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All Journal POSITRON JGE (Jurnal Geofisika Eksplorasi) Jurnal Geosaintek Journal of Geoscience, Engineering, Environment, and Technology JTERA (Jurnal Teknologi Rekayasa) Spektra: Jurnal Fisika dan Aplikasinya Jurnal Geosains dan Teknologi Journal of Multidisciplinary Academic Jurnal Abdi Masyarakat Indonesia Jurnal Geosaintek Global Review of Tourism and Social Sciences
Antosia, Risky Martin
Department Of Geophysical Engineering, Sumatera Institute Of Technology, Jalan Terusan Ryacudu, Way Huwi, Jati Agung, Kabupaten Lampung Selatan, Lampung, Indonesia
Aerospace Engineering Humanities Civil Engineering, Building, Construction & Architecture Computer Science & IT Decision Sciences, Operations Research & Management Earth & Planetary Sciences Economics, Econometrics & Finance Education Electrical & Electronics Engineering Energy Engineering Environmental Science Industrial & Manufacturing Engineering Materials Science & Nanotechnology Mechanical Engineering Physics Public Health Social Sciences

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VOLTMETER DESIGN BASED ON ADS1115 AND ARDUINO UNO FOR DC RESISTIVITY MEASUREMENT Antosia, Risky Martin
JTERA (Jurnal Teknologi Rekayasa) Vol 5, No 1: June 2020
Publisher : Politeknik Sukabumi

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (999.629 KB) | DOI: 10.31544/jtera.v5.i1.2019.73-80

Abstract

One part of the geoelectric method is DC (Direct Current) resistivity measurement. Physical parameters measured by the system are the current and potential difference. From these two parameters, the resistance value is obtained based on Ohm?s law. Based on the current-potential electrodes configuration in the DC resistivity measurement, there is the possibility of contact between the potential-current electrodes and also the position of the potential electrodes that can be exchanged. Thus, an auto-range Voltmeter is needed which can measure the potential difference with the order of mV up to hundreds of volts and can measure negative potential difference value (reversed polarity). This research aims to build a Voltmeter prototype using ADS1115 (namely ADC with 16-bit resolution) and Arduino Uno, which can be applied in DC resistivity measurement. In this system, there is internal resistance and switch. The internal resistance is around 2.4 M?, arranged into a voltage divider circuit to be able to measure the maximum potential input around 1,600 V. The switch function is to set the measurement mode (as auto-range), which is set by Arduino Uno. Furthermore, ADS1115 uses a differential measurement method to be able to measure a negative potential difference. Based on the results of tests on several resistor components with an adjustable voltage source, the Voltmeter is good at measuring the potential difference in resistor values below 10 K? with a confidence level of around 97%.
Peninjauan Ulang Kedalaman Akuifer Menggunakan Metode Resistivitas 1D di Desa Gayau, Kabupaten Pesawaran Antosia, Risky Martin; Putri, Intan Andriani; Farduwin, Alhada; Irawati, Selvi Misnia; Santoso, Nono Agus
Jurnal Abdi Masyarakat Indonesia Vol 2 No 2 (2022): JAMSI - Maret 2022
Publisher : CV Firmos

