The present application incorporates by reference the following concurrently filed U.S. patent applications: Perforating Tubulars, listing Joseph A. Zupanick as inventor and U.S. application Ser. No. 11/019,748 and Enlarging Well Bores Having Tubing Therein, listing Joseph A. Zupanick as inventor and U.S. application Ser. No. 11/019,694.
The present invention relates generally to recovery of subterranean resources, and more particularly, to systems, apparatus, and methods for extraction of resources from a subterranean formation.
Subterranean deposits of coal, also referred to as coal seams, contain substantial quantities of entrained resources, such as coal seam gas (including methane gas or other naturally occurring gases). Production and use of coal seam gas from coal deposits has occurred for many years. However, substantial obstacles have frustrated more extensive development and use of coal seam gas deposits in coal beds.
In the past, coal seam gas was extracted through multiple vertical wells drilled from the surface into the subterranean deposit. Coal seams may extend over large areas of up to several thousand acres. Vertical wells drilled into the coal deposits for obtaining methane gas can drain only a fairly small radius into the coal deposits around the wells. Therefore, to effectively drain a coal seam gas deposit, many vertical well bores must be drilled. Many times, the cost to drill the many vertical well bores is not justified by the value of the gas that is expected to be recovered.
Horizontal drilling patterns have been tried in order to extend the amount of coal seam exposed to a drill bore for gas extraction. However, horizontal drilling patterns require complex and expensive drilling equipment, for example, for tracking location of the drilling bit and directionally drilling drainage patterns. Consequently, drilling horizontal patterns is expensive and the cost must be justified by the value of the gas that will be recovered.
The present disclosure is directed to accessing a subterranean zone with a well bore by facilitating collapse of the subterranean zone into the well bore. The well bore may be provided with a tubing string through which fluids from the subterranean zone can be withdrawn.
One illustrative implementation of the invention includes a method of accessing a subterranean zone from the surface. In the method, a well bore is formed extending from a terranean surface into the subterranean zone. A tubing string is provided within the well bore. The well bore is enlarged to a dimension selected to collapse at least a portion of the subterranean zone about the tubing. The tubing may be used, thereafter, in withdrawing fluids from the subterranean zone.
In some implementations, the method can further include perforating the tubing string while the tubing string is within the well bore. Pressure of fluids within the well bore can be reduced to facilitate collapse of at least a portion of the subterranean zone about the well bore. In some instances pressure can be reduced from an overbalanced condition to an underbalanced condition. The method can be applied to a subterranean zone that includes a coal seam. In some instances, forming a well bore can include forming a first well bore extending from the surface into the subterranean zone and forming a second substantially horizontal well bore through the first well bore. The method can further include forming a third substantially horizontal well bore through the first well bore. The first well bore may extend substantially vertical, be slanted, or otherwise. The first well bore may include a rat hole at an end thereof.
Another illustrative implementation of the invention includes a system for accessing a subterranean zone from a terranean surface. The system includes a well bore extending from the surface into the subterranean zone. A tubing string resides within the well bore. The well bore includes an enlarged cavity having a dimension selected to cause the subterranean zone to collapse inward on the tubing string.
In some implementations, the dimension of the enlarged cavity can be selected to remain substantially stable with no substantial inward collapsed when pressure within the cavity is overbalanced, and collapse when pressure within the cavity is reduced. The dimension of the enlarged cavity can be selected to collapse when the pressure within the cavity is reduced underbalanced. The dimension can include a transverse dimension of the enlarged cavity. The tubing string may be anchored in the well bore. The well bore may include a first portion extending from the surface coupled to a second portion that is oriented substantially horizontal. The first portion may extend beyond the second portion to define a sump. The first portion may be substantially vertical or slanted. The well bore can include a plurality of horizontally oriented bores in communication with a main bore, and the tubing string can include a plurality of tubing strings. The subterranean zone can include a coal seam.
Another illustrative implementation includes an underreamer for forming a cavity within a well bore. The underreamer includes a fluid motor having a first body and a second body arranged about a longitudinal axis. The first body is adapted to rotate about the longitudinal axis in relation to the second body when fluid is passed between the first and second body. The fluid motor further defines a longitudinal tubing passage adapted to allow passage of the fluid motor over a tubing string. The underreamer also includes at least one cutting arm coupled to rotate with the first body of the fluid motor. The least one cutting arm is radially extendable into engagement with an interior of the well bore in forming the cavity.
In some implementations of the illustrative underreamer the at least one cutting arm is pivotally coupled to the first body to rotate radially outward when subjected to centrifugal force. The least one cutting arm is extendable from a radially retracted position adapted to allow the underreamer to pass through the well bore.
Another illustrative implementation includes a method of forming a cavity within a well bore. In the method, an underreamer is passed over a tubing string residing in the well bore to a desired location of the cavity. Fluid is flowed through the underreamer to operate the underreamer in forming the cavity.
