Jökull

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Jökull - 31.12.2001, Qupperneq 40

Jökull - 31.12.2001, Qupperneq 40
Thorsteinsson et al. Figure 9a. Tephra layer from the Hekla 1991 eruption at 40.70—40.83 m depth. - Gjóskulag úr Heklugosinu 1991 á 40,70^40,83 m dýpi. mination of the annual layers. The most promising method for detecting summer layers is the study of wind-blown dust, originating in the surrounding areas and presumably deposited on the ice cap during the period when the land surface is snow-free (late sum- mer to early autumn). In addition, the Hofsjökull core will provide an opportunity to study if the stratigraphy of meltlayers in a temperate ice cap contains a sea- sonal signal. Results of these studies and other mea- surements of the core will be reported elsewhere. Figure 9b. Tephra layer from the Hekla 1980 eruption at 69.94 m depth. - Gjóskulag úr Heklugosinu 1980 á 69,94 m dýpi. CONCLUDING REMARKS Improving the drilling technique Based on the experience gained at Hofsjökull and comparison with the Bárðarbunga drilling some de- sign and engineering modifications are suggested on the AWI-type drill, in order to make it more suitable for drilling in temperate ice: 1. A drill motor built for submersion in water should be used. Other components, such as the slipring unit and cable connectors also need to be thoroughly pro- tected from water. 2. A different chip transporting and storage system is needed. A 1.0-1.2m long core barrel seems suf- ficient, because it is unlikely that core lengths above 1 m can be attained below the water table. Above the core barrel, a narrow shaft should connect the bar- rel to the coupling mechanism that transforms rota- tion from the drill motor to the barrel and drill head. With this arrangement, the chips would be transported upward along the spirals on the core barrel and float directly into the space around the shaft where they be- come collected. The Bárðarbunga drill was designed in this way (Arnason et al., 1974) and similar so- lutions have recently been incorporated into designs of drills used for deep coring on the polar ice sheets (NGRIP/EPICA drill: S.J. Johnsen and others, private communication; Dome F drill: Tanaka et al., 1994). 3. A redesign should permit the free flow of water through or past the different components of the drill and allow for greater clearance between the outer bar- rel and the hole wall. The use of a submersible motor will eliminate the need to operate with a closed motor section. 4. The drill head does not seem to need modifications. The cutters appear well-suited for operations in tem- 38 JÖKULLNo. 51
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