FRACTURE-TOUGHNESS OF ICE AND FIRN DETERMINED FROM THE MODIFIED RING TEST MODIFIED RING TEST

被引:30
作者
FISCHER, MP
ALLEY, RB
ENGELDER, T
机构
[1] PENN STATE UNIV,DEPT GEOSCI,UNIVERSITY PK,PA 16802
[2] PENN STATE UNIV,CTR EARTH SYST SCI,UNIVERSITY PK,PA 16802
关键词
D O I
10.3189/S0022143000016257
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The modified ring test is used to determine the fracture toughness of synthetic, granular, fresh-water ice (average density 0.891 Mg m(-3)) and firn (average density 0.605 Mg m(-3)) from depths between 26 and 27.2 m in the E core of the Greenland Ice Sheet Project II. Average fracture toughness is 145.7 kPa m(1/2) for the manufactured ice and 108.6 kPa m(1/2) for the firn. Comparison between the ice and firn suggests that ice-fracture toughness decreases with decreasing density (i.e. increasing porosity), suggesting lateral and vertical variations in the near-surface fracture resistance of glaciers and ice sheets may be related to firn densification. The modified ring test has many advantages over conventional; notch-based specimens in that complications which arise in notched specimens due to crack-length, loading-rate, notch-acuity and specimen-size effects are irrelevant for a modified ring-specimen geometry.
引用
收藏
页码:383 / 394
页数:12
相关论文
共 41 条
[1]  
Alley R., 1987, ANN GLACIOL, V9, P1
[2]   FIRN DENSIFICATION BY GRAIN-BOUNDARY SLIDING - A 1ST MODEL [J].
ALLEY, RB .
JOURNAL DE PHYSIQUE, 1987, 48 (C-1) :249-256
[3]  
ANDREWS RM, 1984, INT KARAKORAM PROJEC, V1, P147
[4]  
[Anonymous], 1970, QUANTITATIVE STEREOL
[5]  
Barsoum R. S., 1976, International Journal for Numerical Methods in Engineering, V10, P25, DOI 10.1002/nme.1620100103
[6]  
BENTLEY DL, 1988, 9TH P INT S IC SAPP, V1, P152
[7]  
BITTENCOURT TN, 1992, SPECIAL TECHNICAL PU, V2, P69
[8]  
Broek D., 1986, ELEMENTARY ENG FRACT
[9]  
Danilenko V. I., 1985, Mechanics of Solids, V20, P131
[10]  
DEFRANCO SJ, 1991, ANN GLACIOL, V15, P230, DOI 10.3189/1991AoG15-1-230-235