SU(3) Latent Heat and Surface Tension from Tree Level and Tadpole Improved Actions
Phys.Lett. B390 (1997) 268-274 We analyze the latent heat and surface tension at the SU(3) deconfinement phase transition with tree level and tadpole improved Symanzik actions on lattices with temporal extent $N_\tau = 3$ and 4 and spatial extent $N_\sigma/ N_\tau = 4$, 6 and 8. In comparison to the...
Gespeichert in:
Hauptverfasser: | , , |
---|---|
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext bestellen |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | |
---|---|
container_issue | |
container_start_page | |
container_title | |
container_volume | |
creator | Beinlich, B Karsch, F Peikert, A |
description | Phys.Lett. B390 (1997) 268-274 We analyze the latent heat and surface tension at the SU(3) deconfinement
phase transition with tree level and tadpole improved Symanzik actions on
lattices with temporal extent $N_\tau = 3$ and 4 and spatial extent $N_\sigma/
N_\tau = 4$, 6 and 8. In comparison to the standard Wilson action we do find a
drastic reduction of cut-off effects already with tree level improved actions.
On lattices with temporal extent $N_\tau=4$ results for the surface tension and
latent heat obtained with a tree level improved action agree well with those
obtained with a tadpole improved action. A comparison with $N_\tau=3$
calculations, however, shows that results obtained with tadpole action remain
unaffected by cut-off effects even on this coarse lattice, while the tree level
action becomes sensitive to the cut-off. For the surface tension and latent
heat we find $\sigma_I/ T_c^3 = 0.0155~(16)$ and $\Delta\epsilon/T_c^4 =
1.40~(9)$, respectively. |
doi_str_mv | 10.48550/arxiv.hep-lat/9608141 |
format | Article |
fullrecord | <record><control><sourceid>arxiv_GOX</sourceid><recordid>TN_cdi_arxiv_primary_hep_lat_9608141</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>hep_lat_9608141</sourcerecordid><originalsourceid>FETCH-arxiv_primary_hep_lat_96081413</originalsourceid><addsrcrecordid>eNqNzr0KwjAUQOEsDqK-gtzBQYf-0VbqKKJU6GTjHC7tLRbSJKSx6NtbSh_A6Sxn-BjbRqGfZGkaBmg_7eC_yHgSXXA6hlmUREv2KJ_7-AAFOlIOckIHqGoo37bBioCT6lutoLG6A26JoKCB5PRwrI2WBPfOWD1QDefKjW-_ZosGZU-buSu2u135JfcmgjC27dB-xUgRI0XMlPjP7QcDN0Lz</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>SU(3) Latent Heat and Surface Tension from Tree Level and Tadpole Improved Actions</title><source>arXiv.org</source><creator>Beinlich, B ; Karsch, F ; Peikert, A</creator><creatorcontrib>Beinlich, B ; Karsch, F ; Peikert, A</creatorcontrib><description>Phys.Lett. B390 (1997) 268-274 We analyze the latent heat and surface tension at the SU(3) deconfinement
phase transition with tree level and tadpole improved Symanzik actions on
lattices with temporal extent $N_\tau = 3$ and 4 and spatial extent $N_\sigma/
N_\tau = 4$, 6 and 8. In comparison to the standard Wilson action we do find a
drastic reduction of cut-off effects already with tree level improved actions.
On lattices with temporal extent $N_\tau=4$ results for the surface tension and
latent heat obtained with a tree level improved action agree well with those
obtained with a tadpole improved action. A comparison with $N_\tau=3$
calculations, however, shows that results obtained with tadpole action remain
unaffected by cut-off effects even on this coarse lattice, while the tree level
action becomes sensitive to the cut-off. For the surface tension and latent
heat we find $\sigma_I/ T_c^3 = 0.0155~(16)$ and $\Delta\epsilon/T_c^4 =
1.40~(9)$, respectively.</description><identifier>DOI: 10.48550/arxiv.hep-lat/9608141</identifier><language>eng</language><subject>Physics - High Energy Physics - Lattice</subject><creationdate>1996-08</creationdate><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>228,230,780,885</link.rule.ids><linktorsrc>$$Uhttps://arxiv.org/abs/hep-lat/9608141$$EView_record_in_Cornell_University$$FView_record_in_$$GCornell_University$$Hfree_for_read</linktorsrc><backlink>$$Uhttps://doi.org/10.1016/S0370-2693(96)01401-3$$DView published paper (Access to full text may be restricted)$$Hfree_for_read</backlink><backlink>$$Uhttps://doi.org/10.48550/arXiv.hep-lat/9608141$$DView paper in arXiv$$Hfree_for_read</backlink></links><search><creatorcontrib>Beinlich, B</creatorcontrib><creatorcontrib>Karsch, F</creatorcontrib><creatorcontrib>Peikert, A</creatorcontrib><title>SU(3) Latent Heat and Surface Tension from Tree Level and Tadpole Improved Actions</title><description>Phys.Lett. B390 (1997) 268-274 We analyze the latent heat and surface tension at the SU(3) deconfinement
phase transition with tree level and tadpole improved Symanzik actions on
lattices with temporal extent $N_\tau = 3$ and 4 and spatial extent $N_\sigma/
N_\tau = 4$, 6 and 8. In comparison to the standard Wilson action we do find a
drastic reduction of cut-off effects already with tree level improved actions.
