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All Journal JFA (Jurnal Fisika dan Aplikasinya) AGRARIS: Journal of Agribusiness and Rural Development Research Jurnal Agribisnis Terpadu INDONESIAN JOURNAL OF APPLIED PHYSICS PengabdianMu: Jurnal Ilmiah Pengabdian kepada Masyarakat Agriecobis : Journal of Agricultural Socioeconomics and Business Proceedings Series on Physical & Formal Sciences National Multidisciplinary Sciences
Darsono Darsono
Universitas Sebelas Maret
Agriculture, Biological Sciences & Forestry Humanities Astronomy Chemical Engineering, Chemistry & Bioengineering Civil Engineering, Building, Construction & Architecture Computer Science & IT Economics, Econometrics & Finance Education Electrical & Electronics Engineering Energy Engineering Environmental Science Law, Crime, Criminology & Criminal Justice Materials Science & Nanotechnology Mechanical Engineering Physics Public Health Social Sciences

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Journal : INDONESIAN JOURNAL OF APPLIED PHYSICS

 1 
Identifikasi Pola Aliran Sungai Bawah Tanah Daerah Karst di Desa Gebangharjo Kecamatan Pracimantoro Menggunakan Metode Tomography Resistivity Konfigurasi Wenner-Schlumberger Yudi Purwanto; Darsono Darsono; Sorja Koesuma
INDONESIAN JOURNAL OF APPLIED PHYSICS Vol 7, No 2 (2017): IJAP Volume 07 ISSUE 02 YEAR 2017
Publisher : Department of Physics, Sebelas Maret University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13057/ijap.v7i2.12766

Abstract

This research is conducted using 4 lines data with 750 meters in length. Tomography resistivity with Wenner-Schlumberger configuration is used as this research methodology to take the data with a = 50 meters and n=1, 2, 3, 4, 5, 6. Resistivitymeter OYO 2119C McOHM-ELmodel is used as the instrument. Furthermore, the data is processed with two softwares; Res2Dinv ver. 3.56.22 to get 2D resistivity section and RockWork16to make 3D model of the site. The underground river’s chamber is made by hollow carbonate rocks with the resistivity of >412 Ωmand 117,6 Ωm – 412 Ωm for limestone’s resistivity as its capsrock. Researching to the depth of 173 meters, underground rivers are shown in the line 2 in the depth of 65 to 134 meters, 65 to 173 meters in the line 3, and in the cross section of line 3 and line 4. While in the first trajectory, another chamber is found within the depth of 12.5 to 40 meters. It is expected that the underground river is flowing to the south because of the chamber in third and fourth trajectory are lower than second trajectory.
Identifikasi Keberadaan Lapisan Akuifer Tertekan (Confined Aquifer) Berdasarkan Data Geolistrik (Studi Kasus : Desa Sambirejo Kecamatan Plupuh Kabupaten Sragen) Darsono Darsono; Darmanto Darmanto
INDONESIAN JOURNAL OF APPLIED PHYSICS Vol 9, No 01 (2019): April
Publisher : Department of Physics, Sebelas Maret University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13057/ijap.v9i01.30122

Abstract

Air menempati suatu wadah rongga di dalam tanah yang disebut dengan akuifer. Salah satu akuifer yang masih jarang digunakan adalah akuifer tertekan. Akuifer ini terletak lebih dalam, sehingga keberadaan perlu dideteksi lebih dahulu. Untuk mendeteksi keberadaan akuifer menggunakan metode geolistrik resistivitas. Alat yang digunakan adalah resistivitimeter OYO Model 2119C McOHM-EL, dengan konfigurasi Schlumberger dengan bentangan AB/2 samapai 350 meter. Pengambilan data dilakukan di Kecamatan Plupuh Kabupaten Sragen sebanyak 5 titik sounding. Pengolahan dilakukan dengan menggunakan software IP2win.Hasilnya menunjukkan bahwa lapisan akuifer di 5 titik sounding berupa lapisan pasir lempungan, pasir dan lapisan pasir kerikilan. Lapisan akuifer tertekan terdeteksi di: TS1 pada kedalaman 39,9 meter- 110 meter dengan litologi pasir kerikilan, TS2 pada kedalaman 40,25 meter – 66,58 meter dan 80,24 -139,7 meter dengan litologi pasir, TS3 pada kedalaman 47,25 meter – 101 meter dengan litologi pasir lempungan,TS4 pada kedalaman 40,72 meter – 103 meter dengan litologi pasir lempungan dan TS5 pada kedalaman 31,41 meter – 97 meter dengan litologi pasir lempungan.
Co-Authors Adha Nur Hidayat Agung Adi Nugraha Agustono Agustono Darmanto Darmanto Dea Arien Alinda Dewi Ernoiz Antriyandarti Imas Wildan Rafiqah Isti Khomah Joko Sutrisno Legowo, Budi Marwanti, Sri Minar Ferichani Nurul Arifah Fauzi Serli Birlina Sorja Koesuma Susi Wuri Ani Umi Barokah Umma Rizqi Marfu’ah Wiwit Rahayu Yudi Purwanto