PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions
• Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens.
Autor*in: |
You, Ruquan [verfasserIn] |
---|
Format: |
E-Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2017 |
---|
Schlagwörter: |
---|
Umfang: |
13 |
---|
Übergeordnetes Werk: |
Enthalten in: Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics - Radünz, William Corrêa ELSEVIER, 2020, design, processes, equipment, economics, Amsterdam [u.a.] |
---|---|
Übergeordnetes Werk: |
volume:123 ; year:2017 ; pages:1021-1033 ; extent:13 |
Links: |
---|
DOI / URN: |
10.1016/j.applthermaleng.2017.05.162 |
---|
Katalog-ID: |
ELV015382346 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | ELV015382346 | ||
003 | DE-627 | ||
005 | 20230623122308.0 | ||
007 | cr uuu---uuuuu | ||
008 | 180602s2017 xx |||||o 00| ||eng c | ||
024 | 7 | |a 10.1016/j.applthermaleng.2017.05.162 |2 doi | |
028 | 5 | 2 | |a GBV00000000000094A.pica |
035 | |a (DE-627)ELV015382346 | ||
035 | |a (ELSEVIER)S1359-4311(16)33687-0 | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | |a 690 | |
082 | 0 | 4 | |a 690 |q DE-600 |
082 | 0 | 4 | |a 530 |a 620 |q VZ |
084 | |a 52.56 |2 bkl | ||
100 | 1 | |a You, Ruquan |e verfasserin |4 aut | |
245 | 1 | 0 | |a PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions |
264 | 1 | |c 2017 | |
300 | |a 13 | ||
336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
337 | |a nicht spezifiziert |b z |2 rdamedia | ||
338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
520 | |a • Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens. | ||
650 | 7 | |a Turbulent flow |2 Elsevier | |
650 | 7 | |a Smooth channel |2 Elsevier | |
650 | 7 | |a Buoyancy force |2 Elsevier | |
650 | 7 | |a Flow dynamic |2 Elsevier | |
650 | 7 | |a Rotating channel |2 Elsevier | |
700 | 1 | |a Li, Haiwang |4 oth | |
700 | 1 | |a Tao, Zhi |4 oth | |
700 | 1 | |a Wei, Kuan |4 oth | |
700 | 1 | |a Xu, Guoqiang |4 oth | |
773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Radünz, William Corrêa ELSEVIER |t Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics |d 2020 |d design, processes, equipment, economics |g Amsterdam [u.a.] |w (DE-627)ELV003905551 |
773 | 1 | 8 | |g volume:123 |g year:2017 |g pages:1021-1033 |g extent:13 |
856 | 4 | 0 | |u https://doi.org/10.1016/j.applthermaleng.2017.05.162 |3 Volltext |
912 | |a GBV_USEFLAG_U | ||
912 | |a GBV_ELV | ||
912 | |a SYSFLAG_U | ||
936 | b | k | |a 52.56 |j Regenerative Energieformen |j alternative Energieformen |q VZ |
951 | |a AR | ||
952 | |d 123 |j 2017 |h 1021-1033 |g 13 | ||
953 | |2 045F |a 690 |
author_variant |
r y ry |
---|---|
matchkey_str |
youruquanlihaiwangtaozhiweikuanxuguoqian:2017----:imaueetotruetlwiamohhnewtteetdona |
hierarchy_sort_str |
2017 |
bklnumber |
52.56 |
publishDate |
2017 |
allfields |
10.1016/j.applthermaleng.2017.05.162 doi GBV00000000000094A.pica (DE-627)ELV015382346 (ELSEVIER)S1359-4311(16)33687-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 530 620 VZ 52.56 bkl You, Ruquan verfasserin aut PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens. Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel Elsevier Li, Haiwang oth Tao, Zhi oth Wei, Kuan oth Xu, Guoqiang oth Enthalten in Elsevier Science Radünz, William Corrêa ELSEVIER Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics 2020 design, processes, equipment, economics Amsterdam [u.a.] (DE-627)ELV003905551 volume:123 year:2017 pages:1021-1033 extent:13 https://doi.org/10.1016/j.applthermaleng.2017.05.162 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.56 Regenerative Energieformen alternative Energieformen VZ AR 123 2017 1021-1033 13 045F 690 |
spelling |
10.1016/j.applthermaleng.2017.05.162 doi GBV00000000000094A.pica (DE-627)ELV015382346 (ELSEVIER)S1359-4311(16)33687-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 530 620 VZ 52.56 bkl You, Ruquan verfasserin aut PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens. Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel Elsevier Li, Haiwang oth Tao, Zhi oth Wei, Kuan oth Xu, Guoqiang oth Enthalten in Elsevier Science Radünz, William Corrêa ELSEVIER Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics 2020 design, processes, equipment, economics Amsterdam [u.a.] (DE-627)ELV003905551 volume:123 year:2017 pages:1021-1033 extent:13 https://doi.org/10.1016/j.applthermaleng.2017.05.162 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.56 Regenerative Energieformen alternative Energieformen VZ AR 123 2017 1021-1033 13 045F 690 |
allfields_unstemmed |
10.1016/j.applthermaleng.2017.05.162 doi GBV00000000000094A.pica (DE-627)ELV015382346 (ELSEVIER)S1359-4311(16)33687-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 530 620 VZ 52.56 bkl You, Ruquan verfasserin aut PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens. Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel Elsevier Li, Haiwang oth Tao, Zhi oth Wei, Kuan oth Xu, Guoqiang oth Enthalten in Elsevier Science Radünz, William Corrêa ELSEVIER Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics 2020 design, processes, equipment, economics Amsterdam [u.a.] (DE-627)ELV003905551 volume:123 year:2017 pages:1021-1033 extent:13 https://doi.org/10.1016/j.applthermaleng.2017.05.162 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.56 Regenerative Energieformen alternative Energieformen VZ AR 123 2017 1021-1033 13 045F 690 |
allfieldsGer |