In some implementations of the illustrative method, operating the underreamer includes extending at least one cutting arm radially outward from a retracted to an extended position, wherein the retracted position enables the underreamer pass through the interior of the well bore and in the extended position the least one cutting arm is in engagement with an interior of the well bore. In some instances extending the least one cutting arm radially outward from the retracted position to the extended position includes rotating a portion of the underreamer so that centrifugal force acts upon the least one cutting arm to pivot the least one cutting arm radially outward. Rotating a portion of the underreamer can include flowing fluid through a positive displacement motor of the underreamer. The method can further include passing the underreamer over the tubing string to withdraw the underreamer from the well bore. Operating the underreamer in forming a cavity can include operating the underreamer in forming a cavity of a transverse dimension selected to cause the cavity to collapse.
Another illustrative implementation includes a device for perforating a tubing string residing in a well bore. The device includes a tubular housing adapted to be received within the tubing string. At least one perforating body resides in the housing and has a point adapted to pierce the tubing string. A piston is received within the housing and configured such that pressure applied to a first side of the piston causes the piston to move and in a first direction. An actuator body is received within the housing and configured for movement in the first direction with the piston. The actuator body has a sloped wedge surface adapted to wedge the least one perforating body radially outward to pierce the tubing string when the actuator body is moved in the first direction.
In some implementations of the illustrative perforating device, a spring is adapted to move the actuator body in a second direction substantially opposed the first direction. The housing may have at least one window through a lateral wall thereof, and the point of the least one perforating body extends through the least one window in piercing the tubing string. The least one perforating body can be guided by the edge surfaces of the window. The least one perforating body can include a profile adapted to interlock with a profile of the actuator body. The profile radially retains the least one perforating body in relation to the actuator body. The sloped wedge surface can include a substantially conical surface and the least one perforating body can include a plurality of perforating bodies arranged around the substantially conical surface.
Another illustrative implementation includes a method of perforating a tubing string and a well bore. In the method a perforating tool coupled to a working string is positioned in an interior of the tubing string. The perforating tool has a piston and at least one perforating body adapted to pierce the tubing string. Pressure is applied to the piston through the working string to translate the piston. The least one perforating body is radially extended outward to pierce the tubing string in response to the translation of the piston.
In some implementations of the illustrative method, extending the least one perforating body radially outward can include translating a wedge-shaped actuator in response to the translation of the piston and wedging the least one perforating body radially outward with the wedge-shaped actuator body. The method can further include retracting the least one perforating body radially inward, positioning the perforating tool and a second location within the interior of the tubing string, and repeating the steps of applying pressure to the piston and extending at least one perforating body to pierce the tubing string at the second location.
Another illustrative implementation includes a method of accessing a subterranean zone from the surface. In the method and a well bore is formed extending from the surface into the subterranean zone. A tubing string is provided within the well bore. An underreamer is passed over the tubing string to a specified location within the subterranean zone. The underreamer is operated in forming an enlarged cavity in the well bore. Pressure within the enlarged cavity is reduced to facilitate collapse of the subterranean zone about the tubing. Apertures are provided in the tubing string to allow passage of fluids into an interior of the tubing string.
The details of one or more illustrative implementations of the invention are set forth in the accompanying drawings and the description below. Other features, objects, and advantages of the invention will be apparent from the description and drawings, and from the claims.
Reference is now made to the following description taken in conjunction with the accompanying drawings, wherein like numerals represent like parts:
Referring first to
Referring back to
The curved portion 20 and second portion 18, and in some instances the first portion 16, may be drilled using an articulated drill string 24 that includes a down-hole motor and drill bit 26. The first portion 16 may be drilled separately from the curved portion 20 and second portion 18. For example, the first portion 16 may be drilled, and then one or more the curved portions 20 and second portions 18 may be drilled through the first portion 16. A measurement while drilling (MWD) device 28 may be included in the articulated drill string 24 to track the motor and bit 26 position for use in controlling their orientation and direction. A casing 30 may be cemented into a portion of the well bore 10 subsequent to drilling, or the casing 30 may be omitted.
During the process of drilling the well bore 10, drilling fluid or “mud” is pumped down the articulated drill string 24 and circulated out of the drill string 24 in the vicinity of the motor and bit 26. The mud is used to scour the formation and remove formation cuttings produced by drilling or otherwise residing in the well bore 10. The cuttings are entrained in the drilling fluid which circulates up to the surface 12 through the annulus between the drill string 24 and the walls of the well bore 10. At the surface 12, the cuttings are removed from the drilling mud and the mud may then be recirculated. The hydrostatic pressure of the mud within the borehole exerts pressure on the interior of the well bore 10. During drilling operations, the density of mud within the well bore 10 can be selected so that the hydrostatic pressure of the drilling mud in the subterranean zone 14 is greater than the reservoir pressure, and greater than the pressure of fluids, such as coal seam gas, within the subterranean zone 14. The condition when the pressure of the drilling mud in the well bore is greater than the pressure of the formation, e.g. subterranean zone 14, is referred to as “overbalanced.”
