The present invention relates generally to accessing subterranean zones.
Subterranean deposits of coal contain substantial quantities of entrained methane gas. Production of this gas is desirable both when it can be produced in useful quantities as a natural resource as well as when it is present in areas where mining of the coal is planned or in progress. Substantial obstacles, however, have frustrated extensive development and use of methane gas deposits in coal seams.
The foremost problem in producing methane gas from coal seams is recovery efficiency of the gas from the coal. Recovery efficiency in coal varies widely, and in coals where the recovery efficiency is low, vertical well developments obtain only a small amount of gas from around the well. Further, some coal deposits are not amenable to pressure fracturing and other methods often used for increasing gas production from rock formations. As a result, once the gas easily drained from a vertical well bore in a coal seam is produced, further production in some coal is limited in volume. Additionally, coal seams are often associated with subterranean water, which must be drained from the coal seam in order to produce the methane.
Horizontal drilling patterns have been tried in order to extend the amount of coal seams exposed to a drill bore for gas extraction. Such horizontal drilling techniques, however, require the use of a radiused well bore which presents difficulties in removing the entrained water from the coal seam. In most instances, pumping water from a vertical bore is more efficient and less expensive than pumping water from a horizontal or radiused bore.
Systems based on horizontal bores that intersect the cavity in a vertical well bore combine the advantages of horizontal drainage patterns with the efficiency associated with pumping from a vertical well bore. Liners, often installed to enhance the structural integrity of the bores, are joined at the intersections between lined bores by junctions installed using various techniques.
The present invention provides an improved method and system for accessing subterranean zones from the surface. In one aspect, the present invention provides an articulated well bore coupled to a well bore pattern that provides access to a large subterranean area from the surface. The well bore pattern includes two or more well bores, one or more of which can, in some instances, be lined. In illustrative embodiments, the articulated well bore and well bore pattern can be coupled to a vertical well bore. The vertical well bore allows entrained water, hydrocarbons, and other deposits to be efficiently removed (e.g. by pumping the fluid, by using a gas lift, or by natural flow from the well) and/or produced. In some illustrative embodiments, the articulated well bore and well bore pattern can be coupled to a cavity that functions as a junction between multiple lined bores. In some illustrative embodiments, the cavity is packed with gravel (e.g. an unconsolidated mixture of pebbles, rock fragments, or other suitable packing material).
In another aspect, a method for accessing a subterranean zone includes forming a subterranean cavity coupled to a land surface; and forming a plurality of substantially horizontal bores extending at least partially into the subterranean zone and intersecting the cavity.
In another aspect, a system for accessing a subterranean zone includes a subterranean cavity coupled to a land surface, and a plurality of substantially horizontal bores extending at least partially into the subterranean zone and intersecting the cavity.
In another aspect, a method of accessing a coal seam includes forming a cavity proximate the coal seam and coupled to a land surface, gravel packing at least a portion of the cavity; and producing fluid from the cavity to the land surface. The phrase “proximate” a seam or zone is defined herein as near or intersecting the seam or zone.
In another aspect, a system for accessing a coal seam includes a cavity proximate the coal seam and coupled to a land surface wherein at least a portion of the cavity is packed with gravel.
In some embodiments, forming the cavity can include forming the cavity (e.g. a cavity including a substantially cylindrical portion) proximate the subterranean zone. Forming a subterranean cavity coupled to a land surface, forming a first bore (e.g. a substantially vertical bore) extending from the land surface, and forming a cavity in the well bore.
In some instances, forming a plurality of substantially horizontal bores extending at least partially into the subterranean zone and intersecting the cavity includes forming an articulated bore (e.g. an articulated bore offset horizontally from the first bore) extending from a land surface to proximate the subterranean zone and forming the plurality of substantially horizontal bores from the articulated bore. The first bore and the articulated bore can extend from the land surface through an entry bore. In some instances, the subterranean zone can be a portion of coals seam. In some instances, the horizontal bores can be horizontal drainage bores (e.g. bores with liners adapted to communicate fluid between an interior of the liner and the cavity).
In some embodiments, these aspects can also include installing a liner in two or more of the plurality of substantially horizontal bores. In some instances, such liners can terminate proximate the cavity. In other instances, at least one of the liners traverses the cavity.
