The present invention relates generally to the field of subterranean exploration and drilling and, more particularly, to a system and method for multiple wells from a common surface location.
Subterranean deposits of coal contain substantial quantities of entrained methane gas. Limited production in use of methane gas from coal deposits has occurred for many years. Substantial obstacles, however, have frustrated more extensive development in use of methane gas deposits in coal seams. The foremost problem in producing methane gas from coal seams is that while coal seams may extend over large areas of up to several thousand acres, the coal seams are fairly shallow in depth, varying from a few inches to several meters. Thus, while the coal seams are often relatively near the surface, vertical wells drilling into the coal deposits for obtaining methane gas can only drain a fairly small radius around the coal deposits. Further, coal deposits are not amenable to pressure fracturing and other methods often used for increasing methane 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 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 seams. The most efficient method for pumping water from a subterranean well, a sucker rod pump, does not work well in horizontal or radiused bores.
The present invention provides a system and method using multiple articulated and drainage wells from a common surface well that substantially eliminates, reduces, or minimizes the disadvantages and problems associated with previous systems and methods. In particular, certain embodiments of the present invention provide a system and method using multiple articulated and drainage wells from a single surface well for efficiently producing and removing entrained methane gas and water from a coal seam without requiring that multiple wells be drilled from the surface.
In accordance with one embodiment of the present invention, a system for accessing a subterranean zone from an entry well including an entry well extending from the surface. The entry well has a substantially vertical portion. One or more drainage wells extend from the entry well to a subterranean zone. One or more articulated wells extend from the entry well to the subterranean zone. At least one of the articulated wells intersects at least one of the one or more drainage wells at a junction proximate the subterranean zone. A drainage pattern is formed coupled to the junction and operable to conduct fluids from the subterranean zone to the junction.
The technical advantage of the present invention include providing a method and system for using multiple articulated and drainage wells from a common surface well. In particular, a technical advantage may include the formation of an entry well, a plurality of drainage wells, a plurality of articulated wells, and drainage patterns from a single surface location to minimize the number of surface wells needed to access a subterranean zone for draining of gas and liquid resources. This allows for more efficient drilling and production and greatly reduces costs and problems associated with other systems and methods.
Other technical advantages of the present invention will be readily apparent to one skilled in the art from the following figures, description, and claims.
For a more complete understanding of the present invention and its advantages, reference is now made to the following description taken in conjunction with the accompanying drawings, wherein like numerals represent like parts, in which:
Referring to
Entry well 12 is illustrated as being substantially vertical; however, it should be understood that entry well 12 may be formed at any suitable angle relative to surface 22 to accommodate, for example, surface geometries and attitudes and/or the geometric configuration or attitude of a subterranean resource. In the illustrated embodiment, drainage wells 14 are formed as slant wells that angle away from entry well 12 at an angle designated α. The angle α depends, in part, on the depth of subterranean zone 24. It will be understood that drainage wells 14 may be formed at other angles to accommodate surface topologies and other factors similar to those affecting entry well 12. Furthermore, although drainage wells 14 are illustrated as having the same angle of slant over their entire length (below entry well 12), drainage wells 14 may have two or more portions below entry well 12 that are at different angles. For example, the portion of drainage wells 14 from which cavity 18 is formed and/or which is intersected by the corresponding articulated well 16 may be substantially vertical. In the illustrated embodiment, drainage wells 14 are formed in relation to each other at an angular separation of β degrees. In one embodiment, the angle β equals twice the angle α. It will be understood that drainage wells 14 may be separated by other angles depending likewise on the topology and geography of the area and location of subterranean zone 24.
In particular embodiments, an enlarged cavity 18 may be formed from each drainage well 14 at the level of subterranean zone 24. As described in more detail below, cavity 18 provides a junction for the intersection of drainage well 14 by a corresponding articulated well 16 used to form a subterranean drainage bore pattern in subterranean zone 24. Cavity 18 also provides a collection point for fluids drained from subterranean zone 24 during production operations. In one embodiment, cavity 18 has a radius of approximately eight feet; however, any appropriate diameter cavity may be used. Cavity 18 may be formed using suitable under-reaming techniques and equipment. A portion of drainage well 14 may continue below cavity 18 to form a sump 20 for cavity 18. Although cavities 18 and sumps 20 are illustrated, it should be understood that particular embodiments do not include a cavity and/or a sump.
