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All Journal BULETIN OSEANOGRAFI MARINA Jurnal Fisika Unand Jurnal Geocelebes Buletin Sumber Daya Geologi Jurnal Pendidikan Fisika dan Teknologi Indonesian Physical Review Journal of Technomaterial Physics Aceh International Journal of Science and Technology Jurnal Fisika
Al Ansory, Andre Rahmat
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Agriculture, Biological Sciences & Forestry Astronomy Chemical Engineering, Chemistry & Bioengineering Civil Engineering, Building, Construction & Architecture Control & Systems Engineering Decision Sciences, Operations Research & Management Earth & Planetary Sciences Education Electrical & Electronics Engineering Energy Engineering Environmental Science Materials Science & Nanotechnology Physics

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Mapping Flood-Prone Areas Using GIS Through as Geo-Artificial Intelligence (Geo-Ai) Approach in Bengkulu City Apriana, Agnes; Al Ansory, Andre Rahmat; Agustina, Tari; Amalia, Isra; Refrizon, Refrizon
Journal of Technomaterial Physics Vol. 6 No. 1 (2024): Journal of Technomaterial Physics
Publisher : Talenta Publisher

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.32734/jotp.v6i1.16006

Abstract

Bengkulu City is an area prone to flooding due to its proximity to the river estuary. Flooding in Bengkulu City usually occurs during the rainy season, when high rainfall and overflowing rivers can cause inundation in several areas around the city. This research aims to identify flood-prone areas in Bengkulu City through a Geographic Artificial Intelligence (Geo-AI) approach. Geo-AI is an artificial intelligent machine with geospatial data, including satellite images and weather data, whose data analysis is more accurate and efficient in identifying flood-prone areas. Geographic Information System (GIS) can present objects of flood-prone areas from the real world in digital form. Through Google Earth Engine (GEE), satellite imagery data and other geospatial data are processed and analyzed using artificial intelligence algorithms to identify flood patterns and frequently flooded areas. The final result of this research is a map of flood-prone areas in Bengkulu City. On the map, it can be concluded that the red-colored areas including Rawa Makmur, Tanjung Agung, Bentiring, Kebun Tebeng, Penurunan, Sukarami, Pekan Sabtu, and Air Sebakul are areas that are often flooded so that these areas can be confirmed as flood-prone.
Pemanfaatan Citra Satelit Dan Multichannel Analysis of Surface Waves (MASW) Untuk Mitigasi Bencana Abrasi Desa Urai, Bengkulu Rahmawati, Nur Shafira; Farid, Muchammad; Refrizon, Refizon; Al Ansory, Andre Rahmat
Buletin Oseanografi Marina Vol 13, No 3 (2024): Buletin Oseanografi Marina
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/buloma.v13i3.63278

