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Method for analyzing the evolution characteristics of in-situ stress field considering rheology and degradation: A deeply incised valley in Qinghai-Tibet Plateau, case study
The in-situ stress field in deeply incised valleys is an important factor to be considered in major construction projects on the Qinghai-Tibet Plateau. The resulting in-situ stress has a complex distribution and large magnitude due to rapid river erosion. Considering that the few actual measured in-...
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Published in: | Engineering geology 2023-03, Vol.315, p.107029, Article 107029 |
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description | The in-situ stress field in deeply incised valleys is an important factor to be considered in major construction projects on the Qinghai-Tibet Plateau. The resulting in-situ stress has a complex distribution and large magnitude due to rapid river erosion. Considering that the few actual measured in-situ stress values are insufficient to meet the needs of understanding the regional in-situ stress field and its evolution, this research proposes a method, the Svisc model, to study the distribution and evolution characteristics of the in-situ stress field and applies it to a case study of the Jinping-I Hydropower Station. The results show that the Svisc model, which considers the rheological and degradation properties of the rock mass, applies strength parameters that change from peak to residual values rather than remaining constant with rock mass degradation during the downcutting process of valleys. The stress adjustment depth obtained is deeper, and the current in-situ stress field values are higher overall according to the Svisc model. This model is more effective than conventional methods to simulate the long-term evolution of valleys.
•The Svisc model is proposed to study the distribution and evolution characteristics of in-situ stress field.•The rheological and degradation properties of rock mass are fully considered in valley evolution.•The adjustment depth and value of stress obtained by the Svisc model are deeper and higher overall. |
doi_str_mv | 10.1016/j.enggeo.2023.107029 |
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•The Svisc model is proposed to study the distribution and evolution characteristics of in-situ stress field.•The rheological and degradation properties of rock mass are fully considered in valley evolution.•The adjustment depth and value of stress obtained by the Svisc model are deeper and higher overall.</description><identifier>ISSN: 0013-7952</identifier><identifier>EISSN: 1872-6917</identifier><identifier>DOI: 10.1016/j.enggeo.2023.107029</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Deeply incised valley ; Degradation properties ; In-situ stress field ; Long-term evolution characteristics ; Rheological properties</subject><ispartof>Engineering geology, 2023-03, Vol.315, p.107029, Article 107029</ispartof><rights>2023 Elsevier B.V.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a329t-de4daeed3a87be97fc6d8288cacfee361c08d38f19662f1a72538ca4b04e56f53</citedby><cites>FETCH-LOGICAL-a329t-de4daeed3a87be97fc6d8288cacfee361c08d38f19662f1a72538ca4b04e56f53</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Sun, Xiang</creatorcontrib><creatorcontrib>Chen, Guoqing</creatorcontrib><creatorcontrib>Huang, Minyao</creatorcontrib><creatorcontrib>Zhang, Shishu</creatorcontrib><creatorcontrib>Yang, Jingxi</creatorcontrib><creatorcontrib>Ma, Jin'gen</creatorcontrib><title>Method for analyzing the evolution characteristics of in-situ stress field considering rheology and degradation: A deeply incised valley in Qinghai-Tibet Plateau, case study</title><title>Engineering geology</title><description>The in-situ stress field in deeply incised valleys is an important factor to be considered in major construction projects on the Qinghai-Tibet Plateau. The resulting in-situ stress has a complex distribution and large magnitude due to rapid river erosion. Considering that the few actual measured in-situ stress values are insufficient to meet the needs of understanding the regional in-situ stress field and its evolution, this research proposes a method, the Svisc model, to study the distribution and evolution characteristics of the in-situ stress field and applies it to a case study of the Jinping-I Hydropower Station. The results show that the Svisc model, which considers the rheological and degradation properties of the rock mass, applies strength parameters that change from peak to residual values rather than remaining constant with rock mass degradation during the downcutting process of valleys. The stress adjustment depth obtained is deeper, and the current in-situ stress field values are higher overall according to the Svisc model. This model is more effective than conventional methods to simulate the long-term evolution of valleys.
