air (at ambient pressure, or pre-pressurized by another compression system), and can also be fluidly coupled via the gas pathway 212 to the low storage 206 to which gas can be transferred after being compressed. Valves can be used to open and close the fluid communication between the compressor/expander 204 and the source of gas and between the compressor/expander 204 and the low storage 206. In some embodiments, the compressor/expander 204 can also be configured to operate as an expansion device to generate electricity. For example, the compressed gas can be transferred from the low storage 206 to the compressor/expander 204 and stepped down from a relatively high pressure to a relatively lower pressure. The energy released from this pressure differential can be used, for example, to generate electricity.
The low storage 206 can be configured to contain a compressed gas, such as, for example, compressed air. The low storage 206 may be a bored tunnel structure. As the compressor/expander 204 delivers compressed gas to the low storage 206, the pressure within the low storage 206 increases until the pressure reaches a predetermined level and/or substantially equals the pressure of the compressed gas being delivered from the compressor 204.
The low storage 206 can be configured to contain both the compressed gas and a liquid such as, for example, water or brine, at the first elevation. As the compressor/expander 204 delivers compressed gas to the low storage 206, the pressure within the low storage 206 increases until the pressure reaches a predetermined level and/or substantially equals the pressure of the compressed gas being delivered from the compressor/expander 204. After the pressure within the low storage 206 reaches the predetermined level and/or substantially equals the pressure of the compressed gas delivered from the compressor/expander 204, the liquid can be moved (or “displaced” by the compressed gas) out of the low storage 206 to another fluid storage location such as, for example, the high storage 208 via the liquid pathway 214. Furthermore, pressure within the low storage may be managed by controlled admittance of liquid from low storage 206 into high storage 208.
The high storage 208 can be in fluid communication with the low storage 206 via the liquid pathway 214 and configured to contain the liquid at a second elevation, higher than the first elevation. The high storage 208 can be, for example, a brine pond opened directly to the atmosphere at or near ground level. The pressure head of the liquid stored in the high storage 208 produces a pressure on the gas (and liquid) contained in low storage 206.
By employing a pressure compensation system, the pressure in a cavern storage structure can be held relatively constant throughout filling and/or discharge of the cavern, and delivery pressure of the stored gas may be kept relatively constant. This may avoid the problems associated with uncompensated storage of gases, including structural concerns due to over pressuring or under pressuring, or structural concerns due to relatively high rates of pressure change. Furthermore, in applications wherein a stored gas is to be employed to provide power generation (e.g., in a compressed air energy storage system), the delivery pressure of the stored gas can be relatively constant, providing a continuous, relatively constant delivery pressure to power-generation equipment (e.g., turbines), which can provide relatively constant energy generation.
In some embodiments, the present caverns have a relatively gradual and constant incline. Such a gradual, constant incline can prevent trapping of air and/or compensating fluid pockets in the present caverns. In some embodiments, a borehole at the terminus of a cavern may provide venting of the cavern during injection and/or removal of stored gases, for example, to prevent trapping of gas pockets during liquid injection. Further, when pressure compensation systems are employed, a venting system may prevent pockets of compensation liquids from being trapped.
As shown in
Alternatively, as shown in
In some embodiments, the depth of the cavern(s) may be selected based on the lithostatic pressure provided by the overburden of the rock formation in which the caverns are constructed so that the overburden is providing a compressive force on the cavern structure that is equal to or greater than the expansive force imposed on the cavern structure by the pressurized fluid. Said another way, at certain depths, the lithostatic pressure of the overburden can exert a force on an excavated cavern causing the cavern to deform or otherwise become structurally unstable. At greater depths in the same type of rock formation, the lithostatic pressure acting on the excavated cavern in the vertical direction can become more equalized with the pressure acting on the cavern in the horizontal direction, thus exerting forces on the cavern that are more stable. In some embodiments, the depth of the cavern can be selected such that the lithostatic pressure of the overburden is greater than that of the desired working pressure of the storage cavern. Operating the cavern in a regime where the lithostatic pressure is greater than that of the fluid storage pressure can prevent fractures in the cavern walls, which may be formed from fluid pressure exceeding the overburden pressure, i.e. by placing the walls of the cavern in tension rather than in compression.