Each articulated well 16 extends from the terminus of entry well 12 to cavity 18 of a corresponding drainage well 14 (or to the drainage well 14 if no cavity is formed). Each articulated well 16 includes a first portion 34, a second portion 38, and a curved or radiused portion 36 interconnecting portions 34 and 38. In
In the illustrated embodiment, drainage well 14 is sufficiently angled away from a corresponding articulated well 16 to permit the large radiused curved portion 36 and any desired portion 38 to be drilled before intersecting cavity 18. In particular embodiments, curved portion 36 may have a radius of one hundred to one hundred fifty feet; however, any suitable radius may be used. This angle α may be chosen to minimize the angle of curved portion 36 to reduce friction in articulated well 16 during drilling operations. As a result, the length of articulated well 16 is maximized.
After cavity 18 has been successfully intersected by articulated well 16, drilling is continued through cavity 18 using articulated well string 26 to provide a drainage bore pattern 32 in subterranean zone 24. In
During the process of drilling drainage bore pattern 32 in a coal seam or other appropriate formations, drilling fluid or “mud” may be pumped down articulated drill string 26 and circulated out of drill string 26 in the vicinity of a bit 28, where it is used to scour the formation and to remove formation cuttings. The cuttings are then entrained in the drilling fluid which circulates up through the annulus between drill string 26 and the walls of articulated well 16 until it reaches surface 22, where the cuttings are removed from the drilling fluid and the fluid is then recirculated. This conventional drilling operation produces a standard column of drilling fluid having a vertical height equal to the depth of articulated well 16 and produces a hydrostatic pressure on the well bore corresponding to the well bore depth. Because coal seams tend to be porous and fractured, they may be unable to sustain such hydrostatic pressure, even if formation water is also present in subterranean zone 24. Accordingly, if the full hydrostatic pressure is allowed to act on subterranean zone 24, the result may be loss of drilling fluid in entrained cuttings into the formation. Such a circumstance is referred to as an “over-balanced” drilling operation in which they hydrostatic fluid pressured in the well bore exceeds the ability of the formation to withstand the pressure. Loss of drilling fluids and cuttings into the formation not only is expensive in terms of the lost drilling fluids, which must be made up, but also tends to plug the pores in subterranean zone 24, which are needed to drain the coal seam of gas and water.
To prevent over-balanced drilling conditions during formation of drainage bore pattern 32, air compressors or other suitable pumps may be provided to circulate compressed air or other suitable fluids down drainage wells 14 and back up through corresponding articulated wells 16. The circulated air or other fluid will mix with the drilling fluid in the annulus around the articulated drill string 26 and create bubbles throughout the column of drilling fluid. This has the effect of lightening the hydrostatic pressure of the drilling fluid and reducing the down-hole pressure significantly that drilling conditions do not become over-balanced. Aeration of the drilling fluid reduces down-hole pressure to approximately 150–200 pounds per square inch (psi). Accordingly, low pressure coal seams and other subterranean zones can be drilled without substantial loss of drilling fluid and contamination of the zone by the drilling fluid. Alternatively, tubing may be inserted into drainage well 14 such that air pumped down through the tubing forces the fluid back through the annulus between the tubing and drainage well 14.
In yet another embodiment, a down-hole pumping unit 40 may be installed in cavity 18, as illustrated in
Foam, which may be compressed air mixed with water, may also be circulated down through the articulated drill string 26 along with the drilling mud in order to aerate the drilling fluid in the annulus as articulated well 16 is being drilled and, if desired, as drainage bore pattern 32 is being drilled. Drilling of drainage bore pattern 32 with the use of an air hammer bit or an air-powered down-hole motor will also supply compressed air or foam to the drilling fluid. In this case, the compressed air or foam which is used to power the down-hole motor and bit 28 exits articulated drill string 26 in the vicinity of drill bit 28. However, the larger volume of air which can be circulated down drainage wells 14 permits greater aeration of the drilling fluid than generally is possible by air supplied through articulated drill string 26.