Referring to
The tubing string 32 may be anchored in the well bore 10, for example, using an anchoring device 34 on the end of the string 32. The tubing string 32 defines an annulus between the tubing string 32 and the wall of the well bore 10 or the casing 30. The anchoring device 34 is adapted to traverse the annulus to grip or otherwise engage an interior surface of the well bore 10 and substantially resist movement along the longitudinal axis of the well bore 10. There are numerous devices which can be used as anchoring device 34. For example, the anchoring device 34 can be cement introduced into the annulus that, when solidified, will anchor the tubing string 32. In another instance, some of the devices that can be used as anchoring device 34 may have radially extendable members 36, such as slips or dogs, that are mechanically or hydraulic actuated to extend into engagement with and grip the interior diameter of the well bore 10 or another body affixed within the well bore 10.
Turning now to
The cavity cutting tool 40 can be positioned about the end of the well bore 10, and subsequently actuated to begin cutting an enlarged cavity 44. Thereafter, the cavity cutting tool 40 is drawn back up along the longitudinal axis of the well bore 10 to elongate the enlarged cavity 44 along the longitudinal axis of the well bore 10. However, it is with the scope of the methods described herein to begin cutting the enlarged cavity 44 at other positions within the well bore 10, as well as to begin cutting at multiple locations within the well bore 10 to create multiple discrete enlarged cavities 44 along the well bore 10.
Referring now to
Although the drilling operations and formation of the enlarged cavity 44 are described above as being performed overbalanced, the drilling operations and/or formation of the enlarged cavity 44 need not be performed overbalanced. For example, the drilling operations and/or formation of the enlarged cavity 44 can be performed when the pressure in the well bore 10 is balanced or underbalanced. To wit, the dimension, such as the transverse dimension, of the cavity 44 can be selected such that the cavity 44 remains substantially stable with little to no inward collapse at the balanced or underbalanced condition, but tends to collapse when the pressure is reduced. Further, the concepts described herein can be used in forming a well bore 10 with an enlarged cavity 44 without using a pressure change to facilitate collapse of the enlarged cavity 44. For example, the dimension of the cavity 44, such as the transverse dimension, can be selected to collapse without further influence from outside factors such as the reduction in pressure in the cavity 44.
Collapsing the enlarged cavity 44 not only breaks up the material of the subterranean zone 14 surrounding the enlarged cavity 44 thereby releasing the fluids residing therein, it also increases the exposed surface area through which fluids can be withdrawn from the subterranean zone 14 and increases the reach into the subterranean zone 14 from which fluids can be withdrawn. Increasing the exposed surface area through which fluids can be withdrawn increases the amount of fluids and the rate at which fluids can be withdrawn. The collapsed enlarged cavity 44 has a larger transverse dimension than the well bore 10, and a larger transverse dimension than the enlarged cavity 44, because the material surrounding the enlarged cavity 44 has collapsed inward. The larger transverse dimension improves the depth (i.e. reach) into the subterranean zone 14 from which fluids can be withdrawn without the fluids having to migrate through material of the subterranean zone 14. Additionally, the collapse is likely to induce cracks or fractures 54 that extend from the interior of the collapsed cavity 44 even deeper into the subterranean zone 14. The fractures 54 form pathways through which fluids residing in the subterranean zone 14 can travel into the collapsed cavity 44 and be recovered and enable conductivity beyond the skin of the bore (10) plugged or damaged by forming the cavity 44. Accordingly, by collapsing the enlarged cavity 44, more of the subterranean zone can be produced than with a bare well bore 10 or well bore 10 and enlarged cavity 44. Of note, while
Referring to
The subterranean zone 14 can be produced through the tubing string 32 by withdrawing fluids 56 from the subterranean zone 14, through the apertures 46 and up through the tubing string 32. The well bore 10 may be shut in, and the tubing string 32 connected to a surface production pipe 48. Thereafter, the subterranean zone 14 can be produced by withdrawing fluids through the interior of the tubing string 32 to the surface production pipe 48. In an implementation that includes a sump 22 (
At block 712, a tubing string is provided in the well bore. The tubing string may be run into the well bore and thereafter anchored, as is discussed above, to prevent movement of the tubing string along the longitudinal axis of the well bore.
