Model for Rheology of Halloysite Suspensions
A quantitative rheological model was developed for predicting the non‐Newtonian flow behavior of aqueous halloysite suspensions. Halloysite clay from the large Utah deposits was used for this investigation because of its unique tubular morphology. The flow behavior of the suspensions was characteriz...
Gespeichert in:
Veröffentlicht in: | Journal of the American Ceramic Society 1968-05, Vol.51 (5), p.269-273 |
---|---|
Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 273 |
---|---|
container_issue | 5 |
container_start_page | 269 |
container_title | Journal of the American Ceramic Society |
container_volume | 51 |
creator | KENT, RAYMOND C. GORDON, RONALD S. HAHN, SANG J. |
description | A quantitative rheological model was developed for predicting the non‐Newtonian flow behavior of aqueous halloysite suspensions. Halloysite clay from the large Utah deposits was used for this investigation because of its unique tubular morphology. The flow behavior of the suspensions was characterized by the semi empirical Ree‐Eyring generalized viscosity equation. The β parameter in the Ree‐Eyring equation, a measure of the relaxation time for the flow process, was very sensitive to variations in the pH and volume fraction solids. When the logarithm of 0 was plotted versus pH (4 to 11) for halloysite suspensions containing 15, 20, and 25 wt% solids, linear plots with increasing slopes were obtained. Attempts were made to show the physical significance of the parameters introduced in the model. |
doi_str_mv | 10.1111/j.1151-2916.1968.tb13855.x |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1298381828</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1298381828</sourcerecordid><originalsourceid>FETCH-LOGICAL-c3859-780716abeaba04763bea87cdcf00cacae65c4a483847dca6abe3381b5ba88d233</originalsourceid><addsrcrecordid>eNqVkF9PgzAUxRujiXP6HYi-CraUQvHFLDg3zfwTnfHxppSiIK6zZXF8e0tYfPe-3Nv0nN9JDkKnBAfEzUXtFiN-mJI4IGnMgzYnlDMWbPfQiLDd1z4aYYxDP-EhPkRH1tbuSVIejdD5vS5U45XaeM8fSjf6vfN06c1F0-jOVq3yXjZ2rVa20it7jA5K0Vh1sttj9HozXWZzf_E4u80mC1-67NTF4ITEIlciFzhKYuounshClhhLIYWKmYxExCmPkkKKXkkpJznLBedFSOkYnQ3ctdHfG2VbqPXGrFwkkDB1PsJD7lSXg0oaba1RJaxN9SVMBwRD3w7U0LcDfQXQtwO7dmDrzFeD-adqVPcPJ9xNsmkYp47gD4TKtmr7RxDmE-KEJgzeHmbAlk_XjpEBpb_TpntQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1298381828</pqid></control><display><type>article</type><title>Model for Rheology of Halloysite Suspensions</title><source>Periodicals Index Online</source><source>Wiley Online Library All Journals</source><creator>KENT, RAYMOND C. ; GORDON, RONALD S. ; HAHN, SANG J.</creator><creatorcontrib>KENT, RAYMOND C. ; GORDON, RONALD S. ; HAHN, SANG J.</creatorcontrib><description>A quantitative rheological model was developed for predicting the non‐Newtonian flow behavior of aqueous halloysite suspensions. Halloysite clay from the large Utah deposits was used for this investigation because of its unique tubular morphology. The flow behavior of the suspensions was characterized by the semi empirical Ree‐Eyring generalized viscosity equation. The β parameter in the Ree‐Eyring equation, a measure of the relaxation time for the flow process, was very sensitive to variations in the pH and volume fraction solids. When the logarithm of 0 was plotted versus pH (4 to 11) for halloysite suspensions containing 15, 20, and 25 wt% solids, linear plots with increasing slopes were obtained. Attempts were made to show the physical significance of the parameters introduced in the model.</description><identifier>ISSN: 0002-7820</identifier><identifier>EISSN: 1551-2916</identifier><identifier>DOI: 10.1111/j.1151-2916.1968.tb13855.x</identifier><language>eng</language><publisher>Oxford, UK: Blackwell Publishing Ltd</publisher><ispartof>Journal of the American Ceramic Society, 1968-05, Vol.51 (5), p.269-273</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3859-780716abeaba04763bea87cdcf00cacae65c4a483847dca6abe3381b5ba88d233</citedby><cites>FETCH-LOGICAL-c3859-780716abeaba04763bea87cdcf00cacae65c4a483847dca6abe3381b5ba88d233</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fj.1151-2916.1968.tb13855.x$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fj.1151-2916.1968.tb13855.x$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1416,27868,27923,27924,45573,45574</link.rule.ids></links><search><creatorcontrib>KENT, RAYMOND C.