Experimental study of properties of water in thin films and fine capillaries
Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminish...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zheleznyi, B. V. [verfasserIn] Zorin, Z. M. [verfasserIn] Sobolev, W. D. [verfasserIn] Churaev, N. V. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1972 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Bulletin of engineering geology and the environment - Berlin : Springer, 1970, 5(1972), 1 vom: 01. Juni, Seite 57-61 |
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| Übergeordnetes Werk: |
volume:5 ; year:1972 ; number:1 ; day:01 ; month:06 ; pages:57-61 |
| Links: |
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| DOI / URN: |
10.1007/BF02634653 |
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| Katalog-ID: |
SPR008449783 |
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| 100 | 1 | |a Zheleznyi, B. V. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Experimental study of properties of water in thin films and fine capillaries |
| 264 | 1 | |c 1972 | |
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| 520 | |a Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density. | ||
| 650 | 4 | |a Capillary Pressure |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Relative Viscosity |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Fuse Quartz |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Quartz Capillary |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Capillary Radius |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Zorin, Z. M. |e verfasserin |4 aut | |
| 700 | 1 | |a Sobolev, W. D. |e verfasserin |4 aut | |
| 700 | 1 | |a Churaev, N. V. |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Bulletin of engineering geology and the environment |d Berlin : Springer, 1970 |g 5(1972), 1 vom: 01. Juni, Seite 57-61 |w (DE-627)271597011 |w (DE-600)1480689-7 |x 1435-9537 |7 nnns |
| 773 | 1 | 8 | |g volume:5 |g year:1972 |g number:1 |g day:01 |g month:06 |g pages:57-61 |
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10.1007/BF02634653 doi (DE-627)SPR008449783 (SPR)BF02634653-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density. Capillary Pressure (dpeaa)DE-He213 Relative Viscosity (dpeaa)DE-He213 Fuse Quartz (dpeaa)DE-He213 Quartz Capillary (dpeaa)DE-He213 Capillary Radius (dpeaa)DE-He213 Zorin, Z. M. verfasserin aut Sobolev, W. D. verfasserin aut Churaev, N. V. verfasserin aut Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://dx.doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 5 1972 1 01 06 57-61 |
| spelling |
10.1007/BF02634653 doi (DE-627)SPR008449783 (SPR)BF02634653-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density. Capillary Pressure (dpeaa)DE-He213 Relative Viscosity (dpeaa)DE-He213 Fuse Quartz (dpeaa)DE-He213 Quartz Capillary (dpeaa)DE-He213 Capillary Radius (dpeaa)DE-He213 Zorin, Z. M. verfasserin aut Sobolev, W. D. verfasserin aut Churaev, N. V. verfasserin aut Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://dx.doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 5 1972 1 01 06 57-61 |
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10.1007/BF02634653 doi (DE-627)SPR008449783 (SPR)BF02634653-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density. Capillary Pressure (dpeaa)DE-He213 Relative Viscosity (dpeaa)DE-He213 Fuse Quartz (dpeaa)DE-He213 Quartz Capillary (dpeaa)DE-He213 Capillary Radius (dpeaa)DE-He213 Zorin, Z. M. verfasserin aut Sobolev, W. D. verfasserin aut Churaev, N. V. verfasserin aut Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://dx.doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 5 1972 1 01 06 57-61 |
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10.1007/BF02634653 doi (DE-627)SPR008449783 (SPR)BF02634653-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density. Capillary Pressure (dpeaa)DE-He213 Relative Viscosity (dpeaa)DE-He213 Fuse Quartz (dpeaa)DE-He213 Quartz Capillary (dpeaa)DE-He213 Capillary Radius (dpeaa)DE-He213 Zorin, Z. M. verfasserin aut Sobolev, W. D. verfasserin aut Churaev, N. V. verfasserin aut Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://dx.doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 5 1972 1 01 06 57-61 |
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10.1007/BF02634653 doi (DE-627)SPR008449783 (SPR)BF02634653-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density. Capillary Pressure (dpeaa)DE-He213 Relative Viscosity (dpeaa)DE-He213 Fuse Quartz (dpeaa)DE-He213 Quartz Capillary (dpeaa)DE-He213 Capillary Radius (dpeaa)DE-He213 Zorin, Z. M. verfasserin aut Sobolev, W. D. verfasserin aut Churaev, N. V. verfasserin aut Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://dx.doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 5 1972 1 01 06 57-61 |
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Enthalten in Bulletin of engineering geology and the environment 5(1972), 1 vom: 01. Juni, Seite 57-61 volume:5 year:1972 number:1 day:01 month:06 pages:57-61 |
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V.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Experimental study of properties of water in thin films and fine capillaries</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1972</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">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Capillary Pressure</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Relative Viscosity</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fuse Quartz</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Quartz Capillary</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Capillary Radius</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zorin, Z. 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Zheleznyi, B. V. |
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Zheleznyi, B. V. ddc 550 bkl 38.58 bkl 56.00 bkl 56.20 misc Capillary Pressure misc Relative Viscosity misc Fuse Quartz misc Quartz Capillary misc Capillary Radius Experimental study of properties of water in thin films and fine capillaries |
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550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Experimental study of properties of water in thin films and fine capillaries Capillary Pressure (dpeaa)DE-He213 Relative Viscosity (dpeaa)DE-He213 Fuse Quartz (dpeaa)DE-He213 Quartz Capillary (dpeaa)DE-He213 Capillary Radius (dpeaa)DE-He213 |
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ddc 550 bkl 38.58 bkl 56.00 bkl 56.20 misc Capillary Pressure misc Relative Viscosity misc Fuse Quartz misc Quartz Capillary misc Capillary Radius |
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ddc 550 bkl 38.58 bkl 56.00 bkl 56.20 misc Capillary Pressure misc Relative Viscosity misc Fuse Quartz misc Quartz Capillary misc Capillary Radius |
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ddc 550 bkl 38.58 bkl 56.00 bkl 56.20 misc Capillary Pressure misc Relative Viscosity misc Fuse Quartz misc Quartz Capillary misc Capillary Radius |
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Experimental study of properties of water in thin films and fine capillaries |
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Experimental study of properties of water in thin films and fine capillaries |
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Zheleznyi, B. V. |
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Bulletin of engineering geology and the environment |
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Zheleznyi, B. V. Zorin, Z. M. Sobolev, W. D. Churaev, N. V. |
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experimental study of properties of water in thin films and fine capillaries |
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Experimental study of properties of water in thin films and fine capillaries |
| abstract |
Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density. |
| abstractGer |
Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density. |
| abstract_unstemmed |
Abstract The properties of water, introduced from the bulk phase in fine capillaries of radii >0,03 µ drawn from the pure fused quartz, are studied. The enhanced viscosity of water in capillaries less than0,5 µ has been observed. With growing temperature the difference from the bulk data diminishes and disappears at65–70° C. The thermal expansion of water in the same capillaries does not differ from the data for the bulk phase. But the freezing of water in fine capillaries occurs only by strong supercooling, corresponding to the condition of homogeneous crystallization. The high degree of supercooling may be explained by changes in the structure of boundary water layers. The structural changes influences markedly the rheological properties of water in capillaries, but does not cause, indeed, any essential change in density. |
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| title_short |
Experimental study of properties of water in thin films and fine capillaries |
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https://dx.doi.org/10.1007/BF02634653 |
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Zorin, Z. M. Sobolev, W. D. Churaev, N. V. |
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Zorin, Z. M. Sobolev, W. D. Churaev, N. V. |
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10.1007/BF02634653 |
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2024-07-03T21:05:40.434Z |
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| score |
7.4003716 |