Article Per Year (5 Year)
p-Index From 2021 - 2026
0.61
P-Index
This Author published in this journals
All Journal Jurnal Penelitian Fisika dan Aplikasinya (JPFA) Jurnal Geosains dan Teknologi Computational and Experimental Research in Materials and Renewable Energy (CERiMRE)
Fadrian, Dhika Faiz
Unknown Affiliation
Astronomy Computer Science & IT Earth & Planetary Sciences Education Energy Engineering Environmental Science Materials Science & Nanotechnology Physics

Published : 3 Documents Claim Missing Document
Claim Missing Document
Check
Articles

Found 3 Documents
Search

 1 
Identifikasi Sistem Panasbumi Hu’u Daha Kabupaten Dompu, Nusa Tenggara Barat Menggunakan Pemodelan 3D Inversi Metode Gravitasi, Analisis Derivative dan Land Surface Temperature Restiana, Andini; Sari, Feby Puspita; Fadrian, Dhika Faiz; Anjali, Delia; Firmansyah, Aep
Jurnal Geosains dan Teknologi Vol 6, No 2 (2023): Juli 2023
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/jgt.6.2.2023.90-103

Abstract

Ketergantungan pada energi fosil terus meningkat seiring dengan meningkatnya tuntutan kehidupan. Oleh karena itu, ketergantungan kita pada energi fosil perlu dialihkan dengan menggunakan energi panasbumi. Salah satu daerah prospek panasbumi di Kabupaten Dompu, Provinsi Nusa Tenggara Barat adalah Hu’u Daha 35 km di sebelah timur Kabupaten Dompu memiliki potensi terduga ±69 MW. Penelitian lebih lanjut dilakukan pada sistem panasbumi Hu’u Daha melalui korelasi analisis peta Land Surface Temperature (LST), analisis derivative, dan pemodelan inversi 3D sehingga dapat diketahui dugaan keterdapatan lapisan reservoir berupa batuan lava dan breksi berkomposisi andesit dan basalt serta sisipan batuan tufa dengan rerata kedalaman 633 – 1500 m dengan nilai densitas 3,4 - 3,33 gr/cm3 yang dilingkupi oleh lapisan cap rock berupa batuan lava hasil erupsi dengan kedalaman rata-rata 0 – 633 m dengan nilai densitas 3,51 – 3,44 gr/cm3, serta terdapat 11 patahan yang mengontrol sistem panasbumi berupa 2 strike-slip fault, 7 normal fault, dan 2 reverse fault. Berdasarkan analisis peta Land Surface Temperature (LST) yang di overlay dengan peta geologi dapat diketahui pula persebaran suhu permukaan daerah Hu’u Daha berkisar antara 26°C – 28,4°C. 
Identification of Geothermal Potential in Block Ciasmara Sector II, Mount Salak Area, Based on the Correlation of the Active Directory Magnetotelluric (ADMT) and Self-Potential Methods Permana, Nanda Ridki; Fadrian, Dhika Faiz; Gunawan, Belista; Primastika, Ayu Alvita; Zani, Fardhan Rafshan; Rahman, Fadhlur; Binonkan, Zahra Prameswari; Subekti, Faris Fawwas; Melly, Melly; Bahagia, Tazkia Izdihar; Harist, Ahmad Rizieq
Computational And Experimental Research In Materials And Renewable Energy Vol 6 No 2 (2023): November
Publisher : Physics Department, Faculty of Mathematics and Natural Sciences, University of Jember

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.19184/cerimre.v6i2.43848

Abstract

Indonesia possesses significant geothermal potential, with the largest share located in West Java, accounting for up to 21.7% distributed across 44 locations in 11 regencies. One such location with geothermal potential is in Block Ciasmara Sector II, the Mount Salak area, Bogor Regency, characterized by manifestations such as hot spring bathing pools. This research aims to understand the distribution of geothermal reservoirs in the study area, where these reservoirs contain hot fluids that can be harnessed for renewable energy generation. The methodology used in this research involves a correlation between the Active Directory Magnetotelluric (ADMT) and Self-Potential (SP) methods. A total of 3 ADMT measurements were conducted along tracks ranges from 5-8 meters, while the SP method involved 7 measurement points with coordinates distributed around the geothermal manifestations in the Mount Salak area. The data obtained were then visualized in 2D and 3D to gain insights into the distribution and orientation of the reservoir layers in the study area. The results indicate a correlation between the ADMT and Self-Potential methods. In Line 01 of the ADMT, located in the western part, there is a correlation with high potential difference values on the SP map ranges from 47.6-82.1 mV, suggesting the presence of tuff layers rich in alteration minerals. This is confirmed by the 2D ADMT modeling, which shows that the clay cap is thicker compared to Line 02 and Line 03, associated with the presence of alteration minerals in the clay cap. This correlation also applies to Line 03, which has low potential difference values ranges from 4.9-25.3 mV, indicating a response from lapilli rocks. This is corroborated by the 2D model, which reveals thickening of the lapilli rock layer on Line 03.Keywords: ADMT, Geothermal, Mount Salak, Reservoir, Self-Potential.
Distribution of Geological Structures on Java Island Based on Derivative Analysis of Satellite Gravity Data Permana, Nanda Ridki; Fadrian, Dhika Faiz; Gunawan, Belista; Wulandari, Amara
Jurnal Penelitian Fisika dan Aplikasinya (JPFA) Vol. 14 No. 2 (2024)
Publisher : Universitas Negeri Surabaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.26740/jpfa.v14n2.p154-168

Abstract

The island of Java is an interesting place to study geology because of the various tectonic processes that occur starting from volcanic activity, changes in relief, and the relative movement of faults. The aim of this research is to determine the distribution of geological structures spread throughout Java Island based on fault analysis from gravity satellite data. Gravity data was taken via the ICGEM website with a data resolution of 2 km so that 10,000 data were obtained consisting of gravitational disturbances (GD), geoid, and Digital Elevation Model (DEM). The data processing results represent weak zones on the residual anomaly map where fault movement occurs with low anomaly values, namely -55,147 – (-27,175) mGal which stretches from West Java to southern Madura. On the FHD map, it can be seen that the distribution of maximum gravity anomalies is quite numerous and complex with an anomaly value of 1117.18 mGal. It is suspected that the fault near the mountain occurred due to volcanic processes and the southern part occurred due to the shifting process of the Indo-Australian plate and the Eurasian plate. On the TDR map, the weak zones caused by faults spread across Java Island have low gravity anomaly values ranging from -1,353 – (-0.833) mGal. In the Banten to West Java area there are the Baribis Fault and the Cimandiri Fault. In the Central Java region there are the Ajibarang, Ungaran, Baribis Kendeng and Pati faults, as well as parts of the Special Region of Yogyakarta there is the Opak fault. Meanwhile, in the East Java area there are the Baribis Kendeng, Pasuran and Probolinggo faults.
Co-Authors Anjali, Delia Bahagia, Tazkia Izdihar Binonkan, Zahra Prameswari Fadhlur Rahman, Fadhlur Firmansyah, Aep Gunawan, Belista Harist, Ahmad Rizieq Melly, Melly Permana, Nanda Ridki Primastika, Ayu Alvita Restiana, Andini Sari, Feby Puspita Subekti, Faris Fawwas Wulandari, Amara Zani, Fardhan Rafshan