This invention relates to marine seismic systems and more particularly relates to autonomous seismic nodes that may be deployed on the seabed.
Marine seismic data acquisition and processing generates a profile (image) of a geophysical structure under the seafloor. Reflection seismology is a method of geophysical exploration to determine the properties of the Earth's subsurface, which is especially helpful in determining an accurate location of oil and gas reservoirs or any targeted features. Marine reflection seismology is based on using a controlled source of energy (typically acoustic energy) that sends the energy through seawater and subsurface geologic formations. The transmitted acoustic energy propagates downwardly through the subsurface as acoustic waves, also referred to as seismic waves or signals. By measuring the time it takes for the reflections or refractions to come back to seismic receivers (also known as seismic data recorders or nodes), it is possible to evaluate the depth of features causing such reflections. These features may be associated with subterranean hydrocarbon deposits or other geological structures of interest.
In general, either ocean bottom cables (OBC) or ocean bottom nodes (OBN) are placed on the seabed. For OBC systems, a cable is placed on the seabed by a surface vessel and may include a large number of seismic sensors, typically connected every 25 or 50 meters into the cable. The cable provides support to the sensors, and acts as a transmission medium for power to the sensors and data received from the sensors. One such commercial system is offered by Sercel under the name SeaRay®. Regarding OBN systems, and as compared to seismic streamers and OBC systems, OBN systems have nodes that are discrete, autonomous units (no direct connection to other nodes or to the marine vessel) where data is stored and recorded during a seismic survey. One such OBN system is offered by the Applicant under the name Manta®. See, e.g., U.S. Pat. No. 9,523,780. For OBN systems, seismic data recorders are placed directly on the ocean bottom by a variety of mechanisms, including by the use of one or more of Autonomous Underwater Vehicles (AUVs), Remotely Operated Vehicles (ROVs), by dropping or diving from a surface or subsurface vessel, or by attaching autonomous nodes to a cable that is deployed behind a marine vessel. See, e.g., U.S. Pat. No. 9,784,873. In other embodiments, the seismic node may be integrated with an AUV. One such OBN system is offered by the Applicant under the name Spicerack®. See, e.g., U.S. Pat. Nos. 9,873,496; 10,322,783; 10,543,892.
Autonomous ocean bottom seismic nodes are independent seismometers, and in a typical application they are self-contained units comprising a housing, frame, skeleton, or shell that includes various internal components such as geophone and hydrophone sensors, a data recording unit, a reference clock for time synchronization, and a power source. The power sources are typically battery-powered, and in some instances the batteries are rechargeable. In operation, the nodes remain on the seafloor for an extended period of time. Once the data recorders are retrieved, the data is downloaded and batteries may be replaced or recharged in preparation of the next deployment. Various designs of ocean bottom autonomous nodes are well known in the art, and may have any number of configurations. Other prior art systems include a deployment rope/cable with integral node casings or housings for receiving autonomous seismic nodes or data recorders. Traditional prior art nodes are often made of tubes of various shapes that are joined and/or coupled together with cables, which can be vulnerable to handling and assembly errors. Other prior nodes can be made of spherical glass pressure housings that need additional protection and are less than ideal for storage, handling, and stability when on the seabed. Other prior are nodes are expensive to manufacture and difficult to deploy and couple to the seabed.
The referenced shortcomings are not intended to be exhaustive, but rather are among many that tend to impair the effectiveness of previously known techniques in seafloor deployment systems; however, those mentioned here are sufficient to demonstrate that the methodologies appearing in the art have not been satisfactory and that a significant need exists for the systems, apparatuses, and techniques described and claimed in this disclosure.
A need exists for an improved autonomous seismic node design for automated node deployment, recovery, handing, and storage. A need exists for a node that provides increased operational parameters, increased seabed coupling, and more versatile deployment options. A need exists for a seismic node design that can be mass-produced in a cost-effective manner. A need exists for a node that can be used in multiple deployment configurations. A need exists for a seismic node design that enables large numbers of nodes to be operated in the field.
