Mixed Convection Boundary-Layer Flow on a Vertical Surface in a Porous Medium with a Constant Convective Boundary Condition
Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge...
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| Autor*in: |
Merkin, J. H. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Science+Business Media Dordrecht 2013 |
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| Übergeordnetes Werk: |
Enthalten in: Transport in porous media - Springer Netherlands, 1986, 99(2013), 2 vom: 13. Juni, Seite 413-425 |
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| Übergeordnetes Werk: |
volume:99 ; year:2013 ; number:2 ; day:13 ; month:06 ; pages:413-425 |
| Links: |
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| DOI / URN: |
10.1007/s11242-013-0193-3 |
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OLC2054386960 |
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| 520 | |a Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed. | ||
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10.1007/s11242-013-0193-3 doi (DE-627)OLC2054386960 (DE-He213)s11242-013-0193-3-p DE-627 ger DE-627 rakwb eng 530 VZ Merkin, J. H. verfasserin aut Mixed Convection Boundary-Layer Flow on a Vertical Surface in a Porous Medium with a Constant Convective Boundary Condition 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2013 Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed. Porous media Boundary-layer flow Mixed convection Convective boundary condition Lok, Y. Y. aut Pop, I. aut Enthalten in Transport in porous media Springer Netherlands, 1986 99(2013), 2 vom: 13. Juni, Seite 413-425 (DE-627)129206105 (DE-600)54858-3 (DE-576)014457431 0169-3913 nnns volume:99 year:2013 number:2 day:13 month:06 pages:413-425 https://doi.org/10.1007/s11242-013-0193-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 99 2013 2 13 06 413-425 |
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10.1007/s11242-013-0193-3 doi (DE-627)OLC2054386960 (DE-He213)s11242-013-0193-3-p DE-627 ger DE-627 rakwb eng 530 VZ Merkin, J. H. verfasserin aut Mixed Convection Boundary-Layer Flow on a Vertical Surface in a Porous Medium with a Constant Convective Boundary Condition 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2013 Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed. Porous media Boundary-layer flow Mixed convection Convective boundary condition Lok, Y. Y. aut Pop, I. aut Enthalten in Transport in porous media Springer Netherlands, 1986 99(2013), 2 vom: 13. Juni, Seite 413-425 (DE-627)129206105 (DE-600)54858-3 (DE-576)014457431 0169-3913 nnns volume:99 year:2013 number:2 day:13 month:06 pages:413-425 https://doi.org/10.1007/s11242-013-0193-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 99 2013 2 13 06 413-425 |
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10.1007/s11242-013-0193-3 doi (DE-627)OLC2054386960 (DE-He213)s11242-013-0193-3-p DE-627 ger DE-627 rakwb eng 530 VZ Merkin, J. H. verfasserin aut Mixed Convection Boundary-Layer Flow on a Vertical Surface in a Porous Medium with a Constant Convective Boundary Condition 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2013 Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed. Porous media Boundary-layer flow Mixed convection Convective boundary condition Lok, Y. Y. aut Pop, I. aut Enthalten in Transport in porous media Springer Netherlands, 1986 99(2013), 2 vom: 13. Juni, Seite 413-425 (DE-627)129206105 (DE-600)54858-3 (DE-576)014457431 0169-3913 nnns volume:99 year:2013 number:2 day:13 month:06 pages:413-425 https://doi.org/10.1007/s11242-013-0193-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 99 2013 2 13 06 413-425 |
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10.1007/s11242-013-0193-3 doi (DE-627)OLC2054386960 (DE-He213)s11242-013-0193-3-p DE-627 ger DE-627 rakwb eng 530 VZ Merkin, J. H. verfasserin aut Mixed Convection Boundary-Layer Flow on a Vertical Surface in a Porous Medium with a Constant Convective Boundary Condition 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2013 Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed. Porous media Boundary-layer flow Mixed convection Convective boundary condition Lok, Y. Y. aut Pop, I. aut Enthalten in Transport in porous media Springer Netherlands, 1986 99(2013), 2 vom: 13. Juni, Seite 413-425 (DE-627)129206105 (DE-600)54858-3 (DE-576)014457431 0169-3913 nnns volume:99 year:2013 number:2 day:13 month:06 pages:413-425 https://doi.org/10.1007/s11242-013-0193-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 99 2013 2 13 06 413-425 |
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10.1007/s11242-013-0193-3 doi (DE-627)OLC2054386960 (DE-He213)s11242-013-0193-3-p DE-627 ger DE-627 rakwb eng 530 VZ Merkin, J. H. verfasserin aut Mixed Convection Boundary-Layer Flow on a Vertical Surface in a Porous Medium with a Constant Convective Boundary Condition 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2013 Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed. Porous media Boundary-layer flow Mixed convection Convective boundary condition Lok, Y. Y. aut Pop, I. aut Enthalten in Transport in porous media Springer Netherlands, 1986 99(2013), 2 vom: 13. Juni, Seite 413-425 (DE-627)129206105 (DE-600)54858-3 (DE-576)014457431 0169-3913 nnns volume:99 year:2013 number:2 day:13 month:06 pages:413-425 https://doi.org/10.1007/s11242-013-0193-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 99 2013 2 13 06 413-425 |
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Mixed Convection Boundary-Layer Flow on a Vertical Surface in a Porous Medium with a Constant Convective Boundary Condition |
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Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed. © Springer Science+Business Media Dordrecht 2013 |
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Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed. © Springer Science+Business Media Dordrecht 2013 |
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Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed. © Springer Science+Business Media Dordrecht 2013 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2054386960</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230504062730.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2013 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11242-013-0193-3</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2054386960</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11242-013-0193-3-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">530</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Merkin, J. H.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Mixed Convection Boundary-Layer Flow on a Vertical Surface in a Porous Medium with a Constant Convective Boundary Condition</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2013</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media Dordrecht 2013</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The mixed convection boundary-layer flow on a vertical surface heated convectively is considered when a constant surface heat transfer parameter is assumed. The problem is seen to be chararterized by a mixed convection parameter $$\gamma $$. The flow and heat transfer near the leading edge correspond to forced convection solution and numerical solutions are obtained to determine how the solution then develops. The solution at large distances is obtained and this identifies a critical value $$\gamma _c$$ of the parameter $$\gamma $$. For $$\gamma > \gamma _c$$ a solution at large distances is possible and this is approached in the numerical integrations. For $$\gamma <\gamma _c$$ the numerical solution breaks down at a finite distance along the surface with a singularity, the nature of which is discussed.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Porous media</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Boundary-layer flow</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mixed convection</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Convective boundary condition</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lok, Y. Y.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Pop, I.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Transport in porous media</subfield><subfield code="d">Springer Netherlands, 1986</subfield><subfield code="g">99(2013), 2 vom: 13. Juni, Seite 413-425</subfield><subfield code="w">(DE-627)129206105</subfield><subfield code="w">(DE-600)54858-3</subfield><subfield code="w">(DE-576)014457431</subfield><subfield code="x">0169-3913</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:99</subfield><subfield code="g">year:2013</subfield><subfield code="g">number:2</subfield><subfield code="g">day:13</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:413-425</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11242-013-0193-3</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-TEC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">99</subfield><subfield code="j">2013</subfield><subfield code="e">2</subfield><subfield code="b">13</subfield><subfield code="c">06</subfield><subfield code="h">413-425</subfield></datafield></record></collection>
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