This specification relates to the field of mineral and hydrocarbon recovery, and more particularly to the use of high-molecular weight polyglycolic acid as a primary structural member for a dissolvable oilfield tool.
It is well known in the art that certain geological formations have hydrocarbons, including oil and natural gas, trapped inside of them that are not efficiently recoverable in their native form. Hydraulic fracturing (“fracking” for short) is a process used to fracture and partially collapse structures so that economic quantities of minerals and hydrocarbons can be recovered. The formation may be divided into zones, which are sequentially isolated, exposed, and fractured. Fracking fluid is driven into the formation, causing additional fractures and permitting hydrocarbons to flow freely out of the formation.
It is also known to create pilot perforations and pump acid through the pilot perforations into the formation, thereby dissolving the formation and allowing the hydrocarbons to migrate to the larger formed fractures or fissure.
To frac multiple zones, untreated zones must be isolated from already-treated zones so that hydraulic pressure fractures the new zones instead of merely disrupting the already-fracked zones. There are many known methods for isolating zones, including the use of a frac sleeve, which includes a mechanically-actuated sliding sleeve engaged by a ball seat. A plurality of frac sleeves may be inserted into the well. The frac sleeves may have progressively smaller ball seats. The smallest frac ball is inserted first, passing through all but the last frac sleeve, where it seats. Applied pressure from the surface causes the frac ball to press against the ball seat, which mechanically engages a sliding sleeve. The pressure causes the sleeve to mechanically shift, opening a plurality of frac ports and exposing the formation. High-pressure fracking fluid is injected from the surface, forcing the frac fluid into the formation, and the zone is fracked.
After that zone is fracked, the second-smallest frac ball is pumped into the well bore, and seats in the penultimate sleeve. That zone is fracked, and the process is continued with increasingly larger frac balls, the largest ball being inserted last. After all zones are fracked, the pumpdown back pressure may move frac balls off seat, so that hydrocarbons can flow to the surface. In some cases, it is necessary to mill out the frac ball and ball seat, for example if back pressure is insufficient or if the ball was deformed by the applied pressure.
It is known in the prior art to manufacture frac balls out of carbon, composites, metals, and synthetic materials such as nylon. When the frac ball has filled its purpose, it must either naturally flow of the well, or it must be destructively drilled out. Baker Hughes is also known to provide a frac ball constructed of a nanocomposite material known as “In-Tallic.” In-Tallic balls are advertised to begin dissolving within 100 hours in a potassium chloride solution.
Another style of frac ball can be pumped to a different style of ball seat, engaging sliding sleeves. The sliding sleeves open as pressure is increased, causing the sleeves to overcome a shearing mechanism, sliding the sleeve open, in turn exposing ports or slots behind the sleeves. This permits the ports or slots to act as a conduit into the formation for hydraulic fracturing, acidizing or stimulating the formation
In one exemplary embodiment, a plurality of mechanical tools for downhole use are described, each comprising substantial structural elements made with high molecular weight polyglycolic acid (PGA). The PGA material of the present disclosure loses crystalline structure under thermal stresses of at least approximately 250° F. within approximately 48 hours. After the crystalline structure breaks down, the material can be safely left to biodegrade over a period of several months. The products of biodegradation is naturally-occurring glycine within approximately 48 hours. After the crystalline structure breaks down, the material can be safely left to biodegrade over a period of several months. The products of biodegradation is naturally-occurring glycine within approximately 48 hours. After the crystalline structure breaks down, the material can be safely left to biodegrade over a period of several months. The products of biodegradation is naturally-occurring glycine within approximately 48 hours. After the crystalline structure breaks down, the material can be safely left to biodegrade over a period of several months. The products of biodegradation is naturally-occurring glycine.
FIG. 13A1 is a detailed view of the port void designated “DETAIL-C” in
FIG. 13A2 is a cross-section view of the plug voids of the isolation sub of
FIG. 13A3 is a cross-section view of the plug voids of the isolation sub of
FIG. 13B1 is a detailed view of an O-ring groove in the PGA plug designated “DETAIL-A” in
FIG. 13C1 is a detailed view of a of a retaining plug's screw head.
FIG. 13C2 is a detailed view of the O-ring groove designated “DETAIL-A” in
One concern in the use of frac sleeves with PGA frac balls is that the balls themselves can become problematic. Because it is impossible to see what is going on in a well, if something goes wrong, it is difficult to know exactly what has gone wrong. It is suspected that prior art frac balls can become jammed, deformed, or that they can otherwise obstruct hydrocarbon flow.