10.1016/j.applthermaleng.2017.05.162 doi GBV00000000000094A.pica (DE-627)ELV015382346 (ELSEVIER)S1359-4311(16)33687-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 530 620 VZ 52.56 bkl You, Ruquan verfasserin aut PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens. Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel Elsevier Li, Haiwang oth Tao, Zhi oth Wei, Kuan oth Xu, Guoqiang oth Enthalten in Elsevier Science Radünz, William Corrêa ELSEVIER Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics 2020 design, processes, equipment, economics Amsterdam [u.a.] (DE-627)ELV003905551 volume:123 year:2017 pages:1021-1033 extent:13 https://doi.org/10.1016/j.applthermaleng.2017.05.162 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.56 Regenerative Energieformen alternative Energieformen VZ AR 123 2017 1021-1033 13 045F 690 |
allfieldsSound |
10.1016/j.applthermaleng.2017.05.162 doi GBV00000000000094A.pica (DE-627)ELV015382346 (ELSEVIER)S1359-4311(16)33687-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 530 620 VZ 52.56 bkl You, Ruquan verfasserin aut PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens. Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel Elsevier Li, Haiwang oth Tao, Zhi oth Wei, Kuan oth Xu, Guoqiang oth Enthalten in Elsevier Science Radünz, William Corrêa ELSEVIER Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics 2020 design, processes, equipment, economics Amsterdam [u.a.] (DE-627)ELV003905551 volume:123 year:2017 pages:1021-1033 extent:13 https://doi.org/10.1016/j.applthermaleng.2017.05.162 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.56 Regenerative Energieformen alternative Energieformen VZ AR 123 2017 1021-1033 13 045F 690 |
language |
English |
source |
Enthalten in Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics Amsterdam [u.a.] volume:123 year:2017 pages:1021-1033 extent:13 |
sourceStr |
Enthalten in Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics Amsterdam [u.a.] volume:123 year:2017 pages:1021-1033 extent:13 |
format_phy_str_mv |
Article |
bklname |
Regenerative Energieformen alternative Energieformen |
institution |
findex.gbv.de |
topic_facet |
Turbulent flow Smooth channel Buoyancy force Flow dynamic Rotating channel |
dewey-raw |
690 |
isfreeaccess_bool |
false |
container_title |
Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics |
authorswithroles_txt_mv |
You, Ruquan @@aut@@ Li, Haiwang @@oth@@ Tao, Zhi @@oth@@ Wei, Kuan @@oth@@ Xu, Guoqiang @@oth@@ |
publishDateDaySort_date |
2017-01-01T00:00:00Z |
hierarchy_top_id |
ELV003905551 |
dewey-sort |
3690 |
id |
ELV015382346 |
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">ELV015382346</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230623122308.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180602s2017 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.applthermaleng.2017.05.162</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBV00000000000094A.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV015382346</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S1359-4311(16)33687-0</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=" "><subfield code="a">690</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">690</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">530</subfield><subfield code="a">620</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">52.56</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">You, Ruquan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">13</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">• Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Turbulent flow</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Smooth channel</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Buoyancy force</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Flow dynamic</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Rotating channel</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Haiwang</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tao, Zhi</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wei, Kuan</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Guoqiang</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Radünz, William Corrêa ELSEVIER</subfield><subfield code="t">Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics</subfield><subfield code="d">2020</subfield><subfield code="d">design, processes, equipment, economics</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV003905551</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:123</subfield><subfield code="g">year:2017</subfield><subfield code="g">pages:1021-1033</subfield><subfield code="g">extent:13</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.applthermaleng.2017.05.162</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">52.56</subfield><subfield code="j">Regenerative Energieformen</subfield><subfield code="j">alternative Energieformen</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">123</subfield><subfield code="j">2017</subfield><subfield code="h">1021-1033</subfield><subfield code="g">13</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">690</subfield></datafield></record></collection>
|
author |
You, Ruquan |
spellingShingle |
You, Ruquan ddc 690 ddc 530 bkl 52.56 Elsevier Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions |
authorStr |
You, Ruquan |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)ELV003905551 |
format |
electronic Article |
dewey-ones |
690 - Buildings 530 - Physics 620 - Engineering & allied operations |
delete_txt_mv |
keep |
author_role |
aut |
collection |
elsevier |
remote_str |
true |
illustrated |
Not Illustrated |
topic_title |
690 690 DE-600 530 620 VZ 52.56 bkl PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel Elsevier |