In some embodiments, the aspects can also include gravel-packing at least a portion of the cavity.
In some embodiments, these aspects can also include withdrawing fluid from the cavity to the land surface through the first bore. In some instances, withdrawing fluid includes providing artificial lift (e.g. pumping the fluid or using a gas lift) to raise the fluid from the cavity to the land surface. In some instances, the systems can include a pump inlet in the first bore.
The above discussions of aspects of the invention include, for clarity of description, language putting necessary elements in context (e.g. coupled to a land surface). This language is not be construed as necessary elements of an individual aspect.
The details of one or more embodiments 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.
Like reference symbols in the various drawings indicate like elements. The drawings are not to scale.
Referring to
In this instance, the well bore 14 is substantially vertical and will be referred to as the substantially vertical well bore for descriptive purposes. However, embodiments of the systems described below can be implemented where at least a portion of the well bore is a slanted bore.
The substantially vertical well bore 14 extends from a land surface 16 (e.g. directly from the land surface itself, from an entry bore extending directly from the land surface, or from another near-surface feature) to the subterranean zone 12 where the cavity 18 formed in the substantially vertical well bore. In some instances, the cavity 18 is reamed or cut in a cylindrical shape with a diameter that is greater than the diameter of the substantially vertical well bore 14. In other instances, the cavity 18 has a diameter that is approximately equal to or less than the diameter of the vertical well bore 14. The substantially vertical well bore 14 is lined with a suitable well casing 32 that terminates above an upper surface of the cavity 18. An apertured liner 34 extends from the well casing 32 into the cavity 18. The apertures can be holes, slots, or openings of any other suitable size and shape. The apertured liner 34 can be an expandable liner that is expanded radially when positioned in the cavity 18 to both increase the diameter of the liner and increase the transverse dimension of the apertures therein. In the embodiment of
The articulated well bore 20 extends from the land surface 16 towards the cavity 18 of the substantially vertical well bore 14. The articulated well bore 20 includes a first portion 24, a second portion 26, and a curved or radiused portion 28 interconnecting the first and second portions 24 and 26. In some instances, the first portion 24 is substantially vertical bore, and in other instances, the first portion is a slanted bore. The second portion 26 lies substantially in the horizontal plane of the formation (coal seam) and may follow any up or down dip of the formation and can also have a general overall slope. The one or more (three shown) substantially horizontal bores 22 extend from the vicinity of an open end 30 of the second portion 26 of the articulated well bore 20 through the cavity 18 and into the subterranean zone 12. As with the second portion 26, the horizontal bores 22 lie substantially in the horizontal plane of the formation (coal seam) and may follow any up or down dip of the formation and can also have a general overall slope. In some instances, the general slope of the horizontal bores 22 is upwards from the cavity 18 towards the far ends of the horizontal bores 22 such that fluids in the bores are biased to flow towards the cavity 18.
The bores 22 have liners 40 with apertures 42 providing fluid communication between subterranean zone 12 and interior 44 of the liners 40 as well as between the interior of the liners 40 and the cavity 18. Consequently, it is not necessary to form junctions connecting the liners 40 of the bores 22 with each other or with the articulated well bore. In effect, the cavity 18 itself acts as a junction between the bores 22 and the vertical well (e.g. pumping fluid from inside the apertured liner 34 to the land surface 16 draws fluid from the coal seam through the bores and the cavity into the apertured liner 34). In a coal seam, the fluid can be water and entrained coal fines.
The cavity 18 is packed with gravel 38 encompassing the substantially horizontal bores 22 and the apertured liner 34. The gravel pack 38 helps support the cavity 18 and also acts to filter coal fragments out of pumped fluid before it enters the apertured liner 34 of the vertical well bore 14. In some instances, the gravel may be coarse because, for example, coal fragments breaking off from the coal seam tend to be larger than the sands, silts, and clays that are typically produced by pumping in other formations. For example, gravel with the mean diameter of between about 20 and about 30 mm can be used. The coarse gravel is different from finer gravel (i.e. gravel with a smaller mean diameter) used around the apertured liner when producing from a sandy formation. However, finer gravel can be used in accordance with the concepts described herein.