One known solution is to mill out the prior art frac balls and the ball seats. But milling is expensive and takes time away from production. Baker Hughes has introduced a nanocomposite frac ball called In-Tallic. In-Tallic balls will begin to dissolve within about 100 hours of insertion into the well, in the presence of potassium chloride. The In-Tallic material is relatively expensive and relatively unavailable.
Kuredux, and in particular Kuredux grade 100R60 is a biodegradable polyester with excellent mechanical properties and processability. Frazier, et al. have identified a method of processing Kuredux into mechanical tools for downhole drilling applications, for example for hydrocarbon and mineral recovery.
Polyglycolic (PGA) acid is a polyester of glycolic acid. PGA is known in the art to biodegrade within approximately 12 months. PGA also been shown to have excellent short-term stability in ambient conditions. For example, the Applicant has tested PGA frac balls of the present disclosure by leaving them in room temperature tap water for months at a time. After two months, the PGA frac balls showed no signs of substantial degradation or structural changes. PGA frac balls also show no sign of degradation in ambient moisture conditions over a period of several months.
In one test of an exemplary embodiment, a 3.375-inch PGA frac ball withstood 6,633 psi before structural failure. A 2.12-inch frac ball withstood 14,189 psi before failing. A 1.5-inch in frac ball with should at least 15,000 psi for 15 minutes without failing A failure point was not reached because the test rig was not able to exceed 15,000 psi. Thus, a PGA frac ball is suitable for high pressure downhole hydrocarbon recovery operations.
Advantageously, PGA frac balls can be pumped down a well bore from the surface. The pumping fluid is approximately 50 to 75° Fahrenheit, which conditions do not have any appreciable effect on the short-term structural integrity of the frac ball. When fracking operations are commenced, however, the temperature rises dramatically. In south Texas oil wells, temperatures range from 250° F. to 400° F. Temperature ranges vary around the world and thus may be higher or lower and other locations. Once the frac ball is exposed to the higher temperature and pressure conditions of the fracking operation, it begins to rapidly lose its crystalline structure. Under testing, a 140 g sample was placed in water at 150F for four days. After four days, the mass had fallen to 120 g. In a second test, a 160 g sample was placed in water at 200° F. for four days. After four days, the mass of the sample had reduced to 130 g. Acids may expedite dissolution. Kureha has provided the following formula for estimating single-sided degradation from thermal stress alone, measured in mm/h.
Amm 0.5e23.654-9443/K (1)
Because these time spans are consistent which the time in which a conventional frac ball would be drilled out, the frac ball can be used without further intervention from the operator. In an exemplary application, a series of frac balls is used in a fracking operation. As the frac balls begin to lose structure, their volumes decrease slightly and they pass through their respective ball seats and move toward the toe of the well bore. Over succeeding hours, the frac balls continue to lose structure until they eventually form a soft mush without appreciable crystalline structure. This material can be left downhole without concern. Over a period of months, the PGA material itself will biodegrade. In one exemplary embodiment, PGA frac balls substantially lose structure within approximately 48 hours in a well with an average temperature of approximately 250° F., and completely biodegrades over several months.
Further advantageously, degradation of PGA is commonly accomplished by random hydrolysis of ester bonds. The breaking of these ester bonds reduces PGA to glycolic acid, an organic substance that is not considered a pollutant and is not generally harmful to the environment or to people. Indeed, glycolic acid is used in many pharmaceutical preparations for absorption into the skin. Glycolic acid may further breakdown into glycine, or carbon dioxide and water. Thus, even in the case of PGA mechanical tools that are ultimately drilled out, the remnants can be safely discarded without causing environmental harm.
Degradation of PGA commonly takes place in two stages. In the first stage, water diffuses into the amorphous regions. In the second stage, the crystalline areas dissolved. Once serious degradation begins, it can progress rapidly. In many cases, a mechanical tool made of PGA will experience sudden mechanical failure at an advantageous time after it has fulfilled its purpose, for example, within approximately 2 days. It is believed that mechanical failure is achieved by the first stage, wherein the crystalline structure is compromised by hydrolysis. The result is PGA particulate matter that otherwise retains its chemical and mechanical properties. Over time, the particulate matter enters the second stage and begins biodegradation proper.
