TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING
The results are presented of a study of the sintering process as a function of temperature, keeping size distribution, shape, and density nearly constant. The confined compression test method was used. It is shown that the degree of sintering of snow and the rate constant as a function of temperatur...
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creator | Ramseier,Rene O Sander,Gary W |
description | The results are presented of a study of the sintering process as a function of temperature, keeping size distribution, shape, and density nearly constant. The confined compression test method was used. It is shown that the degree of sintering of snow and the rate constant as a function of temperature can be represented satisfactorily by an exponential equation. The results indicate that the sintering process is one of evaporation, diffusion through the ambient temperature, and condensation. (Author) |
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The confined compression test method was used. It is shown that the degree of sintering of snow and the rate constant as a function of temperature can be represented satisfactorily by an exponential equation. The results indicate that the sintering process is one of evaporation, diffusion through the ambient temperature, and condensation. (Author)</description><language>eng</language><subject>COMPACTING ; ICE ; LOW TEMPERATURE ; SINTERING ; SNOW ; Snow, Ice and Permafrost ; TEMPERATURE</subject><creationdate>1966</creationdate><rights>APPROVED FOR PUBLIC RELEASE</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,776,881,27544,27545</link.rule.ids><linktorsrc>$$Uhttps://apps.dtic.mil/sti/citations/AD0640150$$EView_record_in_DTIC$$FView_record_in_$$GDTIC$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Ramseier,Rene O</creatorcontrib><creatorcontrib>Sander,Gary W</creatorcontrib><creatorcontrib>COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H</creatorcontrib><title>TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING</title><description>The results are presented of a study of the sintering process as a function of temperature, keeping size distribution, shape, and density nearly constant. The confined compression test method was used. It is shown that the degree of sintering of snow and the rate constant as a function of temperature can be represented satisfactorily by an exponential equation. The results indicate that the sintering process is one of evaporation, diffusion through the ambient temperature, and condensation. (Author)</description><subject>COMPACTING</subject><subject>ICE</subject><subject>LOW TEMPERATURE</subject><subject>SINTERING</subject><subject>SNOW</subject><subject>Snow, Ice and Permafrost</subject><subject>TEMPERATURE</subject><fulltext>true</fulltext><rsrctype>report</rsrctype><creationdate>1966</creationdate><recordtype>report</recordtype><sourceid>1RU</sourceid><recordid>eNrjZDAMcfUNcA1yDAkNclVwcQ1w9XNx9XN2VXD0c1HwdXX2cPTzDPZV8HdTCPb0C3EN8vRz52FgTUvMKU7lhdLcDDJuriHOHropJZnJ8cUlmXmpJfGOLgZmJgaGpgbGBKQB0Pojew</recordid><startdate>196607</startdate><enddate>196607</enddate><creator>Ramseier,Rene O</creator><creator>Sander,Gary W</creator><scope>1RU</scope><scope>BHM</scope></search><sort><creationdate>196607</creationdate><title>TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING</title><author>Ramseier,Rene O ; Sander,Gary W</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-dtic_stinet_AD06401503</frbrgroupid><rsrctype>reports</rsrctype><prefilter>reports</prefilter><language>eng</language><creationdate>1966</creationdate><topic>COMPACTING</topic><topic>ICE</topic><topic>LOW TEMPERATURE</topic><topic>SINTERING</topic><topic>SNOW</topic><topic>Snow, Ice and Permafrost</topic><topic>TEMPERATURE</topic><toplevel>online_resources</toplevel><creatorcontrib>Ramseier,Rene O</creatorcontrib><creatorcontrib>Sander,Gary W</creatorcontrib><creatorcontrib>COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H</creatorcontrib><collection>DTIC Technical Reports</collection><collection>DTIC STINET</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Ramseier,Rene O</au><au>Sander,Gary W</au><aucorp>COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H</aucorp><format>book</format><genre>unknown</genre><ristype>RPRT</ristype><btitle>TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING</btitle><date>1966-07</date><risdate>1966</risdate><abstract>The results are presented of a study of the sintering process as a function of temperature, keeping size distribution, shape, and density nearly constant. The confined compression test method was used. It is shown that the degree of sintering of snow and the rate constant as a function of temperature can be represented satisfactorily by an exponential equation. The results indicate that the sintering process is one of evaporation, diffusion through the ambient temperature, and condensation. (Author)</abstract><oa>free_for_read</oa></addata></record> |
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subjects | COMPACTING ICE LOW TEMPERATURE SINTERING SNOW Snow, Ice and Permafrost TEMPERATURE |
title | TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING |
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