CD Skripsi

Penggunaan Metode Geolistrik Resistivitas Konfigurasi Schlumberger Untuk Mengetahui Lapisan Struktur Litologi Bawah Tanah Di Taman Ilmu Universitas Riau

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This study aims to determine the layers of underground lithological structures in the Science Park, Riau University, Bina Widya Campus km. 12.5 Simpang Baru, Pekanbaru. The research location is an area that is often flooded, so research is needed to determine the cause of the puddle. Data interpretation uses the one-dimensional Schlumberger configuration resistivity geoelectric method. Data processing using Software Progress. Based on the results of data processing obtained information about the rock layers in the research location. The results of the quantitative interpretation of geoelectrical data show that on track 1 with a track length of 150 meters, a minimum resistivity value of 226.90 ohm-meters and a maximum of 863.14 ohm-meters with a maximum depth of 31.12 meters is obtained. The types of rock layers that are read on track 1 are alluvium, clay, sand and gravel. Track 2 has a track length of 100 m, the lowest resistivity value is 188.08 ohm-meters and the highest is 1027.83 ohm-meters with a maximum depth of 6.16 meters. Based on the resistivity results on track 2, several types of soil layers were read, namely clay, sand and gravel. The cause of waterlogging in the two research locations is thought to be due to the presence of alluvial and clay soil types. This soil layer has a high porosity density so it is difficult to pass water.
Keywords: Subsurface Layers of the Earth, Lithological Structure, Geoelectrical Method, Schlumberger Configuration.

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Ketersediaan

Informasi Detail

Judul Seri

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No. Panggil

1503117007

Penerbit

Pekanbaru : Universitas Riau –FMIPA– FISIKA., 2022

Deskripsi Fisik

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Bahasa

Indonesia

ISBN/ISSN

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Klasifikasi

1503117007

Tipe Isi

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Tipe Media

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Tipe Pembawa

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Edisi

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Subjek

FISIKA

Info Detail Spesifik

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Pernyataan Tanggungjawab

nadya

Versi lain/terkait

Lampiran Berkas

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