Processing of the PGA material comprises purchasing an appropriate PGA and coliform from a supplier. In one embodiment, Kuredux branded PGA can be purchased from the Kureha Corporation. In an exemplary embodiment, grade 100R60 PGA is purchased from Kureha Corporation through its U.S. supplier, Itochu. Kuredux can be purchased in pellet form. The pellets are then melted down and extruded into bars. In one embodiment, the extruded Kuredux bars are cut and machined into at least 63 different sizes of PGA balls ranging in size from 0.75 inches to 4.625 inches in A-inch increments. The 63 different sizes correspond to matching sliding sleeves that can be laid out in series, so that the smallest ball can be put down into the well first and seat onto the smallest valve. The next smallest ball can be pumped down second and a seat on the second smallest seat, and so forth. These ranges and processing methods are provided by way of example only. PGA frac balls smaller than 0.75 inches or larger than 4.625 inches can be manufactured. In other embodiments, injection molding or thermoforming techniques known in the art may also be used.
In an exemplary embodiment of the present invention, a well bore 150 is drilled into a hydrocarbon formation 170. A frac sleeve 100 has been inserted into well bore 150 to isolate the zone 1162 from zone 2164. Zone 1 and zone 2 are conceptual divisions, and are not explicitly delimited except by frac sleeve 100 itself. In an exemplary embodiment, hydrocarbon formation 170 may be divided into 63 or more zones. Zone 1162 has already been fracked, and now zone 2164 needs to be fracked. PGA frac ball 110, which has an outer diameter selected to seat securely into ball seat 120 is pumped down into the well bore 150. In some embodiments, frac sleeve 100 forms part of the tubing or casing string.
Frac sleeve 100 includes a shifting sleeve 130, which is mechanically coupled to ball seat 120. Initially, shifting sleeve 130 covers frac ports, 140. When PGA frac ball 110 is seated into ball seat 120 and high-pressure fracking fluid fills well bore 150, shifting sleeve 130 will mechanically shift, moving in a down-hole direction. This shifting exposes frac ports 140, so that there is fluid communication between frac ports 140 and hydrocarbon formation 170. As the pressure of fracking fluid increases, hydrocarbon formation 170 fractures, freeing trapped hydrocarbons from hydrocarbon formation 170.
Frazier, et al., have found that PGA frac balls made of Kuredux will begin to break down in approximately 48 hours in aqueous solution at approximately 250° F. The presence of acids in the water will enhance solubility.
Advantageously, PGA frac balls made of Kuredux have strength similar to metals. This allows them to be used for effective isolation in the extremely high pressure environment of fracking operations. Once the Kuredux balls start to dissolve, they begin to lose their structural integrity, and easily unseat, moving out of the way of hydrocarbon production. Eventually, the balls dissolve completely.
In the previous example, Kuredux PGA frac balls are provided in sizes between 0.75 inches and 4.625 inches, to facilitate operation of frac sleeves of various sizes. In other embodiments, balls may be provided from 1 inch up to over 4 inches. In some applications, ball sizes may be increased in one-eighth inch increments. In other applications, the incremental increase may be in sixteenths of an inch. Thus, in some cases, provision can be made for fracking up to 63 zones with a single run of frac balls.
Furthermore, in some embodiments of a frac sleeve, multiple balls must be pumped into the sleeve to complete the operation. For example, some prior art systems require up to four frac balls to operate a frac sleeve. In those cases, a plurality of identical PGA frac balls 110 may be used.
In an alternative embodiment, a frac ball 110 is pumped down into the wellbore, seated in an independent ball seat at the lower end of the well, and pressure is applied at the surface to volume test the casing. This enables a volume test on the casing without any intervention necessary to remove the frac ball 110, which naturally biodegrades.
Kuredux can also be used to manufacture downhole tools that are designed to be drilled out. For example, a flapper valve, such as is disclosed in U.S. Pat. No. 7,287,596, can be manufactured with Kuredux, so that it can be more easily broken after a zone has been fracked. A composite bridge plug can also be manufactured with Kuredux. This may obviate the need to mill out the bridge plug after fracking, or may make milling out the bridge plug faster and easier.
Kuredux specifically has been disclosed as an exemplary material for use in creating dissolvable PGA frac balls, but it should be understood that any material with similar properties can be used. Furthermore, while the PGA balls in this exemplary embodiment are referred to as “PGA frac balls,” those having skill in the art will recognize that such balls have numerous applications, including numerous applications in hydrocarbon recovery, and that the term “PGA frac ball” as used herein is intended to encompass any spherical ball constructed substantially of high-molecular weight polyglycolic acid, and in particular any such ball used in hydrocarbon recovery operations.