An autonomous seismic node that is configured for free-fall from the water surface to the seabed and that is capable of popping up and/or rising from the seabed to the water surface on its own. The seismic node is substantially cylindrical and/or tubular in shape and is positively buoyant in water. The node comprises an upper end cap assembly and a lower end cap assembly, each of which is inserted into an end of the tubular housing. The seismic node may be coupled to an anchor weight system to assist in free fall to the seabed, or may be coupled to a seabed coupling device that allows for traditional seabed seismic recording. The anchor weight system may comprise a first part coupled to the seismic node via a tether, and a second part directly attached to the seismic node, each of which may be separately released from the seismic node. The seismic node is positively buoyant, and may be coupled to a detachable/removable anchor weight that provides an overall negative buoyancy to the node and assists in free fall of the seismic node to the seabed. The detachable weight system may be comprised of two separately detachable parts—a first part that comprises a heavy anchor weight and a second part that is not as dense and which gives the seismic node approximately neutral buoyancy. The lower end cap assembly may contain the seismic sensors and battery cells, and the upper end cap assembly may contain any acoustic devices. A plurality of seismic nodes may be dropped from a surface vessel into a body of water, and free-fall to the seabed. After seismic recording is performed as is known in the art, the anchor weight and/or seabed coupling device may be detached, thereby causing the seismic node to rise to the water surface based on the positive buoyancy of the device.
An autonomous seismic node is configured for free-fall from a water surface to the seabed and is capable of rising from the seabed on its own. The seismic node is positively buoyant in water and is substantially tubular in shape, with a length to a diameter ratio of 4:1 or greater. The node comprises a lower section and an upper section, each of which is inserted into an end of a tubular housing. The lower section has a lower end cap assembly with a release mechanism and the upper section has an upper end cap assembly with a plurality of electronic components and a detachable lifting cage. The seismic node may be coupled to a detachable anchor weight or seabed coupling device to assist in free fall to the seabed, and when detached after seismic recording is performed, allows the seismic node to rise to the water surface.
Disclosed is an autonomous seismic node for deployment to the seabed, that comprises a pressurized node housing, wherein at least one seismic sensor, at least one data recording unit, and at least one clock are located within the pressurized node housing, and wherein the node housing is substantially tubular and has a length to a diameter ratio of 4:1 or greater. The node housing may have a length to diameter ratio of 8:1 or greater. The node housing may have a center of gravity and a center of buoyancy, wherein the center of gravity is below the center of buoyancy. The node housing may have an internal buoyancy chamber, such that the node housing is positively buoyant. The buoyancy chamber may be empty space or may be buoyant materials that are less dense than water. The seismic node may comprise a detachable lifting cage coupled to an upper section of the node housing.
The seismic node may have a node housing that comprises an upper section, a lower section, an upper end cap assembly coupled to the upper section, and a lower end cap assembly coupled to the lower section. The end cap assemblies may be coupled to the upper and lower sections of the node housing via a plurality of clips. Each of clips may be substantially flat and have wedge and/or dog-boned shapes. A first plurality of clips may attach the upper end cap assembly to the node housing and a second plurality of clips may attach the lower end cap assembly to the node housing. Each of the first plurality of clip may fit within a first plurality of corresponding recesses on the upper section and the upper end cap assembly and the second plurality of clip may fit within a second plurality of corresponding recesses on the lower section and the lower end cap assembly. The upper end cap assembly may have a hydrophone, an acoustic transducer, a satellite transducer, and an electronic connector. The lower cap assembly may be comprise a release mechanism, which may be coupled to a tether, anchor weight, or seabed coupling device that can be detached from the seismic node. The lower cap assembly may comprise and/or be coupled to a plurality of battery cells and a plurality of seismic sensors within the node housing. The upper and lower end cap assemblies may comprise a polymer material.
The seismic node may further comprise at least one anchor weight coupled to the node housing that is configured to be released from the seismic node by an acoustic signal. The seismic node housing may be positively buoyant in water. The at least one anchor weight may be coupled to the node housing via a flexible tether or directly attached to the bottom of the seismic node. The at least one anchor weight may comprise a seabed coupling device. The at least one anchor weight may comprise a first anchor weight and a second anchor weight, such that the first anchor weight is directly attached to the node housing and the second anchor weight is coupled to the first anchor weight via a tether, wherein the first anchor weight is positioned between the seismic node and the second anchor weight. The first and second anchor weights can be released from the seismic node by an acoustic signal by the use of a release mechanism assembly on the lower end cap of the seismic node. The second anchor weight may be coupled to the seabed when the seismic node is near the bottom of the ocean and has fully descended. A combination of the seismic node housing and the at least one anchor weight may be negatively buoyant in water. A combination of the seismic node and the first anchor weight may be approximately neutrally buoyant in water. A combination of the seismic node, the first anchor weight, and the second anchor weight may be negatively buoyant in water. The first and second anchor weights may be different weights, such that the second anchor weight is heavier than the first anchor weight.