At block 714, the well bore is enlarged to form an enlarged cavity. The dimensions of the enlarged cavity, such as the transverse dimension, is selected to facilitate collapse of the subterranean formation into the well bore and onto the tubing string. As is discussed above, the enlarged cavity may be formed with a cavity cutting tool that is introduced over the tubing string and run into the well bore. Once at the desired location to begin the formation of the enlarged cavity, for example at the end of the well bore, the cavity cutting tool is activated to begin cutting the enlarged cavity. While the cavity cutting tool is being operated to cut the subterranean zone, it may be drawn back up the longitudinal axis of the well bore to elongate the enlarged cavity. The cavity cutting tool can be operated at multiple locations within the well bore to create multiple discrete enlarged cavities or can be operated to create a single elongate enlarged cavity. As the enlarged cavity is being cut, the well bore and cavity can be maintained overbalanced. Alternately, pressure can be reduced a intermediate amount or reduced to a balanced or underbalanced condition while cutting the cavity, thereby aiding cutting.
Pressure maintained within the cavity, whether overbalanced or not, may provide support to prevent collapse of the cavity into the well bore during the formation of the enlarged cavity. Thereafter the cavity cutting tool may be withdrawn.
At block 716, the pressure within the cavity is reduced. The reduction in pressure reduces the support provided by the pressure to the interior of the enlarged cavity, and thus facilitates the cavity's collapse inward into the well bore. In an instance where the pressure within the well bore is overbalanced, the pressure may be reduced underbalanced. In an instance where the pressure within the well bore is balanced or underbalanced, the pressure may be reduced further. After collapse, loosely packed and therefore highly permeable remains of the subterranean zone reside about the tubing string.
At block 718, if the tubing string has not already been provided with slots or apertures, the tubing string may be perforated. In one instance, the tubing string is perforated by providing a perforating tool introduced through the interior of the tubing string. The perforating tool can be positioned within the interior of the tubing string and actuated to perforate the tubing string. Thereafter, the perforating tool can be repositioned and actuated to begin perforating the tubing string at a different location or may be withdrawn.
Finally, at block 718, fluids, such as coal seam gas, can be withdrawn from the subterranean zone through the tubing string. The fluids can flow into the tubing string through the apertures, and up the tubing string to the surface. In one instance, the tubing string can be coupled to a production pipeline and gases withdrawn from the subterranean zone through the interior of the tubing string. In an instance where the well bore includes a sump, liquids, such as water from the subterranean zone, will travel down the well bore and collect in the sump. Thereafter, the liquids in the sump may be periodically withdrawn. Allowing the liquids to collect in the sump reduces the amount of liquids in the fluids produced to the surface, and thus, the likelihood that the liquids will form a hydraulic head within the tubing string and hinder production of gases to the surface.
Of note, in an instance where the well bore has additional curved portions and second portions, for example for accessing additional subterranean zones, the operations at blocks 712 through 720 can be repeated for each additional curved portion and second portion. Multiple operations at blocks 712 through 720 for different curved portions and second portions may occur concurrently, or operations at blocks 712 through 720 for different curved portions and second portions may be performed alone.
As is best seen in
Referring to
In operation, the illustrative cavity cutting tool 40 is coupled to the tool string 38.
The tool string 38, including the cavity cutting tool 40, is received over the tubing string 32 and lowered into the well bore 10. When the cavity cutting tool 40 reaches the point in the well bore 10 at which it is desired to begin the cavity 44, fluid, for example drilling mud, is pumped down the tool string 38 into the cavity cutting tool 40. The fluid passes between the inner body 818 and the outer body 820 to cause the inner body 818 to begin rotating. The fluid exits the cavity cutting tool 40 at the base of the tool and is recirculated up through the annulus between the tool string 38 and the interior of the well bore 10. Centrifugal force acts upon the cutting arms 836 causing the cutting arms 836 to pivot radially outward into contact with the interior of the well bore 10. Continued rotation of the inner body 818 causes the cutting arms 836 to remove material from the interior of the well bore 10 thereby forming the cavity 44. The cavity cutting tool 40 can be maintained in place within the well bore 10 until the cutting arms 836 have removed enough material to fully extend. Thereafter the cavity cutting tool 40 can be drawn up hole through the well bore 10, to elongate the cavity 44. Of note, during operation the cutting arms 836 may not extend to be substantially perpendicular to the longitudinal axis of the cavity cutting tool 40, but rather may reside at an acute angle to the longitudinal axis, when fully extended. When the desired length of the cavity 44 is achieved, fluid circulation through the cavity cutting tool 40 can be ceased. Ceasing the fluid circulation through the cavity tool 40 stops rotation of the inner body 818 and allows the cutting arms 836 to retract in-line with remainder of the cavity cutting tool 40. Thereafter, the tool string 38 can be withdrawn from the well bore 10.
Although described above as having the outer body 820 fixed in relation to the tool string 38 and having the inner body 818 rotate in relation to the tool string 38, the outer body 820 and inner body 818 could be configured differently such that the inner body 818 is fixed in relation to the tool string 38 (operating as a stator) and the outer body 820 rotates in relation to the tool string 38 (operating as a rotor). In such different configuration, the cutting arms 836 would then be attached to the outer body 820. Further, the inner body 818 and the outer body 820 need not be the helically lobed inner body 818 and corresponding outer body 820 described above. The inner body 818 and the outer body 820 can be numerous other types of devices able to translate fluid flow into rotational movement, such as a finned turbine and turbine housing or a Archimedes screw and screw housing.