On lattices with temporal extent $N_\tau=4$ results for the surface tension and
latent heat obtained with a tree level improved action agree well with those
obtained with a tadpole improved action. A comparison with $N_\tau=3$
calculations, however, shows that results obtained with tadpole action remain
unaffected by cut-off effects even on this coarse lattice, while the tree level
action becomes sensitive to the cut-off. For the surface tension and latent
heat we find $\sigma_I/ T_c^3 = 0.0155~(16)$ and $\Delta\epsilon/T_c^4 =
1.40~(9)$, respectively.</description><subject>Physics - High Energy Physics - Lattice</subject><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1996</creationdate><recordtype>article</recordtype><sourceid>GOX</sourceid><recordid>eNqNzr0KwjAUQOEsDqK-gtzBQYf-0VbqKKJU6GTjHC7tLRbSJKSx6NtbSh_A6Sxn-BjbRqGfZGkaBmg_7eC_yHgSXXA6hlmUREv2KJ_7-AAFOlIOckIHqGoo37bBioCT6lutoLG6A26JoKCB5PRwrI2WBPfOWD1QDefKjW-_ZosGZU-buSu2u135JfcmgjC27dB-xUgRI0XMlPjP7QcDN0Lz</recordid><startdate>19960827</startdate><enddate>19960827</enddate><creator>Beinlich, B</creator><creator>Karsch, F</creator><creator>Peikert, A</creator><scope>GOX</scope></search><sort><creationdate>19960827</creationdate><title>SU(3) Latent Heat and Surface Tension from Tree Level and Tadpole Improved Actions</title><author>Beinlich, B ; Karsch, F ; Peikert, A</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-arxiv_primary_hep_lat_96081413</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1996</creationdate><topic>Physics - High Energy Physics - Lattice</topic><toplevel>online_resources</toplevel><creatorcontrib>Beinlich, B</creatorcontrib><creatorcontrib>Karsch, F</creatorcontrib><creatorcontrib>Peikert, A</creatorcontrib><collection>arXiv.org</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Beinlich, B</au><au>Karsch, F</au><au>Peikert, A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>SU(3) Latent Heat and Surface Tension from Tree Level and Tadpole Improved Actions</atitle><date>1996-08-27</date><risdate>1996</risdate><abstract>Phys.Lett. B390 (1997) 268-274 We analyze the latent heat and surface tension at the SU(3) deconfinement
phase transition with tree level and tadpole improved Symanzik actions on
lattices with temporal extent $N_\tau = 3$ and 4 and spatial extent $N_\sigma/
N_\tau = 4$, 6 and 8. In comparison to the standard Wilson action we do find a
drastic reduction of cut-off effects already with tree level improved actions.
On lattices with temporal extent $N_\tau=4$ results for the surface tension and
latent heat obtained with a tree level improved action agree well with those
obtained with a tadpole improved action. A comparison with $N_\tau=3$
calculations, however, shows that results obtained with tadpole action remain
unaffected by cut-off effects even on this coarse lattice, while the tree level
action becomes sensitive to the cut-off. For the surface tension and latent
heat we find $\sigma_I/ T_c^3 = 0.0155~(16)$ and $\Delta\epsilon/T_c^4 =
1.40~(9)$, respectively.</abstract><doi>10.48550/arxiv.hep-lat/9608141</doi><oa>free_for_read</oa></addata></record> |
fulltext | fulltext_linktorsrc |
identifier | DOI: 10.48550/arxiv.hep-lat/9608141 |
ispartof | |
issn | |
language | eng |
recordid | cdi_arxiv_primary_hep_lat_9608141 |
source | arXiv.org |
subjects | Physics - High Energy Physics - Lattice |
title | SU(3) Latent Heat and Surface Tension from Tree Level and Tadpole Improved Actions |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-19T11%3A47%3A13IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-arxiv_GOX&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=SU(3)%20Latent%20Heat%20and%20Surface%20Tension%20from%20Tree%20Level%20and%20Tadpole%20Improved%20Actions&rft.au=Beinlich,%20B&rft.date=1996-08-27&rft_id=info:doi/10.48550/arxiv.hep-lat/9608141&rft_dat=%3Carxiv_GOX%3Ehep_lat_9608141%3C/arxiv_GOX%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true |