The seismic node comprises a positively buoyant section and a negatively buoyant section, wherein the negatively buoyant section is removably detached from the positively buoyant section. The negatively buoyant section may comprise an anchor weight or a seabed coupling device. The positively buoyant section may comprise an internal buoyancy chamber of the seismic node, or may comprise an external buoyancy jacket or sleeve. The seismic node may comprise or be coupled to a flotation jacket configured to substantially surround the seismic node housing. The combination of the seismic node housing and the flotation jacket may be positively buoyant in water.
Disclosed is an autonomous seismic node for deployment to the seabed, comprising a pressurized node housing, wherein at least one seismic sensor, at least one data recording unit, and at least one clock are located within the pressurized node housing, and an anchor weight removably attached to a lower section of the node housing. The node housing may be substantially tubular and/or cylindrical and has a length to a diameter ratio of 4:1 or greater. An upper section and a lower section may be inserted into the node housing. An anchor weight may be coupled to the node housing via a flexible tether. The anchor weight may comprise a seabed coupling device that is directly coupled to the node housing. The seabed coupling device may comprise one or more of a plate, a tripod, a tripod base, one or more ribbed spears, and/or an open-ended pipe base. The anchor weight may comprise a biodegradable material. The anchor weight may be configured to be released from the seismic node by an acoustic signal.
Disclosed is a method for deploying an autonomous seismic node to the seabed, comprising providing a seismic node on a back deck of a marine vessel, coupling an anchor weight to the node housing while the seismic node is on the back deck of the marine vessel, and deploying the seismic node with the coupled anchor weight from the surface vessel to the bottom of the ocean. The method may further comprise coupling the anchor weight to the bottom of the ocean. The method may further comprise retrieving the node housing from the bottom of the ocean. The method may further comprise releasing the anchor weight from the node housing based on an acoustic signal and surfacing the node housing near a surface of a body of water. The method may further comprise recording seismic signals on the ocean bottom. The seismic node may comprise a pressurized node housing, wherein at least one seismic sensor, at least one data recording unit, and at least one clock are located within the pressurized node housing, wherein the node housing is substantially tubular and has a length to a diameter ratio of 4:1 or greater.
The following drawings form part of the present specification and are included to further demonstrate certain aspects of the present invention. The invention may be better understood by reference to one or more of these drawings in combination with the detailed description of specific embodiments presented herein.
Various features and advantageous details are explained more fully with reference to the non-limiting embodiments that are illustrated in the accompanying drawings and detailed in the following description. Descriptions of well-known starting materials, processing techniques, components, and equipment are omitted so as not to unnecessarily obscure the invention in detail. It should be understood, however, that the detailed description and the specific examples, while indicating embodiments of the invention, are given by way of illustration only, and not by way of limitation. Various substitutions, modifications, additions, and/or rearrangements within the spirit and/or scope of the underlying inventive concept will become apparent to those skilled in the art from this disclosure. The following detailed description does not limit the invention.
Reference throughout the specification to “one embodiment” or “an embodiment” means that a particular feature, structure, or characteristic described in connection with an embodiment is included in at least one embodiment of the subject matter disclosed. Thus, the appearance of the phrases “in one embodiment” or “in an embodiment” in various places throughout the specification is not necessarily referring to the same embodiment. Further, the particular features, structures, or characteristics may be combined in any suitable manner in one or more embodiments.
Disclosed is an autonomous seismic node that, in one embodiment, is designed for free-fall from the water surface to the seabed and that is capable of popping up and/or rising from the seabed to the water surface on its own. In one embodiment, the seismic node is substantially cylindrical and/or tubular in shape. The seismic node may have a length to a diameter ratio of 4:1 or greater. The seismic node comprises a positively buoyant section and a negatively buoyant section, wherein the negatively buoyant section is removably detached from the positively buoyant section. The seismic node may be coupled to one or more anchor weights. The anchor weight may be directly coupled to the seismic node or coupled to the seismic node via a flexible tether. In other embodiments, the anchor weight may be a seabed coupling device that allows for traditional seabed seismic recording. The seismic node comprises one or more seismic sensors that are configured to record seismic signals while on the ocean floor, a digital recording device, a clock, and one or more power sources (such as battery cells). The seismic node may also have a radio or satellite transponder with GPS positioning capability and any necessary acoustic communication devices, such as an integrated USBL. In one embodiment, the seismic node comprises an upper end cap assembly and a lower end cap assembly, each of which is inserted into the tubular housing. The lower end cap assembly may be coupled to the geophones and battery cells, and the upper end cap assembly may be coupled to any acoustic devices. A buoyancy chamber may be located between the upper and lower end cap assemblies to provide positive buoyancy to the seismic node.
