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Disaster Mechanism and Frost Heave Effect of Railway Tunnel Induced by Drainage System Failure in High Latitude Cold Region
In this study, temperature monitoring and freezing disaster investigation in winter were conducted in three high latitude cold regional tunnels of Northeast China. Observations indicate that the air temperature in the tunnel middle section and the deep buried central drainage pipe remains stable at...
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Published in: | KSCE journal of civil engineering 2024, 28(10), , pp.4190-4213 |
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container_title | KSCE journal of civil engineering |
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creator | Zhou, Feicong Xie, Shenghao Wang, Lei Ma, Zhifu Zhou, Ping Jiang, Yifan Chen, Shougen Wang, Zhijie |
description | In this study, temperature monitoring and freezing disaster investigation in winter were conducted in three high latitude cold regional tunnels of Northeast China. Observations indicate that the air temperature in the tunnel middle section and the deep buried central drainage pipe remains stable at 0–5°C, while at the entrance section and the side ditch, it fluctuates around −15°C for about 2 months. Consequently, warm water from the middle section supplies both ends of the tunnel, making the entrance section drainage system prone to ice jams and freezing damage. Field investigation reveals 5 types of freezing-induced catastrophic behavior in tunnel drainage systems. In addition, frost heave effects from drainage system failure are simulated, showing that the lining compressive stress due to frost heave of drainage system is about 450 kPa, which is 200% of the surrounding rock frost heave. Moreover, the tensile stress due to frost heave of the side wall crack seepage or cavity water is the most significant, followed by the arch springing, then the hance, and finally the vault. Finally, consideration of the frost heave effect induced by drainage system is crucial for ensuring tunnel operation safety in high latitude cold regions. |
doi_str_mv | 10.1007/s12205-024-5458-6 |
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Observations indicate that the air temperature in the tunnel middle section and the deep buried central drainage pipe remains stable at 0–5°C, while at the entrance section and the side ditch, it fluctuates around −15°C for about 2 months. Consequently, warm water from the middle section supplies both ends of the tunnel, making the entrance section drainage system prone to ice jams and freezing damage. Field investigation reveals 5 types of freezing-induced catastrophic behavior in tunnel drainage systems. In addition, frost heave effects from drainage system failure are simulated, showing that the lining compressive stress due to frost heave of drainage system is about 450 kPa, which is 200% of the surrounding rock frost heave. Moreover, the tensile stress due to frost heave of the side wall crack seepage or cavity water is the most significant, followed by the arch springing, then the hance, and finally the vault. 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Observations indicate that the air temperature in the tunnel middle section and the deep buried central drainage pipe remains stable at 0–5°C, while at the entrance section and the side ditch, it fluctuates around −15°C for about 2 months. Consequently, warm water from the middle section supplies both ends of the tunnel, making the entrance section drainage system prone to ice jams and freezing damage. Field investigation reveals 5 types of freezing-induced catastrophic behavior in tunnel drainage systems. In addition, frost heave effects from drainage system failure are simulated, showing that the lining compressive stress due to frost heave of drainage system is about 450 kPa, which is 200% of the surrounding rock frost heave. Moreover, the tensile stress due to frost heave of the side wall crack seepage or cavity water is the most significant, followed by the arch springing, then the hance, and finally the vault. Finally, consideration of the frost heave effect induced by drainage system is crucial for ensuring tunnel operation safety in high latitude cold regions.</description><subject>Air monitoring</subject><subject>Air temperature</subject><subject>Buried pipes</subject><subject>Civil Engineering</subject><subject>Cold regions</subject><subject>Compressive properties</subject><subject>Disasters</subject><subject>Drainage</subject><subject>Drainage ditches</subject><subject>Drainage systems</subject><subject>Engineering</subject><subject>Field investigations</subject><subject>Freezing</subject><subject>Frost</subject><subject>Frost damage</subject><subject>Frost heaving</subject><subject>Geotechnical Engineering</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Heaving</subject><subject>Ice jams</subject><subject>Industrial Pollution Prevention</subject><subject>Latitude</subject><subject>Railway tunnels</subject><subject>Seepage</subject><subject>Tensile stress</subject><subject>Tunnels</subject><subject>Warm water</subject><subject>Water damage</subject><subject>Water