This invention relates to the establishment of an anchor somewhere in the surface of an iceberg which allows the iceberg to be towed to a predetermined designated destination. The anchor is embedded in the iceberg by drilling and the anchor bit may be in the order of 100 feet long and it will be expected that about 15-20 feet of the drill will be permanently anchored in the iceberg. The diameter of the anchor drill bit will be about 12-18 inches in order to provide the necessary robustness to tow the iceberg and yet provide the necessary passages inside the bit for the water and ice chips which are allowed to flow inside the anchor bit during a drilling operation. Passages are also provided for the flow of liquid nitrogen etc. which are necessary to cool the exterior surface of the anchor so as to freeze the anchor in place in the selected iceberg.
Icebergs are a peculiar phenomenon. The process by which they are formed varies as to whether the icebergs themselves originate in the Arctic or Antarctic Oceans. The icebergs produced in the Antarctic tend to be of a flatter nature than those produced in the north and the Antarctic icebergs have become know as “tabular” or flattened icebergs. The northern variety of icebergs are formed in a completely different manner such as those formed off the coast of Greenland and these icebergs may be found in a variety of shapes, having no particular dominant shape.
The icebergs which are formed in the Antarctic are generally flat elongated bergs having a flat appearance. Both types of icebergs can be very large, weighing in the order of several billion tons and the water which composes the iceberg is essentially “fresh”.
So there are basically two entirely different forms of iceberg to deal with, tabular and non-tabular. Both are produced by a process known as calving, that is breaking off the large ice formation which has been formed over the years at either pole. The breaking up of an iceberg whilst it is floating in the ocean current is also known as calving.
There are generally only two reasons why one would seek to alter the path of an iceberg; first to prevent or limit damage to a structure which stands in the path way of the drifting iceberg, usually a drilling rig or platform, and the second reason is to attempt to deliver the iceberg to a country where fresh water is in demand. It must be remembered that all icebergs are composed of water which is low in salinity.
This invention seeks to provide an anchor in an iceberg of either the tabular or the non-tabular type, and then tow the iceberg to its final destination using tugs or ocean going ships. The power requirements are high; in the order of hundreds of tons to pull a drifting iceberg to a predetermined destination.
The anchor must fulfill several conditions.
It must be rigidly attached to the iceberg to permit a towing force (of several hundred tons) to be transferred to the iceberg during the transit of the iceberg; the voyage from the mid Atlantic Ocean to a final destination in an equatorial country which may take several months to complete, and during this time the non-tabular icebergs from the Arctic Ocean may roll over several times due to a shift in the center of gravity. During this time, regardless of the constant erosion of the iceberg caused by melting, the anchor must remain securely fastened to the iceberg.
The anchor used in this application takes the general shape of a giant drill, one end having a cutting head mounted thereon, for piercing its way into the body of the iceberg.
Next there must be a passageway provided in the drill for the removal of ice and water produced during a drilling operation. This same passageway may be used during the transfer of the iceberg to carry liquid nitrogen into the anchor which is buried in the iceberg so as to cause any water contained in the pierced cavity to freeze solidly around the anchor and thus enable the iceberg to be “towed”.
Lastly, the drilling device must contain a heating element so that the device may be removed when it is necessary to remove the anchor from the iceberg. With the non-tabular icebergs it may be advantageous to completely relocate the anchor once a new center of gravity for the iceberg is established.
The drill may be provided with a series of circumferential grooves in the outer surface of the stepped cylindrical shaft of the drill to increase the interference fit of the drill in the iceberg to thus increase the force which may be transferred to the iceberg.
The water passage previously used to collect water and ice particles during a drilling operation may be used upon some slight modification to provide a conduit in the drill through which liquid nitrogen may be circulated to assure that the drill is rigidly fixed in the drilled hole by freezing the ice surrounding the anchor during the entire towing operation.
Referring now to
Before proceeding further with the boring and mounting of the drill bit in the iceberg a word or two about the operation should be given here. First, a suitable iceberg must be chosen for haulage. If the tug 10 is operating the north Atlantic, then the icebergs will be from the ice shelf at the Arctic Ocean and the iceberg will have any irregular shape, being of the non-tabular type. The iceberg will be chosen for its size and shape, both attributes are important because it may be almost impossible to influence the drift course of a really large ice berg (3,000,000,000 tons) and if possible it would be expedient to find an iceberg that was amenable to drilling a hole in a surface thereof for setting the anchor in the iceberg.
The apparatus of this invention must be capable of operation in rough waters thus the jib crane and the drill rig must be operable in all sorts of weather.
When a suitable iceberg has been selected for the towing operation, the drill rig and jib crane are activated and the drilling operation at the surface selected of iceberg 12 begins. The drilling begins and the drill bit 30 as shown in
While the drilling operation progresses, the drill is provided with a water flush to capture and carry any chips and crushed bits of ice which are collected at end 32 of drill 30 and are delivered via port 38. There the water mixes and carries the crushed ice back to the end 40 of drilling bit 30 via conduit 40 in drill 30. Water is delivered to the head end 32 of drill 30 via conduit 42.
The exterior surface of drill 30 is interrupted by a series of stepped grooves 44, 46 shown in
Separate water conduits 40 and 42 are used to circulate the water in the drill 30.
Next liquid nitrogen is circulated through the drill once the desired penetration of the drill 30 has been achieved in the iceberg 12. The temperature of the liquid nitrogen is about −196° C. By keeping the temperature of the anchor drill at this low value, the possibility of the iceberg calving during the transit operation at the point of anchor is greatly reduced. The liquid nitrogen is circulated in this instance in chamber 48 of drill 30. It will be seen that once the outside water has been frozen by the circulating liquid nitrogen that ridges 44-46 hold the drill bit in the iceberg.
Lastly, the contacting surface of the anchor drill and the iceberg may be heated using coil 50 as shown in
The liquid nitrogen may be circulated in the same channels 40 and 42 in which the drilling water has previously circulated or it may be circulated in a separate channel designed for that purpose such as shown here.
The swivel device 24 allows the iceberg 12 freedom to move around during a towing operation. Swivel 24 can be constructed in accordance with universal joint knowledge.
It is believed that many modifications and other embodiments of the invention will come to the mind of one skilled in the art having the benefit of the teachings presented in the foregoing descriptions and the associated drawings. Therefore, it is understood that the invention is not to be limited to the specific embodiments disclosed, and that the modifications and embodiments are intended to be included within the scope of the dependent claims.
Number | Name | Date | Kind |
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629539 | Bertram | Jul 1899 | A |
2786652 | Wells | Mar 1957 | A |
3680645 | Horbach et al. | Aug 1972 | A |
3951220 | Phillips et al. | Apr 1976 | A |
4100981 | Chaffin | Jul 1978 | A |
4178872 | Mougin et al. | Dec 1979 | A |
4223627 | Mougin | Sep 1980 | A |
4640552 | Page | Feb 1987 | A |
6688105 | Shick | Feb 2004 | B1 |
Number | Date | Country | |
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20090120688 A1 | May 2009 | US |