In one embodiment, a plurality of seismic nodes may be dropped from a surface vessel into a body of water, and free-fall to the bottom of the water, such as the seabed. The combination of the seismic node and the coupled anchor weight is overall negatively buoyant, such that the seismic node sinks to the ocean bottom. On the seafloor the position and orientation of the seismic node must be known, and in one embodiment the location of each seismic node may be determined by USBL position and any necessary acoustic transducers. After seismic recording is performed, as is known in the art, the anchor weight and/or seabed coupling device may be detached, thereby causing the seismic node to rise to the water surface based on the overall positive buoyancy of the device without the anchor weight. In one embodiment, the seismic node is configured to receive an acoustic command to autonomously return to the surface at the end of the survey and release any anchor weight for the seismic node to rise. In one embodiment, the seismic node does not have a separate propulsion system (and is thus not an AUV), and merely falls to and rises from the seabed based on its own static buoyancy.
In one embodiment, the seismic node is designed for rapid descent and minimal drift during descent to the seabed due to lateral current forces. The design and configuration of the seismic node is ideal for storage and transportation. In one embodiment (see
FIG . 1B is a schematic diagram illustrating another embodiment of an autonomous seismic node 101 according to the present disclosure. The embodiment in
In one embodiment, the node housing may contain electronics internally and externally to the housing, as is known in the art. On the upper end of the housing may be located various external acoustic devices and/or communication devices 111, such as a USBL transducer, antennae, hydrophones, and other connectors, as is known in the art. Within the housing may be located all of the electronic equipment, such as seismic recording devices 117 (geophones), PCB assemblies 113, battery packs 115, etc.
In one embodiment, the battery cells may be lithium-ion battery cells or rechargeable battery packs for an extended endurance (such as 90 days) on the seabed, but one of ordinary skill will recognize that a variety of alternative battery cell types or configurations may also be used. Additionally, the seismic node may include a pressure release valve configured to release unwanted pressure from the seismic node at a pre-set level. The valve protects against fault conditions like water intrusion and outgas sing from a battery package. Additionally, the seismic node may include an electrical connector configured to allow external access to information stored by internal electrical components, data communication, and power transfer. During the deployment the connector may be covered by a pressure proof watertight cap. In other embodiments, the node does not have an external connector and data is transferred to and from the node wirelessly, such as via electromagnetic or optical links.
In an embodiment, the internal electrical components may include one or more hydrophones, one or more (preferably three) geophones or accelerometers, and a data recorder. In an embodiment, the data recorder may be a digital autonomous recorder configured to store digital data generated by the sensors or data receivers, such as the hydrophone and the one or more geophones or accelerometers. One of ordinary skill will recognize that more or fewer components may be included in the seismic node. For example, there are a variety of sensors that can be incorporated into the node including and not exclusively, inclinometers, rotation sensors, translation sensors, heading sensors, and magnetometers. Except for the hydrophone, these components are preferably contained within the node housing that is resistant to temperatures and pressures at the bottom of the ocean, as is well known in the art.
In one embodiment, the seismic sensor may include one or more of a hydrophone, geophone, accelerometer, etc. For example, if a 4C (four component) survey is desired, the seismic sensors may include three geophones and a hydrophone, i.e., a total of four sensors. Alternatively, the seismic sensor may additionally include one or more accelerometers. Of course, other sensor combinations are possible, and may include one or more of a hydrophone, geophone, accelerometer, electromagnetic sensor, depth sensor, MEMs, Inertial Measurement Unit (IMU) or a combination thereof and which could be used together to measure up to six degrees of freedom. The seismic sensor may be located completely or partially inside body housing, while in some embodiments it may be located outside body housing when better water coupling/exposure is needed (e.g., for hydrophones). A memory unit may be connected to processor and/or seismic sensor for storing seismic data recorded by seismic sensor. A power system (such as one or more batteries) may be used to power all these components. The node may also include a clock and digital data recorder (not shown).
