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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Hauptverfasser: Ramseier,Rene O, Sander,Gary W
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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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