temperature</subject><subject>토목공학</subject><issn>1226-7988</issn><issn>1976-3808</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNpFkUtLxDAUhYsoKOoPcHfBnVDNo2nTpczDGRgRxnEd0vS2RmuqSasM_nkzjuDdnLv4OBz4kuSCkmtKSHETKGNEpIRlqciETPOD5ISWRZ5ySeRh_BnL06KU8jg5D-GFxOOskFycJN9TG3QY0MM9mmftbHgD7WqY-z4MsED9iTBrGjQD9A2ste2-9BY2o3PYwdLVo8Eaqi1MvbZOtwiP29j2BvNIjh7BOljY9hlWerDDWCNM-q6GNba2d2fJUaO7gOd_eZo8zWebySJdPdwtJ7er1PBSDqlhgmOmKeFENJgj15oLhpUxKJmpykI33FTcFELWrKoIL0RGqRSlIbmuJOWnydW-1_lGvRqrem1_s-3Vq1e3681SUZLTrJAswpd7-N33HyOGQb30o3dxn-KUlCKPoIwU21Ph3VvXov-nKFE7KWovRUUpaidF5fwH-j5-aA</recordid><startdate>20241001</startdate><enddate>20241001</enddate><creator>Zhou, Feicong</creator><creator>Xie, Shenghao</creator><creator>Wang, Lei</creator><creator>Ma, Zhifu</creator><creator>Zhou, Ping</creator><creator>Jiang, Yifan</creator><creator>Chen, Shougen</creator><creator>Wang, Zhijie</creator><general>Korean Society of Civil Engineers</general><general>Springer Nature B.V</general><general>대한토목학회</general><scope>7QH</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope><scope>ACYCR</scope></search><sort><creationdate>20241001</creationdate><title>Disaster Mechanism and Frost Heave Effect of Railway Tunnel Induced by Drainage System Failure in High Latitude Cold Region</title><author>Zhou, Feicong ; Xie, Shenghao ; Wang, Lei ; Ma, Zhifu ; Zhou, Ping ; Jiang, Yifan ; Chen, Shougen ; Wang, Zhijie</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c398t-c253e4a10305fe6e3aa352ebcce82cb97af3cb3c758d2bb0375411859c06ab813</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Air monitoring</topic><topic>Air temperature</topic><topic>Buried pipes</topic><topic>Civil Engineering</topic><topic>Cold regions</topic><topic>Compressive properties</topic><topic>Disasters</topic><topic>Drainage</topic><topic>Drainage ditches</topic><topic>Drainage systems</topic><topic>Engineering</topic><topic>Field investigations</topic><topic>Freezing</topic><topic>Frost</topic><topic>Frost damage</topic><topic>Frost heaving</topic><topic>Geotechnical Engineering</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Heaving</topic><topic>Ice jams</topic><topic>Industrial Pollution Prevention</topic><topic>Latitude</topic><topic>Railway tunnels</topic><topic>Seepage</topic><topic>Tensile stress</topic><topic>Tunnels</topic><topic>Warm water</topic><topic>Water damage</topic><topic>Water temperature</topic><topic>토목공학</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhou, Feicong</creatorcontrib><creatorcontrib>Xie, Shenghao</creatorcontrib><creatorcontrib>Wang, Lei</creatorcontrib><creatorcontrib>Ma, Zhifu</creatorcontrib><creatorcontrib>Zhou, Ping</creatorcontrib><creatorcontrib>Jiang, Yifan</creatorcontrib><creatorcontrib>Chen, Shougen</creatorcontrib><creatorcontrib>Wang, Zhijie</creatorcontrib><collection>Aqualine</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Korean Citation Index (Open Access)</collection><jtitle>KSCE journal of civil engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhou, Feicong</au><au>Xie, Shenghao</au><au>Wang, Lei</au><au>Ma, Zhifu</au><au>Zhou, Ping</au><au>Jiang, Yifan</au><au>Chen, Shougen</au><au>Wang, Zhijie</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Disaster Mechanism and Frost Heave Effect of Railway Tunnel Induced by Drainage System Failure in High Latitude Cold Region</atitle><jtitle>KSCE journal of civil engineering</jtitle><stitle>KSCE J Civ Eng</stitle><date>2024-10-01</date><risdate>2024</risdate><volume>28</volume><issue>10</issue><spage>4190</spage><epage>4213</epage><pages>4190-4213</pages><issn>1226-7988</issn><eissn>1976-3808</eissn><abstract>In this study, temperature monitoring and freezing disaster investigation in winter were conducted in three high latitude cold regional tunnels of Northeast China. Observations indicate that the air temperature in the tunnel middle section and the deep buried central drainage pipe remains stable at 0–5°C, while at the entrance section and the side ditch, it fluctuates around −15°C for about 2 months. Consequently, warm water from the middle section supplies both ends of the tunnel, making the entrance section drainage system prone to ice jams and freezing damage. Field investigation reveals 5 types of freezing-induced catastrophic behavior in tunnel drainage systems. In addition, frost heave effects from drainage system failure are simulated, showing that the lining compressive stress due to frost heave of drainage system is about 450 kPa, which is 200% of the surrounding rock frost heave. Moreover, the tensile stress due to frost heave of the side wall crack seepage or cavity water is the most significant, followed by the arch springing, then the hance, and finally the vault. Finally, consideration of the frost heave effect induced by drainage system is crucial for ensuring tunnel operation safety in high latitude cold regions.</abstract><cop>Seoul</cop><pub>Korean Society of Civil Engineers</pub><doi>10.1007/s12205-024-5458-6</doi><tpages>24</tpages><oa>free_for_read</oa></addata></record> |
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source | ScienceDirect; Springer Nature |
subjects | Air monitoring Air temperature Buried pipes Civil Engineering Cold regions Compressive properties Disasters Drainage Drainage ditches Drainage systems Engineering Field investigations Freezing Frost Frost damage Frost heaving Geotechnical Engineering Geotechnical Engineering & Applied Earth Sciences Heaving Ice jams Industrial Pollution Prevention Latitude Railway tunnels Seepage Tensile stress Tunnels Warm water Water damage Water temperature 토목공학 |
title | Disaster Mechanism and Frost Heave Effect of Railway Tunnel Induced by Drainage System Failure in High Latitude Cold Region |
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