The seismic node may include a compass and other sensors as, for example, an altimeter for measuring its altitude, a pressure gauge, an interrogator module, etc. The node may optionally include an obstacle avoidance system and a communication device (e.g., Wi-Fi or other wireless interface, such as a device that uses an acoustic link) or other data transfer device capable of wirelessly transferring seismic data and/or control status data. One or more of these elements may be linked to processor. The seismic node may further include an antenna (which may be flush with or protrude from the housing) and a corresponding acoustic system for subsea communications. For surface communications (e.g., while the seismic node is on a ship), one or more of an antenna and communication device may be used to transfer data to and from the seismic node.
The seismic node systems may use an acoustic system as is known in the art. The acoustic system may be an Ultra-Short Baseline (USBL) system, also sometimes known as Super Short Base Line (SSBL) or Short Base Line (SBL) This system uses a method of underwater acoustic positioning. A complete USBL system may include a transceiver or acoustic positioning system mounted on a pole under a vessel or ROV (such as Hi-PAP or μPAP, commercially available by Kongsberg and Sonardyne) and a transponder on the seismic node. In general, a hydro-acoustic positioning system consists of both a transmitter and a receiver, and any Hi-PAP or μPAP or transponder system acts as both a transmitter and a receiver. An acoustic positioning system uses any combination of communications principles for measurements and calculations, such as SSBL. In one embodiment, the acoustic positioning system transceiver comprises a spherical transducer with hundreds of individual transducer elements. A signal (pulse) is sent from the transducer (such as a Hi-PAP or μPAP head on the surface vessel), and is aimed towards the seabed transponder located on the seismic node. This pulse activates the transponder on the seismic node, which responds to the vessel transducer after a short time delay. The transducer detects this return pulse and, with corresponding electronics, calculates an accurate position of the transponder (seismic node) relative to the vessel based on the ranges and bearing measured by the transceiver. In one embodiment, to calculate a subsea position, the USBL system measures the horizontal and vertical angles together with the range to the transponder (located in the seismic node) to calculate a 3D position projection of the seismic node relative to a separate station, basket, ROV, or vessel. An error in the angle measurement causes the position error to be a function of the range to the transponder, so an USBL system has an accuracy error increasing with the range. Alternatively, a Short Base Line (SBL) system, an inverted short baseline (iSBL) system, or an inverted USBL (iUSBL) system may be used, the technology of which is known in the art. For example, in an iUSBL system, the transceiver is mounted on or inside the seismic node while the transponder/responder is mounted on a separate vessel/station and the seismic node has knowledge of its individual position rather than relying on such position from a surface vessel (as is the case in a typical USBL system). In another embodiment, a long baseline (LBL) acoustic positioning system may be used. In a LBL system, reference beacons or transponders are mounted on the seabed around a perimeter of a work site as reference points for navigation. The LBL system may use an USBL system to obtain precise locations of these seabed reference points. Thus, in one embodiment, the reference beacon may comprise both an USBL transponder and a LBL transceiver. The LBL system results in very high positioning accuracy and position stability that is independent of water depth, and each seismic node can have its position further determined by the LBL system. The acoustic positioning system may also use an acoustic protocol that utilizes wideband Direct Sequence Spread Spectrum (DSSS) signals. In one embodiment, the seismic node is equipped with a plurality of communication devices, such as an USBL beacon capable of receiving and transmitting acoustic signals, a phased array receiver (or system) that is able to determine the direction of an incoming acoustic signal by analysis of the signal phase, and an acoustic modem.
Those skilled in the art would appreciate that more or less components and electronic devices may be added to or removed from the seismic node.