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.54082/jamsi.309

Abstract

Kegiatan pengabdian kepada masyarakat (PkM) telah dilakukan di desa Gaya, kecamatan Padang Cermin, kabupaten Pesawaran, provinsi Lampung. Permasalahan yang dialami desa tersebut adalah sarana penampungan air yang sudah dibuat tidak optimal digunakan karena sumur bor yang dimiliki, kondisi airnya sering kering. Sarana tersebut diperuntukkan bagi warga desa ketika musim kemarau tiba. Tim PkM mengajukan suatu pendekatan dari segi kerekayasaan geofisika untuk mengatasi permasalahan tersebut, berupa peninjauan kembali kedalaman akuifer sumur bor desa. Pendekatan tersebut menggunakan metode resistivitas 1D. Metode ini bertujuan untuk mengetahui lapisan batuan bawah permukaan bumi dengan dilihat dari distribusi nilai resistivitas terhadap kedalaman. Ada 3 titik pengukuran di sekitar sumur desa tersebut dengan posisi sumur berada di antara ketiga titik tersebut. 1 titik memiliki bentangan 400 m dan 2 titik yang lain sepanjang 600 m. Hasil analisis dari metode resistivitas 1D menjelaskan bahwa estimasi jenis batuannya berupa endapan alluvium, lempung tufaan, batu pasir tufaan, kerakal/ kerikil, dan lava andesit. Akuifer berada pada batu pasir tufaan atau kerakal/kerikil. Hasil analisis juga memberikan informasi bahwa posisi dan kedalaman sumur tidak berada pada akuifer. Dengan demikian, memberikan rekomendasi perlu adanya pengeboran ulang. Kemudian tim juga memberikan gambaran bahwa ada 2 posisi yang cocok untuk dibor beserta dengan kedalamannya.
Pemanfaatan Metode Geolistrik 2 Dimensi dalam Mengidentifikasi Kemenerusan Lapisan Air Tanah di Dusun IID, Desa Jatimulyo, Kecamatan Jati Agung, Kabupaten Lampung Selatan Antosia, Risky Martin; Putri, Intan Andriani; Pesma, Rhahmi Adni; Erlangga, Mokhammad Puput; Ekawati, Gestin Mey
Jurnal Abdi Masyarakat Indonesia Vol 2 No 2 (2022): JAMSI - Maret 2022
Publisher : CV Firmos

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.54082/jamsi.324

Abstract

Sebagian warga yang tinggal di sekitar Dusun IID, Desa Jatimulyo, Kecamatan Jati Agung, Kabupaten Lampung Selatan; sering mengalami kekeringan air tanah pada sumur bor yang dimilikinya. Kedalaman sumur bor tersebut sekitar 10 meter, padahal ada sumur bor dengan kedalaman yang sama, kuantitas airnya banyak. Untuk mengatasi permasalahan ini, tim pengabdian kepada masyarakat menggunakan metode geolistrik untuk mengidentifikasi kemenerusan lapisan air tanah di dusun tersebut. Metode geolistrik 2 dimensi diaplikasikan di lokasi pengukuran agar dapat memberikan informasi persebaran nilai tahanan jenis listrik di area tersebut (secara horizontal dan vertical) sepanjang bentangan 210 meter dengan jarak antar elektroda sebesar 14 meter. Hasil pengolahan data menunjukkan bahwa lapisan air tanah di sekitar lokasi memiliki kuantitas air tanah yang berbeda, dilihat dari persebaran nilai resistivitasnya (tahanan jenis listrik). Informasi warga terkait kedalaman air tanah dan kuantitas air tanah, cocok dengan penampang resistivitas. Bagi warga yang tinggal di sebelah Barat, dapat memanfaatkan air tanah hanya dengan kedalaman sumur bor sekitar 10 meter. Namun, sebagai rekomendasi bagi warga di sebelah Timur, tim menyarankan untuk membuat sumur bor dengan kedalaman lebih dari 25 meter.
INVERSI DATA GEOLISTRIK MENGGUNAKAN PARTICLE SWARM OPTIMIZATION: STUDI KASUS DESA GAYAU Alhada Farduwin; Risky Martin Antosia; Intan Andriani Putri; Nono Agus Santoso; Selvi Misnia Irawati
Jurnal Geofisika Eksplorasi Vol 7, No 2 (2021)
Publisher : Engineering Faculty Universitas Lampung