Cement retainer 200 also includes PGA slips, which may be structurally similar to prior art iron slips, but which are molded or machined PGA according to methods disclosed herein. Teeth may be added to the tips of PGA slips 220 to aid in gripping the well casing, and may be made of iron, tungsten-carbide, or other hardened materials known in the art. In other embodiments, PGA slip may include a PGA base material with hardened buttons of ceramic, iron, tungsten-carbide, or other hardened materials embedded therein. Some embodiments of cement retainer 200 may be configured for use with a PGA frac ball 110.
Once sufficient set down weight has been established, applied pressure (cement) is pumped down the workstring, opening the one-way check valve and allowing communication beneath the cement retainer 200. Cement retainer 200 has a low metallic content and in some embodiments, may require no drilling whatsoever. Rather, cement retainer 200 is left in the well bore and PGA structural members 210 and PGA slips 220 are permitted to break down naturally. In some embodiments, the remaining metallic pieces may be sufficiently small to pump out of the well bore. In other embodiments, minimal drilling is required to clean out remaining metallic pieces.
Cement retainer 300 has a low metallic content and in some embodiments, may require no drilling whatsoever. Rather, cement retainer 300 is left in the well bore and PGA structural members 310 are permitted to break down naturally. In some embodiments, the remaining metallic pieces may be sufficiently small to pump out of the well bore. In other embodiments, minimal drilling is required to clean out remaining metallic pieces. Some embodiments of cement retainer 300 may be configured for use with a PGA frac ball 110.
During the cementing operation, simple valve control can be accomplished through surface pipe manipulation, causing the hydraulic forces to either add or subtract weight to cement retainer 400. The operator should complete the hydraulic calculations to prevent overloading or pumping out of the retainer. The cementing process can then begin.
Cement retainer 400 has a low metallic content and in some embodiments, may require no drilling whatsoever. Rather, cement retainer 400 is left in the well bore and PGA structural members 410 are permitted to break down naturally. In some embodiments, the remaining metallic pieces may be sufficiently small to pump out of the well bore. In other embodiments, minimal drilling is required to clean out remaining metallic pieces. Some embodiments of cement retainer 400 may be configured for use with a PGA frac ball 110.
In an exemplary embodiment, PGA frac plug 500 is operated according to methods known in the prior art. For example, after performing the setting procedure known in the art, frac plug 500 remains open for fluid flow and allows wireline services to continue until the ball drop isolation procedure has started. The ball drop isolation procedure may include use of a PGA frac ball 110. Once the surface-dropped ball is pumped down and seated into the inner funnel top of the tool, the operator can pressure up against the plug to achieve isolation.
Frac plug 500 has a low metallic content and in some embodiments, may require no drilling whatsoever. Rather, PGA frac plug 500 is left in the well bore and PGA main body 510 and PGA slip 520 are permitted to break down naturally. In some embodiments, the remaining metallic pieces may be sufficiently small to pump out of the well bore. In other embodiments, minimal drilling is required to clean out remaining metallic pieces. Some embodiments of frac plug 500 may be configured for use with a PGA frac ball 110.
In the prior art, frac plugs such as PGA frac plug 500 are used primarily for horizontal applications. But PGA frac plug 500's slim, lightweight design makes deployment fast and efficient in both vertical and horizontal wells.
Built with a one-way check valve, temporary isolation tool 600 temporarily prevents sand from invading the upper zone and eliminates cross-flow problems for example by using a PGA frac ball 110 as a sealer. After PGA frac ball 110 has been dissolved by pressure, temperature or fluid, the check valve will allow the two zones to commingle. The operator can then independently treat or test each zone and remove flow-back plugs in an underbalanced environment in one trip.
Temporary isolation tool 600 has a low metallic content and in some embodiments, may require no drilling whatsoever. Rather, cement retainer 600 is left in the well bore and PGA structural members 610 are permitted to break down naturally. In some embodiments, the remaining metallic pieces may be sufficiently small to pump out of the well bore. In other embodiments, minimal drilling is required to clean out remaining metallic pieces.
Snub-nose plug 700 may be provided in several configurations with various types of valves. In one embodiment, snub-nose plug 700 may be used in conjunction with a PGA frac ball 110.
Snub-nose plug 700 has a low metallic content and in some embodiments, may require no drilling whatsoever. Rather, cement retainer 700 is left in the well bore and PGA structural members 710 are permitted to break down naturally. In some embodiments, the remaining metallic pieces may be sufficiently small to pump out of the well bore. In other embodiments, minimal drilling is required to clean out remaining metallic pieces.
