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
Autor*in: |
Zheleznyi, B. V. [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
1972 |
---|
Schlagwörter: |
---|
Anmerkung: |
© International Association of Engineering Geology 1972 |
---|
Übergeordnetes Werk: |
Enthalten in: Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur - Springer Berlin Heidelberg, 1970, 5(1972), 1 vom: 01. Juni, Seite 57-61 |
---|---|
Übergeordnetes Werk: |
volume:5 ; year:1972 ; number:1 ; day:01 ; month:06 ; pages:57-61 |
Links: |
---|
DOI / URN: |
10.1007/BF02634653 |
---|
Katalog-ID: |
OLC2061663532 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2061663532 | ||
003 | DE-627 | ||
005 | 20230502165230.0 | ||
007 | tu | ||
008 | 200819s1972 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/BF02634653 |2 doi | |
035 | |a (DE-627)OLC2061663532 | ||
035 | |a (DE-He213)BF02634653-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |a 600 |q VZ |
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 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © International Association of Engineering Geology 1972 | ||
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 | |
650 | 4 | |a Relative Viscosity | |
650 | 4 | |a Fuse Quartz | |
650 | 4 | |a Quartz Capillary | |
650 | 4 | |a Capillary Radius | |
700 | 1 | |a Zorin, Z. M. |4 aut | |
700 | 1 | |a Sobolev, W. D. |4 aut | |
700 | 1 | |a Churaev, N. V. |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur |d Springer Berlin Heidelberg, 1970 |g 5(1972), 1 vom: 01. Juni, Seite 57-61 |w (DE-627)129378666 |w (DE-600)164473-7 |w (DE-576)014761408 |x 0074-1612 |7 nnns |
773 | 1 | 8 | |g volume:5 |g year:1972 |g number:1 |g day:01 |g month:06 |g pages:57-61 |
856 | 4 | 1 | |u https://doi.org/10.1007/BF02634653 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-TEC | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OPC-GGO | ||
912 | |a SSG-OPC-GEO | ||
912 | |a GBV_ILN_30 | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_2016 | ||
912 | |a GBV_ILN_4046 | ||
951 | |a AR | ||
952 | |d 5 |j 1972 |e 1 |b 01 |c 06 |h 57-61 |
author_variant |
b v z bv bvz z m z zm zmz w d s wd wds n v c nv nvc |
---|---|
matchkey_str |
article:00741612:1972----::xeietltdopoeteowtrnhnima |
hierarchy_sort_str |
1972 |
publishDate |
1972 |
allfields |
10.1007/BF02634653 doi (DE-627)OLC2061663532 (DE-He213)BF02634653-p DE-627 ger DE-627 rakwb eng 550 600 VZ Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © International Association of Engineering Geology 1972 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 Relative Viscosity Fuse Quartz Quartz Capillary Capillary Radius Zorin, Z. M. aut Sobolev, W. D. aut Churaev, N. V. aut Enthalten in Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur Springer Berlin Heidelberg, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)129378666 (DE-600)164473-7 (DE-576)014761408 0074-1612 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_30 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2016 GBV_ILN_4046 AR 5 1972 1 01 06 57-61 |
spelling |
10.1007/BF02634653 doi (DE-627)OLC2061663532 (DE-He213)BF02634653-p DE-627 ger DE-627 rakwb eng 550 600 VZ Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © International Association of Engineering Geology 1972 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 Relative Viscosity Fuse Quartz Quartz Capillary Capillary Radius Zorin, Z. M. aut Sobolev, W. D. aut Churaev, N. V. aut Enthalten in Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur Springer Berlin Heidelberg, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)129378666 (DE-600)164473-7 (DE-576)014761408 0074-1612 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_30 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2016 GBV_ILN_4046 AR 5 1972 1 01 06 57-61 |
allfields_unstemmed |
10.1007/BF02634653 doi (DE-627)OLC2061663532 (DE-He213)BF02634653-p DE-627 ger DE-627 rakwb eng 550 600 VZ Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © International Association of Engineering Geology 1972 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 Relative Viscosity Fuse Quartz Quartz Capillary Capillary Radius Zorin, Z. M. aut Sobolev, W. D. aut Churaev, N. V. aut Enthalten in Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur Springer Berlin Heidelberg, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)129378666 (DE-600)164473-7 (DE-576)014761408 0074-1612 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_30 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2016 GBV_ILN_4046 AR 5 1972 1 01 06 57-61 |
allfieldsGer |
