Frost growth behavior according to the cold surface inclination angle

•Frost growth behavior according to the cold surface inclination angle was observed.•Frost thickness increased and the density decreased as the angle increased.•Scattering of the frost particles and initial shape of the frost crystals were observed.•Frost layer was strongly bound as the cold surface...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:International journal of heat and mass transfer 2020-01, Vol.146, p.118841, Article 118841
Hauptverfasser: Kim, Junghan, Byun, Sungjoon, Lee, Jaehwan, Lee, Kwan-Soo
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page
container_issue
container_start_page 118841
container_title International journal of heat and mass transfer
container_volume 146
creator Kim, Junghan
Byun, Sungjoon
Lee, Jaehwan
Lee, Kwan-Soo
description •Frost growth behavior according to the cold surface inclination angle was observed.•Frost thickness increased and the density decreased as the angle increased.•Scattering of the frost particles and initial shape of the frost crystals were observed.•Frost layer was strongly bound as the cold surface temperature increased. Frosting experiments were performed to analyze the frost growth behavior according to the inclination angle of a cold surface. The thickness and density of frost on an inclined cold surface were analyzed with respect to a horizontal cold surface. The scattering of the frost particles and the initial shape of the frost crystals were observed. The frost thickness increased and the frost density decreased as the cold surface inclination angle increased, even with variable operating conditions (humidity and cold surface temperature). In the case of varying humidity, the initial frost crystals exhibited feather shapes under relatively high humidity conditions, and needle and pole shapes under relatively low humidity conditions. The decrease in frost density owing to frost particle scattering was significant when feather-shaped crystals were observed. As the cold surface temperature increased, the frost layer was strongly bound, and frost particle scattering occurred less frequently.
doi_str_mv 10.1016/j.ijheatmasstransfer.2019.118841
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2330585953</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0017931019323555</els_id><sourcerecordid>2330585953</sourcerecordid><originalsourceid>FETCH-LOGICAL-c407t-9e606b0323dd63ec650d62a17de7898cd4efda44bbed52eca1f6f55224aa37a13</originalsourceid><addsrcrecordid>eNqNkMtOwzAQRS0EEqXwD5bYsEnxI3GSHahqeagSG1hbjj1pHKV2sd0i_p5UYceG1Wg0V2d0D0J3lCwooeK-X9i-A5V2KsYUlIsthAUjtF5QWlU5PUMzWpV1xmhVn6MZIbTMak7JJbqKsT-tJBcztFoHHxPeBv-VOtxAp47WB6y09sFYt8XJ49QB1n4wOB5CqzRg6_RgnUrWO6zcdoBrdNGqIcLN75yjj_Xqffmcbd6eXpaPm0znpExZDYKIhnDGjREctCiIEUzR0kBZ1ZU2ObRG5XnTgCkYaEVb0RYFY7lSvFSUz9HtxN0H_3mAmGTvD8GNLyXjnBRVURd8TD1MKT12iwFauQ92p8K3pESe5Mle_pUnT_LkJG9EvE4IGNsc7XiN2oLTYGwAnaTx9v-wH3B4hYg</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2330585953</pqid></control><display><type>article</type><title>Frost growth behavior according to the cold surface inclination angle</title><source>Elsevier ScienceDirect Journals</source><creator>Kim, Junghan ; Byun, Sungjoon ; Lee, Jaehwan ; Lee, Kwan-Soo</creator><creatorcontrib>Kim, Junghan ; Byun, Sungjoon ; Lee, Jaehwan ; Lee, Kwan-Soo</creatorcontrib><description>•Frost growth behavior according to the cold surface inclination angle was observed.•Frost thickness increased and the density decreased as the angle increased.•Scattering of the frost particles and initial shape of the frost crystals were observed.•Frost layer was strongly bound as the cold surface temperature increased. Frosting experiments were performed to analyze the frost growth behavior according to the inclination angle of a cold surface. The thickness and density of frost on an inclined cold surface were analyzed with respect to a horizontal cold surface. The scattering of the frost particles and the initial shape of the frost crystals were observed. The frost thickness increased and the frost density decreased as the cold surface inclination angle increased, even with variable operating conditions (humidity and cold surface temperature). In the case of varying humidity, the initial frost crystals exhibited feather shapes under relatively high humidity conditions, and needle and pole shapes under relatively low humidity conditions. The decrease in frost density owing to frost particle scattering was significant when feather-shaped crystals were observed. As the cold surface temperature increased, the frost layer was strongly bound, and frost particle scattering occurred less frequently.