When built with a one-way check valve, frac plug 800 temporarily prevents sand from invading the upper zone and eliminates cross-flow problems, in some embodiments by utilizing a PGA frac ball 110. After PGA frac ball 110 has been dissolved, the check valve will allow the two zones to commingle. The operator can then independently treat or test each zone and remove the flow-back plugs in an under-balanced environment in one trip.
Frac plug 800 has a low metallic content and in some embodiments, may require no drilling whatsoever. Rather, cement retainer 800 is left in the well bore and PGA structural members 810 are permitted to break down naturally. In some embodiments, the remaining metallic pieces may be sufficiently small to pump out of the well bore. In other embodiments, minimal drilling is required to clean out remaining metallic pieces.
In operation, PGA disks 910 are configured to withstand conditions such as intense heat and heavy mud loads. The isolation sub 900 is run on the bottom of the tubing or below a production packer bottom hole assembly. After the production packer is set, the disks isolate the wellbore reservoir.
After the upper production bottom hole assembly is run in hole, latched into the packer, and all tests are performed, PGA disks 910 can be knocked out using a drop bar, coil tubing, slickline or sand line, or they can be left to dissolve on their own. Once PGA disks 910 are removed, the wellbore fluids can then be produced up the production tubing or casing string. The individual PGA pieces then biodegrade in an environmentally-responsible manner.
For both snubbing and pump-out applications, isolation sub 1000 provides an economical alternative to traditional methods. Designed to work in a variety of conditions, isolation sub 1000 provides a dependable solution for a range of isolation operations.
Isolation sub 1000 is run on the bottom of the tubing or below a production packer bottom hole assembly. Once the production packer is set, isolation sub 1000 isolates the wellbore reservoir.
After the upper production bottom hole assembly is run in hole, latched in to the packer, and all tests are performed, PGA disk 1010 can be pumped out. In an exemplary embodiment, removal comprises applying overbalance pressure from surface to pump out PGA disk 1010. In other embodiments, drop bar, coil tubing, slickline or sand line can also be used. In yet other embodiments, PGA disk 1010 is left to dissolve on its own. Once disk 1010 is removed, wellbore fluids can be produced up the production tubing.
Advantageously, pumpdown dart 1400 permits threaded frac ball 1410 to be seated with substantially less pressure and fluid than is required to seat PGA frac ball 110.
While the subject of this specification has been described in connection with one or more exemplary embodiments, it is not intended to limit the claims to the particular forms set forth. On the contrary, the appended claims are intended to cover such alternatives, modifications and equivalents as may be included within their spirit and scope.
This application claims priority to U.S. patent application Ser. No. 13/843,051, filed Mar. 15, 2013; U.S. Provisional Application 61/648,749, filed May 18, 2012; U.S. Provisional Application 61/738,519, filed Dec. 18, 2012; and US Patent Publication No. 2010/0155050, published Jun. 24, 2010, all of which are incorporated herein by reference. U.S. Pat. No. 6,951,956 is also incorporated herein by reference.
