The effects of atmospheric pressure, air concentration in the fluid, and the surface roughness on the solid-sphere motion along a wall

A phenomenological model for describing a slow steady gravity-driven motion of a solid sphere down an inclined wall in a fluid under the conditions when an air (in the case of a fluid with dissolved air) bubble arises in the sphere-wall lubrication layer between the sphere and the wall is proposed....

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Physics of fluids (1994) 2007-11, Vol.19 (11), p.113601-113601-10
1. Verfasser: Prokunin, Alexander N.
Format: Artikel
Sprache:eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 113601-10
container_issue 11
container_start_page 113601
container_title Physics of fluids (1994)
container_volume 19
creator Prokunin, Alexander N.
description A phenomenological model for describing a slow steady gravity-driven motion of a solid sphere down an inclined wall in a fluid under the conditions when an air (in the case of a fluid with dissolved air) bubble arises in the sphere-wall lubrication layer between the sphere and the wall is proposed. In the case under consideration, both contact and contactless motion of the sphere is possible. The sphere surface roughness and the concentration of the air dissolved in the fluid are taken into account. The relevant experiment studying the sphere motion accompanied by cavitation was carried out. We used fluids with various air concentration including a limiting case of degasified fluid and spheres of various surface roughness. We find a parameter whose constant value specifies a stationary motion of the sphere including a limiting case of degasified fluid. This parameter turns out to be proportional to the difference between atmospheric pressure and one corresponding to the equilibrium concentration of the air dissolved in fluid. The numerical results found were compared with the experimental data of our investigation and a good quantitative agreement was obtained in a certain domain of parameters. A possibility of unsteady motion of the sphere had been shown.
doi_str_mv 10.1063/1.2817687
format Article
fullrecord <record><control><sourceid>scitation_cross</sourceid><recordid>TN_cdi_scitation_primary_10_1063_1_2817687</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>scitation_primary_10_1063_1_2817687The_effects_of_atmos</sourcerecordid><originalsourceid>FETCH-LOGICAL-c384t-5798581b25580dc806edb4026685c778a1c2c429dd2490f11d85a41997c3da4b3</originalsourceid><addsrcrecordid>eNqNkMtKAzEARYMoWKsL_yAbF4qjSWYmj40gxRcU3NR1SPNoI9NkSKaKP-B3O50WulJcJSHnnsUB4ByjG4xoeYtvCMeMcnYARhhxUTBK6eHmzlBBaYmPwUnO7wihUhA6At-zpYXWOau7DKODqlvF3C5t8hq2yea8TvYaKp-gjkHb0CXV-RigD7Drl65Ze9P_BzM8e9opbWGK68Uy9GsYt1yOjTfFILZwFQeFamJYQAU_VdOcgiOnmmzPducYvD0-zCbPxfT16WVyPy10yauuqJngNcdzUtccGc0RtWZeIUIprzVjXGFNdEWEMaQSyGFseK0qLATTpVHVvByDy61Xp5hzsk62ya9U-pIYyU1AieUuYM9ebNlWZa0al1TQPu8HQpCK4A13t-Wy9t1Q53dpX1vuasvo5FC7F1z9W_AX_BHTHpStceUPqUCirQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>The effects of atmospheric pressure, air concentration in the fluid, and the surface roughness on the solid-sphere motion along a wall</title><source>AIP Journals Complete</source><source>AIP Digital Archive</source><creator>Prokunin, Alexander N.</creator><creatorcontrib>Prokunin, Alexander N.</creatorcontrib><description>A phenomenological model for describing a slow steady gravity-driven motion of a solid sphere down an inclined wall in a fluid under the conditions when an air (in the case of a fluid with dissolved air) bubble arises in the sphere-wall lubrication layer between the sphere and the wall is proposed. In the case under consideration, both contact and contactless motion of the sphere is possible. The sphere surface roughness and the concentration of the air dissolved in the fluid are taken into account. The relevant experiment studying the sphere motion accompanied by cavitation was carried out. We used fluids with various air concentration including a limiting case of degasified fluid and spheres of various surface roughness. We find a parameter whose constant value specifies a stationary motion of the sphere including a limiting case of degasified fluid. This parameter turns out to be proportional to the difference between atmospheric pressure and one corresponding to the equilibrium concentration of the air dissolved in fluid. The numerical results found were compared with the experimental data of our investigation and a good quantitative agreement was obtained in a certain domain of parameters. A possibility of unsteady motion of the sphere had been shown.</description><identifier>ISSN: 1070-6631</identifier><identifier>EISSN: 1089-7666</identifier><identifier>DOI: 10.1063/1.2817687</identifier><identifier>CODEN: PHFLE6</identifier><language>eng</language><publisher>Melville, NY: American Institute of Physics</publisher><ispartof>Physics of fluids (1994), 2007-11, Vol.19 (11), p.113601-113601-10</ispartof><rights>American Institute of Physics</rights><rights>2007 American Institute of Physics</rights><rights>2008 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c384t-5798581b25580dc806edb4026685c778a1c2c429dd2490f11d85a41997c3da4b3</citedby><cites>FETCH-LOGICAL-c384t-5798581b25580dc806edb4026685c778a1c2c429dd2490f11d85a41997c3da4b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,794,1558,4510,27923,27924</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=19924217$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Prokunin, Alexander N.