Abstract

Desa Urai merupakan salah satu desa yang terkena dampak abrasi parah di Kabupaten Bengkulu Utara. Abrasi yang terjadi menyebabkan perubahan garis pantai sehingga mengakibatkan kerusakan sarana dan prasarana yang ada di pantai. Pada riset ini memperoleh data primer menggunakan metode MASW dan data sekunder berupa data garis pantai pesisir Desa Urai selama 16 tahun (2006-2022) dengan menggunakan citra satelit. Analisis perubahan garis pantai Desa Urai, Kabupaten Bengkulu Utara dari 2006 hingga 2022 menunjukkan adanya abrasi signifikan. Titik-titik utama mengalami abrasi sekitar ±8 meter/tahun, sedangkan titik dengan perlindungan pantai memiliki abrasi minimal, hanya sekitar 0,1-0,5 meter/tahun. Ini menunjukkan keberhasilan infrastruktur perlindungan pantai dalam mengurangi dampak abrasi. Penelitian menemukan perubahan garis pantai rata-rata ±8 meter/tahun. Analisis menggunakan MASW dan citra satelit menunjukkan abrasi terparah di titik 1, 2, 4, 6, dan 8 (±3,4-8 meter/tahun), sedangkan titik 3 dan 7 mengalami abrasi paling rendah (±0,1-0,5 meter/tahun). Struktur batuan pada kedalaman ±30 meter terdiri dari 3 lapisan. Penelitian bertujuan untuk mitigasi bencana abrasi demi pembangunan berkelanjutan dari pemerintah provinsi hingga desa di Desa Urai, Kabupaten Bengkulu Utara. Urai Village is one of the villages affected by severe abrasion in North Bengkulu Regency. The abrasion that occurs causes changes in the coastline, causing damage to the facilities and infrastructure on the beach. In this research, primary data was obtained using the MASW method and secondary data in the form of coastal coastal data of Urai Village for 16 years (2006-2022) using satellite imagery. Analysis of changes in the coastline of Urai Village, North Bengkulu Regency from 2006 to 2022 showed significant abrasion. The main points experience abrasion of about ±8 meters/year, while the points with coastal protection have minimal abrasion, only about 0.1-0.5 meters/year. This shows the success of coastal protection infrastructure in reducing the impact of abrasion. Research found an average change in the coastline of ±8 meters/year. Analysis using MASW and satellite imagery showed the worst abrasion at points 1, 2, 4, 6, and 8 (±3.4-8 meters/year), while points 3 and 7 experienced the lowest abrasion (±0.1-0.5 meters/year). The rock structure at a depth of ±30 meters consists of 3 layers. The research aims to mitigate abrasion disasters for sustainable development from the provincial government to the village in Urai Village, North Bengkulu Regency.
Perubahan Garis Pantai Rawan Gempabumi di Lokasi Terabrasi Menggunakan Data Geofisika Priscilla, Viona Azhari; Farid, Muchammad; Lidiawati, Liza; Al Ansory, Andre Rahmat
Buletin Oseanografi Marina Vol 14, No 1 (2025): Buletin Oseanografi Marina
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/buloma.v14i1.64643

Abstract

Kabupaten Bengkulu Utara mempunyai garis pantai yang panjangnya sekitar 262,63 km dan berada di wilayah rawan Gempabumi yang ditunjukkan dengan besarnya nilai Peak Ground Acceleration (PGA > 300). Salah satu sumber daya pesisir di Kabupaten Bengkulu Utara yang memberikan manfaat bagi masyarakat setempat adalah kawasan di sepanjang pantai. Namun, manfaat bagi masyarakat sekitar terancam akibat fenomena abrasi di wilayah pesisir. Kabupaten Bengkulu Utara merupakan kabupaten ke-70 di indonesia yang rentan terhadap bencana abrasi pantai, sehingga masuk dalam kategori kabupaten yang sangat rentan terhadap bencana jenis tersebut. Desa Urai merupakan salah satu wilayah yang rentan terhadap abrasi pantai di Kabupaten Bengkulu Utara. Berdasarkan keadaan yang terjadi di Desa Urai, maka perlu dilakukan penelitian untuk mengetahui kecepatan perubahan garis pantai menggunakan data Citra Satelit dan data Seismik Pasif dalam bentuk kecepatan gelombang geser ( ) dengan menggunakan metode HVSR (Horizontal to Vertical Spectral Ratio). Hasil penelitian menunjukkan daerah yang mengalami abrasi memiliki kecepatan perubahan garis pantai pada rentang antara 1,41-5,04 m/tahun, dengan kecepatan gelombang geser ( ) antara 176,30-237,12 m/s. Daerah yang mengalami abrasi memiliki nilai kecepatan perubahan garis pantai yang tinggi yang didukung dengan nilai  rendah yang mengindikasikan klasifikasi tanah berada pada jenis tanah lunak sampai sedang. 
Estimation of Geothermal Potential Area in Kabawetan Sub-District, Using 2D Magnetotelluric Inversion Method Gumanty, Usman; Farid*, Muchammad; Refrizon, Refrizon; Azzahra, Gusti Ayu Zahwa; Nurhayati, Ratna Dewi; Al Ansory, Andre Rahmat; Raihana, Hana
Aceh International Journal of Science and Technology Vol 14, No 1 (2025): April 2025
Publisher : Graduate School of Universitas Syiah Kuala

