The investigation of static and dynamic capillary by water absorption in porous building stones under normal and salty water conditions
The presence of water in building stones is one of the main factors in deterioration. Capillary rise is the most usual mechanism of water penetration into building materials. In this study, the kinetics of the capillary rise phenomenon was studied for three porous building stones: two tuff stones an...
Gespeichert in:
Veröffentlicht in: | Environmental earth sciences 2016-02, Vol.75 (4), p.1, Article 307 |
---|---|
Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | |
---|---|
container_issue | 4 |
container_start_page | 1 |
container_title | Environmental earth sciences |
container_volume | 75 |
creator | Çelik, Mustafa Yavuz Kaçmaz, Ahmet Uğur |
description | The presence of water in building stones is one of the main factors in deterioration. Capillary rise is the most usual mechanism of water penetration into building materials. In this study, the kinetics of the capillary rise phenomenon was studied for three porous building stones: two tuff stones and andesite. For each of the examined natural stones the capillary water absorption, pore size distribution, mineralogical–petrographic (optical microscope, XRD, SEM), chemical (XRF) and mechanical–physical properties were determined. The mechanism of capillary water absorption depends mainly on the pore size and the shape of the pore system. The pore size distribution was determined by means of high pressure mercury porosimetry. İscehisar andesite, Ayazini tuffs and Seydiler tuffs have pore sizes ranging from about 0.01 to 10, 0.01 to 20 and 0.01 to 4 µm, respectively. The capillary water absorption of the building stones was determined on the basis of TS EN 1925. The effects were analyzed with a static and dynamic capillary by water absorption under normal and salty water conditions of porous building stones. Water content was determined by weighing after 1, 3, 5, 10, 15, 30, 60, 480, 1440 min until the free saturation was reached and the liquid uptake stopped. The results indicated considerable differences in the water absorption shown as a function of elapsed time. NaCl crystals are observed under SEM in pores and surface of the tested stones. According to the results, capillary absorption of salty water value is bigger than pure water in all stones at the end of test. It could be shown that primarily moisture properties, i.e., capillary and sorptive water uptake and salt crystallisation can be addressed to the deterioration processes. |
doi_str_mv | 10.1007/s12665-015-5132-x |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1772363429</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>3981594811</sourcerecordid><originalsourceid>FETCH-LOGICAL-a339t-58411de82d83cd384fff5e9de20e01e696db4231149312271c519ebcef8a060f3</originalsourceid><addsrcrecordid>eNp1kM1OwzAQhC0EElXpA3CzxDngtRMnPqKKP6kSl3K2nNgprlI72Am0T8Br47aAuLCXncPMt9pB6BLINRBS3kSgnBcZgSIrgNFse4ImUHGecSrE6a-uyDmaxbgmaRgwQfgEfS5fDbbu3cTBrtRgvcO-xXFIssHKaax3Tm2SblRvu06FHa53-EMNJmBVRx_6Q8Y63Pvgx4jr0XbaulVieGciHp1OVufDRnUHYFTd8ENovNN2D4gX6KxVXTSz7z1FL_d3y_ljtnh-eJrfLjLFmBiyosoBtKmorlijWZW3bVsYoQ0lhoDhgus6pwwgFwwoLaEpQJi6MW2lCCctm6KrI7cP_m1MX8u1H4NLJyWUJWWc5VQkFxxdTfAxBtPKPthNel4CkfvK5bFymSqX-8rlNmXoMROT161M-EP-N_QFqNyHFw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1772363429</pqid></control><display><type>article</type><title>The investigation of static and dynamic capillary by water absorption in porous building stones under normal and salty water conditions</title><source>SpringerNature Journals</source><creator>Çelik, Mustafa Yavuz ; Kaçmaz, Ahmet Uğur</creator><creatorcontrib>Çelik, Mustafa Yavuz ; Kaçmaz, Ahmet Uğur</creatorcontrib><description>The presence of water in building stones is one of the main factors in deterioration. Capillary rise is the most usual mechanism of water penetration into building materials. In this study, the kinetics of the capillary rise phenomenon was studied for three porous building stones: two tuff stones and andesite. For each of the examined natural stones the capillary water absorption, pore size distribution, mineralogical–petrographic (optical microscope, XRD, SEM), chemical (XRF) and mechanical–physical properties were determined. The mechanism of capillary water absorption depends mainly on the pore size and the shape of the pore system. The pore size distribution was determined by means of high pressure mercury porosimetry. İscehisar andesite, Ayazini tuffs and Seydiler tuffs have pore sizes ranging from about 0.01 to 10, 0.01 to 20 and 0.01 to 4 µm, respectively. The capillary water absorption of the building stones was determined on the basis of TS EN 1925. The effects were analyzed with a static and dynamic capillary by water absorption under normal and salty water conditions of porous building stones. Water content was determined by weighing after 1, 3, 5, 10, 15, 30, 60, 480, 1440 min until the free saturation was reached and the liquid uptake stopped. The results indicated considerable differences in the water absorption shown as a function of elapsed time. NaCl crystals are observed under SEM in pores and surface of the tested stones. According to the results, capillary absorption of salty water value is bigger than pure water in all stones at the end of test. It could be shown that primarily moisture properties, i.e., capillary and sorptive water uptake and salt crystallisation can be addressed to the deterioration processes.