Analisis Potensi Likuifaksi di Area PLTU Pacitan
One of Indonesia's regions, Pacitan, is an earthquake-prone area where one of the consequences of the earthquake is the phenomenon of soil liquefaction. Soil liquefaction is the process of changing or transforming the form from a solid to a liquid form. The purpose of this study was to analyze...
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| Format: | Article |
| Language: | English |
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University of Brawijaya
2022-06-01
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| Series: | Rekayasa Sipil |
| Subjects: | |
| Online Access: | https://rekayasasipil.ub.ac.id/index.php/rs/article/view/935 |
| _version_ | 1811209974976610304 |
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| author | Mesra Srya Ariefin As'ad Munawir Arief Rachmansyah |
| author_facet | Mesra Srya Ariefin As'ad Munawir Arief Rachmansyah |
| author_sort | Mesra Srya Ariefin |
| collection | DOAJ |
| description | One of Indonesia's regions, Pacitan, is an earthquake-prone area where one of the consequences of the earthquake is the phenomenon of soil liquefaction. Soil liquefaction is the process of changing or transforming the form from a solid to a liquid form. The purpose of this study was to analyze the potential for liquefaction based on field data at the finite element PLTU Sudimoro Pacitan or FEM method. There are three location plans for the liquefaction potential analysis point, namely C-36, S-58, and TC-32 based on earthquake data. Point C-36 has the possibility of liquefaction. For the point S-58 has conditions that will definitely experience liquefaction. Meanwhile, Point TC-32 has the possibility of liquefaction. The subsidence that occurs due to the earthquake load has a large enough impact on land subsidence, namely at point C-36. |
| first_indexed | 2024-04-12T04:49:04Z |
| format | Article |
| id | doaj.art-94a9940104e74a66b39b1fcc67bb151e |
| institution | Directory Open Access Journal |
| issn | 1978-5658 2502-6348 |
| language | English |
| last_indexed | 2024-04-12T04:49:04Z |
| publishDate | 2022-06-01 |
| publisher | University of Brawijaya |
| record_format | Article |
| series | Rekayasa Sipil |
| spelling | doaj.art-94a9940104e74a66b39b1fcc67bb151e2022-12-22T03:47:23ZengUniversity of BrawijayaRekayasa Sipil1978-56582502-63482022-06-01162125131https://doi.org/10.21776/ub.rekayasasipil.2022.016.02.8Analisis Potensi Likuifaksi di Area PLTU PacitanMesra Srya Ariefin0As'ad Munawir1Arief Rachmansyah2Universitas BrawijayaUniversitas BrawijayaUniversitas BrawijayaOne of Indonesia's regions, Pacitan, is an earthquake-prone area where one of the consequences of the earthquake is the phenomenon of soil liquefaction. Soil liquefaction is the process of changing or transforming the form from a solid to a liquid form. The purpose of this study was to analyze the potential for liquefaction based on field data at the finite element PLTU Sudimoro Pacitan or FEM method. There are three location plans for the liquefaction potential analysis point, namely C-36, S-58, and TC-32 based on earthquake data. Point C-36 has the possibility of liquefaction. For the point S-58 has conditions that will definitely experience liquefaction. Meanwhile, Point TC-32 has the possibility of liquefaction. The subsidence that occurs due to the earthquake load has a large enough impact on land subsidence, namely at point C-36.https://rekayasasipil.ub.ac.id/index.php/rs/article/view/935liquifactionpltu sudimoro pacitanquake |
| spellingShingle | Mesra Srya Ariefin As'ad Munawir Arief Rachmansyah Analisis Potensi Likuifaksi di Area PLTU Pacitan Rekayasa Sipil liquifaction pltu sudimoro pacitan quake |
| title | Analisis Potensi Likuifaksi di Area PLTU Pacitan |
| title_full | Analisis Potensi Likuifaksi di Area PLTU Pacitan |
| title_fullStr | Analisis Potensi Likuifaksi di Area PLTU Pacitan |
| title_full_unstemmed | Analisis Potensi Likuifaksi di Area PLTU Pacitan |
| title_short | Analisis Potensi Likuifaksi di Area PLTU Pacitan |
| title_sort | analisis potensi likuifaksi di area pltu pacitan |
| topic | liquifaction pltu sudimoro pacitan quake |
| url | https://rekayasasipil.ub.ac.id/index.php/rs/article/view/935 |
| work_keys_str_mv | AT mesrasryaariefin analisispotensilikuifaksidiareapltupacitan AT asadmunawir analisispotensilikuifaksidiareapltupacitan AT ariefrachmansyah analisispotensilikuifaksidiareapltupacitan |