</description><identifier>ISSN: 0017-9310</identifier><identifier>EISSN: 1879-2189</identifier><identifier>DOI: 10.1016/j.ijheatmasstransfer.2019.118841</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Cold ; Cold surfaces ; Crystals ; Density ; Frost morphology ; Frost particle scattering ; Frosting ; Humidity ; Ice ; Inclination angle ; Scattering ; Snow removal ; Surface temperature ; Thickness</subject><ispartof>International journal of heat and mass transfer, 2020-01, Vol.146, p.118841, Article 118841</ispartof><rights>2019 Elsevier Ltd</rights><rights>Copyright Elsevier BV Jan 2020</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c407t-9e606b0323dd63ec650d62a17de7898cd4efda44bbed52eca1f6f55224aa37a13</citedby><cites>FETCH-LOGICAL-c407t-9e606b0323dd63ec650d62a17de7898cd4efda44bbed52eca1f6f55224aa37a13</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0017931019323555$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65534</link.rule.ids></links><search><creatorcontrib>Kim, Junghan</creatorcontrib><creatorcontrib>Byun, Sungjoon</creatorcontrib><creatorcontrib>Lee, Jaehwan</creatorcontrib><creatorcontrib>Lee, Kwan-Soo</creatorcontrib><title>Frost growth behavior according to the cold surface inclination angle</title><title>International journal of heat and mass transfer</title><description>•Frost growth behavior according to the cold surface inclination angle was observed.•Frost thickness increased and the density decreased as the angle increased.•Scattering of the frost particles and initial shape of the frost crystals were observed.•Frost layer was strongly bound as the cold surface temperature increased. Frosting experiments were performed to analyze the frost growth behavior according to the inclination angle of a cold surface. The thickness and density of frost on an inclined cold surface were analyzed with respect to a horizontal cold surface. The scattering of the frost particles and the initial shape of the frost crystals were observed. The frost thickness increased and the frost density decreased as the cold surface inclination angle increased, even with variable operating conditions (humidity and cold surface temperature). In the case of varying humidity, the initial frost crystals exhibited feather shapes under relatively high humidity conditions, and needle and pole shapes under relatively low humidity conditions. The decrease in frost density owing to frost particle scattering was significant when feather-shaped crystals were observed. As the cold surface temperature increased, the frost layer was strongly bound, and frost particle scattering occurred less frequently.</description><subject>Cold</subject><subject>Cold surfaces</subject><subject>Crystals</subject><subject>Density</subject><subject>Frost morphology</subject><subject>Frost particle scattering</subject><subject>Frosting</subject><subject>Humidity</subject><subject>Ice</subject><subject>Inclination angle</subject><subject>Scattering</subject><subject>Snow removal</subject><subject>Surface temperature</subject><subject>Thickness</subject><issn>0017-9310</issn><issn>1879-2189</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNqNkMtOwzAQRS0EEqXwD5bYsEnxI3GSHahqeagSG1hbjj1pHKV2sd0i_p5UYceG1Wg0V2d0D0J3lCwooeK-X9i-A5V2KsYUlIsthAUjtF5QWlU5PUMzWpV1xmhVn6MZIbTMak7JJbqKsT-tJBcztFoHHxPeBv-VOtxAp47WB6y09sFYt8XJ49QB1n4wOB5CqzRg6_RgnUrWO6zcdoBrdNGqIcLN75yjj_Xqffmcbd6eXpaPm0znpExZDYKIhnDGjREctCiIEUzR0kBZ1ZU2ObRG5XnTgCkYaEVb0RYFY7lSvFSUz9HtxN0H_3mAmGTvD8GNLyXjnBRVURd8TD1MKT12iwFauQ92p8K3pESe5Mle_pUnT_LkJG9EvE4IGNsc7XiN2oLTYGwAnaTx9v-wH3B4hYg</recordid><startdate>202001</startdate><enddate>202001</enddate><creator>Kim, Junghan</creator><creator>Byun, Sungjoon</creator><creator>Lee, Jaehwan</creator><creator>Lee, Kwan-Soo</creator><general>Elsevier Ltd</general><general>Elsevier