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-015-5132-x</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Absorption ; Biogeosciences ; Building materials ; Capillary water ; Crystals ; Earth and Environmental Science ; Earth Sciences ; Environmental Science and Engineering ; Geochemistry ; Geology ; High pressure ; Hydrology/Water Resources ; Mercury ; Moisture absorption ; Original Article ; Physical properties ; Pore size ; Porous materials ; Rocks ; Sodium chloride ; Terrestrial Pollution ; Water ; Water content ; Water uptake</subject><ispartof>Environmental earth sciences, 2016-02, Vol.75 (4), p.1, Article 307</ispartof><rights>Springer-Verlag Berlin Heidelberg 2016</rights><rights>Environmental Earth Sciences is a copyright of Springer, 2016.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-58411de82d83cd384fff5e9de20e01e696db4231149312271c519ebcef8a060f3</citedby><cites>FETCH-LOGICAL-a339t-58411de82d83cd384fff5e9de20e01e696db4231149312271c519ebcef8a060f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12665-015-5132-x$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-015-5132-x$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Çelik, Mustafa Yavuz</creatorcontrib><creatorcontrib>Kaçmaz, Ahmet Uğur</creatorcontrib><title>The investigation of static and dynamic capillary by water absorption in porous building stones under normal and salty water conditions</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>The presence of water in building stones is one of the main factors in deterioration. Capillary rise is the most usual mechanism of water penetration into building materials. In this study, the kinetics of the capillary rise phenomenon was studied for three porous building stones: two tuff stones and andesite. For each of the examined natural stones the capillary water absorption, pore size distribution, mineralogical–petrographic (optical microscope, XRD, SEM), chemical (XRF) and mechanical–physical properties were determined. The mechanism of capillary water absorption depends mainly on the pore size and the shape of the pore system. The pore size distribution was determined by means of high pressure mercury porosimetry. İscehisar andesite, Ayazini tuffs and Seydiler tuffs have pore sizes ranging from about 0.01 to 10, 0.01 to 20 and 0.01 to 4 µm, respectively. The capillary water absorption of the building stones was determined on the basis of TS EN 1925. The effects were analyzed with a static and dynamic capillary by water absorption under normal and salty water conditions of porous building stones. Water content was determined by weighing after 1, 3, 5, 10, 15, 30, 60, 480, 1440 min until the free saturation was reached and the liquid uptake stopped. The results indicated considerable differences in the water absorption shown as a function of elapsed time. NaCl crystals are observed under SEM in pores and surface of the tested stones. According to the results, capillary absorption of salty water value is bigger than pure water in all stones at the end of test. It could be shown that primarily moisture properties, i.e., capillary and sorptive water uptake and salt crystallisation can be addressed to the deterioration processes.</description><subject>Absorption</subject><subject>Biogeosciences</subject><subject>Building materials</subject><subject>Capillary water</subject><subject>Crystals</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental Science and Engineering</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>High pressure</subject><subject>Hydrology/Water Resources</subject><subject>Mercury</subject><subject>Moisture absorption</subject><subject>Original Article</subject><subject>Physical properties</subject><subject>Pore size</subject><subject>Porous materials</subject><subject>Rocks</subject><subject>Sodium chloride</subject><subject>Terrestrial Pollution</subject><subject>Water</subject><subject>Water content</subject><subject>Water uptake</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kM1OwzAQhC0EElXpA3CzxDngtRMnPqKKP6kSl3K2nNgprlI72Am0T8Br47aAuLCXncPMt9pB6BLINRBS3kSgnBcZgSIrgNFse4ImUHGecSrE6a-uyDmaxbgmaRgwQfgEfS5fDbbu3cTBrtRgvcO-xXFIssHKaax3Tm2SblRvu06FHa53-EMNJmBVRx_6Q8Y63Pvgx4jr0XbaulVieGciHp1OVufDRnUHYFTd8ENovNN2D4gX6KxVXTSz7z1FL_d3y_ljtnh-eJrfLjLFmBiyosoBtKmorlijWZW3bVsYoQ0lhoDhgus6pwwgFwwoLaEpQJi6MW2lCCctm6KrI7cP_m1MX8u1H4NLJyWUJWWc5VQkFxxdTfAxBtPKPthNel4CkfvK5bFymSqX-8rlNmXoMROT161M-EP-N_QFqNyHFw</recordid><startdate>20160201</startdate><enddate>20160201</enddate><creator>Çelik, Mustafa Yavuz</creator><creator>Kaçmaz, Ahmet Uğur</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>20160201</creationdate><title>The