The substantially vertical well bore 14 is logged either during or after drilling in order to locate the exact vertical depth of the subterranean zone 12. The cavity 18 is formed in the substantially vertical well bore 14 at the level of the subterranean zone 12. In some instances, the cavity 18 is formed using suitable under-reaming techniques and equipment. Alternatively, other techniques and equipment (e.g. hydrojet technology) can be used. A vertical portion of the substantially vertical well bore 14 continues below the cavity 18 to form a sump 25 for the cavity 18. As described above, the cavity 18 provides a junction for intersection of the substantially vertical well bore by articulated well bore used to form a substantially horizontal drainage pattern 46 in the subterranean zone 12. The cavity 18 also provides a collection point for fluids drained from the subterranean zone 12 during production operations. In embodiments that include a sump 25, the sump also provides a collection point for fluids. In this illustrative embodiment, the cavity 18 has a radius of approximately two meters and a vertical dimension which approximates the vertical dimension of the subterranean zone 12.
Appropriate drilling techniques for installing the system 10 described in U.S. Pat. No. 6,357,523 issued to Zupanik which is incorporated herein, by reference, in its entirety. The discussion below focuses deviations from these methods due to differences in the systems being installed.
Conventional drilling operations can result in an “over balanced” drilling operation in which the hydrostatic fluid pressure in the well bore exceeds the reservoir pressure. This can lead to loss of drilling fluid and entrained cuttings into permeable formations. In systems with intersecting wells as described above, gas compressors can be used to circulate compressed gas down the substantially vertical well bore 14 and back up through the articulated well bore 20 to prevent over balance drilling conditions during formation of the horizontal bores 22. In some instances, this approach can be used to achieve “under balanced” drilling conditions (i.e. conditions in which pressure in the formation exceeds the pressure of the drilling mud). Alternatively, “under balanced” drilling conditions can be achieved by withdrawing fluid from the vertical bore 14 or by introducing foam into the drilling mud. Factors including rock stability influence the determination of whether “over balanced” or “under balanced” drilling conditions are most appropriate for a specific formation.
The first portion 24 of the articulated well bore 20 is offset a sufficient distance from the cavity 18 to permit the radius curved section 28 and any desired second section 26 to be drilled while leaving sufficient space to also drill so as to achieve the desired spacing between the separate bores 22 before they intersect the cavity 18. This spacing allows for an increase in the radius of the curved portion 28 to reduce friction in the articulated well bore 20 during drilling operations. As a result, reach of a drill string drilled through the articulated well bore 20 is increased over articulated bores with tighter radiuses.
The articulated well bore 20 is drilled using a drill string that includes a suitable down-hole motor and bit. A measurement while drilling (MWD) device is included in the drill string for controlling the orientation and direction of the well bore drilled by the motor and bit. The first portion 24, the curved portion 28, and at least part of the second portion 26 of the articulated well bore 20 may be lined with a suitable casing.
Now referring also to
The order in which individual horizontal bores are drilled can be varied. The terms “first,” “second,” and “third” are used simply describe the process of forming the horizontal bores rather to denote a specific horizontal bore 22.
After the first horizontal bore is drilled, the drilling apparatus is withdrawn and liner 40, mounted on a running tool, is extended through the articulated well bore 20 and into the first horizontal bore 22a. After the liner 40 reaches the end of the first horizontal bore 22a, the running tool is operated to release the liner 40 and is then withdrawn. The second horizontal bore 22b is deflected from the first horizontal bore 22a using a directional drilling assembly or a whipstock. The location and angle of deflection are chosen such that the second horizontal bore 22b is oriented to intersect and pass through the cavity 18 again leaving a space clear for a working string or tubing to be inserted while filling the cavity with gravel. This orientation is also set such that the second horizontal bore 22b extends into the zone at an angle which achieves lateral separation from the first horizontal bore 22a to form part of the desired drainage pattern 46.