</creatorcontrib><creatorcontrib>GORDON, RONALD S.</creatorcontrib><creatorcontrib>HAHN, SANG J.</creatorcontrib><title>Model for Rheology of Halloysite Suspensions</title><title>Journal of the American Ceramic Society</title><description>A quantitative rheological model was developed for predicting the non‐Newtonian flow behavior of aqueous halloysite suspensions. Halloysite clay from the large Utah deposits was used for this investigation because of its unique tubular morphology. The flow behavior of the suspensions was characterized by the semi empirical Ree‐Eyring generalized viscosity equation. The β parameter in the Ree‐Eyring equation, a measure of the relaxation time for the flow process, was very sensitive to variations in the pH and volume fraction solids. When the logarithm of 0 was plotted versus pH (4 to 11) for halloysite suspensions containing 15, 20, and 25 wt% solids, linear plots with increasing slopes were obtained. Attempts were made to show the physical significance of the parameters introduced in the model.</description><issn>0002-7820</issn><issn>1551-2916</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1968</creationdate><recordtype>article</recordtype><sourceid>K30</sourceid><recordid>eNqVkF9PgzAUxRujiXP6HYi-CraUQvHFLDg3zfwTnfHxppSiIK6zZXF8e0tYfPe-3Nv0nN9JDkKnBAfEzUXtFiN-mJI4IGnMgzYnlDMWbPfQiLDd1z4aYYxDP-EhPkRH1tbuSVIejdD5vS5U45XaeM8fSjf6vfN06c1F0-jOVq3yXjZ2rVa20it7jA5K0Vh1sttj9HozXWZzf_E4u80mC1-67NTF4ITEIlciFzhKYuounshClhhLIYWKmYxExCmPkkKKXkkpJznLBedFSOkYnQ3ctdHfG2VbqPXGrFwkkDB1PsJD7lSXg0oaba1RJaxN9SVMBwRD3w7U0LcDfQXQtwO7dmDrzFeD-adqVPcPJ9xNsmkYp47gD4TKtmr7RxDmE-KEJgzeHmbAlk_XjpEBpb_TpntQ</recordid><startdate>196805</startdate><enddate>196805</enddate><creator>KENT, RAYMOND C.</creator><creator>GORDON, RONALD S.</creator><creator>HAHN, SANG J.</creator><general>Blackwell Publishing Ltd</general><general>American Ceramic Society</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>HDMVH</scope><scope>K30</scope><scope>PAAUG</scope><scope>PAWHS</scope><scope>PAWZZ</scope><scope>PAXOH</scope><scope>PBHAV</scope><scope>PBQSW</scope><scope>PBYQZ</scope><scope>PCIWU</scope><scope>PCMID</scope><scope>PCZJX</scope><scope>PDGRG</scope><scope>PDWWI</scope><scope>PETMR</scope><scope>PFVGT</scope><scope>PGXDX</scope><scope>PIHIL</scope><scope>PISVA</scope><scope>PJCTQ</scope><scope>PJTMS</scope><scope>PLCHJ</scope><scope>PMHAD</scope><scope>PNQDJ</scope><scope>POUND</scope><scope>PPLAD</scope><scope>PQAPC</scope><scope>PQCAN</scope><scope>PQCMW</scope><scope>PQEME</scope><scope>PQHKH</scope><scope>PQMID</scope><scope>PQNCT</scope><scope>PQNET</scope><scope>PQSCT</scope><scope>PQSET</scope><scope>PSVJG</scope><scope>PVMQY</scope><scope>PZGFC</scope></search><sort><creationdate>196805</creationdate><title>Model for Rheology of Halloysite Suspensions</title><author>KENT, RAYMOND C. ; GORDON, RONALD S. ; HAHN, SANG J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3859-780716abeaba04763bea87cdcf00cacae65c4a483847dca6abe3381b5ba88d233</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1968</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>KENT, RAYMOND C.</creatorcontrib><creatorcontrib>GORDON, RONALD S.</creatorcontrib><creatorcontrib>HAHN, SANG J.</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Periodicals Index Online Segment 15</collection><collection>Periodicals Index Online</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - West</collection><collection>Primary Sources Access (Plan D) - International</collection><collection>Primary Sources Access & Build (Plan A) - MEA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Midwest</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Northeast</collection><collection>Primary Sources Access (Plan D) - Southeast</collection><collection>Primary Sources Access (Plan D) - North Central</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Southeast</collection><collection>Primary Sources Access (Plan D) - South Central</collection><collection>Primary Sources Access & Build (Plan A) - UK / I</collection><collection>Primary