THEORY OF DENSIFICATION OF DRY SNOW ON HIGH POLAR GLACIERS, II

Abstract

The theory of snow densification is further developed on the basis of an exponential relation between viscosity and density. A linear relation between load-stress and strain rate is not valid for high stresses, and is replaced by a hyperbolic sine function. An empirical function is given for the temperature cycle correction. Two equations are derived for calculating depthdensity curves with computers, and a simplified one for use with desk calculators. InstructionsARE GIVEN FOR DETERMINATION OF FUNCTION PARAMETERS FROM FIELD DATA. Four depth-density curves for Greenland and Antarctic locations are computed and graphed to show that the theory is useful. (Author)

Document Details

Document Type
Technical Report
Publication Date
Sep 01, 1962
Accession Number
AD0294158

Entities

People

  • Henri Bader

Organizations

  • Cold Regions Research and Engineering Laboratory

Tags

DTIC Thesaurus Topics

  • Calculators
  • Computers
  • Equations
  • Greenland
  • Strain Rate
  • Viscosity

Readers

  • Mechanical Engineering/Mechanics of Materials.
  • Polar and Arctic Studies