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13170/aijst.14.1.44628

Abstract

Kabawetan is located in the subduction zone of the magmatic arc in the Indonesian tectonic system. The geothermal energy potential in this region is closely tied to volcanic activity, which is prevalent along the Ring of Fire on the island of Sumatra. This study aims to identify the distribution of subsurface resistivity values related to geothermal potential in the Kabawetan Region. To achieve this, the magnetotelluric (MT) method is used, utilizing electrical and magnetic sensors. Data were collected using two horizontal electrical sensors (Ex, Ey) and three magnetic sensors, including two horizontal sensors (Hx, Hy) and one vertical sensor (Hz). Measurements using the magnetotelluric method can be used to determine the subsurface rock layers based on resistivity values. The results of data processing yield a 2D cross-section of the resistivity value, which characterizes the potential for geothermal energy. This study used four measurement points to analyze resistivity variations and determine geothermal potential. Field measurement data were processed using MAPROS software, and a 2D cross-section model was created using ZONDMT2D. The results showed that resistivity values of 20-60 m, thought to be impermeable overburden, were at depths of 0-1.5 km and 2.5-4 km, resistivity values of 0.54-1 m indicated permeable reservoirs at depths of 1.5-2.5 km, and resistivity values of 290-550 m indicated geothermal rocks at depths of 4-10 km. The findings of this research are expected to enhance the understanding of geothermal energy as a renewable resource, thereby supporting the Sustainable Development program.
DELINEASI NILAI RESISTIVITAS DI LAPANGAN PANAS BUMI TAMBANG SAWAH MENGGUNAKAN METODE MAGNETOTELLURIK Al Ansory, Andre Rahmat; Hana Raihana; Pritama, Vinki Loverly; Saputri, Welly; Maghribi, Faritz Bagda; Muchammad Farid; Arif Ismul Hadi; Halauddin; Harlianto, Budi; Sugianto, Nanang
Buletin Sumber Daya Geologi Vol 18 No 3 (2023): Buletin Sumber Daya Geologi
Publisher : Pusat Sumber Daya Mineral Batubara dan Panas Bumi

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.47599/bsdg.v18i3.386

Abstract

The subsurface structure of the geothermal field in Desa Tambang Sawah has been mapped. This research aims to delineate the resistivity values in the area of Tambang Sawah Village, Lebong Regency, Bengkulu Province based on magnetotelluric measurements which can later identify low, medium, and high resistivity values to interpret geothermal in the research area. The magnetotelluric (MT) method with electrical and magnetic sensors is used to collect data in the field. There are two electrical sensors in horizontal direction (Ex, Ey) and three magnetic sensors in horizontal direction. (Hx, Hy) and vertical (Hz). The results obtained from this study are that resistivity values of 20-50 ohm.m are considered as reservoirs, while resistivity of 0.26-0.8 ohm.m is considered as caprock, and resistivity greater than 300 ohm.m is considered as hot rock.
DELINEASI PROSPEK PANAS BUMI DI KAWASAN WISATA AIR PUTIH KABUPATEN LEBONG BENGKULU MENGGUNAKAN METODE MAGNETOTELURIK : GEOTHERMAL PROSPECT DELINEATION STUDY IN AIR PUTIH TOURISM AREA LEBONG DISTRICT BENGKULU USING MAGNETOTELLURIC METHOD Della Zakia Soleha; Farid, Muchammad; Refrizon; Maesaroh, Rina; Hardianza, Meno; Hasugian, Basdiki; Gea, Jessica Agnes Soroinama; Al Ansory, Andre Rahmat
Buletin Sumber Daya Geologi Vol 20 No 1 (2025): Buletin Sumber Daya Geologi
Publisher : Pusat Sumber Daya Mineral Batubara dan Panas Bumi

