Waves in an elastic medium generated by a point source moving in an overlying fluid medium
Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ d...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Ungar, A. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1973 |
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| Schlagwörter: |
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| Anmerkung: |
© Birkhäuser-Verlag 1973 |
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| Übergeordnetes Werk: |
Enthalten in: Pure and applied geophysics - Birkhäuser-Verlag, 1964, 110(1973), 1 vom: Dez., Seite 1932-1938 |
|---|---|
| Übergeordnetes Werk: |
volume:110 ; year:1973 ; number:1 ; month:12 ; pages:1932-1938 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00876556 |
|---|
| Katalog-ID: |
OLC2069455572 |
|---|
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| 520 | |a Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ describing a conic shock wave whose vertex is moving uniformly with a velocity δ, δ=v/cosα>v. An exact expression is derived for the motion of an elastic half-space excited by the moving point source in an overlying fluid half-space. | ||
| 650 | 4 | |a Shock Wave | |
| 650 | 4 | |a Compressional Wave | |
| 650 | 4 | |a Point Source | |
| 650 | 4 | |a Elastic Wave | |
| 650 | 4 | |a Elastic Medium | |
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10.1007/BF00876556 doi (DE-627)OLC2069455572 (DE-He213)BF00876556-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ungar, A. verfasserin aut Waves in an elastic medium generated by a point source moving in an overlying fluid medium 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1973 Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ describing a conic shock wave whose vertex is moving uniformly with a velocity δ, δ=v/cosα>v. An exact expression is derived for the motion of an elastic half-space excited by the moving point source in an overlying fluid half-space. Shock Wave Compressional Wave Point Source Elastic Wave Elastic Medium Alterman, Z. aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 110(1973), 1 vom: Dez., Seite 1932-1938 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:110 year:1973 number:1 month:12 pages:1932-1938 https://doi.org/10.1007/BF00876556 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 110 1973 1 12 1932-1938 |
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10.1007/BF00876556 doi (DE-627)OLC2069455572 (DE-He213)BF00876556-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ungar, A. verfasserin aut Waves in an elastic medium generated by a point source moving in an overlying fluid medium 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1973 Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ describing a conic shock wave whose vertex is moving uniformly with a velocity δ, δ=v/cosα>v. An exact expression is derived for the motion of an elastic half-space excited by the moving point source in an overlying fluid half-space. Shock Wave Compressional Wave Point Source Elastic Wave Elastic Medium Alterman, Z. aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 110(1973), 1 vom: Dez., Seite 1932-1938 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:110 year:1973 number:1 month:12 pages:1932-1938 https://doi.org/10.1007/BF00876556 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 110 1973 1 12 1932-1938 |
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10.1007/BF00876556 doi (DE-627)OLC2069455572 (DE-He213)BF00876556-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ungar, A. verfasserin aut Waves in an elastic medium generated by a point source moving in an overlying fluid medium 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1973 Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ describing a conic shock wave whose vertex is moving uniformly with a velocity δ, δ=v/cosα>v. An exact expression is derived for the motion of an elastic half-space excited by the moving point source in an overlying fluid half-space. Shock Wave Compressional Wave Point Source Elastic Wave Elastic Medium Alterman, Z. aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 110(1973), 1 vom: Dez., Seite 1932-1938 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:110 year:1973 number:1 month:12 pages:1932-1938 https://doi.org/10.1007/BF00876556 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 110 1973 1 12 1932-1938 |
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10.1007/BF00876556 doi (DE-627)OLC2069455572 (DE-He213)BF00876556-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ungar, A. verfasserin aut Waves in an elastic medium generated by a point source moving in an overlying fluid medium 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1973 Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ describing a conic shock wave whose vertex is moving uniformly with a velocity δ, δ=v/cosα>v. An exact expression is derived for the motion of an elastic half-space excited by the moving point source in an overlying fluid half-space. Shock Wave Compressional Wave Point Source Elastic Wave Elastic Medium Alterman, Z. aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 110(1973), 1 vom: Dez., Seite 1932-1938 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:110 year:1973 number:1 month:12 pages:1932-1938 https://doi.org/10.1007/BF00876556 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 110 1973 1 12 1932-1938 |
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10.1007/BF00876556 doi (DE-627)OLC2069455572 (DE-He213)BF00876556-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ungar, A. verfasserin aut Waves in an elastic medium generated by a point source moving in an overlying fluid medium 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1973 Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ describing a conic shock wave whose vertex is moving uniformly with a velocity δ, δ=v/cosα>v. An exact expression is derived for the motion of an elastic half-space excited by the moving point source in an overlying fluid half-space. Shock Wave Compressional Wave Point Source Elastic Wave Elastic Medium Alterman, Z. aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 110(1973), 1 vom: Dez., Seite 1932-1938 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:110 year:1973 number:1 month:12 pages:1932-1938 https://doi.org/10.1007/BF00876556 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 110 1973 1 12 1932-1938 |
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Waves in an elastic medium generated by a point source moving in an overlying fluid medium |
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Waves in an elastic medium generated by a point source moving in an overlying fluid medium |
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Ungar, A. |
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1973 |
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Ungar, A. Alterman, Z. |
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waves in an elastic medium generated by a point source moving in an overlying fluid medium |
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Waves in an elastic medium generated by a point source moving in an overlying fluid medium |
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Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ describing a conic shock wave whose vertex is moving uniformly with a velocity δ, δ=v/cosα>v. An exact expression is derived for the motion of an elastic half-space excited by the moving point source in an overlying fluid half-space. © Birkhäuser-Verlag 1973 |
| abstractGer |
Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ describing a conic shock wave whose vertex is moving uniformly with a velocity δ, δ=v/cosα>v. An exact expression is derived for the motion of an elastic half-space excited by the moving point source in an overlying fluid half-space. © Birkhäuser-Verlag 1973 |
| abstract_unstemmed |
Summary Elastic waves coupled to atmospheric compressional waves radiated from a supersonic moving point source are considered. The point source has the form.$$\operatorname{Re} [(vt - z\cos \alpha )^2 - r^2 \sin ^2 \alpha ]^{ - 1/2} fort > zcos\alpha /v,0< \alpha \leqslant \frac{\pi }{2},$$ describing a conic shock wave whose vertex is moving uniformly with a velocity δ, δ=v/cosα>v. An exact expression is derived for the motion of an elastic half-space excited by the moving point source in an overlying fluid half-space. © Birkhäuser-Verlag 1973 |
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