The drilling apparatus is then withdrawn and the liner 40 for the second horizontal bore 22b is then installed using the process already described. The drilling and lining process is reapeated using a slightly different deflection location and angle to form the third horizontal bore 22c. The locations where the second and third horizontal bores 22b, 22c deflect, or kick off, from the first horizontal bore 22a maybe separated along the length of the first horizontal bore 22a. In some instances, the bores are separated by about 3 meters. The liners 40 can be provided with apertures before they are installed or can be perforated downhole.
In this illustrative embodiment, the liners 40 extend from the distal ends of the horizontal bores 22 back through the cavity 18 to or near the proximal ends of the horizontal bores. In the second, third and subsequent horizontal bores 22, the liners 40 terminate near the kick off point of the bore from the first horizontal bore 22a. Because the liner 40 terminate near the kick off point, if a liner 40 is unintentionally run into a bore that has been previously lined, the liner 40 will travel only a short distance into the bore before colliding with the previously placed liner.
In this illustrative embodiment, the cavity is filled with gravel after the horizontal bores 22 are drilled and lined. Tubing 33 or a working string is inserted through the vertical well bore 14 and into the cavity 18. As discussed above, the horizontal bores 22 are installed so as to leave space in the center of the cavity 18 for subsequent installation of the apertured liner 34. The tubing 33 or working string extends into the space towards the lower portion of the cavity 18. A gravel slurry is pumped down into the cavity 18 through the tubing 33. The tubing 33 or working string is withdrawn as gravel fills the cavity 18. Keeping the end of the tubing 33 or working string near the top of the gravel pack provides feedback as to the level of gravel in the cavity 18 and allows up-and-down motion of the tubing 33 or working string to be used to ‘tamp’ the gravel down. In other embodiments, the gravel slurry is pumped down an annulus between a working string and the casing 32 of the vertical well bore 14. The fluid portion of the gravel slurry is pumped out through the working string leaving the gravel in place in the cavity 18. Other approaches (e.g. pumping a gravel slurry down the interior of a working string to a crossover tool which discharges it out of the working string) can also be employed to install the gravel pack.
In this embodiment, the apertured liner 34 is installed after the gravel pack 38 is in place. Thus, the apertured liner 34 can be provided with an end cap or tip at least a portion of which is conical, fustoconical, hemispherical, otherwise pointed or another shape that facilitates driving the liner 34 through the gravel pack 38. Driving the liner 34 through the gravel pack 38 takes advantage of both the compressibility of the gravel pack 38 (i.e. compressing the gravel pack 38) and any resilience of the formation itself. In particular, coal seams typically exhibit some degree of “give” in response to such pressure. If the apertured liner 34 is of an expandable type, expansion of the liner also compresses the gravel pack 38. After the apertured liner 34 is in place, the running tool and working string are withdrawn. An alternative embodiments, the apertured liner 34 is placed in the cavity 18 before the gravel pack 38 is installed with the gravel slurry pumped into the cavity 18 around the apertured liner 34. As discussed above, the apertured liner is attached to the tubing 33.
Liquid (e.g. water and entrained coal fines in a coal seam) collected in the cavity 18 and/or the sump 25 is withdrawn through bore 14 while gas is withdrawn through bore 14 or bore 20. If the system 10 is being used for injection, fluid may be input through either bore 14 or bore 20. The pump inlet 36 is installed in the vertical well bore 14 after the apertured liner 34 and gravel pack 38 are in place. The pump inlet 36 can be positioned within the casing or within the apertured liner 34.
The apertured liners 40 of the horizontal bores are exposed to both the subterranean zone 12 and the cavity 18 containing the apertured liner 34. The resulting fluid communication between the zone 12 and the substantially vertical bore 14 means that is not necessary to construct and line multi-lateral junctions joining the horizontal bores 22 to each other and/or to the vertical bore 14. As discussed above, the cavity 18, in effect, acts as the junction.
Referring to
After a horizontal bore 122 has been drilled and a liner 140 is installed therein, a subsequent horizontal bore 122 may be drilled and a liner 140 placed in the latter drilled horizontal bore 122. Although the liner 140 is inserted back through the articulated well bore 120 and oriented to enter the latter drilled horizontal bore 122, the liner 140 may sometimes inadvertently enter a horizontal bore 122 that has already been lined. Because the liner 140 in the previously lined horizontal bore 122 terminates about the far side of the cavity 118, it may not be apparent that the liner 140 being run-in is entering a previously drilled and lined horizontal bore 122 until after the liner 140 has traversed the cavity 118.
