Repo Dosen ULM

peer review Identifikasi Struktur Batuan Bawah Permukaan Menggunakan Metode Sieismik Refraksi di Kampung Baru Banjarbaru

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dc.contributor.author Triningsih, Sumaos
dc.contributor.author Sota, Iberahim
dc.contributor.author Wahyono, Sri Cahyo
dc.date.accessioned 2022-04-26T03:37:35Z
dc.date.available 2022-04-26T03:37:35Z
dc.date.issued 2013-08-01
dc.identifier.issn 2541-1713
dc.identifier.issn 1829-796X
dc.identifier.uri https://repo-dosen.ulm.ac.id//handle/123456789/23959
dc.description.abstract It has been researched graving hole of ex-coal mining using refraction seismic method in Kampung Baru Banjarbaru. The hole is filled by water as acid puddle, where it is worried to flow through to soil layer by following the plot of rock layer’s slope. Identification of subsurface structure of the area is in order to know the direction of the water’s flow. Seismograph PASI 24 Channel has been used to collect data. The data has been processed using intercept time method. Interpretation results show the subsurface in residential area has 3 layers. First layer is decayed layer with wave velocity (295-413 m/s) and thickness (2.8-5.57) m. Second layer with wave velocity (787.4-919) m/s and thickness (10-11.66) m is interpreted as sand and gravel. Whereas, third layer with wave velocity (1282-2020) m/s and area boundary between h2 dan h3 about (13.42-16.01) m is interpreted as clay (waterproof layer). en_US
dc.language.iso en en_US
dc.publisher 'Lambung Mangkurat University Press en_US
dc.subject Seismic refraction, Intercept time method, Banjarbaru en_US
dc.title peer review Identifikasi Struktur Batuan Bawah Permukaan Menggunakan Metode Sieismik Refraksi di Kampung Baru Banjarbaru en_US
dc.type Article en_US


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