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https://hdl.handle.net/11681/2693
Title: | On the deformation of excavations in the Greenland névé |
Authors: | Landauer, J. K. (Joseph K.) |
Keywords: | Excavation Ice excavation Snow excavation Snow Plasticity Viscosity Deformation Snow tunnels Snow mechanics |
Publisher: | U.S. Army Snow, Ice, and Permafrost Research Establishment. Engineer Research and Development Center (U.S.) |
Series/Report no.: | Research report (U.S. Army Snow |
Description: | Research Report Summary: Deformations occurring in a tunnel, two trenches, and a 30 m deep pit excavated in the Greenland névé in the summer of 1954 have been measured over a period of 2 years. The experimental results indicate that closure rates increase with lateral distance from a restraining boundary up to distances of about 1 m. At larger distances, the effect of the boundary is not appreciable. Closure rates for deep excavations are not found to be strongly depth-dependent. This is due to a roughly parallel increase of viscosity and pressure with depth. Vertical compaction results from the pit agree well with those calculated from the depth-density relation using Sorge's Law. A theoretical calculation for the tunnel and pit closure, which is a modification of existing theories for the deformation of an elastic, compressible, thick-walled cylinder, is in fair agreement with the observed deformations. From this agreement it appears that the flow behavior of the névé can be described on the basis of a Newtonian viscosity. The trench closure is described as the-squeezing out of horizontal layers, fixed at some distance from the trench, and modified only slightly by the drag of neighboring layers. Measurements will be continued during future summers. |
Rights: | Approved for public release; distribution is unlimited. |
URI: | http://hdl.handle.net/11681/2693 |
Appears in Collections: | Research Report |
Files in This Item:
File | Description | Size | Format | |
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SIPRE-Research-Report-30.pdf | 717.62 kB | Adobe PDF | ![]() View/Open |