In this system, the horizontal drainage system 146 is shown laid out with an optional herringbone pattern. Each of the horizontal bores 122 has one or more laterals 123 extending into the subterranean zone 112. These laterals 123 may also be lined, and their liners can be tied back to the liners of the horizontal bores 122 using cavities as described herein or with other types of tieback systems. Horizontal drainage patterns are laid out according to the characteristics of the formation and the access desired by the designer. Therefore, other patterns (e.g. pinnate patterns) can be used with this system as appropriate.
Referring to
Referring to
Referring to
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, although the illustrative systems included at most three (e.g. zero, one, or three) horizontal bores, some embodiments include four or more horizontal bores intersecting a cavity in a subterranean zone. In another example, although the discussions above have focused on applications where fluids are being withdrawn from a subterranean zone, these systems can also be used for injection of fluids into or sequestration of fluids into a formation. 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 |
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 |
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 |
2452654 | Hayes et al. | Nov 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 |
2797893 | McCune et al. | Jul 1957 | A |
2847189 | Shook | Aug 1958 | A |
2911008 | Du Bois | Nov 1959 | A |
2934904 | Hendrix | May 1960 | A |
2980142 | Turak | Apr 1961 | A |
3163211 | Henley | Dec 1964 | A |
3208537 | Scarborough | Sep 1965 | A |
3347595 | Dahms et al. | Oct 1967 | A |
3362475 | Huitt et al. | Jan 1968 | A |
3385382 | Canalizo et al. | May 1968 | 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 |
3534822 | Campbell et al. | Oct 1970 | A |
3578077 | Glenn, Jr. et al. | May 1971 | A |
3582138 | Loofbourow et al. | Jun 1971 | A |
3587743 | Howard | Jun 1971 | A |
3684041 | Kammerer, Jr. et al. | Aug 1972 | A |
3687204 | Marshall et al. | Aug 1972 | A |
3692041 | Bondi | Sep 1972 | A |
3744565 | Brown | Jul 1973 | A |
3757876 | Pereau | Sep 1973 | A |
3757877 | Leathers | Sep 1973 | A |
3759328 | Ueber et al. | Sep 1973 | A |
3763652 | Rinta | Oct 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 |
4020901 | Pisio et al. | May 1977 | A |
4022279 | Driver | May 1977 | A |
4030310 | Schirtzinger | Jun 1977 | A |
4037658 | Anderson | Jul 1977 | A |
4060130 | Hart | Nov 1977 | A |
4073351 | Baum | Feb 1978 | A |
4089374 | Terry | May 1978 | A |
4116012 | Abe et al. | Sep 1978 | A |
4134463 | Allen | Jan 1979 | A |
4136996 | Burns | Jan 1979 | A |
4151880 | Vann | May 1979 | A |
4156437 | Chivens et al. | May 1979 | A |
4169510 | Meigs | Oct 1979 | A |
4182423 | Ziebarth et al. | Jan 1980 | A |
4189184 | Green | Feb 1980 | A |
4220203 | Steeman | Sep 1980 | A |
4221433 | Jacoby | Sep 1980 | A |
4222611 | Larson et al. | Sep 1980 | A |
4224989 | Blount | Sep 1980 | A |
4226475 | Frosch et al. | Oct 1980 | 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 |
4296969 | Willman | Oct 1981 | A |