The lower housing portion 914 is adapted to join with the upper housing portion 912, for example by including threads 930 adapted to engage mating threads 932 on the upper housing portion 912. The lower housing portion 914 is tubular and includes a plurality of lateral windows 934. The illustrative lower housing 914 includes three equally spaced windows 934; however, it is anticipated that other numbers of windows 934 could be provided. The windows 934 allow an equal number of perforating wedges 936 to protrude therethrough, with a perforating wedge 936 in each window 934 (
Each perforating wedge 936 has an outward facing surface 937 and an inward facing surface 938. The inward facing surface 938 is slanted relative to the outward facing surface 937, and includes a T-shaped protrusion 946. The outward facing surface 937 has one or more pyramid or conical perforating points 939 adapted to pierce a tubing, such as that of tubing string 32. The illustrative perforating tool 50 of
The actuator body 940 reacts against a spring 952, for example with a radially extending flange 950 proximate the end of the conical portion 942. The spring 952, in turn, reacts against a cap 954 joined to an end of the lower housing 914. The cap 954 can include threads 956 that are received in mating threads 958 on the lower housing 914. The spring 952 operates to bias the actuator body 940 upward. The flange 950 operates to limit upward movement of the actuator body 940 by abutting the perforating wedges 936.
Accordingly, in operation, the illustrative perforating tool 50 is positioned within a tubing such as the tubing string 32 (
As is best seen in
A number of embodiments of the invention have been described. Nevertheless, it will be understood that various modifications may be made without departing from the spirit and scope of the invention. For example, while the concepts described herein are described with reference to a coal seam, it should be understood that the concepts are applicable to other types of subterranean fluid bearing formations. Accordingly, other embodiments are within the scope of the following claims.
Number | Name | Date | Kind |
---|---|---|---|
54144 | Hamar | Apr 1866 | A |
274740 | Douglass | Mar 1883 | A |
526708 | Horton | Oct 1894 | A |
639036 | Heald | Dec 1899 | A |
1162601 | Graham | Nov 1915 | A |
1189560 | Gondos | Jul 1916 | A |
1285347 | Otto | Nov 1918 | A |
1467480 | Hogue | Sep 1923 | A |
1485615 | Jones | Mar 1924 | A |
1488106 | Fitzpatrick | Mar 1924 | A |
1497919 | Layne | Jun 1924 | A |
1500829 | Layne | Jul 1924 | A |
1520737 | Wright | Dec 1924 | A |
1674392 | Flansburg | Jun 1928 | A |
1777961 | Capeliuschnicoff | Oct 1930 | A |
2018285 | Schweitzer et al. | Oct 1935 | A |
2069482 | Seay | Feb 1937 | A |
2150228 | Lamb | Mar 1939 | A |
2169718 | Böll et al. | Aug 1939 | A |
2335085 | Roberts | Nov 1943 | A |
2450223 | Barbour | Sep 1948 | A |
2490350 | Grable | Dec 1949 | A |
2679903 | McGowen, Jr. et al. | Jun 1954 | A |
2726063 | Ragland et al. | Dec 1955 | A |
2726847 | McCune et al. | Dec 1955 | A |
2783018 | Lytle | Feb 1957 | A |
2847189 | Shook | Aug 1958 | A |
2911008 | Du Bois | Nov 1959 | A |
2980142 | Turak | Apr 1961 | A |
3208537 | Scarborough | Sep 1965 | A |
3347595 | Dahms et al. | Oct 1967 | A |
3443648 | Howard | May 1969 | A |
3473571 | Dugay | Oct 1969 | A |
3503377 | Beatenbough et al. | Mar 1970 | A |
3528516 | Brown | Sep 1970 | A |