10.1007/BF02634653 doi (DE-627)OLC2061663532 (DE-He213)BF02634653-p DE-627 ger DE-627 rakwb eng 550 600 VZ Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © International Association of Engineering Geology 1972 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 Relative Viscosity Fuse Quartz Quartz Capillary Capillary Radius Zorin, Z. M. aut Sobolev, W. D. aut Churaev, N. V. aut Enthalten in Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur Springer Berlin Heidelberg, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)129378666 (DE-600)164473-7 (DE-576)014761408 0074-1612 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_30 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2016 GBV_ILN_4046 AR 5 1972 1 01 06 57-61 |
allfieldsSound |
10.1007/BF02634653 doi (DE-627)OLC2061663532 (DE-He213)BF02634653-p DE-627 ger DE-627 rakwb eng 550 600 VZ Zheleznyi, B. V. verfasserin aut Experimental study of properties of water in thin films and fine capillaries 1972 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © International Association of Engineering Geology 1972 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 Relative Viscosity Fuse Quartz Quartz Capillary Capillary Radius Zorin, Z. M. aut Sobolev, W. D. aut Churaev, N. V. aut Enthalten in Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur Springer Berlin Heidelberg, 1970 5(1972), 1 vom: 01. Juni, Seite 57-61 (DE-627)129378666 (DE-600)164473-7 (DE-576)014761408 0074-1612 nnns volume:5 year:1972 number:1 day:01 month:06 pages:57-61 https://doi.org/10.1007/BF02634653 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_30 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2016 GBV_ILN_4046 AR 5 1972 1 01 06 57-61 |
language |
English |
source |
Enthalten in Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur 5(1972), 1 vom: 01. Juni, Seite 57-61 volume:5 year:1972 number:1 day:01 month:06 pages:57-61 |
sourceStr |
Enthalten in Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur 5(1972), 1 vom: 01. Juni, Seite 57-61 volume:5 year:1972 number:1 day:01 month:06 pages:57-61 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Capillary Pressure Relative Viscosity Fuse Quartz Quartz Capillary Capillary Radius |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur |
authorswithroles_txt_mv |
Zheleznyi, B. V. @@aut@@ Zorin, Z. M. @@aut@@ Sobolev, W. D. @@aut@@ Churaev, N. V. @@aut@@ |
publishDateDaySort_date |
1972-06-01T00:00:00Z |
hierarchy_top_id |
129378666 |
dewey-sort |
3550 |
id |
OLC2061663532 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2061663532</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502165230.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1972 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF02634653</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2061663532</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF02634653-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">550</subfield><subfield code="a">600</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zheleznyi, B. 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">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">© International Association of Engineering Geology 1972</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></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Relative Viscosity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fuse Quartz</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Quartz Capillary</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Capillary Radius</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zorin, Z. M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sobolev, W. D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Churaev, N. V.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur</subfield><subfield code="d">Springer Berlin Heidelberg, 1970</subfield><subfield code="g">5(1972), 1 vom: 01. Juni, Seite 57-61</subfield><subfield code="w">(DE-627)129378666</subfield><subfield code="w">(DE-600)164473-7</subfield><subfield code="w">(DE-576)014761408</subfield><subfield code="x">0074-1612</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:5</subfield><subfield code="g">year:1972</subfield><subfield code="g">number:1</subfield><subfield code="g">day:01</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:57-61</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF02634653</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-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_30</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_2016</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">5</subfield><subfield code="j">1972</subfield><subfield code="e">1</subfield><subfield code="b">01</subfield><subfield code="c">06</subfield><subfield code="h">57-61</subfield></datafield></record></collection>
|
author |
Zheleznyi, B. V. |
spellingShingle |
Zheleznyi, B. V. ddc 550 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 |
authorStr |
Zheleznyi, B. V. |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)129378666 |
format |
Article |
dewey-ones |
550 - Earth sciences 600 - Technology |
delete_txt_mv |
keep |
author_role |
aut aut aut aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0074-1612 |
topic_title |
