Electromagnetic properties of ice near the water-ice phase transition temperature
Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them in...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Bordonskii, G. S. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2005 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Inc. 2005 |
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| Übergeordnetes Werk: |
Enthalten in: Physics of the solid state - Nauka/Interperiodica, 1993, 47(2005), 4 vom: Apr., Seite 715-719 |
|---|---|
| Übergeordnetes Werk: |
volume:47 ; year:2005 ; number:4 ; month:04 ; pages:715-719 |
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| DOI / URN: |
10.1134/1.1913986 |
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OLC2040702326 |
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| 520 | |a Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them increasing near 0°C. In such a medium, two waves with identical polarizations and similar wavenumbers can exist. This assumption was confirmed experimentally by measuring the 13-GHz radiation transmission through a natural freshwater ice cover. These measurements detected signal oscillations caused by the interference of two waves, with alternation of maxima and minima with a period of 4.6 m, which corresponds to a beat frequency of ∼37 MHz. | ||
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10.1134/1.1913986 doi (DE-627)OLC2040702326 (DE-He213)1.1913986-p DE-627 ger DE-627 rakwb eng 530 VZ Bordonskii, G. S. verfasserin aut Electromagnetic properties of ice near the water-ice phase transition temperature 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2005 Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them increasing near 0°C. In such a medium, two waves with identical polarizations and similar wavenumbers can exist. This assumption was confirmed experimentally by measuring the 13-GHz radiation transmission through a natural freshwater ice cover. These measurements detected signal oscillations caused by the interference of two waves, with alternation of maxima and minima with a period of 4.6 m, which corresponds to a beat frequency of ∼37 MHz. Radiation Phase Transition Transition Temperature Transmission Line Vibrational Mode Enthalten in Physics of the solid state Nauka/Interperiodica, 1993 47(2005), 4 vom: Apr., Seite 715-719 (DE-627)16567332X (DE-600)1159011-7 (DE-576)038490706 1063-7834 nnns volume:47 year:2005 number:4 month:04 pages:715-719 https://doi.org/10.1134/1.1913986 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_40 GBV_ILN_70 GBV_ILN_4700 AR 47 2005 4 04 715-719 |
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10.1134/1.1913986 doi (DE-627)OLC2040702326 (DE-He213)1.1913986-p DE-627 ger DE-627 rakwb eng 530 VZ Bordonskii, G. S. verfasserin aut Electromagnetic properties of ice near the water-ice phase transition temperature 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2005 Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them increasing near 0°C. In such a medium, two waves with identical polarizations and similar wavenumbers can exist. This assumption was confirmed experimentally by measuring the 13-GHz radiation transmission through a natural freshwater ice cover. These measurements detected signal oscillations caused by the interference of two waves, with alternation of maxima and minima with a period of 4.6 m, which corresponds to a beat frequency of ∼37 MHz. Radiation Phase Transition Transition Temperature Transmission Line Vibrational Mode Enthalten in Physics of the solid state Nauka/Interperiodica, 1993 47(2005), 4 vom: Apr., Seite 715-719 (DE-627)16567332X (DE-600)1159011-7 (DE-576)038490706 1063-7834 nnns volume:47 year:2005 number:4 month:04 pages:715-719 https://doi.org/10.1134/1.1913986 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_40 GBV_ILN_70 GBV_ILN_4700 AR 47 2005 4 04 715-719 |
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10.1134/1.1913986 doi (DE-627)OLC2040702326 (DE-He213)1.1913986-p DE-627 ger DE-627 rakwb eng 530 VZ Bordonskii, G. S. verfasserin aut Electromagnetic properties of ice near the water-ice phase transition temperature 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2005 Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them increasing near 0°C. In such a medium, two waves with identical polarizations and similar wavenumbers can exist. This assumption was confirmed experimentally by measuring the 13-GHz radiation transmission through a natural freshwater ice cover. These measurements detected signal oscillations caused by the interference of two waves, with alternation of maxima and minima with a period of 4.6 m, which corresponds to a beat frequency of ∼37 MHz. Radiation Phase Transition Transition Temperature Transmission Line Vibrational Mode Enthalten in Physics of the solid state Nauka/Interperiodica, 1993 47(2005), 4 vom: Apr., Seite 715-719 (DE-627)16567332X (DE-600)1159011-7 (DE-576)038490706 1063-7834 nnns volume:47 year:2005 number:4 month:04 pages:715-719 https://doi.org/10.1134/1.1913986 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_40 GBV_ILN_70 GBV_ILN_4700 AR 47 2005 4 04 715-719 |