Number | Name | Date | Kind |
---|---|---|---|
2040889 | Whinnen | May 1936 | A |
2160228 | Pustmueller | May 1939 | A |
2223602 | Cox | Dec 1940 | A |
2230447 | Bassinger | Feb 1941 | A |
2286126 | Thornhill | Jun 1942 | A |
2331532 | Bassinger | Oct 1943 | A |
2555627 | Baker | Jun 1951 | A |
2589506 | Morrisett | Mar 1952 | A |
2593520 | Baker | Apr 1952 | A |
2616502 | Lenz | Nov 1952 | A |
2640546 | Baker | Jun 1953 | A |
2713910 | Baker | Jul 1955 | A |
2833354 | Sailers | May 1956 | A |
2830666 | Rhodes | Apr 1958 | A |
3013612 | Angel | Dec 1961 | A |
3054453 | Bonner | Sep 1962 | A |
3062296 | Brown | Nov 1962 | A |
3163225 | Perkins | Dec 1964 | A |
3273588 | Dollison | Sep 1966 | A |
3298437 | Conrad | Jan 1967 | A |
3298440 | Current | Jan 1967 | A |
3306362 | Urbanosky | Feb 1967 | A |
3308895 | Oxford | Mar 1967 | A |
3356140 | Young | Dec 1967 | A |
3517742 | Williams | Jun 1970 | A |
3623551 | Randermann | Nov 1971 | A |
3687202 | Young | Aug 1972 | A |
3787101 | Sugden | Jan 1974 | A |
3818987 | Ellis | Jun 1974 | A |
3851706 | Ellis | Dec 1974 | A |
3860066 | Pearce | Jan 1975 | A |
3926253 | Duke | Dec 1975 | A |
4035024 | Fink | Jul 1977 | A |
4049015 | Brown | Sep 1977 | A |
4134455 | Read | Jan 1979 | A |
4151875 | Sullaway | May 1979 | A |
4185689 | Harris | Jan 1980 | A |
4189183 | Borowski | Feb 1980 | A |
4250960 | Chammas | Feb 1981 | A |
4314608 | Richardson | Feb 1982 | A |
4381038 | Sugden | Apr 1983 | A |
4391547 | Jackson | Jul 1983 | A |
4405017 | Allen | Sep 1983 | A |
4432418 | Mayland | Feb 1984 | A |
4436151 | Callihan | Mar 1984 | A |
4457376 | Carmody | Jul 1984 | A |
4532995 | Kaufman | Aug 1985 | A |
4548442 | Sugden | Oct 1985 | A |
4554981 | Davies | Nov 1985 | A |
4566541 | Moussy | Jan 1986 | A |
4585067 | Blizzard | Apr 1986 | A |
4595052 | Kristiansen | Jun 1986 | A |
4602654 | Stehling | Jul 1986 | A |
4688641 | Knieriemen | Aug 1987 | A |
4708163 | Deaton | Nov 1987 | A |
D293798 | Johnson | Jan 1988 | S |
4776410 | Perkin | Oct 1988 | A |
4784226 | Wyatt | Nov 1988 | A |
4792000 | Perkin | Dec 1988 | A |
4830103 | Blackwell | May 1989 | A |
4848459 | Blackwell | Jul 1989 | A |
4893678 | Stokley | Jan 1990 | A |
5020590 | McLeod | Jun 1991 | A |
5074063 | Vannette | Dec 1991 | A |
5082061 | Dollison | Jan 1992 | A |
5095980 | Watson | Mar 1992 | A |
5113940 | Glaser | May 1992 | A |
5117915 | Mueller | Jun 1992 | A |
5154228 | Gambertoglio | Oct 1992 | A |
5183068 | Prosser | Feb 1993 | A |
5188182 | Echols | Feb 1993 | A |
5207274 | Streich | May 1993 | A |
5209310 | Clydesdale | May 1993 | A |
5219380 | Young | Jun 1993 | A |
5230390 | Zastresek | Jul 1993 | A |
5234052 | Coone | Aug 1993 | A |
5253705 | Clary | Oct 1993 | A |
5295735 | Cobbs | Mar 1994 | A |
5316081 | Baski | May 1994 | A |
5318131 | Baker | Jun 1994 | A |
D350887 | Sjolander | Sep 1994 | S |
5343954 | Bohlen | Sep 1994 | A |
D353756 | Graves | Dec 1994 | S |
D355428 | Hatcher | Feb 1995 | S |
5390737 | Jacobi | Feb 1995 | A |
5392540 | Cooper | Feb 1995 | A |
RE35088 | Gilbert | Nov 1995 | E |
5484191 | Sollami | Jan 1996 | A |
5490339 | Accettola | Feb 1996 | A |
5540279 | Branch | Jul 1996 | A |
5564502 | Crow | Oct 1996 | A |
5593292 | Ivey | Jan 1997 | A |
D377969 | Grantham | Feb 1997 | S |