550 600 VZ Experimental study of properties of water in thin films and fine capillaries Capillary Pressure Relative Viscosity Fuse Quartz Quartz Capillary Capillary Radius |
topic |
ddc 550 misc Capillary Pressure misc Relative Viscosity misc Fuse Quartz misc Quartz Capillary misc Capillary Radius |
topic_unstemmed |
ddc 550 misc Capillary Pressure misc Relative Viscosity misc Fuse Quartz misc Quartz Capillary misc Capillary Radius |
topic_browse |
ddc 550 misc Capillary Pressure misc Relative Viscosity misc Fuse Quartz misc Quartz Capillary misc Capillary Radius |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur |
hierarchy_parent_id |
129378666 |
dewey-tens |
550 - Earth sciences & geology 600 - Technology |
hierarchy_top_title |
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)129378666 (DE-600)164473-7 (DE-576)014761408 |
title |
Experimental study of properties of water in thin films and fine capillaries |
ctrlnum |
(DE-627)OLC2061663532 (DE-He213)BF02634653-p |
title_full |
Experimental study of properties of water in thin films and fine capillaries |
author_sort |
Zheleznyi, B. V. |
journal |
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur |
journalStr |
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science 600 - Technology |
recordtype |
marc |
publishDateSort |
1972 |
contenttype_str_mv |
txt |
container_start_page |
57 |
author_browse |
Zheleznyi, B. V. Zorin, Z. M. Sobolev, W. D. Churaev, N. V. |
container_volume |
5 |
class |
550 600 VZ |
format_se |
Aufsätze |
author-letter |
Zheleznyi, B. V. |
doi_str_mv |
10.1007/BF02634653 |
dewey-full |
550 600 |
title_sort |
experimental study of properties of water in thin films and fine capillaries |
title_auth |
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. © International Association of Engineering Geology 1972 |
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. © International Association of Engineering Geology 1972 |
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. © International Association of Engineering Geology 1972 |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_30 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2016 GBV_ILN_4046 |
container_issue |
1 |
title_short |
Experimental study of properties of water in thin films and fine capillaries |
url |
https://doi.org/10.1007/BF02634653 |
remote_bool |
false |
author2 |
Zorin, Z. M. Sobolev, W. D. Churaev, N. V. |
author2Str |
Zorin, Z. M. Sobolev, W. D. Churaev, N. V. |
ppnlink |
129378666 |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/BF02634653 |
up_date |
2024-07-04T04:06:37.599Z |
_version_ |
1803619923510951936 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2061663532</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502165230.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1972 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF02634653</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2061663532</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF02634653-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">550</subfield><subfield code="a">600</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zheleznyi, B. 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">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">© International Association of Engineering Geology 1972</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></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Relative Viscosity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fuse Quartz</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Quartz Capillary</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Capillary Radius</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zorin, Z. M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sobolev, W. D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Churaev, N. V.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur</subfield><subfield code="d">Springer Berlin Heidelberg, 1970</subfield><subfield code="g">5(1972), 1 vom: 01. Juni, Seite 57-61</subfield><subfield code="w">(DE-627)129378666</subfield><subfield code="w">(DE-600)164473-7</subfield><subfield code="w">(DE-576)014761408</subfield><subfield code="x">0074-1612</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:5</subfield><subfield code="g">year:1972</subfield><subfield code="g">number:1</subfield><subfield code="g">day:01</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:57-61</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF02634653</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-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_30</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_2016</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">5</subfield><subfield code="j">1972</subfield><subfield code="e">1</subfield><subfield code="b">01</subfield><subfield code="c">06</subfield><subfield code="h">57-61</subfield></datafield></record></collection>
|
score |
7.3986187 |