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Rapid Access Ice Drill: a new tool for exploration of the deep Antarctic ice sheets and subglacial geology

Published online by Cambridge University Press:  09 September 2016

JOHN W. GOODGE*
Affiliation:
Department of Earth and Environmental Sciences, University of Minnesota, Duluth, MN 55812, USA
JEFFREY P. SEVERINGHAUS
Affiliation:
Scripps Institution of Oceanography, UC San Diego, La Jolla, CA 92093, USA
*
Correspondence: John W. Goodge <jgoodge@d.umn.edu>
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Abstract

A new Rapid Access Ice Drill (RAID) will penetrate the Antarctic ice sheets in order to create borehole observatories and take cores in deep ice, the glacial bed and bedrock below. RAID is a mobile drilling system to make multiple long, narrow boreholes in a single field season in Antarctica. RAID is based on a mineral exploration-type rotary rock-coring system using threaded drill pipe to cut through ice using reverse circulation of a non-freezing fluid for pressure-compensation, maintenance of temperature and removal of ice cuttings. Near the bottom of the ice sheet, a wireline latching assembly will enable rapid coring of ice, the glacial bed and bedrock below. Once complete, boreholes will be kept open with fluid, capped and available for future down-hole measurement of temperature gradient, heat flow, ice chronology and ice deformation. RAID is designed to penetrate up to 3300 m of ice and take cores in <200 hours, allowing completion of a borehole and coring in ~10 d at each site. Together, the rapid drilling capability and mobility of the system, along with ice-penetrating imaging methods, will provide a unique 3-D picture of interior and subglacial features of the Antarctic ice sheets.

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Papers
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright
Copyright © The Author(s) 2016
Figure 0

Fig. 1. Maps of Antarctica showing (a) ice velocity derived from satellite interferometry (from Rignot and others, 2011) and (b) sub-ice surface elevations (from BEDMAP2; Fretwell and others, 2013). In (a), black lines show major ice divides; white circles show existing ice cores, with depth of penetration and age of ice record; white outlines show major subglacial lakes. In (b), area of high seismic velocity anomalies at 150 km depth attributed to fast cratonic lithosphere (dashed white line) from Ritzwoller and others (2001). Area of high topography in East Antarctica (magenta dashed line) from Wilson and others (2011). Nimrod igneous province, Terre Adélie craton and Neoproterozoic rift margin from Goodge and Finn (2010). White box labeled RAID shows area initially targeted for rapid-access drilling. A, Dome A; C, Dome C; F, Dome Fuji; M, McMurdo Station; MR, Miller Range; RI, Ross Island; SP, South Pole; T, Titan Dome. Glaciers: BdG, Beardmore; ByG, Byrd; NG, Nimrod; ScG, Scott.

Figure 1

Table 1. Summary of various methods employed for deep-ice drilling

Figure 2

Table 2. Summary of RAID design specifications and operating parameters.*

Figure 3

Fig. 2. Schematic diagram showing the main elements of the RAID design using a conventional rotary drilling rig operating in flooded reverse circulation mode in jointed hollow drill pipe. The RAID system involves three stages of drilling and coring, divided here into casing, borehole and coring sections (a–c). Firn casing is capped at the surface and sealed in non-porous ice by an inflatable packer in order to maintain borehole fluid pressure. The ice borehole will be made with hardened ice-cutting bits in a reverse fluid circulation mode in order to evacuate cuttings. Coring will be done with a wire line BHA using thin-kerf diamond drill bits in a normal fluid circulation format.

Figure 4

Fig. 3. Field layout for RAID (schematic and approximately to scale), including five main drilling modules (brown). Tower shows location of drill rig platform. Not shown are hoses and wiring to connect drilling components, fuel bladders, camp facilities, tractors and other equipment. Drill pipe rack can hold up to 3500 m of drill rod, depending on rod diameter. Drilling fluid and fuel will be supplied in flexible bladders.

Figure 5

Fig. 4. Field deployment of drill and rod modules on sleds. Drill rig (background) and drill-rod racks are joined by a work platform and covered by a canopy of reinforced fabric.

Figure 6

Fig. 5. Generalized schematic diagram illustrating the closed-loop fluid recirculation system that connects the surface fluid reservoirs with the wellhead and borehole. Details of the fluid-processing module are shown in Figure 6.

Figure 7

Fig. 6. Simplified schematic diagram of fluid recirculation system (FRS) shown to scale as built out in a 40 × 9.5 ft (12.2 × 2.9 m) Hi-Cube ISO container. FRS is divided by a partition wall into unheated and heated spaces (cold and warm rooms, respectively). Blue lines show general path of drilling fluid; magenta lines show warm fluid circulation loop. Not shown: electrical panels, power distribution, fire suppression, lighting, gauges and readouts and other minor components.

Figure 8

Fig. 7. Schematic diagrams showing bottom-hole tools, including: (a) non-coring bottom-hole assembly (BHA), with reaming shell and outer ice-cutting bit; (b) face-centered bit for cutting ice, latched into position within the BHA; (c) diamond coring bit, substituted by removing the inner ice-cutting bit and latching in on wire line; and (d) a sequence of coring steps showing progressive advance of the coring bit and core barrel with extensions as needed. Core barrels are available in 1.5 and 3 m lengths. Not to actual scale. Not shown are inner landing ring, latching mechanisms for vertical and rotational locking and pulling tools.

Figure 9

Fig. 8. Schematic diagram showing the upper portion of the drill string from the surface down to non-porous ice. Fluid circulates from the borehole to the fluid recirculation module via the drill-pipe swivel and diverter at the surface. Firn casing is sealed below within non-porous ice by use of an inflatable packer, through which the drill string penetrates. Fast ice cutting is made possible by use of flooded reverse circulation, in which drilling fluid flows downward within the annulus surrounding the drill rods, passes over the cutting face and then carries ice cuttings away up the inside of the drill rods (inset).

Figure 10

Fig. 9. Modeled steady-state temperature and velocity profiles at an East Antarctic plateau RAID site. Ice thickness is assumed to be 3000 m, geothermal heat flux of 50 mW m−2, mean annual surface temperature of −55°C and snow accumulation rate of 3 cm a−1 of water equivalent.

Figure 11

Fig. 10. Modeled dynamic pressure losses for a typical RAID hole, expressed as the difference between fluid pressure and ice hydrostatic pressure. Thus, a negative value indicates that the borehole will tend to close. During operations, the surface injection pump (Bean pump) and/or the airlift will be used to compensate for the differences shown here. Static curve shows pressure differences when fluid is not flowing. Assumptions: 30 gal min−1 (113.6 l/min−1) fluid flow; 3.5 in (8.9 cm) hole diameter; 2.75 in (7.0 cm) pipe O.D.; 0.0057 m wall roughness; Darcy–Weisbach formulation; Re >2300 (turbulent); 50 mW m−2 geothermal flux; −55°C mean annual surface temperature; 2 cm/a w.e. snow accumulation; ESTISOL 140 drilling fluid.

Figure 12

Table 3. Design, construction and deployment schedule