3530675 | Turzillo | Sep 1970 | A |
3684041 | Kammerer, Jr. et al. | Aug 1972 | A |
3692041 | Bondi | Sep 1972 | A |
3757876 | Pereau | Sep 1973 | A |
3757877 | Leathers | Sep 1973 | A |
3800830 | Etter | Apr 1974 | A |
3809519 | Garner | May 1974 | A |
3825081 | McMahon | Jul 1974 | A |
3828867 | Elwood | Aug 1974 | A |
3874413 | Valdez | Apr 1975 | A |
3887008 | Canfield | Jun 1975 | A |
3902322 | Watanabe | Sep 1975 | A |
3907045 | Dahl et al. | Sep 1975 | A |
3934649 | Pasini, III et al. | Jan 1976 | A |
3957082 | Fuson et al. | May 1976 | A |
3961824 | Van Eek et al. | Jun 1976 | A |
4011890 | Andersson | Mar 1977 | A |
4022279 | Driver | May 1977 | A |
4037658 | Anderson | Jul 1977 | A |
4073351 | Baum | Feb 1978 | A |
4089374 | Terry | May 1978 | A |
4116012 | Abe et al. | Sep 1978 | A |
4134463 | Allen | Jan 1979 | A |
4156437 | Chivens et al. | May 1979 | A |
4169510 | Meigs | Oct 1979 | A |
4189184 | Green | Feb 1980 | A |
4194580 | Messenger | Mar 1980 | A |
4220203 | Steeman | Sep 1980 | A |
4221433 | Jacoby | Sep 1980 | A |
4224989 | Blount | Sep 1980 | A |
4245699 | Steeman | Jan 1981 | A |
4257650 | Allen | Mar 1981 | A |
4278137 | Van Eek | Jul 1981 | A |
4283088 | Tabakov et al. | Aug 1981 | A |
4296785 | Vitello et al. | Oct 1981 | A |
4299295 | Gossard | Nov 1981 | A |
4303127 | Freel et al. | Dec 1981 | A |
4303274 | Thakur | Dec 1981 | A |
4305464 | Masszi | Dec 1981 | A |
4312377 | Knecht | Jan 1982 | A |
4317492 | Summers et al. | Mar 1982 | A |
4328577 | Abbott et al. | May 1982 | A |
4333539 | Lyons et al. | Jun 1982 | A |
4366988 | Bodine | Jan 1983 | A |
4372398 | Kuckes | Feb 1983 | A |
4386665 | Dellinger | Jun 1983 | A |
4390067 | Willman | Jun 1983 | A |
4396076 | Inoue | Aug 1983 | A |
4397360 | Schmidt | Aug 1983 | A |
4398769 | Jacoby | Aug 1983 | A |
4401171 | Fuchs | Aug 1983 | A |
4407376 | Inoue | Oct 1983 | A |
4437706 | Johnson | Mar 1984 | A |
4442896 | Reale et al. | Apr 1984 | A |
4494616 | McKee | Jan 1985 | A |
4512422 | Knisley | Apr 1985 | A |
4519463 | Schuh | May 1985 | A |
4527639 | Dickinson, III et al. | Jul 1985 | A |
4532986 | Mims et al. | Aug 1985 | A |
4544037 | Terry | Oct 1985 | A |
4558744 | Gibb | Dec 1985 | A |
4565252 | Campbell et al. | Jan 1986 | A |
4573541 | Josse et al. | Mar 1986 | A |
4599172 | Gardes | Jul 1986 | A |
4600061 | Richards | Jul 1986 | A |
4605076 | Goodhart | Aug 1986 | A |
4611855 | Richards | Sep 1986 | A |
4618009 | Carter et al. | Oct 1986 | A |
4638949 | Mancel | Jan 1987 | A |
4646836 | Goodhart | Mar 1987 | A |
4651836 | Richards et al. | Mar 1987 | A |
4674579 | Geller et al. | Jun 1987 | A |
4702314 | Huang et al. | Oct 1987 | A |
4705431 | Gadelle et al. | Nov 1987 | A |
4715440 | Boxell et al. | Dec 1987 | A |
4754819 | Dellinger | Jul 1988 | A |
4756367 | Puri et al. | Jul 1988 | A |
4763734 | Dickinson et al. | Aug 1988 | A |
4773488 | Bell et al. | Sep 1988 | A |
4830105 | Petermann | May 1989 | A |
4830110 | Perkins | May 1989 | A |
4836611 | El-Saie | Jun 1989 | A |
4842081 | Parant | Jun 1989 | A |
4844182 | Tolle | Jul 1989 | A |
4852666 | Brunet et al. | Aug 1989 | A |
4883122 | Puri et al. | Nov 1989 | A |
4929348 | Rice et al. | May 1990 | A |
4978172 | Schwoebel et al. | Dec 1990 | A |
5016710 | Renard et al. | May 1991 | A |
5035605 | Dinerman et al. | Jul 1991 | A |
5036921 | Pittard et al. | Aug 1991 | A |
5074360 | Guinn | Dec 1991 | A |