BV</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>202001</creationdate><title>Frost growth behavior according to the cold surface inclination angle</title><author>Kim, Junghan ; Byun, Sungjoon ; Lee, Jaehwan ; Lee, Kwan-Soo</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c407t-9e606b0323dd63ec650d62a17de7898cd4efda44bbed52eca1f6f55224aa37a13</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Cold</topic><topic>Cold surfaces</topic><topic>Crystals</topic><topic>Density</topic><topic>Frost morphology</topic><topic>Frost particle scattering</topic><topic>Frosting</topic><topic>Humidity</topic><topic>Ice</topic><topic>Inclination angle</topic><topic>Scattering</topic><topic>Snow removal</topic><topic>Surface temperature</topic><topic>Thickness</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kim, Junghan</creatorcontrib><creatorcontrib>Byun, Sungjoon</creatorcontrib><creatorcontrib>Lee, Jaehwan</creatorcontrib><creatorcontrib>Lee, Kwan-Soo</creatorcontrib><collection>CrossRef</collection><collection>Mechanical &amp; Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>International journal of heat and mass transfer</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kim, Junghan</au><au>Byun, Sungjoon</au><au>Lee, Jaehwan</au><au>Lee, Kwan-Soo</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Frost growth behavior according to the cold surface inclination angle</atitle><jtitle>International journal of heat and mass transfer</jtitle><date>2020-01</date><risdate>2020</risdate><volume>146</volume><spage>118841</spage><pages>118841-</pages><artnum>118841</artnum><issn>0017-9310</issn><eissn>1879-2189</eissn><abstract>•Frost growth behavior according to the cold surface inclination angle was observed.•Frost thickness increased and the density decreased as the angle increased.•Scattering of the frost particles and initial shape of the frost crystals were observed.•Frost layer was strongly bound as the cold surface temperature increased. Frosting experiments were performed to analyze the frost growth behavior according to the inclination angle of a cold surface. The thickness and density of frost on an inclined cold surface were analyzed with respect to a horizontal cold surface. The scattering of the frost particles and the initial shape of the frost crystals were observed. The frost thickness increased and the frost density decreased as the cold surface inclination angle increased, even with variable operating conditions (humidity and cold surface temperature). In the case of varying humidity, the initial frost crystals exhibited feather shapes under relatively high humidity conditions, and needle and pole shapes under relatively low humidity conditions. The decrease in frost density owing to frost particle scattering was significant when feather-shaped crystals were observed. As the cold surface temperature increased, the frost layer was strongly bound, and frost particle scattering occurred less frequently.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.ijheatmasstransfer.2019.118841</doi></addata></record>
fulltext fulltext
identifier ISSN: 0017-9310
ispartof International journal of heat and mass transfer, 2020-01, Vol.146, p.118841, Article 118841
issn 0017-9310
1879-2189
language eng
recordid cdi_proquest_journals_2330585953
source Elsevier ScienceDirect Journals
subjects Cold
Cold surfaces
Crystals
Density
Frost morphology
Frost particle scattering
Frosting
Humidity
Ice
Inclination angle
Scattering
Snow removal
Surface temperature
Thickness
title Frost growth behavior according to the cold surface inclination angle
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-14T14%3A20%3A11IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Frost%20growth%20behavior%20according%20to%20the%20cold%20surface%20inclination%20angle&rft.jtitle=International%20journal%20of%20heat%20and%20mass%20transfer&rft.au=Kim,%20Junghan&rft.date=2020-01&rft.volume=146&rft.spage=118841&rft.pages=118841-&rft.artnum=118841&rft.issn=0017-9310&rft.eissn=1879-2189&rft_id=info:doi/10.1016/j.ijheatmasstransfer.2019.118841&rft_dat=%3Cproquest_cross%3E2330585953%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2330585953&rft_id=info:pmid/&rft_els_id=S0017931019323555&rfr_iscdi=true