Creep of Ice Containing Dispersed Fine Sand
Cylindrical samples of ice with 0.0 to 0.35 volume fraction fine sand were tested in unconfined uniaxial compression at stresses between 5.3 and 6.4 bar and at temperatures between −7.4 and −9.4° C. Secondary creep rates were obtained from the slope of the total strain vs. time curve and were normal...
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| Veröffentlicht in: | Journal of glaciology 1972, Vol.11 (63), p.327-336 |
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| container_end_page | 336 |
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| container_issue | 63 |
| container_start_page | 327 |
| container_title | Journal of glaciology |
| container_volume | 11 |
| creator | Hooke, Roger LeB Dahlin, Brian B. Kauper, Michael T. |
| description | Cylindrical samples of ice with 0.0 to 0.35 volume fraction fine sand were tested in unconfined uniaxial compression at stresses between 5.3 and 6.4 bar and at temperatures between −7.4 and −9.4° C. Secondary creep rates were obtained from the slope of the total strain vs. time curve and were normalized to 5.6 bar and −9.1° C. Creep rates in ice with low sand concentrations were in some cases higher and in other cases lower than in clean ice. However at higher sand concentrations the creep rate decreases exponentially with increasing volume fraction sand. The latter results are in general agreement with theories developed to explain dispersion hardening of metals, and suggest that each sand grain is surrounded by a tangled network of secondary dislocations which impede passage of primary glide dislocations. |
| doi_str_mv | 10.3189/S0022143000022309 |
| format | Article |
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Secondary creep rates were obtained from the slope of the total strain vs. time curve and were normalized to 5.6 bar and −9.1° C. Creep rates in ice with low sand concentrations were in some cases higher and in other cases lower than in clean ice. However at higher sand concentrations the creep rate decreases exponentially with increasing volume fraction sand. 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Glaciol</addtitle><description>Cylindrical samples of ice with 0.0 to 0.35 volume fraction fine sand were tested in unconfined uniaxial compression at stresses between 5.3 and 6.4 bar and at temperatures between −7.4 and −9.4° C. Secondary creep rates were obtained from the slope of the total strain vs. time curve and were normalized to 5.6 bar and −9.1° C. Creep rates in ice with low sand concentrations were in some cases higher and in other cases lower than in clean ice. However at higher sand concentrations the creep rate decreases exponentially with increasing volume fraction sand. 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Glaciol</addtitle><date>1972</date><risdate>1972</risdate><volume>11</volume><issue>63</issue><spage>327</spage><epage>336</epage><pages>327-336</pages><issn>0022-1430</issn><eissn>1727-5652</eissn><abstract>Cylindrical samples of ice with 0.0 to 0.35 volume fraction fine sand were tested in unconfined uniaxial compression at stresses between 5.3 and 6.4 bar and at temperatures between −7.4 and −9.4° C. Secondary creep rates were obtained from the slope of the total strain vs. time curve and were normalized to 5.6 bar and −9.1° C. Creep rates in ice with low sand concentrations were in some cases higher and in other cases lower than in clean ice. However at higher sand concentrations the creep rate decreases exponentially with increasing volume fraction sand. The latter results are in general agreement with theories developed to explain dispersion hardening of metals, and suggest that each sand grain is surrounded by a tangled network of secondary dislocations which impede passage of primary glide dislocations.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><doi>10.3189/S0022143000022309</doi><tpages>10</tpages><oa>free_for_read</oa></addata></record> |
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| ispartof | Journal of glaciology, 1972, Vol.11 (63), p.327-336 |
| issn | 0022-1430 1727-5652 |
| language | eng |
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| source | EZB-FREE-00999 freely available EZB journals |
| title | Creep of Ice Containing Dispersed Fine Sand |
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