5074365 | Kuckes | Dec 1991 | A |
5074366 | Karlsson et al. | Dec 1991 | A |
5082054 | Kiamanesh | Jan 1992 | A |
5099921 | Puri et al. | Mar 1992 | A |
5111893 | Kvello-Aune | May 1992 | A |
5135058 | Millgard et al. | Aug 1992 | A |
5148875 | Karlsson et al. | Sep 1992 | A |
5165491 | Wilson | Nov 1992 | A |
5168942 | Wydrinski | Dec 1992 | A |
5174374 | Hailey | Dec 1992 | A |
5193620 | Braddick | Mar 1993 | A |
5194859 | Warren | Mar 1993 | A |
5197553 | Leturno | Mar 1993 | A |
5197783 | Theimer et al. | Mar 1993 | A |
5199496 | Redus et al. | Apr 1993 | A |
5201817 | Hailey | Apr 1993 | A |
5217076 | Masek | Jun 1993 | A |
5240350 | Yamaguchi et al. | Aug 1993 | A |
5242017 | Hailey | Sep 1993 | A |
5242025 | Neill et al. | Sep 1993 | A |
5246273 | Rosar | Sep 1993 | A |
5255741 | Alexander | Oct 1993 | A |
5271472 | Leturno | Dec 1993 | A |
5289881 | Schuh | Mar 1994 | A |
5301760 | Graham | Apr 1994 | A |
5363927 | Frank | Nov 1994 | A |
5385205 | Hailey | Jan 1995 | A |
5394950 | Gardes | Mar 1995 | A |
5402851 | Baiton | Apr 1995 | A |
5411082 | Kennedy | May 1995 | A |
5411085 | Moore et al. | May 1995 | A |
5411088 | LeBlanc et al. | May 1995 | A |
5411104 | Stanley | May 1995 | A |
5411105 | Gray | May 1995 | A |
5419396 | Palmer et al. | May 1995 | A |
5431220 | Lennon et al. | Jul 1995 | A |
5435400 | Smith | Jul 1995 | A |
5447416 | Wittrisch | Sep 1995 | A |
5450902 | Matthews | Sep 1995 | A |
5454419 | Vloedman | Oct 1995 | A |
5458209 | Hayes et al. | Oct 1995 | A |
5462116 | Carroll | Oct 1995 | A |
5462120 | Gondouin | Oct 1995 | A |
5469155 | Archambeault et al. | Nov 1995 | A |
5477923 | Jordan, Jr. et al. | Dec 1995 | A |
5485089 | Kuckes | Jan 1996 | A |
5494121 | Nackerud | Feb 1996 | A |
5499687 | Lee | Mar 1996 | A |
5501273 | Puri | Mar 1996 | A |
5501279 | Garg et al. | Mar 1996 | A |
5533573 | Jordan, Jr. et al. | Jul 1996 | A |
5562159 | Smith et al. | Oct 1996 | A |
5584605 | Beard et al. | Dec 1996 | A |
5613242 | Oddo | Mar 1997 | A |
5615739 | Dallas | Apr 1997 | A |
5653286 | McCoy et al. | Aug 1997 | A |
5655605 | Matthews | Aug 1997 | A |
5669444 | Riese et al. | Sep 1997 | A |
5680901 | Gardes | Oct 1997 | A |
5690390 | Bithell | Nov 1997 | A |
5706871 | Andersson et al. | Jan 1998 | A |
5720356 | Gardes | Feb 1998 | A |
5727629 | Blizzard, Jr. et al. | Mar 1998 | A |
5735350 | Longbottom et al. | Apr 1998 | A |
5771976 | Talley | Jun 1998 | A |
5775433 | Hammett et al. | Jul 1998 | A |
5785133 | Murray et al. | Jul 1998 | A |
5832958 | Cheng | Nov 1998 | A |
5853054 | McGarian et al. | Dec 1998 | A |
5853056 | Landers | Dec 1998 | A |
5853224 | Riese | Dec 1998 | A |
5863283 | Gardes | Jan 1999 | A |
5868202 | Hsu | Feb 1999 | A |
5868210 | Johnson et al. | Feb 1999 | A |
5879057 | Schwoebel et al. | Mar 1999 | A |
5884704 | Longbottom et al. | Mar 1999 | A |
5917325 | Smith | Jun 1999 | A |
5934390 | Uthe | Aug 1999 | A |
5938004 | Roberts et al. | Aug 1999 | A |
5941308 | Malone et al. | Aug 1999 | A |
5957539 | Durup et al. | Sep 1999 | A |
5971074 | Longbottom et al. | Oct 1999 | A |
6012520 | Yu et al. | Jan 2000 | A |
6015012 | Reddick | Jan 2000 | A |
6024171 | Montgomery et al. | Feb 2000 | A |
6050335 | Parsons | Apr 2000 | A |
6056059 | Ohmer | May 2000 | A |
6065550 | Gardes | May 2000 | A |
6119771 | Gano et al. | Sep 2000 | A |
6123159 | Brookey et al. | Sep 2000 | A |
6135208 | Gano et al. | Oct 2000 | A |