As shown in
In some embodiments, the system may operate with a cavern pressure greater than the hydrostatic pressure at the depth of the cavern (i.e. the pressure produced by a column of the compensating liquid equal in height to the depth of the cavern). For example, the cavern can be operated at a pressure in a range between the hydrostatic pressure PH2O and lithostatic pressure or vertical stress σV. In some embodiments, the operating pressure of the cavern can be selected to optimize the compressed gas storage capacity of the cavern and provide structural integrity to the cavern. Said another way, increasing the operating pressure of the cavern increases the mass of compressed gas that can be stored in the cavern and can provide additional structural support for the cavern itself since the pressure differential between the lithostatic pressure and the pressure of the fluids being stored is reduced.
The operating pressure of the storage cavern can be increased above the hydrostatic pressure by pumping or otherwise increasing the pressure of the compensating liquid used in the system. For example, referring now back to
Embodiments of the storage caverns can be installed below natural and man-made surface features that have depth; such as, within quarries, mines, at the base of hydro-dams, at the bottom of canyons, into the side of cliffs, mountains, near oceans or other bodies of water (e.g. lakes or reservoirs). The lithostatic stress below these features reflects the stress at a depth measured from the top of these features. The apparent depth, for reaching the caverns, is shallower then the depth that defines the lithostatic stress in the formation (top of the surface feature). This results in potentially lower cost to bore a shaft to the cavern. There is also value in co-locating the construction site for a cavern at an existing mine or quarry because the site already has much of the industrial and regulatory accoutrements required to construct the caverns. If co-located at the base of a hydro-electric dam, a CAES unit utilizing cavern air storage may utilize the power lines at the site distributing power for the dam, and the water head behind the dam will assist in the pressure compensation requirements of the tunnel air storage.
Individual caverns may also be combined in an array. For example,
The spacing of the nested spirals shown in
While the nested spiral array of
In some embodiments, multiple boreholes can be used, for example, at the beginning and the end of each individual cavern.
Individual caverns in an array may have the same or similar geometry (e.g., length, diameter, plan geometry). Alternatively, in some embodiments, individual caverns in an array may have different geometries. For example, a spiral array may include individual spirals having different lengths. The length of individual caverns may be selected such that the termini are arrayed for interconnection. In other embodiments, individual caverns may have different shapes (e.g., circles, spirals, linear or zigzag shapes) which may be combined in array. Such combinations may allow for avoidance of undesirable geologic features, or may facilitate interconnection of individual caverns. For example, an array may comprise spiral caverns and straight caverns intersecting one or more segments of spiral caverns in an array. Alternatively, in some embodiments, tangent circles, spiral, and straight segments may be combined to provide an interconnecting array of caverns. The combination of shapes in the array is generally limited only by the technical limitations of, e.g., a TBM to cut those shapes (e.g., turning radius).
Some embodiments may combine cavern geometries in an array to, e.g., allow for expeditious removal of cutting debris during the formation of the array, or to allow for use of excavated portions of a cavern or cavern array while other portions are being constructed. Thus, a storage cavern array can be constructed and certain portions of individual caverns or portions of an array may be used for storage of fluid while constructing other portions of a cavern array. In such embodiments, pressure isolation of potions of single cavern, several individual caverns, or portions of an array of caverns may be fluidically isolated as described herein to allow for use of completed portions of an array, while construction of other portions of an array are being constructed. Thus, the present array can provide a high degree of flexibility for simultaneous construction of caverns while employing portions that have previously been constructed for storage applications.
In addition, as described above with respect to
As shown in
The parameters described above with respect to individual caverns and cavern arrays are applicable to patterns of arrays. For example, a single array may comprise multiple shapes or geometries of individual caverns, and individual caverns of different geometries may be interconnected in a single array. Then a single array, comprising several caverns of differing geometries, can be configured to provide an extended array of either isolated or interconnected caverns with varying individual cavern geometries. Similarly, multiple arrays may be interconnected by straight or curved segments, and multiple arrays may be connected by one or more vertical boreholes. Further, various array geometries may be combined in an extended array. For example, in some embodiments, a single array of spiral caverns may be coupled or interconnected to other array geometries. In certain embodiments, an array of cotangent circles (e.g., internal, external) can be combined with one or more spiral arrays, linear arrays, or combinations thereof. The overall plan geometry is not limited, and the selection of shapes may be selected to minimize excavation costs, and/or to avoid undesirable geologic features while maximizing storage area. Furthermore, the present extended arrays may allow for planning and construction of a storage facility to allow for use of some excavated caverns in an array while other caverns are constructed. Furthermore, the overall plan geometry of an extended array of caverns can be selected to minimize construction costs, avoid undesirable geologic features, and/or maximize storage density. Further, as described above, the present extended cavern arrays may be operated in an uncompensated manner, or may employ a pressure compensation system. In the present extended arrays, different arrays can be either interconnected or selectively isolated or interconnected to provide multiple extended caverns with different working pressures.
