Effects of natural convection on high-pressure droplet combustion
Burning behavior of a suspended fuel droplet under both normal and microgravity fields has been studied experimentally to explore the effects of natural convection at high ambient pressure levels up to four times the fuel critical pressure. The fuel employed was n-octane. Experiments have shown that...
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Veröffentlicht in: | Combustion and flame 1990-11, Vol.82 (2), p.142-150 |
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creator | Sato, Jun'ichi Tsue, Mitsuhiro Niwa, Mario Kono, Michikata |
description | Burning behavior of a suspended fuel droplet under both normal and microgravity fields has been studied experimentally to explore the effects of natural convection at high ambient pressure levels up to four times the fuel critical pressure. The fuel employed was
n-octane. Experiments have shown that the burning rate constant increases with the increase of the ambient pressure at subcritical pressures and decreases at supercritical pressures for both microgravity and normal gravity fields. The maximum value of the burning rate constant appears at the critical pressure of the fuel. The natural convection increases the burning rate constant and its effect becomes stronger as the ambient pressure increases. The natural convection effect is expressed as
(
K
K
0
− 1) ∼
Gr
0.25
or
(
(K
K
0
− 1) ∼ P
0.5
for high pressures, where Gr is the Grashof number and
K and
K
0 are the burning rate constants in natural gravity and microgravity fields. |
doi_str_mv | 10.1016/0010-2180(90)90093-7 |
format | Article |
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n-octane. Experiments have shown that the burning rate constant increases with the increase of the ambient pressure at subcritical pressures and decreases at supercritical pressures for both microgravity and normal gravity fields. The maximum value of the burning rate constant appears at the critical pressure of the fuel. The natural convection increases the burning rate constant and its effect becomes stronger as the ambient pressure increases. The natural convection effect is expressed as
(
K
K
0
− 1) ∼
Gr
0.25
or
(
(K
K
0
− 1) ∼ P
0.5
for high pressures, where Gr is the Grashof number and
K and
K
0 are the burning rate constants in natural gravity and microgravity fields.</description><identifier>ISSN: 0010-2180</identifier><identifier>EISSN: 1556-2921</identifier><identifier>DOI: 10.1016/0010-2180(90)90093-7</identifier><identifier>CODEN: CBFMAO</identifier><language>eng</language><publisher>New York, NY: Elsevier Inc</publisher><subject>400800 - Combustion, Pyrolysis, & High-Temperature Chemistry ; 420400 - Engineering- Heat Transfer & Fluid Flow ; CHEMICAL REACTION KINETICS ; Chemistry ; COMBUSTION KINETICS ; Combustion. Flame ; CONVECTION ; DATA ; DROPLETS ; ENERGY TRANSFER ; ENGINEERING ; Exact sciences and technology ; EXPERIMENTAL DATA ; FLAMES ; FUELS ; General and physical chemistry ; HEAT TRANSFER ; HIGH PRESSURE ; INFORMATION ; INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY ; KINETICS ; MASS TRANSFER ; NATURAL CONVECTION ; NUMERICAL DATA ; PARTICLES ; pressure ; REACTION KINETICS</subject><ispartof>Combustion and flame, 1990-11, Vol.82 (2), p.142-150</ispartof><rights>1990</rights><rights>1991 