4299295 | Gossard | Nov 1981 | A |
4303127 | Freel et al. | 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 |
4356866 | Savins | Nov 1982 | A |
4366988 | Bodine | Jan 1983 | A |
4372398 | Kuckes | Feb 1983 | A |
4386665 | Dellinger | Jun 1983 | A |
4390067 | Willman | Jun 1983 | A |
4396075 | Wood et al. | Aug 1983 | A |
4396076 | Inoue | Aug 1983 | A |
4397360 | Schmidt | Aug 1983 | A |
4401171 | Fuchs | Aug 1983 | A |
4407376 | Inoue | Oct 1983 | A |
4415205 | Rehm et al. | Nov 1983 | A |
4417829 | Berezoutzky | Nov 1983 | A |
4422505 | Collins | Dec 1983 | A |
4437706 | Johnson | Mar 1984 | A |
4442896 | Reale et al. | Apr 1984 | A |
4458767 | Hoehn, Jr. | Jul 1984 | A |
4463988 | Bouck et al. | Aug 1984 | A |
4494616 | McKee | Jan 1985 | A |
4502733 | Grubb | Mar 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 |
4533182 | Richards | Aug 1985 | A |
4536035 | Huffman 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 |
4600061 | Richards | Jul 1986 | A |
4603592 | Siebold et al. | Aug 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 | Mar 1987 | A |
4662440 | Harmon et al. | May 1987 | A |
4674579 | Geller et al. | Jun 1987 | A |
4676313 | Rinaldi | Jun 1987 | A |
4702314 | Huang et al. | Oct 1987 | A |
4705109 | Ledent et al. | Nov 1987 | A |
4705431 | Gadelle et al. | Nov 1987 | A |
4715440 | Boxell et al. | Dec 1987 | A |
4718485 | Brown et al. | Jan 1988 | A |
RE32623 | Marshall et al. | Mar 1988 | E |
4727937 | Shum et al. | Mar 1988 | A |
4753485 | Goodhart | Jun 1988 | A |
4754808 | Harmon et al. | Jul 1988 | 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 |
4776638 | Hahn | Oct 1988 | A |
4830105 | Petermann | May 1989 | A |
4832122 | Corey et al. | 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 |
4889186 | Hanson et al. | Dec 1989 | A |
4978172 | Schwoebel et al. | Dec 1990 | A |
5016709 | Combe et al. | May 1991 | A |
5016710 | Renard et al. | May 1991 | A |
5033550 | Johnson et al. | Jul 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 |
5111893 | Kvello-Aune | May 1992 | A |
5115872 | Brunet et al. | May 1992 | A |
5127457 | Stewart et al. | Jul 1992 | A |
5135058 | Millgard et al. | Aug 1992 | A |
5148875 | Karlsson et al. | Sep 1992 | A |
5148877 | MacGregor | 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 |
5207271 | Sanchez et al. | May 1993 | A |
5217076 | Masek | Jun 1993 | A |
5226495 | Jennings, Jr. | Jul 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 |
5287926 | Grupping | Feb 1994 | A |
5289888 | Talley | Mar 1994 | A |
5301760 | Graham | Apr 1994 | A |
5343965 | Talley et al. | Sep 1994 | A |
5355967 | Mueller et al. | Oct 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 |
5431220 | Lennon et al. | Jul 1995 | A |
5431482 | Russo | 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 |
5520252 | McNair | May 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 |
5664911 | Bridges et al. | Sep 1997 | A |
5669444 | Riese et al. | Sep 1997 | A |
5676207 | Simon et al. | Oct 1997 | A |
5680901 | Gardes | Oct 1997 | A |
5690390 | Bithell | Nov 1997 | A |
5697445 | Graham | Dec 1997 | A |
