Boring (earth)
Boring is drilling a hole, tunnel, or well in the Earth. It is used for various applications in geology, agriculture, hydrology, civil engineering, and mineral exploration. Today, most Earth drilling serves one of the following purposes:
- return samples of the soil and/or rock through which the drill passes
- access rocks from which material can be extracted
- access rocks which can then be measured
- provide access to rock for purposes of providing engineering support
Image:Boring Machine 1911 Illustration.jpg|thumb|A boring machine illustration from the 1911 Encyclopædia Britannica.
Image:Boring machine.jpg|thumb|Mud log in process, a common way to study the lithology when drilling wells.
History
Borehole drilling has a long history. Han dynasty China used deep borehole drilling for mining and other projects. Chinese borehole sites could reach as deep as 600 m.Methods
When drilling in stone, one must pay particular attention to the type of material. There are three different classifications of drill bits used for drilling into stone: soft, medium, and hard. Soft formation rock bits are used in unconsolidated sands, clays, and soft limestones, etc. Medium formation bits are used in dolomites, limestones, and shale, while hard formation bits are used in hard shale, mudstones, granite, limestones and other hard and/or abrasive formations.Soft ground drilling can be undertaken using a rotary auger or wash boring techniques, while rock drilling often use methods such as NMLC which allow for recovery of a core of material which can be examined to determine the strength, degree of weathering, understanding of any how intact the rock is and identify any discontinuities or other planes of weakness.
Testing of the material in boreholes is also possible. In soft ground the standard penetration test can be used to determine the strength of the material. In rock in-situ stress testing using hydrofracturing or overcoring, Acoustic Televiewer can be used to map discontinuities to determine their orientation. It is also possible once a borehole is complete to measure the permeability. Samples of water and material are also taken for examination and lab testing.
Superdeep Borehole
In 1961 the United States began Project Mohole, an ambitious attempt to drill through the Earth's crust into the Mohorovičić discontinuity. The project was discontinued due to high cost.The Kola Superdeep Borehole was a similar project of the USSR in the 1970s and early 1980s the USSR attempted to drill a hole through the crust, to sample the Mohorovičić discontinuity. The deepest hole ever drilled failed not because of lack of money or time, but because of rock physics at depth. At approximately 12,000 metres depth, rock begins to act more like a plastic solid than a rigid solid. Rock temperatures of several hundred degrees Celsius, required that the drilling fluid be refrigerated before being sent to the cutting face of the drill. As the drill bits burnt out and were removed for replacement, the hole simply flowed closed, and the rock had to be re-drilled. The hole was scrapped.
Further attempts are planned by American consortia and further Russian attempts in Finland.