Sources Access (Plan D) - Canada</collection><collection>Primary Sources Access (Plan D) - EMEALA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - North Central</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - South Central</collection><collection>Primary Sources Access & Build (Plan A) - International</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - International</collection><collection>Primary Sources Access (Plan D) - West</collection><collection>Periodicals Index Online Segments 1-50</collection><collection>Primary Sources Access (Plan D) - APAC</collection><collection>Primary Sources Access (Plan D) - Midwest</collection><collection>Primary Sources Access (Plan D) - MEA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Canada</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - UK / I</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - EMEALA</collection><collection>Primary Sources Access & Build (Plan A) - APAC</collection><collection>Primary Sources Access & Build (Plan A) - Canada</collection><collection>Primary Sources Access & Build (Plan A) - West</collection><collection>Primary Sources Access & Build (Plan A) - EMEALA</collection><collection>Primary Sources Access (Plan D) - Northeast</collection><collection>Primary Sources Access & Build (Plan A) - Midwest</collection><collection>Primary Sources Access & Build (Plan A) - North Central</collection><collection>Primary Sources Access & Build (Plan A) - Northeast</collection><collection>Primary Sources Access & Build (Plan A) - South Central</collection><collection>Primary Sources Access & Build (Plan A) - Southeast</collection><collection>Primary Sources Access (Plan D) - UK / I</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - APAC</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - MEA</collection><jtitle>Journal of the American Ceramic Society</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>KENT, RAYMOND C.</au><au>GORDON, RONALD S.</au><au>HAHN, SANG J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Model for Rheology of Halloysite Suspensions</atitle><jtitle>Journal of the American Ceramic Society</jtitle><date>1968-05</date><risdate>1968</risdate><volume>51</volume><issue>5</issue><spage>269</spage><epage>273</epage><pages>269-273</pages><issn>0002-7820</issn><eissn>1551-2916</eissn><abstract>A quantitative rheological model was developed for predicting the non‐Newtonian flow behavior of aqueous halloysite suspensions. Halloysite clay from the large Utah deposits was used for this investigation because of its unique tubular morphology. The flow behavior of the suspensions was characterized by the semi empirical Ree‐Eyring generalized viscosity equation. The β parameter in the Ree‐Eyring equation, a measure of the relaxation time for the flow process, was very sensitive to variations in the pH and volume fraction solids. When the logarithm of 0 was plotted versus pH (4 to 11) for halloysite suspensions containing 15, 20, and 25 wt% solids, linear plots with increasing slopes were obtained. Attempts were made to show the physical significance of the parameters introduced in the model.</abstract><cop>Oxford, UK</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/j.1151-2916.1968.tb13855.x</doi><tpages>5</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0002-7820 |
ispartof | Journal of the American Ceramic Society, 1968-05, Vol.51 (5), p.269-273 |
issn | 0002-7820 1551-2916 |
language | eng |
recordid | cdi_proquest_journals_1298381828 |
source | Periodicals Index Online; Wiley Online Library All Journals |
title | Model for Rheology of Halloysite Suspensions |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-12T16%3A28%3A19IST&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=Model%20for%20Rheology%20of%20Halloysite%20Suspensions&rft.jtitle=Journal%20of%20the%20American%20Ceramic%20Society&rft.au=KENT,%20RAYMOND%20C.&rft.date=1968-05&rft.volume=51&rft.issue=5&rft.spage=269&rft.epage=273&rft.pages=269-273&rft.issn=0002-7820&rft.eissn=1551-2916&rft_id=info:doi/10.1111/j.1151-2916.1968.tb13855.x&rft_dat=%3Cproquest_cross%3E1298381828%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=1298381828&rft_id=info:pmid/&rfr_iscdi=true |