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10.1134/1.1913986 doi (DE-627)OLC2040702326 (DE-He213)1.1913986-p DE-627 ger DE-627 rakwb eng 530 VZ Bordonskii, G. S. verfasserin aut Electromagnetic properties of ice near the water-ice phase transition temperature 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2005 Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them increasing near 0°C. In such a medium, two waves with identical polarizations and similar wavenumbers can exist. This assumption was confirmed experimentally by measuring the 13-GHz radiation transmission through a natural freshwater ice cover. These measurements detected signal oscillations caused by the interference of two waves, with alternation of maxima and minima with a period of 4.6 m, which corresponds to a beat frequency of ∼37 MHz. Radiation Phase Transition Transition Temperature Transmission Line Vibrational Mode Enthalten in Physics of the solid state Nauka/Interperiodica, 1993 47(2005), 4 vom: Apr., Seite 715-719 (DE-627)16567332X (DE-600)1159011-7 (DE-576)038490706 1063-7834 nnns volume:47 year:2005 number:4 month:04 pages:715-719 https://doi.org/10.1134/1.1913986 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_40 GBV_ILN_70 GBV_ILN_4700 AR 47 2005 4 04 715-719 |
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Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them increasing near 0°C. In such a medium, two waves with identical polarizations and similar wavenumbers can exist. This assumption was confirmed experimentally by measuring the 13-GHz radiation transmission through a natural freshwater ice cover. These measurements detected signal oscillations caused by the interference of two waves, with alternation of maxima and minima with a period of 4.6 m, which corresponds to a beat frequency of ∼37 MHz. © Pleiades Publishing, Inc. 2005 |
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Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them increasing near 0°C. In such a medium, two waves with identical polarizations and similar wavenumbers can exist. This assumption was confirmed experimentally by measuring the 13-GHz radiation transmission through a natural freshwater ice cover. These measurements detected signal oscillations caused by the interference of two waves, with alternation of maxima and minima with a period of 4.6 m, which corresponds to a beat frequency of ∼37 MHz. © Pleiades Publishing, Inc. 2005 |
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Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them increasing near 0°C. In such a medium, two waves with identical polarizations and similar wavenumbers can exist. This assumption was confirmed experimentally by measuring the 13-GHz radiation transmission through a natural freshwater ice cover. These measurements detected signal oscillations caused by the interference of two waves, with alternation of maxima and minima with a period of 4.6 m, which corresponds to a beat frequency of ∼37 MHz. © Pleiades Publishing, Inc. 2005 |
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S.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Electromagnetic properties of ice near the water-ice phase transition temperature</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2005</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">© Pleiades Publishing, Inc. 2005</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Freshwater ice in a cavity was studied under heating to 0°C followed by cooling at a frequency of 6.3 GHz. Splitting of a resonant transmission line at 60–70 MHz was detected. This effect may be associated with the existence of two vibrational modes in ice, with the coupling between them increasing near 0°C. In such a medium, two waves with identical polarizations and similar wavenumbers can exist. This assumption was confirmed experimentally by measuring the 13-GHz radiation transmission through a natural freshwater ice cover. These measurements detected signal oscillations caused by the interference of two waves, with alternation of maxima and minima with a period of 4.6 m, which corresponds to a beat frequency of ∼37 MHz.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Radiation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Phase Transition</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Transition Temperature</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Transmission Line</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vibrational Mode</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Physics of the solid state</subfield><subfield code="d">Nauka/Interperiodica, 1993</subfield><subfield code="g">47(2005), 4 vom: Apr., Seite 715-719</subfield><subfield code="w">(DE-627)16567332X</subfield><subfield code="w">(DE-600)1159011-7</subfield><subfield code="w">(DE-576)038490706</subfield><subfield code="x">1063-7834</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:47</subfield><subfield code="g">year:2005</subfield><subfield code="g">number:4</subfield><subfield code="g">month:04</subfield><subfield code="g">pages:715-719</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1134/1.1913986</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-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">47</subfield><subfield code="j">2005</subfield><subfield code="e">4</subfield><subfield code="c">04</subfield><subfield code="h">715-719</subfield></datafield></record></collection>
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