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23960/jge.v7i2.118

Abstract

Desa Gayau yang terletak di Kecamatan Padang Cermin, Kabupaten Pesawaran sering mengalami kekeringan air pada saat musim kemarau sehingga perlu dilakukannya pengukuran geolistrik untuk mengidentifikasi keberadaan lapisan akuifer air tanah. Pada penelitian ini konfigurasi yang digunakan adalah Schlumberger dengan panjang bentangan MN/2 sebesar 1, 5, 10, dan 20 meter. Sedangkan panjang bentangan AB/2 sebesar 6 hingga 300 meter. Pada tahapan inversi data VES, kami menggunakan algoritma Particle Swarm Optimization (PSO) untuk memperoleh nilai parameter resistivitas dan ketebalan lapisan. Algoritma ini dipilih karena cepat menuju konvergen dan relatif stabil. Hasil dari inversi ini diperoleh bahwa lapisan akuifer pertama berada pada kedalaman 21.4 - 52.1 meter dengan litologi batupasir berbutir halus dengan sisipan tufa Lapisan akuifer kedua berada pada kedalaman 52.1-70 meter dengan litologi breksi. Pada kedalaman 70 meter diinterpretasikan sebagai akuifer air tanah, namun memiliki debit yang kecil. Hal ini disebabkan karena litologi lapisan berupa breksi, dasit dan lava basal dari Formasi Hulusimpang. Sistem aliran air tanah pada lapisan ini merupakan sistem media pori yang berakibat pada debit rendah dan waktu pengisian kembali lapisan air tanah relatif lama.
Identifikasi Lapisan Akuifer Menggunakan Metode Seismik Refraksi di Desa Jatimulyo, Kecamatan Jati Agung, Kabupaten Lampung Selatan Rhahmi Adni Pesma; Mokhammad Puput Erlangga; Intan Adiani Putri; Risky Martin Antosia; Ruhul Firdaus; Gestin Mey Ekawati
Jurnal Geofisika Eksplorasi Vol 6, No 2 (2020)
Publisher : Engineering Faculty Universitas Lampung

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23960/jge.v6i2.66

Abstract

An initial subsurface survey to predict the aquifer is important to avoid the unprospect drill location and getting groundwater with the right discharge. In this study, prediction of the aquifer was carried out using the seismic refraction method in Jatimulyo Village, Jati Agung District, South Lampung Regency. The data was collected on October 6, 2019 using the SUMMIT X One seismic tool with 24 Geophones. The first break data from p-wave travel time is processed and interpreted using the Hagiwara method. Interpretation results show that there are three layers of subsurface lithology in the study area. The weathering layer was found at 2 m to 3.5 m depth with average velocity of 360 m/s. The second layer is dry sand with a velocity of 890 m/s at a depth of 2 m to 8 m. The third layer with a 2300 m/s velocity is a mixture of clay rock and saturated sand at depths of more than 8 m. As a comparison there is resistivity distribution data on the same measurement line in the study area. The overall interpretation shows that at a depth of 12 m with saturated clay sedimentary rock as a prospect of aquifer in this study area.
Voltmeter Design Based on ADS1115 and Arduino Uno for DC Resistivity Measurement Risky Martin Antosia
JTERA (Jurnal Teknologi Rekayasa) Vol 5, No 1: June 2020
Publisher : Politeknik Sukabumi

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31544/jtera.v5.i1.2019.73-80

Abstract

One part of the geoelectric method is DC (Direct Current) resistivity measurement. Physical parameters measured by the system are the current and potential difference. From these two parameters, the resistance value is obtained based on Ohm’s law. Based on the current-potential electrodes configuration in the DC resistivity measurement, there is the possibility of contact between the potential-current electrodes and also the position of the potential electrodes that can be exchanged. Thus, an auto-range Voltmeter is needed which can measure the potential difference with the order of mV up to hundreds of volts and can measure negative potential difference value (reversed polarity). This research aims to build a Voltmeter prototype using ADS1115 (namely ADC with 16-bit resolution) and Arduino Uno, which can be applied in DC resistivity measurement. In this system, there is internal resistance and switch. The internal resistance is around 2.4 MΩ, arranged into a voltage divider circuit to be able to measure the maximum potential input around 1,600 V. The switch function is to set the measurement mode (as auto-range), which is set by Arduino Uno. Furthermore, ADS1115 uses a differential measurement method to be able to measure a negative potential difference. Based on the results of tests on several resistor components with an adjustable voltage source, the Voltmeter is good at measuring the potential difference in resistor values below 10 KΩ with a confidence level of around 97%.
Basaltic Lava Characteristic in Goa Pandan Area, Sukadana, East Lampung: Inferences from Stratigraphy and Petrography Analysis Happy Christin Natalia Sirait; Bilal Al Farishi; Nono Agus Santoso; Andreas Maruli Pakpahan; Hissy Ijitiha Sari; Angga Jati Widiyatama; Risky Martin Antosia
Journal of Geoscience, Engineering, Environment, and Technology Vol. 8 No. 2 (2023): JGEET Vol 08 No 02 : June (2023)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25299/jgeet.2023.8.2.12118