5655614 | Azar | Aug 1997 | A |
5701959 | Hushbeck | Dec 1997 | A |
5785135 | Crawley | Jul 1998 | A |
5791825 | Gardner | Aug 1998 | A |
5803173 | Fraser | Sep 1998 | A |
5810083 | Kilgore | Sep 1998 | A |
5819846 | Bolt | Oct 1998 | A |
D415180 | Rosanwo | Oct 1999 | S |
5961185 | Friant | Oct 1999 | A |
5984007 | Yuan | Nov 1999 | A |
5988277 | Vick | Nov 1999 | A |
6012519 | Allen | Jan 2000 | A |
6085446 | Posch | Jul 2000 | A |
6098716 | Hromas | Aug 2000 | A |
6105694 | Scott | Aug 2000 | A |
RE17217 | Burch | Oct 2000 | E |
6142226 | Vick | Nov 2000 | A |
6152232 | Webb | Nov 2000 | A |
6167963 | McMahan | Jan 2001 | B1 |
6182752 | Smith | Feb 2001 | B1 |
6189618 | Beeman | Feb 2001 | B1 |
6199636 | Harrison | Mar 2001 | B1 |
6220349 | Vargus | Apr 2001 | B1 |
6283148 | Spears | Sep 2001 | B1 |
6341823 | Sollami | Jan 2002 | B1 |
6367569 | Walk | Apr 2002 | B1 |
6394180 | Berscheidt | May 2002 | B1 |
6457267 | Porter | Oct 2002 | B1 |
6491108 | Slup | Dec 2002 | B1 |
6543963 | Bruso | Apr 2003 | B2 |
6581681 | Zimmerman | Jun 2003 | B1 |
6629563 | Doane | Oct 2003 | B2 |
6695049 | Ostocke | Feb 2004 | B2 |
6725935 | Szarka | Apr 2004 | B2 |
6739398 | Yokley | May 2004 | B1 |
6779948 | Bruso | Aug 2004 | B2 |
6799633 | McGregor | Oct 2004 | B2 |
6834717 | Bland | Dec 2004 | B2 |
6851489 | Hinds | Feb 2005 | B2 |
6854201 | Hunter | Feb 2005 | B1 |
6902006 | Myerley | Jun 2005 | B2 |
6918439 | Dallas | Jul 2005 | B2 |
6938696 | Dallas | Sep 2005 | B2 |
6944977 | Deniau | Sep 2005 | B2 |
7040410 | McGuire | May 2006 | B2 |
7055632 | Dallas | Jun 2006 | B2 |
7069997 | Coyes | Jul 2006 | B2 |
7107875 | Haugen | Sep 2006 | B2 |
7124831 | Turley | Oct 2006 | B2 |
7128091 | Istre | Oct 2006 | B2 |
7134505 | Fehr | Nov 2006 | B2 |
7150131 | Barker | Dec 2006 | B2 |
7168494 | Starr | Jan 2007 | B2 |
7281584 | McGarian | Oct 2007 | B2 |
D560109 | Huang | Jan 2008 | S |
7325617 | Murray | Feb 2008 | B2 |
7337847 | McGarian | Mar 2008 | B2 |
7353879 | Todd | Apr 2008 | B2 |
7363967 | Burris | Apr 2008 | B2 |
7373973 | Smith | May 2008 | B2 |
7464764 | Xu | Dec 2008 | B2 |
7527104 | Branch | May 2009 | B2 |
7552779 | Murray | Jun 2009 | B2 |
D579110 | Antua | Jul 2009 | S |
7600572 | Slup | Oct 2009 | B2 |
7604058 | McGuire | Oct 2009 | B2 |
7637326 | Bolding | Dec 2009 | B2 |
7644767 | Kalb | Jan 2010 | B2 |
7644772 | Avant | Jan 2010 | B2 |
7644774 | Branch | Jan 2010 | B2 |
7647964 | Akbar | Jan 2010 | B2 |
D612875 | Beynon | Mar 2010 | S |
7673677 | King | Mar 2010 | B2 |
7681645 | McMillin | Mar 2010 | B2 |
D618715 | Corcoran | Jun 2010 | S |
7735549 | Nish | Jun 2010 | B1 |
7775278 | Willberg et al. | Aug 2010 | B2 |
7775286 | Duphorne | Aug 2010 | B2 |
7775291 | Jacob | Aug 2010 | B2 |
7784550 | Nutley | Aug 2010 | B2 |
7798236 | McKeachnie | Sep 2010 | B2 |
7810558 | Shkurti | Oct 2010 | B2 |
D629820 | Van Ryswyk | Dec 2010 | S |
7866396 | Rytlewski | Jan 2011 | B2 |
7878242 | Gray | Feb 2011 | B2 |
7886830 | Bolding | Feb 2011 | B2 |
7900696 | Nish | Mar 2011 | B1 |
7909108 | Swor | Mar 2011 | B2 |
7909109 | Angman | Mar 2011 | B2 |
D635429 | Hakki | Apr 2011 | S |
7918278 | Barbee | Apr 2011 | B2 |
7921923 | McGuire | Apr 2011 | B2 |
7921925 | Maguire et al. | Apr 2011 | B2 |
7926571 | Hofman | Apr 2011 | B2 |
8074718 | Roberts | Dec 2011 | B2 |
8079413 | Frazier | Dec 2011 | B2 |
8113276 | Greenlee | Feb 2012 | B2 |