investigation of static and dynamic capillary by water absorption in porous building stones under normal and salty water conditions</title><author>Çelik, Mustafa Yavuz ; Kaçmaz, Ahmet Uğur</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-58411de82d83cd384fff5e9de20e01e696db4231149312271c519ebcef8a060f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Absorption</topic><topic>Biogeosciences</topic><topic>Building materials</topic><topic>Capillary water</topic><topic>Crystals</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Environmental Science and Engineering</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>High pressure</topic><topic>Hydrology/Water Resources</topic><topic>Mercury</topic><topic>Moisture absorption</topic><topic>Original Article</topic><topic>Physical properties</topic><topic>Pore size</topic><topic>Porous materials</topic><topic>Rocks</topic><topic>Sodium chloride</topic><topic>Terrestrial Pollution</topic><topic>Water</topic><topic>Water content</topic><topic>Water uptake</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Çelik, Mustafa Yavuz</creatorcontrib><creatorcontrib>Kaçmaz, Ahmet Uğur</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Environmental earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Çelik, Mustafa Yavuz</au><au>Kaçmaz, Ahmet Uğur</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The investigation of static and dynamic capillary by water absorption in porous building stones under normal and salty water conditions</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2016-02-01</date><risdate>2016</risdate><volume>75</volume><issue>4</issue><spage>1</spage><pages>1-</pages><artnum>307</artnum><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>The presence of water in building stones is one of the main factors in deterioration. Capillary rise is the most usual mechanism of water penetration into building materials. In this study, the kinetics of the capillary rise phenomenon was studied for three porous building stones: two tuff stones and andesite. For each of the examined natural stones the capillary water absorption, pore size distribution, mineralogical–petrographic (optical microscope, XRD, SEM), chemical (XRF) and mechanical–physical properties were determined. The mechanism of capillary water absorption depends mainly on the pore size and the shape of the pore system. The pore size distribution was determined by means of high pressure mercury porosimetry. İscehisar andesite, Ayazini tuffs and Seydiler tuffs have pore sizes ranging from about 0.01 to 10, 0.01 to 20 and 0.01 to 4 µm, respectively. The capillary water absorption of the building stones was determined on the basis of TS EN 1925. The effects were analyzed with a static and dynamic capillary by water absorption under normal and salty water conditions of porous building stones. Water content was determined by weighing after 1, 3, 5, 10, 15, 30, 60, 480, 1440 min until the free saturation was reached and the liquid uptake stopped. The results indicated considerable differences in the water absorption shown as a function of elapsed time. NaCl crystals are observed under SEM in pores and surface of the tested stones. According to the results, capillary absorption of salty water value is bigger than pure water in all stones at the end of test. It could be shown that primarily moisture properties, i.e., capillary and sorptive water uptake and salt crystallisation can be addressed to the deterioration processes.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12665-015-5132-x</doi></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1866-6280 |
ispartof | Environmental earth sciences, 2016-02, Vol.75 (4), p.1, Article 307 |
issn | 1866-6280 1866-6299 |
language | eng |
recordid | cdi_proquest_journals_1772363429 |
source | SpringerNature Journals |
subjects | Absorption Biogeosciences Building materials Capillary water Crystals Earth and Environmental Science Earth Sciences Environmental Science and Engineering Geochemistry Geology High pressure Hydrology/Water Resources Mercury Moisture absorption Original Article Physical properties Pore size Porous materials Rocks Sodium chloride Terrestrial Pollution Water Water content Water uptake |
title | The investigation of static and dynamic capillary by water absorption in porous building stones under normal and salty water conditions |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-25T03%3A52%3A06IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20investigation%20of%20static%20and%20dynamic%20capillary%20by%20water%20absorption%20in%20porous%20building%20stones%20under%20normal%20and%20salty%20water%20conditions&rft.jtitle=Environmental%20earth%20sciences&rft.au=%C3%87elik,%20Mustafa%20Yavuz&rft.date=2016-02-01&rft.volume=75&rft.issue=4&rft.spage=1&rft.pages=1-&rft.artnum=307&rft.issn=1866-6280&rft.eissn=1866-6299&rft_id=info:doi/10.1007/s12665-015-5132-x&rft_dat=%3Cproquest_cross%3E3981594811%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1772363429&rft_id=info:pmid/&rfr_iscdi=true |