</creatorcontrib><title>The effects of atmospheric pressure, air concentration in the fluid, and the surface roughness on the solid-sphere motion along a wall</title><title>Physics of fluids (1994)</title><description>A phenomenological model for describing a slow steady gravity-driven motion of a solid sphere down an inclined wall in a fluid under the conditions when an air (in the case of a fluid with dissolved air) bubble arises in the sphere-wall lubrication layer between the sphere and the wall is proposed. In the case under consideration, both contact and contactless motion of the sphere is possible. The sphere surface roughness and the concentration of the air dissolved in the fluid are taken into account. The relevant experiment studying the sphere motion accompanied by cavitation was carried out. We used fluids with various air concentration including a limiting case of degasified fluid and spheres of various surface roughness. We find a parameter whose constant value specifies a stationary motion of the sphere including a limiting case of degasified fluid. This parameter turns out to be proportional to the difference between atmospheric pressure and one corresponding to the equilibrium concentration of the air dissolved in fluid. The numerical results found were compared with the experimental data of our investigation and a good quantitative agreement was obtained in a certain domain of parameters. A possibility of unsteady motion of the sphere had been shown.</description><issn>1070-6631</issn><issn>1089-7666</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNqNkMtKAzEARYMoWKsL_yAbF4qjSWYmj40gxRcU3NR1SPNoI9NkSKaKP-B3O50WulJcJSHnnsUB4ByjG4xoeYtvCMeMcnYARhhxUTBK6eHmzlBBaYmPwUnO7wihUhA6At-zpYXWOau7DKODqlvF3C5t8hq2yea8TvYaKp-gjkHb0CXV-RigD7Drl65Ze9P_BzM8e9opbWGK68Uy9GsYt1yOjTfFILZwFQeFamJYQAU_VdOcgiOnmmzPducYvD0-zCbPxfT16WVyPy10yauuqJngNcdzUtccGc0RtWZeIUIprzVjXGFNdEWEMaQSyGFseK0qLATTpVHVvByDy61Xp5hzsk62ya9U-pIYyU1AieUuYM9ebNlWZa0al1TQPu8HQpCK4A13t-Wy9t1Q53dpX1vuasvo5FC7F1z9W_AX_BHTHpStceUPqUCirQ</recordid><startdate>20071101</startdate><enddate>20071101</enddate><creator>Prokunin, Alexander N.</creator><general>American Institute of Physics</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20071101</creationdate><title>The effects of atmospheric pressure, air concentration in the fluid, and the surface roughness on the solid-sphere motion along a wall</title><author>Prokunin, Alexander N.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c384t-5798581b25580dc806edb4026685c778a1c2c429dd2490f11d85a41997c3da4b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Prokunin, Alexander N.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Physics of fluids (1994)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Prokunin, Alexander N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The effects of atmospheric pressure, air concentration in the fluid, and the surface roughness on the solid-sphere motion along a wall</atitle><jtitle>Physics of fluids (1994)</jtitle><date>2007-11-01</date><risdate>2007</risdate><volume>19</volume><issue>11</issue><spage>113601</spage><epage>113601-10</epage><pages>113601-113601-10</pages><issn>1070-6631</issn><eissn>1089-7666</eissn><coden>PHFLE6</coden><abstract>A phenomenological model for describing a slow steady gravity-driven motion of a solid sphere down an inclined wall in a fluid under the conditions when an air (in the case of a fluid with dissolved air) bubble arises in the sphere-wall lubrication layer between the sphere and the wall is proposed. In the case under consideration, both contact and contactless motion of the sphere is possible. The sphere surface roughness and the concentration of the air dissolved in the fluid are taken into account. The relevant experiment studying the sphere motion accompanied by cavitation was carried out. We used fluids with various air concentration including a limiting case of degasified fluid and spheres of various surface roughness. We find a parameter whose constant value specifies a stationary motion of the sphere including a limiting case of degasified fluid. This parameter turns out to be proportional to the difference between atmospheric pressure and one corresponding to the equilibrium concentration of the air dissolved in fluid. The numerical results found were compared with the experimental data of our investigation and a good quantitative agreement was obtained in a certain domain of parameters. A possibility of unsteady motion of the sphere had been shown.</abstract><cop>Melville, NY</cop><pub>American Institute of Physics</pub><doi>10.1063/1.2817687</doi><tpages>10</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1070-6631
ispartof Physics of fluids (1994), 2007-11, Vol.19 (11), p.113601-113601-10
issn 1070-6631
1089-7666
language eng
recordid cdi_scitation_primary_10_1063_1_2817687
source AIP Journals Complete; AIP Digital Archive
title The effects of atmospheric pressure, air concentration in the fluid, and the surface roughness on the solid-sphere motion along a wall
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-11T06%3A56%3A29IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-scitation_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20effects%20of%20atmospheric%20pressure,%20air%20concentration%20in%20the%20fluid,%20and%20the%20surface%20roughness%20on%20the%20solid-sphere%20motion%20along%20a%20wall&rft.jtitle=Physics%20of%20fluids%20(1994)&rft.au=Prokunin,%20Alexander%20N.&rft.date=2007-11-01&rft.volume=19&rft.issue=11&rft.spage=113601&rft.epage=113601-10&rft.pages=113601-113601-10&rft.issn=1070-6631&rft.eissn=1089-7666&rft.coden=PHFLE6&rft_id=info:doi/10.1063/1.2817687&rft_dat=%3Cscitation_cross%3Escitation_primary_10_1063_1_2817687The_effects_of_atmos%3C/scitation_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true