Referring to
Each down-hole pump 40 is connected to surface 22 via a respective tubing string 42 and may be powered by sucker rods extending down through wells 14 of tubing strings 42. Sucker rods are reciprocated by a suitable surface mounted apparatus, such as a powered walking beam 46 to operate each down-hole pump 40. Each down-hole pump 40 is used to remove water and entrained coal finds from subterranean zone 24 via drainage bore patterns 32. In the case of a coal seam, once the water is removed to the surface, it may be treated for separation of methane which may be dissolved in the water and for removal of entrained finds. After sufficient water has been removed from subterranean zone 24, pure coal seam gas may be allowed to flow to surface 22 through the annulus of wells 14 around tubing strings 42 and removed via piping attached to a well head apparatus. At surface 22, the methane is treated, compressed and pumped through a pipeline for use as fuel in a conventional manner. Each down-hole pump 40 may be operated continuously or as needed to remove water drained from subterranean zone 24 into cavities 18.
One or more secondary lateral bores 152 may be formed off one or more of the primary lateral bores 152. In a particular embodiment, a set of secondary laterals 154 may be formed off the primary lateral bores 152 of each pattern 32a and 32b closest to the corresponding cavity 18a and 18b. The secondary laterals 154 may provide coverage in the area between the primary lateral bores 152 of patterns 32a and 32b. In a particular embodiment, a first primary lateral 154 may include a reversed radius section to provide more uniform coverage of subterranean zone 24.
The subterranean patterns 32a and 32b with their central bore and generally symmetrically arranged and appropriately spaced auxiliary bores on each side may provide a substantial uniform pattern for draining fluids from subterranean zone 24 or other subterranean zone. The number and spacing of the lateral bores may be adjusted depending on the absolute, relative and/or effective permeability of the coal seam and the size of the area covered by the pattern. The area covered by the pattern may be the area drained by the pattern, the area of a spacing unit that the pattern is designed to drain, the area within the distal points or periphery of the pattern and/or the area within the periphery of the pattern as well as surrounding area out to a periphery intermediate to adjacent or neighboring patterns. The coverage area may also include the depth, or thickness of the coal seam or, for thick coal seams, a portion of the thickness of the seam. Thus, the pattern may include upward or downward extending branches in addition to horizontal branches. The coverage area may be a square, other quadrilateral, or other polygon, circular, oval or other ellipsoid or grid area and may be nested with other patterns of the same or similar type. It will be understood that other suitable drainage bore patterns may be used.
As previously described, the well bore 150 and the lateral bores 152 and 154 of patterns 32a and 32b are formed by drilling through the corresponding cavity 18a or 18b using the drill string 26 in appropriate drilling apparatus. During this operation, gamma ray logging tools and conventional MWD technologies may be employed to control the direction and orientation of drill bit 28 so as to retain the drainage bore pattern within the confines of subterranean zone 24 and to maintain proper spacing and orientation of wells 150 and 152. In a particular embodiment, the main well bore 150 of each pattern 32a and 32b is drilled with an incline at each of the plurality of lateral branch points 156. After the main well bore 150 is complete, the drill string 26 is backed up to each successive lateral point 156 from which a primary lateral bore 152 is drilled on each side of the well bore 150. The secondary laterals 154 may be similarly formed. It will be understood that the subterranean patterns 32a and 32b may be otherwise suitably formed. Furthermore, as described above, a pattern (as illustrated in
At step 406, drill string 26 is inserted through entry well 12 and one of the guide tubes in the guide tube bundle. At step 408, drill string 26 is used to drill approximately fifty feet past the casing. At step 410, the drill is oriented to the desired angle of the drainage well 14 and, at step 412, drainage well bore 14 is drilled down into and through target subterranean zone 24.