5706871 | Andersson et al. | Jan 1998 | A |
5720356 | Gardes | Feb 1998 | A |
5727629 | Blizzard, Jr. et al. | Mar 1998 | A |
5733067 | Hunt et al. | Mar 1998 | A |
5735350 | Longbottom et al. | Apr 1998 | A |
5771976 | Talley | Jun 1998 | A |
5775433 | Hammett et al. | Jul 1998 | A |
5775443 | Lott | 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 |
5941307 | Tubel | Aug 1999 | A |
5941308 | Malone et al. | Aug 1999 | A |
5944107 | Ohmer | Aug 1999 | A |
5957539 | Durup et al. | Sep 1999 | A |
5971074 | Longbottom et al. | Oct 1999 | A |
5988278 | Johnson | Nov 1999 | A |
5992524 | Graham | Nov 1999 | A |
6012520 | Yu et al. | Jan 2000 | A |
6015012 | Reddick | Jan 2000 | A |
6019173 | Saurer et al. | Feb 2000 | A |
6024171 | Montgomery et al. | Feb 2000 | A |
6030048 | Hsu | Feb 2000 | A |
6050335 | Parsons | Apr 2000 | A |
6056059 | Ohmer | May 2000 | A |
6062306 | Gano et al. | May 2000 | A |
6065550 | Gardes | May 2000 | A |
6065551 | Gourley et al. | May 2000 | A |
6079495 | Ohmer | Jun 2000 | A |
6089322 | Kelley et al. | Jul 2000 | A |
6119771 | Gano et al. | Sep 2000 | A |
6119776 | Graham et al. | Sep 2000 | A |
6135208 | Gano et al. | Oct 2000 | A |
6170571 | Ohmer | Jan 2001 | B1 |
6179054 | Stewart | Jan 2001 | B1 |
6189616 | Gano et al. | Feb 2001 | B1 |
6192988 | Tubel | Feb 2001 | B1 |
6199633 | Longbottom | Mar 2001 | B1 |
6209636 | Roberts et al. | Apr 2001 | B1 |
6237284 | Erickson | May 2001 | B1 |
6244340 | McGlothen et al. | Jun 2001 | B1 |
6247532 | Ohmer | Jun 2001 | B1 |
6263965 | Schmidt et al. | Jul 2001 | B1 |
6279658 | Donovan et al. | Aug 2001 | B1 |
6280000 | Zupanick | Aug 2001 | B1 |
6283216 | Ohmer | Sep 2001 | B1 |
6318457 | Den Boer et al. | Nov 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 |
6457525 | Scott | Oct 2002 | B1 |
6457540 | Gardes | Oct 2002 | B2 |
6470978 | Trueman et al. | Oct 2002 | B2 |
6478085 | Zupanick | Nov 2002 | B2 |
6491101 | Ohmer | Dec 2002 | B2 |
6497556 | Zupanick et al. | Dec 2002 | B2 |
6554063 | Ohmer | Apr 2003 | B2 |
6557628 | Ohmer | May 2003 | B2 |
6561277 | Algeory et al. | May 2003 | B2 |
6561288 | Zupanick | May 2003 | B2 |
6564867 | Ohmer | May 2003 | B2 |
6566649 | Mickael | May 2003 | B1 |
6571888 | Comeau et al. | Jun 2003 | B2 |
6575235 | Zupanick et al. | Jun 2003 | B2 |
6575255 | Rial et al. | Jun 2003 | B1 |
6577129 | Thompson et al. | Jun 2003 | B1 |
6581455 | Berger et al. | Jun 2003 | B1 |
6581685 | Burgess et al. | Jun 2003 | B2 |
6585061 | Radzinski et al. | Jul 2003 | B2 |
6590202 | Mickael | Jul 2003 | B2 |
6591903 | Ingle et al. | Jul 2003 | B2 |
6591922 | Rial et al. | Jul 2003 | B1 |
6595301 | Diamond et al. | Jul 2003 | B1 |
6595302 | Diamond et al. | Jul 2003 | B1 |
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 |
6644422 | Rial et al. | Nov 2003 | B1 |
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 |
6722452 | Rial et al. | Apr 2004 | B1 |
6725922 | Zupanick | Apr 2004 | B2 |
6732792 | Zupanick | May 2004 | B2 |
6745855 | Gardes | Jun 2004 | B2 |
6758279 | Moore et al. | Jul 2004 | B2 |
6758289 | Kelley et al. | Jul 2004 | B2 |
6766859 | Haugen et al. | Jul 2004 | B2 |
RE38642 | Gondouin | Nov 2004 | E |