•The Svisc model is proposed to study the distribution and evolution characteristics of in-situ stress field.•The rheological and degradation properties of rock mass are fully considered in valley evolution.•The adjustment depth and value of stress obtained by the Svisc model are deeper and higher overall.</description><subject>Deeply incised valley</subject><subject>Degradation properties</subject><subject>In-situ stress field</subject><subject>Long-term evolution characteristics</subject><subject>Rheological properties</subject><issn>0013-7952</issn><issn>1872-6917</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp9kMtKBDEQRYMoOD7-wEU-wB6T9Ew_XAgivkBRQdehJql0Z4gdSTID7T_5j6YZ166KW1X3VHEJOeNszhmvLtZzHLoO_VwwUeZWzUS7R2a8qUVRtbzeJzPGeFnU7VIckqMY15NkrJ6Rn2dMvdfU-EBhADd-26GjqUeKW-82yfqBqh4CqITBxmRVpN5QOxTRpg2NKWCM1Fh0mio_RKvzWiaEHr3z3ZihmmrsAmiYYJf0Okv8cmNmKBtR0y04h5Okb9nZgy3e7QoTfXWQEDbnVEHEfGmjxxNyYMBFPP2rx-Tj7vb95qF4erl_vLl-KqAUbSo0LjQg6hKaeoVtbVSlG9E0CpRBLCuuWKPLxvC2qoThUItlmYeLFVvgsjLL8pgsdlwVfIwBjfwK9hPCKDmTU-RyLXeRyylyuYs82652Nsy_bS0GGZXFQaG2AVWS2tv_Ab_9f5F0</recordid><startdate>20230320</startdate><enddate>20230320</enddate><creator>Sun, Xiang</creator><creator>Chen, Guoqing</creator><creator>Huang, Minyao</creator><creator>Zhang, Shishu</creator><creator>Yang, Jingxi</creator><creator>Ma, Jin'gen</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20230320</creationdate><title>Method for analyzing the evolution characteristics of in-situ stress field considering rheology and degradation: A deeply incised valley in Qinghai-Tibet Plateau, case study</title><author>Sun, Xiang ; Chen, Guoqing ; Huang, Minyao ; Zhang, Shishu ; Yang, Jingxi ; Ma, Jin'gen</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a329t-de4daeed3a87be97fc6d8288cacfee361c08d38f19662f1a72538ca4b04e56f53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Deeply incised valley</topic><topic>Degradation properties</topic><topic>In-situ stress field</topic><topic>Long-term evolution characteristics</topic><topic>Rheological properties</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sun, Xiang</creatorcontrib><creatorcontrib>Chen, Guoqing</creatorcontrib><creatorcontrib>Huang, Minyao</creatorcontrib><creatorcontrib>Zhang, Shishu</creatorcontrib><creatorcontrib>Yang, Jingxi</creatorcontrib><creatorcontrib>Ma, Jin'gen</creatorcontrib><collection>CrossRef</collection><jtitle>Engineering geology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sun, Xiang</au><au>Chen, Guoqing</au><au>Huang, Minyao</au><au>Zhang, Shishu</au><au>Yang, Jingxi</au><au>Ma, Jin'gen</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Method for analyzing the evolution characteristics of in-situ stress field considering rheology and degradation: A deeply incised valley in Qinghai-Tibet Plateau, case study</atitle><jtitle>Engineering geology</jtitle><date>2023-03-20</date><risdate>2023</risdate><volume>315</volume><spage>107029</spage><pages>107029-</pages><artnum>107029</artnum><issn>0013-7952</issn><eissn>1872-6917</eissn><abstract>The in-situ stress field in deeply incised valleys is an important factor to be considered in major construction projects on the Qinghai-Tibet Plateau. The resulting in-situ stress has a complex distribution and large magnitude due to rapid river erosion. Considering that the few actual measured in-situ stress values are insufficient to meet the needs of understanding the regional in-situ stress field and its evolution, this research proposes a method, the Svisc model, to study the distribution and evolution characteristics of the in-situ stress field and applies it to a case study of the Jinping-I Hydropower Station. The results show that the Svisc model, which considers the rheological and degradation properties of the rock mass, applies strength parameters that change from peak to residual values rather than remaining constant with rock mass degradation during the downcutting process of valleys. The stress adjustment depth obtained is deeper, and the current in-situ stress field values are higher overall according to the Svisc model. This model is more effective than conventional methods to simulate the long-term evolution of valleys.
•The Svisc model is proposed to study the distribution and evolution characteristics of in-situ stress field.•The rheological and degradation properties of rock mass are fully considered in valley evolution.•The adjustment depth and value of stress obtained by the Svisc model are deeper and higher overall.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.enggeo.2023.107029</doi></addata></record> |
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source | ScienceDirect Freedom Collection 2022-2024 |
subjects | Deeply incised valley Degradation properties In-situ stress field Long-term evolution characteristics Rheological properties |
title | Method for analyzing the evolution characteristics of in-situ stress field considering rheology and degradation: A deeply incised valley in Qinghai-Tibet Plateau, case study |
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