Safety Factor on Rock Slopes with Tensile Cracks Using Numerical and Limit Equilibrium Models
Through the research it describes an analytic methodology, which allows to determine the minimum safety factor depending on the depth of tensile crack and the inclination of surface failure on the most critical condition, considering at the same time, surcharge, seismic effect and water pressure. Th...
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Veröffentlicht in: | Geotechnical and geological engineering 2021-03, Vol.39 (3), p.2287-2300 |
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creator | Belandria, Norly Úcar, Roberto Corredor, Alfredo Hassani, Ferri |
description | Through the research it describes an analytic methodology, which allows to determine the minimum safety factor depending on the depth of tensile crack and the inclination of surface failure on the most critical condition, considering at the same time, surcharge, seismic effect and water pressure. Therefore, it studies the stability of rock slopes considering that the potential of failure surface it is constituted by two blocks with different inclinations. The superior block is limited by a tensile crack that is represented by a fracture without displacement. On the other hand, on the inferior block, geometry is formed by a potential slide plane of α inclination with the horizontal axis, in which are acting shear stresses. Fracture on superior block is characterized by a normal-tensile stresses field that act over the crack whose presence originates when the rock loses its original cohesion. Finally, comparisons are made through examples with the limit equilibrium method and finite elements method, where it determines the safety factor on dry state, water and seism, being all of them too similar. Besides, the methodology compares the track depth and the distance between the intersection point of tensile crack and the edge of the slope face, results shows that the analytic methodology is very conservative and throws the less values of this distances. |
doi_str_mv | 10.1007/s10706-020-01624-8 |
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Therefore, it studies the stability of rock slopes considering that the potential of failure surface it is constituted by two blocks with different inclinations. The superior block is limited by a tensile crack that is represented by a fracture without displacement. On the other hand, on the inferior block, geometry is formed by a potential slide plane of α inclination with the horizontal axis, in which are acting shear stresses. Fracture on superior block is characterized by a normal-tensile stresses field that act over the crack whose presence originates when the rock loses its original cohesion. Finally, comparisons are made through examples with the limit equilibrium method and finite elements method, where it determines the safety factor on dry state, water and seism, being all of them too similar. 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Therefore, it studies the stability of rock slopes considering that the potential of failure surface it is constituted by two blocks with different inclinations. The superior block is limited by a tensile crack that is represented by a fracture without displacement. On the other hand, on the inferior block, geometry is formed by a potential slide plane of α inclination with the horizontal axis, in which are acting shear stresses. Fracture on superior block is characterized by a normal-tensile stresses field that act over the crack whose presence originates when the rock loses its original cohesion. Finally, comparisons are made through examples with the limit equilibrium method and finite elements method, where it determines the safety factor on dry state, water and seism, being all of them too similar. Besides, the methodology compares the track depth and the distance between the intersection point of tensile crack and the edge of the slope face, results shows that the analytic methodology is very conservative and throws the less values of this distances.</description><subject>Civil Engineering</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Failure surface</subject><subject>Finite element method</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hydrogeology</subject><subject>Hydrostatic pressure</subject><subject>Inclination</subject><subject>Methodology</subject><subject>Original Paper</subject><subject>Pressure effects</subject><subject>Rocks</subject><subject>Safety</subject><subject>Safety factors</subject><subject>Seismic effects</subject><subject>Seismic stability</subject><subject>Shear stress</subject><subject>Slope stability</subject><subject>Stresses</subject><subject>Terrestrial Pollution</subject><subject>Waste Management/Waste Technology</subject><subject>Water pressure</subject><issn>0960-3182</issn><issn>1573-1529</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNp9kMtOwzAQRS0EEqXwA6wssTaM7cRJlqhqAamARNslslxnUtzm0dqJUP-eQJDYsZrNvedqDiHXHG45QHIXOCSgGAhgwJWIWHpCRjxOJOOxyE7JCDIFTPJUnJOLELYAIBTwEXlfmALbI50Z2zaeNjV9a-yOLspmj4F-uvaDLrEOrkQ68cbuAl0FV2_oS1ehd9aU1NQ5nbvKtXR66Fzp1t51FX1ucizDJTkrTBnw6veOyWo2XU4e2fz14WlyP2dGRqJlhUq4ghRQIfTvKMBoLWFtAfLMKm4wxSKWQiAqk-SYJBYKUJIbFeUqLoQck5uBu_fNocPQ6m3T-bqf1CLugRkHFfUpMaSsb0LwWOi9d5XxR81Bf2vUg0bda9Q_GnXal-RQCn243qD_Q__T-gKqeHR5</recordid><startdate>20210301</startdate><enddate>20210301</enddate><creator>Belandria, Norly</creator><creator>Úcar, Roberto</creator><creator>Corredor, Alfredo</creator><creator>Hassani, Ferri</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>7UA</scope><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>L6V</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><orcidid>https://orcid.org/0000-0002-9485-0860</orcidid></search><sort><creationdate>20210301</creationdate><title>Safety Factor on Rock Slopes with Tensile Cracks Using Numerical and Limit Equilibrium Models</title><author>Belandria, Norly ; 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Therefore, it studies the stability of rock slopes considering that the potential of failure surface it is constituted by two blocks with different inclinations. The superior block is limited by a tensile crack that is represented by a fracture without displacement. On the other hand, on the inferior block, geometry is formed by a potential slide plane of α inclination with the horizontal axis, in which are acting shear stresses. Fracture on superior block is characterized by a normal-tensile stresses field that act over the crack whose presence originates when the rock loses its original cohesion. Finally, comparisons are made through examples with the limit equilibrium method and finite elements method, where it determines the safety factor on dry state, water and seism, being all of them too similar. 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subjects | Civil Engineering Earth and Environmental Science Earth Sciences Failure surface Finite element method Geotechnical Engineering & Applied Earth Sciences Hydrogeology Hydrostatic pressure Inclination Methodology Original Paper Pressure effects Rocks Safety Safety factors Seismic effects Seismic stability Shear stress Slope stability Stresses Terrestrial Pollution Waste Management/Waste Technology Water pressure |
title | Safety Factor on Rock Slopes with Tensile Cracks Using Numerical and Limit Equilibrium Models |
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