In some embodiments, the caverns may also be constructed in a three-dimensional array.
Vertical spacing of arrays may be determined based on rock strength and properties of the geologic formation in which the present storage caverns are constructed. For example, spacing may be selected to ensure mechanical stability of vertically disposed caverns, and to ensure fluidic isolation of each level of caverns in a vertical arrangement. In addition, as described above, a cavern or caverns at a first depth can be fluidically isolated from a cavern or caverns at a second depth (e.g., deeper or shallower) such that each level of cavern(s) may be operated at different working pressures. Alternatively, a cavern or caverns at a first depth can be connected to a cavern or caverns at a second depth (e.g., deeper or shallower) for operation at the same or similar working pressure. Selection of depths and number of levels in a vertical arrangement of caverns or arrays of cavern may selected such that the lithostatic pressure differential from the top of a vertical arrangement to the bottom of a vertical arrangement is small enough to allow for interconnection of multiple levels, and allow for use of the vertical arrangement of caverns to be operated over a selected working pressure.
As shown in
Vertical arrangements of horizontal arrays may employ levels of caverns having the same geometry, or individual levels may employ different geometries. For example, certain levels may comprise caverns with geometries selected to avoid undesirable geometric features, while other levels may, in the absence of such geologic features at the level which they are constructed, need not terminate to avoid such features. Accordingly, design considerations applicable to single caverns, arrays of caverns, and interconnected arrays of caverns on a single level are also applicable to the present vertical dispositions of caverns and/or cavern arrays. Accordingly, multiple geometries, number of caverns, length of individual caverns, number of vertical boreholes, sharing of vertical boreholes between individual caverns, and spacing of caverns both vertically and horizontally, may be selected to maximize the storage density for a given area.
As shown in
The present caverns, and combinations of individual caverns in horizontal arrays, interconnection of horizontal arrays, and vertical disposition of horizontal arrays provides a wide range of design, construction and installation possibilities to provide increased storage density, design flexibility, and freedom with respect to location of a storage facility relative to conventional subsurface storage facilities (e.g., salt domes, depleted hydrocarbon reservoirs). Furthermore, the use of surface manifolds, selective interconnection of caverns, arrays and levels, coupled with pressure compensation systems, allows for a many possible combinations which confer a high degree of flexibility for operation of the present storage caverns and facilities employing those caverns, e.g., in compressed air energy storage and generation facilities. Accordingly, embodiments of the present invention provide high density storage facilities, and may provide a cost effective alternative to conventional subsurface and above ground storage facilities, which may be conveniently located for specific applications.
Certain embodiments of the present invention are described above. It is, however, expressly noted that the present invention is not limited to those embodiments, but rather the intention is that additions and modifications to what is expressly described herein are also included within the scope of the invention. Moreover, it is to be understood that the features of the various embodiments described herein are not mutually exclusive and can exist in various combinations and permutations, even if such combinations or permutations are not made express herein, without departing from the spirit and scope of the invention. In fact, variations, modifications, and other implementations of what is described herein will occur to those of ordinary skill in the art without departing from the spirit and the scope of the invention. As such, the invention is not to be defined only by the preceding illustrative description, but rather by the claims.
This application claims priority to and the benefit of U.S. Provisional Patent Application No. 61/648,972, filed May 18, 2012, and entitled “Excavated Underground Caverns for Fluid Storage,” the entirety of which is hereby incorporated herein by reference.
Filing Document | Filing Date | Country | Kind |
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PCT/US2013/041576 | 5/17/2013 | WO | 00 |
Number | Date | Country | |
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61648972 | May 2012 | US |