At step 414, down-hole logging equipment may be utilized to identify the location of the subterranean zone 24. At step 416, cavity 18a is formed in first drainage well 14 at the location of subterranean zone 24. As previously discussed, cavity 18 may be formed by underreaming and other conventional techniques. At decisional step 418, if additional drainage wells are to be drilled, the method returns to step 406. If no additional drainage wells 14 are to be drilled, then the method proceeds to step 420.
At step 420, articulated well 16 is drilled to intersect cavity 18. At step 422, drainage bore pattern 32 is drilled into subterranean zone 24. At step 424, production equipment is installed into drainage wells 14 and at step 426 the process ends with the production of fluids (such as water and gas) from the subterranean zone 24.
Although the steps have been described in a certain order, it will be understood that they may be performed in any other appropriate order. Furthermore, one or more steps may be omitted, or additional steps performed, as appropriate.
Corresponding with step 404 of
In operation, drill string 26 is positioned to enter one of the guide tubes 48. In order to keep drill string 26 relatively centered in casing 50, a stabilizer 54 may be employed. Stabilizer 54 may be a ring and fin type stabilizer or any other stabilizer suitable to keep drill string 26 relatively centered. To keep stabilizer 54 at a desired depth in well bore 12, stop ring 56 may be employed. Stop ring 56 may be constructed of rubber or metal or any other foreign down-hole environment material suitable. Drill string 26 may be inserted randomly into any of a plurality of guide tubes 48, or drill string 26 may be directed into a selected guide tube 48a. This corresponds to step 406 of
Although the present invention has been described with several embodiments, various changes and modifications may be suggested to one skilled in the art. It is intended that the present invention encompass such changes and modifications as fall within the scope of the appended 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 |
| 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 | Lytel | 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 |
| 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 |
| 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 |
| RE38642 | Gondouin | Nov 2004 | E |
| 20020043404 | Trueman et al. | Apr 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 |
| 20030164253 | Trueman et al. | Sep 2003 | A1 |
| 20030217842 | Zupanick et al. | Nov 2003 | A1 |
| 20030221836 | Gardes | Dec 2003 | A1 |
| 20030234120 | Paluch et al. | Dec 2003 | A1 |
| 20040007389 | Zupanick | Jan 2004 | A1 |
| 20040007390 | Zupanick | Jan 2004 | A1 |
| 20040011560 | Rial et al. | Jan 2004 | A1 |
| 20040020655 | Rusby et al. | Feb 2004 | A1 |
| 20040031609 | Zupanick | Feb 2004 | A1 |
| 20040033557 | Scott et al. | Feb 2004 | A1 |
| 20040035582 | Zupanick | Feb 2004 | A1 |
| 20040050552 | Zupanick | Mar 2004 | A1 |
| 20040050554 | Zupanick et al. | Mar 2004 | A1 |
| 20040055787 | Zupanick | Mar 2004 | A1 |
| 20040060351 | Gunter et al. | Apr 2004 | A1 |
| 20040140129 | Gardes | Jul 2004 | A1 |
| 20040226719 | Morgan et al. | Nov 2004 | A1 |
| 20050133219 | Zupanick | Jun 2005 | A1 |
| 20050252689 | Gardes | Nov 2005 | A1 |
| 20050257962 | Zupanick | Nov 2005 | A1 |
| 20060096755 | Zupanic | May 2006 | A1 |
| Number | Date | Country |
|---|---|---|
| 8549964 | Nov 1986 | AU |
| 2210866 | Jan 1998 | CA |
| 2278735 | Aug 1998 | CA |
| 653741 | Jan 1986 | CH |
| 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 |
| 2 225 033 | Oct 1992 | GB |
| 2 297 988 | Aug 1996 | GB |
| 2 347 157 | Aug 2000 | GB |
| 750108 | Jun 1975 | SU |
| 876968 | Oct 1981 | SU |
| 1448078 | Mar 1987 | SU |
| 1770570 | Mar 1990 | 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 | |
|---|---|---|---|
| 20050189114 A1 | Sep 2005 | US |