8127856 | Nish | Mar 2012 | B1 |
D657807 | Frazier | Apr 2012 | S |
8231947 | Vaidya | Jul 2012 | B2 |
20010040035 | Appleton | Nov 2001 | A1 |
20030024706 | Allamon | Feb 2003 | A1 |
20030188860 | Zimmerman | Oct 2003 | A1 |
20040150533 | Hall | Aug 2004 | A1 |
20050173126 | Starrt | Aug 2005 | A1 |
20060001283 | Bakke | Jan 2006 | A1 |
20060011389 | Booth | Jan 2006 | A1 |
20060278405 | Turley | Dec 2006 | A1 |
20070051521 | Fike | Mar 2007 | A1 |
20070068670 | Booth | Mar 2007 | A1 |
20070107908 | Vaidya | May 2007 | A1 |
20070227745 | Roberts | Oct 2007 | A1 |
20070240883 | Telfer | Oct 2007 | A1 |
20080110635 | Loretz | May 2008 | A1 |
20090044957 | Clayton | Feb 2009 | A1 |
20090114401 | Purkis | May 2009 | A1 |
20090126933 | Telfer | May 2009 | A1 |
20090211749 | Nguyen | Aug 2009 | A1 |
20100064859 | Stephens | Mar 2010 | A1 |
20100084146 | Roberts | Apr 2010 | A1 |
20100101803 | Clayton et al. | Apr 2010 | A1 |
20100132960 | Shkurti | Jun 2010 | A1 |
20100155050 | Frazier | Jun 2010 | A1 |
20100252252 | Harris | Oct 2010 | A1 |
20100276159 | Mailand | Nov 2010 | A1 |
20100288503 | Cuiper | Nov 2010 | A1 |
20110005779 | Lembcke | Jan 2011 | A1 |
20110036564 | Williamson | Feb 2011 | A1 |
20110061856 | Kellner | Mar 2011 | A1 |
20110088915 | Stanojcic | Apr 2011 | A1 |
20110103915 | Tedeschi | May 2011 | A1 |
20110147014 | Chen et al. | Jun 2011 | A1 |
20110168404 | Telfer | Jul 2011 | A1 |
20110198082 | Stromquist | Aug 2011 | A1 |
20110240295 | Porter | Oct 2011 | A1 |
20110259610 | Shkurti | Oct 2011 | A1 |
20120073819 | Richard et al. | Mar 2012 | A1 |
20130008666 | Cherewyk | Jan 2013 | A1 |
20130008671 | Booth | Jan 2013 | A1 |
20130014936 | Griffith | Jan 2013 | A1 |
20130068474 | Hofman et al. | Mar 2013 | A1 |
20130300066 | Xu et al. | Nov 2013 | A1 |
20130306327 | Williamson | Nov 2013 | A1 |
20130319668 | Tschetter et al. | Dec 2013 | A1 |
20130319682 | Tschetter et al. | Dec 2013 | A1 |
20130333891 | Fripp et al. | Dec 2013 | A1 |
20140000894 | Coffey et al. | Jan 2014 | A1 |
20140020911 | Martinez | Jan 2014 | A1 |
20140027128 | Johnson et al. | Jan 2014 | A1 |
20140041857 | Xu et al. | Feb 2014 | A1 |
20140060813 | Naedler et al. | Mar 2014 | A1 |
20140096970 | Andrew et al. | Apr 2014 | A1 |
20140102709 | Arabskyy | Apr 2014 | A1 |
20140116677 | Sherlin | May 2014 | A1 |
20140116721 | Hofman et al. | May 2014 | A1 |
20140116731 | Themig et al. | May 2014 | A1 |
20140116775 | Coffey et al. | May 2014 | A1 |
20140182862 | Derby | Jul 2014 | A1 |
20140196899 | Jordan et al. | Jul 2014 | A1 |
20140224476 | Frazier | Aug 2014 | A1 |
20140224477 | Wiese et al. | Aug 2014 | A1 |
20140231069 | VanLue | Aug 2014 | A1 |
20140231099 | Barbee et al. | Aug 2014 | A1 |
20140246189 | Beason et al. | Sep 2014 | A1 |
20140246208 | Themig et al. | Sep 2014 | A1 |
20140248448 | Sjostedt | Sep 2014 | A1 |
20140251594 | Garcia et al. | Sep 2014 | A1 |
20140251612 | Powers | Sep 2014 | A1 |
20140251636 | Hofman et al. | Sep 2014 | A1 |
Number | Date | Country |
---|---|---|
914030 | Dec 1962 | GB |
2010127457 | Nov 2010 | WO |
Number | Date | Country | |
---|---|---|---|
20140083717 A1 | Mar 2014 | US |
Number | Date | Country | |
---|---|---|---|
61648749 | May 2012 | US | |
61738519 | Dec 2012 | US |
Number | Date | Country | |
---|---|---|---|
Parent | 13843051 | Mar 2013 | US |
Child | 13894649 | US |