In one embodiment, the node is designed to keep the center of buoyancy high in the seismic node and the center of gravity low. In this embodiment, the center of gravity (COG) is below the center of buoyancy (COB). In one embodiment, a positive buoyancy chamber is designed in the upper section of the node, while the battery packs and geophones are positioned in the bottom of the node. In one embodiment, the geophones are designed as close to the lower end cap as possible. In one embodiment, the geophones are velocity sensors, and the further away from the pivot point of the node, the larger the generated signal as a result of inadvertent movement, which could negatively impact the fidelity of the intended signal. Having the COB located above the COG ensures that the node descends the water column as vertically as possible such that the upper section of the node faces towards the water surface or sky during descent. The same trait is preferred when the node is released from the seafloor. When the nodes surfaces to the ocean surface, the wireless transponder located on the top cap should have a clear, un-obstructed view of the sky. The farther the COB is away from the COG, the more stable the node becomes. In one embodiment, the node's design and shape allows the nope to remain substantially vertical in the ocean bottom and near the ocean surface, which facilitates methods for the automated recovery of the nodes.
In one embodiment, the seismic node of
In each of the embodiments illustrated in
In one embodiment, upper end cap 803 can be a CNC machined component made from polymer, and may be formed by injection mold. Using a polymer based material eliminates and/or reduces corrosion issues. The upper end cap may be inserted into an open end of the seismic node housing (such as housing 701 from
A detachable lifting cage 1111 is illustrated in
In one embodiment, disclosed is a method for deploying a plurality of autonomous seismic nodes to the seabed. In one embodiment, the method comprises providing a seismic node on a back deck of a marine vessel, coupling an anchor weight to the node housing while the seismic node is on the back deck of the marine vessel, and deploying the seismic node with the coupled anchor weight from the surface vessel to the bottom of the ocean by allowing the node to free fall and/or descend on its own to the bottom of the seabed because of the coupled anchor weight. The method may further comprise coupling the anchor weight to the bottom of the ocean and retrieving the node housing from the bottom of the ocean. In one embodiment, the method may further comprise releasing the anchor weight from the node housing based on an acoustic signal and surfacing the node housing near a surface of a body of water. In one embodiment, the seismic node is substantially similar to the nodes described herein. For example, the seismic node may comprise a pressurized node housing, wherein at least one seismic sensor, at least one data recording unit, and at least one clock are located within the pressurized node housing, wherein the node housing is substantially tubular and has a length to a diameter ratio of 4:1 or greater.
Many other variations in the overall configuration of the node, node housing, anchor weight, and seabed coupling device are possible within the scope of the invention. For example, the node itself may be positively buoyant by itself and/or with a buoyant flotation jacket. The node may or may not use a detachable lifting cage. All or some of the components left on the seabed may be biodegradable or environmentally friendly. The nodes may be dropped from a marine surface vessel or an underwater ROV. The diameter of the tube may range between 3″ to 12″, and the length of the tube may range from 12″ to 96″. Portions of the node may be metallic or non-metallic, including the pressurized node housing. Clips and/or fasteners may or may not be used to couple the end caps to the node housing. It is emphasized that the foregoing embodiments are only examples of the very many different structural and material configurations that are possible within the scope of the present invention.
Although the invention(s) is/are described herein with reference to specific embodiments, various modifications and changes can be made without departing from the scope of the present invention(s), as set forth in the claims below. Accordingly, the specification and figures are to be regarded in an illustrative rather than a restrictive sense, and all such modifications are intended to be included within the scope of the present invention(s). Any benefits, advantages, or solutions to problems that are described herein with regard to specific embodiments are not intended to be construed as a critical, required, or essential feature or element of any or all the claims.
Unless stated otherwise, terms such as “first” and “second” are used to arbitrarily distinguish between the elements such terms describe. Thus, these terms are not necessarily intended to indicate temporal or other prioritization of such elements. The terms “coupled” or “operably coupled” are defined as connected, although not necessarily directly, and not necessarily mechanically. The terms “a” and “an” are defined as one or more unless stated otherwise. The terms “comprise” (and any form of comprise, such as “comprises” and “comprising”), “have” (and any form of have, such as “has” and “having”), “include” (and any form of include, such as “includes” and “including”) and “contain” (and any form of contain, such as “contains” and “containing”) are open-ended linking verbs. As a result, a system, device, or apparatus that “comprises,” “has,” “includes” or “contains” one or more elements possesses those one or more elements but is not limited to possessing only those one or more elements. Similarly, a method or process that “comprises,” “has,” “includes” or “contains” one or more operations possesses those one or more operations but is not limited to possessing only those one or more operations.
This application claims priority to U.S. provisional patent application No. 63/277,907, filed on Nov. 10, 2021, the entire contents of which is incorporated herein by reference.
Number | Date | Country | |
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63277907 | Nov 2021 | US |