topic |
ddc 690 ddc 530 bkl 52.56 Elsevier Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel |
topic_unstemmed |
ddc 690 ddc 530 bkl 52.56 Elsevier Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel |
topic_browse |
ddc 690 ddc 530 bkl 52.56 Elsevier Turbulent flow Elsevier Smooth channel Elsevier Buoyancy force Elsevier Flow dynamic Elsevier Rotating channel |
format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
zu |
author2_variant |
h l hl z t zt k w kw g x gx |
hierarchy_parent_title |
Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics |
hierarchy_parent_id |
ELV003905551 |
dewey-tens |
690 - Building & construction 530 - Physics 620 - Engineering |
hierarchy_top_title |
Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)ELV003905551 |
title |
PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions |
ctrlnum |
(DE-627)ELV015382346 (ELSEVIER)S1359-4311(16)33687-0 |
title_full |
PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions |
author_sort |
You, Ruquan |
journal |
Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics |
journalStr |
Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
600 - Technology 500 - Science |
recordtype |
marc |
publishDateSort |
2017 |
contenttype_str_mv |
zzz |
container_start_page |
1021 |
author_browse |
You, Ruquan |
container_volume |
123 |
physical |
13 |
class |
690 690 DE-600 530 620 VZ 52.56 bkl |
format_se |
Elektronische Aufsätze |
author-letter |
You, Ruquan |
doi_str_mv |
10.1016/j.applthermaleng.2017.05.162 |
dewey-full |
690 530 620 |
title_sort |
piv measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions |
title_auth |
PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions |
abstract |
• Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens. |
abstractGer |
• Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens. |
abstract_unstemmed |
• Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens. |
collection_details |
GBV_USEFLAG_U GBV_ELV SYSFLAG_U |
title_short |
PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions |
url |
https://doi.org/10.1016/j.applthermaleng.2017.05.162 |
remote_bool |
true |
author2 |
Li, Haiwang Tao, Zhi Wei, Kuan Xu, Guoqiang |
author2Str |
Li, Haiwang Tao, Zhi Wei, Kuan Xu, Guoqiang |
ppnlink |
ELV003905551 |
mediatype_str_mv |
z |
isOA_txt |
false |
hochschulschrift_bool |
false |
author2_role |
oth oth oth oth |
doi_str |
10.1016/j.applthermaleng.2017.05.162 |
up_date |
2024-07-06T17:34:24.102Z |
_version_ |
1803851938245115904 |
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">ELV015382346</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230623122308.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180602s2017 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.applthermaleng.2017.05.162</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBV00000000000094A.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV015382346</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S1359-4311(16)33687-0</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=" "><subfield code="a">690</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">690</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">530</subfield><subfield code="a">620</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">52.56</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">You, Ruquan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">PIV measurements of turbulent flows in a smooth channel with the heated boundary under rotation conditions</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">13</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">• Velocity profile and Reynolds shear stress are shown by PIV with four wall heated. • Separated flow is captured for the first time on the leading side. • A leap increase of Reynolds shear stress is generated when separated flow happens.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Turbulent flow</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Smooth channel</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Buoyancy force</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Flow dynamic</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Rotating channel</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Haiwang</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tao, Zhi</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wei, Kuan</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Guoqiang</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Radünz, William Corrêa ELSEVIER</subfield><subfield code="t">Wind resource mapping and energy estimation in complex terrain: A framework based on field observations and computational fluid dynamics</subfield><subfield code="d">2020</subfield><subfield code="d">design, processes, equipment, economics</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV003905551</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:123</subfield><subfield code="g">year:2017</subfield><subfield code="g">pages:1021-1033</subfield><subfield code="g">extent:13</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.applthermaleng.2017.05.162</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">52.56</subfield><subfield code="j">Regenerative Energieformen</subfield><subfield code="j">alternative Energieformen</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">123</subfield><subfield code="j">2017</subfield><subfield code="h">1021-1033</subfield><subfield code="g">13</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">690</subfield></datafield></record></collection>
|
score |
7.4000893 |