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c490t-92dbaabd28001afc2bdb9eb2a2c13420307f1ed3446cf1fc2b4a4494fd75710e3</citedby><cites>FETCH-LOGICAL-c490t-92dbaabd28001afc2bdb9eb2a2c13420307f1ed3446cf1fc2b4a4494fd75710e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/0010218090900937$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,776,780,881,3537,27901,27902,65534</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=19364905$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.osti.gov/biblio/5758968$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Sato, Jun'ichi</creatorcontrib><creatorcontrib>Tsue, Mitsuhiro</creatorcontrib><creatorcontrib>Niwa, Mario</creatorcontrib><creatorcontrib>Kono, Michikata</creatorcontrib><title>Effects of natural convection on high-pressure droplet combustion</title><title>Combustion and flame</title><description>Burning behavior of a suspended fuel droplet under both normal and microgravity fields has been studied experimentally to explore the effects of natural convection at high ambient pressure levels up to four times the fuel critical pressure. The fuel employed was
n-octane. Experiments have shown that the burning rate constant increases with the increase of the ambient pressure at subcritical pressures and decreases at supercritical pressures for both microgravity and normal gravity fields. The maximum value of the burning rate constant appears at the critical pressure of the fuel. The natural convection increases the burning rate constant and its effect becomes stronger as the ambient pressure increases. The natural convection effect is expressed as
(
K
K
0
− 1) ∼
Gr
0.25
or
(
(K
K
0
− 1) ∼ P
0.5
for high pressures, where Gr is the Grashof number and
K and
K
0 are the burning rate constants in natural gravity and microgravity fields.</description><subject>400800 - Combustion, Pyrolysis, & High-Temperature Chemistry</subject><subject>420400 - Engineering- Heat Transfer & Fluid Flow</subject><subject>CHEMICAL REACTION KINETICS</subject><subject>Chemistry</subject><subject>COMBUSTION KINETICS</subject><subject>Combustion. Flame</subject><subject>CONVECTION</subject><subject>DATA</subject><subject>DROPLETS</subject><subject>ENERGY TRANSFER</subject><subject>ENGINEERING</subject><subject>Exact sciences and technology</subject><subject>EXPERIMENTAL DATA</subject><subject>FLAMES</subject><subject>FUELS</subject><subject>General and physical chemistry</subject><subject>HEAT TRANSFER</subject><subject>HIGH PRESSURE</subject><subject>INFORMATION</subject><subject>INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY</subject><subject>KINETICS</subject><subject>MASS TRANSFER</subject><subject>NATURAL CONVECTION</subject><subject>NUMERICAL DATA</subject><subject>PARTICLES</subject><subject>pressure</subject><subject>REACTION KINETICS</subject><issn>0010-2180</issn><issn>1556-2921</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1990</creationdate><recordtype>article</recordtype><recordid>eNp9kE1r3DAQhkVJoJuk_6AHU2ibHJyMPiytLoEQ8gWBXJqzkOVRV8VrbSQ70H9fiQ3pLfCCQPPMzDsvIV8pnFOg8gKAQsvoGk41nGkAzVv1iaxo18mWaUYPyOod-UyOcv4DAEpwviJXN96jm3MTfTPZeUl2bFycXstfiFNTtAm_N-0uYc5LwmZIcTfiXJhtv-TKnJBDb8eMX97eY_J8e_Pr-r59fLp7uL56bJ3QMLeaDb21_cDWxYr1jvVDr7FnljnKBQMOylMcuBDSeVrrwgqhhR9UpyggPybf9nNjWWuyCzO6TbE6FaumU91ay3WBfu6hXYovC-bZbEN2OI52wrhko0RXpCUv5I8PSdZJSaXqCij2oEsx54Te7FLY2vTXUDA1flOzNTVbo6tK_EaVtu9v8212dvTJTi7k_72ay5JLHX-557Bk9xow1dNwcjiEVC8bYvh40T_MgphR</recordid><startdate>19901101</startdate><enddate>19901101</enddate><creator>Sato, Jun'ichi</creator><creator>Tsue, Mitsuhiro</creator><creator>Niwa, Mario</creator><creator>Kono, Michikata</creator><general>Elsevier Inc</general><general>Elsevier Science</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><scope>7TC</scope><scope>OTOTI</scope></search><sort><creationdate>19901101</creationdate><title>Effects of natural convection on high-pressure droplet combustion</title><author>Sato, Jun'ichi ; Tsue, Mitsuhiro ; Niwa, Mario ; Kono, Michikata</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c490t-92dbaabd28001afc2bdb9eb2a2c13420307f1ed3446cf1fc2b4a4494fd75710e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1990</creationdate><topic>400800 - Combustion, Pyrolysis, & High-Temperature Chemistry</topic><topic>420400 - Engineering- Heat Transfer & Fluid Flow</topic><topic>CHEMICAL REACTION KINETICS</topic><topic>Chemistry</topic><topic>COMBUSTION KINETICS</topic><topic>Combustion. Flame</topic><topic>CONVECTION</topic><topic>DATA</topic><topic>DROPLETS</topic><topic>ENERGY TRANSFER</topic><topic>ENGINEERING</topic><topic>Exact sciences and technology</topic><topic>EXPERIMENTAL DATA</topic><topic>FLAMES</topic><topic>FUELS</topic><topic>General and physical chemistry</topic><topic>HEAT TRANSFER</topic><topic>HIGH PRESSURE</topic><topic>INFORMATION</topic><topic>INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY</topic><topic>KINETICS</topic><topic>MASS TRANSFER</topic><topic>NATURAL CONVECTION</topic><topic>NUMERICAL DATA</topic><topic>PARTICLES</topic><topic>pressure</topic><topic>REACTION KINETICS</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sato, Jun'ichi</creatorcontrib><creatorcontrib>Tsue, Mitsuhiro</creatorcontrib><creatorcontrib>Niwa, Mario</creatorcontrib><creatorcontrib>Kono, Michikata</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Mechanical Engineering Abstracts</collection><collection>OSTI.GOV</collection><jtitle>Combustion and flame</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sato, Jun'ichi</au><au>Tsue, Mitsuhiro</au><au>Niwa, Mario</au><au>Kono, Michikata</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effects of natural convection on high-pressure droplet combustion</atitle><jtitle>Combustion and flame</jtitle><date>1990-11-01</date><risdate>1990</risdate><volume>82</volume><issue>2</issue><spage>142</spage><epage>150</epage><pages>142-150</pages><issn>0010-2180</issn><eissn>1556-2921</eissn><coden>CBFMAO</coden><abstract>Burning behavior of a suspended fuel droplet under both normal and microgravity fields has been studied experimentally to explore the effects of natural convection at high ambient pressure levels up to four times the fuel critical pressure. The fuel employed was
n-octane. Experiments have shown that the burning rate constant increases with the increase of the ambient pressure at subcritical pressures and decreases at supercritical pressures for both microgravity and normal gravity fields. The maximum value of the burning rate constant appears at the critical pressure of the fuel. The natural convection increases the burning rate constant and its effect becomes stronger as the ambient pressure increases. The natural convection effect is expressed as
(
K
K
0
− 1) ∼
Gr
0.25
or
(
(K
K
0
− 1) ∼ P
0.5
for high pressures, where Gr is the Grashof number and
K and
K
0 are the burning rate constants in natural gravity and microgravity fields.</abstract><cop>New York, NY</cop><pub>Elsevier Inc</pub><doi>10.1016/0010-2180(90)90093-7</doi><tpages>9</tpages></addata></record> |
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source | Elsevier ScienceDirect Journals |
subjects | 400800 - Combustion, Pyrolysis, & High-Temperature Chemistry 420400 - Engineering- Heat Transfer & Fluid Flow CHEMICAL REACTION KINETICS Chemistry COMBUSTION KINETICS Combustion. Flame CONVECTION DATA DROPLETS ENERGY TRANSFER ENGINEERING Exact sciences and technology EXPERIMENTAL DATA FLAMES FUELS General and physical chemistry HEAT TRANSFER HIGH PRESSURE INFORMATION INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY KINETICS MASS TRANSFER NATURAL CONVECTION NUMERICAL DATA PARTICLES pressure REACTION KINETICS |
title | Effects of natural convection on high-pressure droplet combustion |
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