Abstract

The presence of extensive basalt formations in East Lampung has its own attractions in the field of geology, particularly the presence of Goa Pandan as a lava cave and tourist attraction in East Lampung. The presence of basalt lava in the southern part of the South Sumatra Basin has drawn attention to the presence of this lava, but detailed research on the characteristics of the lava and its formation process is still very rare. This study aims to determine the eruption period of the basalt lava and magma evolution process based on the correlation between lava stratigraphy and petrography analysis. Field observations show a lava sequence that forms Goa Pandan. Each lava sequence is characterized by autobreccia and vesicular structures on the surface. In addition, the presence of columnar joints, sheeting joints, massive lava, and other additional structures indicate the characteristics of low-viscosity basalt lava. The presence of mineral structures and abundance under the microscope clearly shows the magma formation process when basalt lava flowed on the surface. Resorption-overgrowth of plagioclase and pyroxene minerals indicates an open system when basalt lava flowed on the surface. In addition, the presence of zoning and patching in plagioclase minerals indicates that magma variability is influenced by temperature. The documentation of this lava stratigraphy can serve as a basis for further understanding of magma characteristics and formation processes. There is still much geological work that can be done in the research area to get a detailed picture of the evolution process of magma and the presence of basalt lava in this area.
IDENTIFIKASI PERSEBARAN BATUAN ANDESIT SEBAGAI BAHAN UTAMA AGREGAT MENGGUNAKAN METODE GEOLISTRIK PROFILING KONFIGURASI WENNER-ALPHA Dimas Setiawan; Risky Martin Antosia; Purwaditya Nugraha
Jurnal Geosaintek Vol 9, No 2 (2023)
Publisher : Institut Teknologi Sepuluh Nopember

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.12962/j25023659.v9i2.16986

Abstract

Penelitian ini dilakukan untuk mengidentifikasi persebaran batuan andesit sebagai bahan utama agregat menggunakan metode geolistrik profiling dengan konfigurasi elektroda Wenner-Alpha. Lokasi penelitian dilakukan di Desa Tarahan, Kecamatan Katibung, Kabupaten Lampung Selatan karena daerah tersebut memiliki potensi andesit yang melimpah secara geologi. Akuisisi data di daerah tersebut difokuskan pada daerah “andesit 01” dengan luas area sekitar 10.000 m2 sebanyak 3 lintasan, masing-masing sepanjang 100 m dengan spasi elektroda 5 m. Kemudian, ada satu lintasan tambahan diletakan pada singkapan di luar daerah tersebut. Lalu, terdapat juga sampel batuan tufa dan andesit yang dilakukan uji nilai resistivitas di laboratorium. Pengukuran singkapan dan sampel batuan dilakukan untuk mengonfirmasi batas nilai resistivitas pada penampang 2D. Berdasarkan profil resistivitas pada singkapan, andesit memiliki nilai resistivitas lebih dari 173,5 Ωm. Sedangkan, hasil pengujian sampel menunjukkan bahwa nilai resistivitas batu andesit sebesar kurang lebih 171 Ωm dan batu tufa sekitar 131 Ωm. Maka, hampir di seluruh area studi dipenuhi dengan batuan andesit dan menyebar ke segala arah walaupun ada sedikit sebaran batuan tufa ke arah selatan mulai kedalaman 8-10 m. Dengan demikian, potensi andesit tersebut layak diproduksi untuk keperluan domestik
Identification of Aquifer, Ground Water-Bearing Rock, using Vertical Electrical Sounding (VES): East Lampung Case Study Intan Andriani Putri; Risky Martin Antosia; Alhada Farduwin; Reza Rizki; Yudha Styawan; Sillak Hasiany
Journal of Multidisciplinary Academic Vol 7, No 1 (2023): Science, Engineering and Social Science Series
Publisher : Penerbit Kemala Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar

Abstract

A one-dimensional geo-electrical method using Vertical Electrical Sounding (VES) has been carried out to model lithology and identify an aquifer, a water-bearing rock, in East Lampung to provide the water needs of the poultry breeding industry (PT. X) that is going to be established in the near future. Two VES points had been surveyed using Schlumberger electrode configuration to achieve good depth penetration and good vertical resolution. Geophysical modeling is not unique, overcoming this issue could be done using a global inversion method. A global inversion technique called Particle Swarm Optimization (PSO) was performed to create more reliable subsurface lithology, resulting in around 5 – 11% errors. The PSO algorithm deployed here took 1.000 particle numbers with ω=0.8; αl=1.8; and αg=2. The result shows that the study area’s lithology consists of Tuff, Sandy Tuffaceous, and Shaley Tuff. Sandy Tuffaceous is identified as a confining aquifer zone. There are two potential aquifer zones, Aquifer I and Aquifer II. Aquifer II has more potential as water resources of the industry due to its thickness, moreover, it is topped by impermeable Shaley tuff that prevents local climate effects such as rain that could decrease water quality.
Beneath the Surface: Identifying Subsurface Caves in "Gua Pandan" Using Integrated Electrical Profiling Method Antosia, Risky Martin; Akbar, Hendra Hidayat; Santoso, Nono Agus; Putri, Intan Andriani; Farishi, Bilal Al; Natalia, Happy Christin
POSITRON Vol 13, No 1 (2023): Vol. 13 No. 1 Edition
Publisher : Fakultas Matematika dan Ilmu Pengetahuan Alam, Univetsitas Tanjungpura

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.26418/positron.v13i1.63558

Abstract

One of the geopark tourism areas in East Lampung Regency, "Gua Pandan," has run into rock subsidence on the surface. As part of the subsidence prevention, indirect electrical methods between resistivity and chargeability profiling were applied to identify the presence of a subsurface cave in the study area. Two measurement lines were carried out with Wenner Alpha and Wenner Schlumberger arrays. Because the depth target is shallow (approximately 10 m) and to obtain a better resolution, each line has a stretch length of 70 m and 2 m electrode spacing. A line was measured over a known underground cave to produce a desired outcome, and the other was in an area with no cavities. Based on the results from each profile of resistivity and chargeability, an air-filled target has a value of over 5,000  and under 6 ms, respectively. Then, integrated processing of both methods generated a metal factor (MF) profile to view the presence and estimated shape of the cave/ cavities. The result represents that an MF value under 1.5 ms/Ωm is a cavity, and solid rock is over 1.5 ms/Ωm. Also, the MF level from both configurations delineates a similar section. However, a modest difference occurs in estimating the cavity shape geometry,  for Wenner Apha and  for Wenner Schlumberger. Furthermore, this study can be an initial step in safety assessment in the area.
Co-Authors Aganda, Riyanto Dedinta Akbar, Hendra Hidayat Al Farishi, Bilal Andreas Maruli Pakpahan Andri Yadi Paembonan Angga Jati Widiyatama Bilal Al Farishi Depri Dimas Setiawan Dimas Setiawan Ekawati, Gestin Mey Erlangga, Mokhammad Puput Faranabila, Syifa Farduwin, Alhada Farishi, Bilal Al Hissy Ijitiha Sari Hita Kirana Intan Adiani Putri Irawati, Selvi Misna Irawati, Selvi Misnia Natalia, Happy Christin Naufal, Rifqi Andi Nugraha, Purwaditya Octafiani, Aulia Pakpahan, Andreas Maruli Prima, Gilbert Purwaditya Nugraha Putri, Intan Andriani Putri, Uci Amelia Rahadian, Zatalini Syadni Ramdan, Muhammad Reza Rizki Rhahmi Adni Pesma Ruhul Firdaus Santoso, Nono Agus Sari, Hissy Ijitiha Sillak Hasiany Yudha Styawan