6848508 | Zupanick | Feb 2005 | B2 |
6851479 | Zupanick et al. | Feb 2005 | B1 |
6860147 | Gunter et al. | Mar 2005 | B2 |
6866106 | Trueman et al. | Mar 2005 | B2 |
6923275 | Gardes | Aug 2005 | B2 |
6932168 | Morgan et al. | Aug 2005 | B2 |
6942030 | Zupanick | Sep 2005 | B2 |
6953088 | Rial et al. | Oct 2005 | B2 |
6962030 | Conn | Nov 2005 | B2 |
6964298 | Zupanick | Nov 2005 | B2 |
6964308 | Zupanick | Nov 2005 | B1 |
6968893 | Rusby et al. | Nov 2005 | B2 |
6976533 | Zupanick | Dec 2005 | B2 |
6976547 | Rial et al. | Dec 2005 | B2 |
6986388 | Zupanick et al. | Jan 2006 | B2 |
6988548 | Diamond et al. | Jan 2006 | B2 |
6991047 | Zupanick | Jan 2006 | B2 |
6991048 | Zupanick | Jan 2006 | B2 |
7025137 | Zupanick | Apr 2006 | B2 |
7025154 | Zupanick | Apr 2006 | B2 |
7036584 | Zupanick et al. | May 2006 | B2 |
7048049 | Zupanick | May 2006 | B2 |
7100687 | Pauley | Sep 2006 | B2 |
20020043404 | Trueman et al. | Apr 2002 | A1 |
20020096336 | Zupanick et al. | Jul 2002 | A1 |
20030234120 | Paluch et al. | Dec 2003 | A1 |
20040033557 | Scott et al. | Feb 2004 | A1 |
20040035582 | Zupanick | Feb 2004 | A1 |
20040050554 | Zupanick et al. | Mar 2004 | A1 |
20040108110 | Zupanick | Jun 2004 | A1 |
20040140129 | Gardes | Jul 2004 | A1 |
20040206493 | Zupanick et al. | Oct 2004 | A1 |
20040244974 | Zupanick et al. | Dec 2004 | A1 |
20050087340 | Zupanick et al. | Apr 2005 | A1 |
20050109505 | Seams | May 2005 | A1 |
20050115709 | Zupanick et al. | Jun 2005 | A1 |
20050133219 | Zupanick | Jun 2005 | A1 |
20050167156 | Zupanick | Aug 2005 | A1 |
20050189114 | Zupanick | Sep 2005 | A1 |
20050211473 | Zupanick | Sep 2005 | A1 |
20050252689 | Gardes | Nov 2005 | A1 |
20050257962 | Zupanick | Nov 2005 | A1 |
20060000607 | Surjaatmadja et al. | Jan 2006 | A1 |
20060096755 | Zupanick | May 2006 | A1 |
Number | Date | Country |
---|---|---|
8549964 | Nov 1986 | AU |
2210866 | Jan 1998 | CA |
2278735 | Aug 1998 | CA |
653741 | Jan 1986 | CH |
2248254 | Feb 1997 | CN |
197 25 996 | Jan 1998 | DE |
0 819 834 | Jan 1998 | EP |
0 875 661 | Nov 1998 | EP |
0 952 300 | Oct 1999 | EP |
1 316 673 | Jun 2003 | EP |
964503 | Aug 1950 | FR |
442008 | Jan 1936 | GB |
444484 | Mar 1936 | GB |
651468 | Apr 1951 | GB |
893869 | Apr 1962 | GB |
2 255 033 | Oct 1992 | GB |
2 297 988 | Aug 1996 | GB |
2 347 157 | Aug 2000 | GB |
2097536 | Nov 1997 | RU |
2136566 | Sep 1999 | RU |
2176311 | Nov 2001 | RU |
2179234 | Feb 2002 | RU |
2205935 | Jun 2003 | RU |
750108 | Jun 1975 | SU |
876968 | Oct 1981 | SU |
1448078 | Mar 1987 | SU |
1770570 | Mar 1990 | SU |
1709076 | Jan 1992 | SU |
37720 | May 2001 | UA |
WO 9421889 | Sep 1994 | WO |
WO 9428280 | Dec 1994 | WO |
WO 9721900 | Jun 1997 | WO |
WO 9825005 | Jun 1998 | 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 0218738 | Mar 2002 | WO |
WO 02059455 | Aug 2002 | WO |
WO 02061238 | Aug 2002 | WO |
WO 03036023 | May 2003 | WO |
WO 03038233 | May 2003 | WO |
WO 03102348 | Dec 2003 | WO |
WO 2004035984 | Apr 2004 | WO |
WO 2005003509 | Jan 2005 | WO |
WO 2005012688 | Feb 2005 | WO |
Number | Date | Country | |
---|---|---|---|
20060266521 A1 | Nov 2006 | US |