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.47599/bsdg.v20i1.488

Abstract

Geothermal energy is renewable and can be used as an energy reserve in the future. This research aims to determine locations that have geothermal potential in the Air Putih Tourism area, Lebong Regency, Bengkulu Province based on resistivity values using the magnetoteluric method. The resistivity values obtained vary from low, medium, and high which can be used as a reference to describe subsurface conditions. In this data acquisition, measurements were made using the ADU-07e Magnetotelurik tool which has a measurement time of 16 hours with a low frequency bandwidth of 128 Hz, a medium frequency bandwidth of 1024 Hz, and a high frequency bandwidth of 4096 Hz. The sensor in the recording has two sensors: a magnetic sensor and an electrical sensor. The magnetic sensor consists of 3 sensors/coils (Hx, Hy, and Hz), while the electrical sensor uses 4 orthogonally placed pot shafts (Ex and Ey). Based on the results of data processing using the Magnetoteluric method with ZondMT software, there is a range of resistivity values of 10-700 (Ωm) which provides information on the structure of the subsurface layer. Layers with low resistivity (18-30 Ωm), medium resistivity (40-160 Ωm) and the highest resistivity (>300 Ωm).
ABRASION INVESTIGATION USING SHEAR WAVE VELOCITY AND POISSON’S RATIO APPROACHES IN URAI VILLAGE NORTH BENGKULU REGENCY Sesilia, Tiara; Farid, Muchammad; Hadi, Arif Ismul; Al Ansory, Andre Rahmat
Indonesian Physical Review Vol. 8 No. 1 (2025)
Publisher : Universitas Mataram

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/ipr.v8i1.348

Abstract

The coastal areas of North Bengkulu Regency, particularly Urai Village, have been severely impacted by widespread abrasion, posing a high risk of coastal erosion within Bengkulu Province. This study aims to assess the extent of coastal degradation and support disaster mitigation efforts by investigating the properties and structure of rocks using geophysical methods, specifically the Multichannel Analysis of Surface Waves (MASW). The research focuses on determining shear wave velocity (Vs) to model the rock layers and produce a stratigraphic profile with a minimal misfit value. The obtained Vs30 values, ranging from 146 m/s to 603 m/s, indicate that the coastal region primarily comprises soft soils, which are highly susceptible to deformation, including abrasion. These findings provide essential data for understanding the underlying causes of coastal erosion and contribute to future disaster mitigation strategies.
CHARACTERIZATION OF GEOTHERMAL POTENTIAL USING 2D MAGNETOTELLURIC INVERSION AT TELAGA TUJUH WARNA, LEBONG REGENCY, BENGKULU PROVINCE, INDONESIA Maesaroh, Rina Maesaroh; Farid, Muchammad; Refrizon, Refrizon; Sumajaya, Erlan; Al Ansory, Andre Rahmat; Naldo, Asrol
Indonesian Physical Review Vol. 8 No. 3 (2025)
Publisher : Universitas Mataram

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/ipr.v8i3.478

Abstract

The Telaga Tujuh Warna area in Lebong Regency exhibits geothermal manifestations such as hot water, mud craters, and fumaroles. This research aims to characterize the geothermal potential using 2D Magnetotelluric (MT) inversion. Measurements were conducted with the ADU-07e Magnetotelluric device, involving a 16-hour measurement period. Data collection followed the sounding principle with three frequency levels: high (4096 Hz), medium (1024 Hz), and low (128 Hz), spaced approximately 500 meters apart. Analysis confirms the consistency between 1D and 2D resistivity models, generating a resistivity distribution cross-section. Key findings include: (1) a low-resistivity cap layer (20–40 Ω-m) at approximately 1 km depth; (2) a medium-resistivity reservoir (40–160 Ω-m) at depths of 1–2 km; (3) a high-resistivity geothermal resource (>300 Ω-m) at depths of 1–2.5 km; and (4) a zone with very low resistivity values (2–16 Ω-m) at depths less than 1 km, potentially indicating a fumarole emitting hot water vapor and gas through rock fractures. These findings aim to advance geothermal exploration in Lebong Regency and support Indonesia's renewable energy objectives.
Investigation of Sediment Layer Thickness Estimation at Bengkulu University Hospital Based on Microtremor Data Al Ansory, Andre Rahmat; Raihana, Hana; Farid, M; Hadi, Arif Ismul
JURNAL GEOCELEBES Vol. 8 No. 1: April 2024
Publisher : Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20956/geocelebes.v8i1.28144