6179054 | Stewart | Jan 2001 | B1 |
6209636 | Roberts et al. | Apr 2001 | B1 |
6280000 | Zupanick | Aug 2001 | B1 |
6349769 | Ohmer | Feb 2002 | B1 |
6357523 | Zupanick | Mar 2002 | B1 |
6357530 | Kennedy et al. | Mar 2002 | B1 |
6425448 | Zupanick et al. | Jul 2002 | B1 |
6439320 | Zupanick | Aug 2002 | B2 |
6450256 | Mones | Sep 2002 | B2 |
6454000 | Zupanick | Sep 2002 | B1 |
6457540 | Gardes | Oct 2002 | B2 |
6478085 | Zupanick | Nov 2002 | B2 |
6497556 | Zupanick et al. | Dec 2002 | B2 |
6561277 | Algeory | May 2003 | B2 |
6561288 | Zupanick | May 2003 | B2 |
6566649 | Mickael | May 2003 | B1 |
6571888 | Comeau et al. | Jun 2003 | B2 |
6575235 | Zupanick et al. | Jun 2003 | B2 |
6577129 | Thompson et al. | Jun 2003 | B1 |
6585061 | Radzinski et al. | Jul 2003 | B2 |
6590202 | Mickael | Jul 2003 | B2 |
6591903 | Ingle et al. | Jul 2003 | B2 |
6598686 | Zupanick | Jul 2003 | B1 |
6604580 | Zupanick et al. | Aug 2003 | B2 |
6604910 | Zupanick | Aug 2003 | B1 |
6607042 | Hoyer et al. | Aug 2003 | B2 |
6636159 | Winnacker | Oct 2003 | B1 |
6639210 | Odom et al. | Oct 2003 | B2 |
6646441 | Thompson et al. | Nov 2003 | B2 |
6653839 | Yuratich et al. | Nov 2003 | B2 |
6662870 | Zupanick et al. | Dec 2003 | B1 |
6668918 | Zupanick | Dec 2003 | B2 |
6679322 | Zupanick | Jan 2004 | B1 |
6681855 | Zupanick et al. | Jan 2004 | B2 |
6688388 | Zupanick | Feb 2004 | B2 |
6708764 | Zupanick | Mar 2004 | B2 |
6712138 | Mandal | Mar 2004 | B2 |
6725922 | Zupanick | Apr 2004 | B2 |
6732792 | Zupanick | May 2004 | B2 |
6745855 | Gardes | Jun 2004 | B2 |
6755249 | Robison et al. | Jun 2004 | B2 |
6758289 | Kelly et al. | Jul 2004 | B2 |
6761219 | Snider et al. | Jul 2004 | B2 |
6923275 | Gardes | Aug 2005 | B2 |
7037881 | Growcock et al. | May 2006 | B2 |
7063164 | Hilsman et al. | Jun 2006 | B2 |
7163063 | Seams | Jan 2007 | B2 |
20020074120 | Scott | Jun 2002 | A1 |
20020096336 | Zupanick et al. | Jul 2002 | A1 |
20020189801 | Zupanick et al. | Dec 2002 | A1 |
20030066686 | Conn | Apr 2003 | A1 |
20030075334 | Haugen et al. | Apr 2003 | A1 |
20030217842 | Zupanick et al. | Nov 2003 | A1 |
20040007389 | Zupanick | Jan 2004 | A1 |
20040007390 | Zupanick | Jan 2004 | A1 |
20040035582 | Zupanick | Feb 2004 | A1 |
20040050552 | Zupanick | Mar 2004 | A1 |
20040050554 | Zupanick et al. | Mar 2004 | A1 |
20040055787 | Zupanick | Mar 2004 | A1 |
20040118558 | Rial et al. | Jun 2004 | A1 |
20040149428 | Kvernstuen et al. | Aug 2004 | A1 |
20050109505 | Seams | May 2005 | A1 |
20050183859 | Seams | Aug 2005 | A1 |
20060006004 | Terry et al. | Jan 2006 | A1 |
20060131076 | Zupanick | Jun 2006 | A1 |
20060201714 | Seams et al. | Sep 2006 | A1 |
Number | Date | Country |
---|---|---|
2 278 735 | Jan 1998 | CA |
653 741 | Jan 1986 | CH |
0 875 661 | Nov 1998 | EP |
0 952 300 | Oct 1999 | EP |
2 255 033 | Oct 1992 | GB |
2 297 988 | Aug 1996 | GB |
2 332 224 | Jun 1999 | GB |
2 347 157 | Aug 2002 | GB |
750108 | Jun 1975 | SU |
1448078 | Mar 1987 | SU |
1770570 | Mar 1990 | SU |
WO 9421889 | Sep 1994 | WO |
WO 9835133 | Aug 1998 | WO |
WO 9960248 | Nov 1999 | WO |
WO 0031376 | Jun 2000 | WO |
WO 0079099 | Dec 2000 | WO |
WO 0144620 | Jun 2001 | WO |
WO 0151760 | Jul 2001 | WO |
WO 0151760 | Jul 2001 | WO |
WO 0218738 | Mar 2002 | WO |
WO 02059455 | Aug 2002 | WO |
WO 02061238 | Aug 2002 | WO |
WO 03102348 | Dec 2003 | WO |
Number | Date | Country | |
---|---|---|---|
20060131024 A1 | Jun 2006 | US |