Abstract

Bengkulu is the capital of Bengkulu Province and is located in the subduction zone between the Eurasian and Indo-Australian plates. Bengkulu is also close to the major faults of Sumatra, namely the Musi fault, the Ketahun fault, and the Manna fault. Therefore, regional planning and infrastructure development for earthquake mitigation is necessary. The purpose of this study is to estimate the thickness of the sedimentary layers in the construction zone of Bengkulu Hospital during the earthquake attenuation phase. This study is conducted by surface geological analysis using the HVSR method; data analysis using microtremor data. The microtremor data were analyzed using the HVSR method to obtain the amplification value (A0) and the dominant frequency (f0). HVSR analysis gave dominant frequency (f0) values from 5.1 to 5.8 Hz, amplification (A0) from 1.64 to 5.91 times, and dominant period (T0) from 1.49 to 2.81 seconds. The values of A0, f0, T0 are interpreted with reference to the literature and surface geology as a moderate risk of seismic vulnerability, characterized by moderate to weak sedimentation and moderate amplification values.
Identification of Sub-Fault Zone Using Magnetotelluric Inversion (Case Study: Ketaun Fault, Lemeu Village, Lebong Regency) Rahmawati, Nurul Ilmi; Farid, Muchammad; Hadi, Arif Ismul; Al Ansory, Andre Rahmat
JURNAL GEOCELEBES Vol. 8 No. 2: October 2024
Publisher : Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.70561/geocelebes.v8i2.34588

Abstract

Lemeu Village, Lebong Regency, borders the Bukit Barisan Mountain range and is crossed by the Ketaun Fault, which causes a high level of seismic activity, so it is necessary to conduct research on the potential existence of the Ketaun sub-fault as one of the efforts to mitigate natural disasters such as earthquakes. The Magnetotelluric method utilises the earth's natural electromagnetic field, which is used to determine the distribution of resistivity in the subsurface using the ADU-07e Magnetotelluric tool with two horizontal electrical sensors (Ex, Ey) and three horizontal (Hx, Hy) and vertical (Hz) magnetic sensors and uses seven research points with an interval of 1 km. Data processing uses MAPROS software to convert data from the time domain to the frequency domain and ZONDMT2D to obtain subsurface resistivity values. The results obtained from this study are 2D magnetotelluric cross sections showing a zone with low resistivity values between research points P4 and P5 which is thought to be a new fault zone with resistivity values ranging from 1.3 – 6.1 Ωm from a depth of 2.5 km to a depth of 10 km. The zone is assumed to be a new fault that is a branch of the Ketaun fault.
Co-Authors Abimayu, Dadin Mars Agustina, Tari Al Akbar, M Riski Al Rafly, Tegar Amalia, Isra Apriana, Agnes Apriana, Yelda Arif Ismul Hadi Arif Ismul Hadi Azzahra, Gusti Ayu Zahwa Della Zakia Soleha Farid*, Muchammad Farid, M Farid Farid, Muchammad Fauzi, M. Wilzam Gea, Jessica Agnes Soroinama Gumanty, Usman Halauddin Halauddin Halauddin Hana Raihana Hardianza, Meno Harlianto, Budi Hasugian, Basdiki Jaya, Shara Ashari Prana Jaya Kamila, Nur Husniatin Lizalidiawati Lizalidiawati M Farid Maesaroh, Rina Maesaroh, Rina Maesaroh Maghribi, Faritz Bagda Muchammad Farid Naldo, Asrol Nanang Sugianto Nurhayati, Ratna Dewi Nurul ‘Ilmi Rahmawati Olga Triutami Priscilla, Viona Azhari Pritama, Vinki Loverly Rabbani, M Rifqi Rahmawati, Nur Shafira Rahmawati, Nurul 'Ilmi Rahmawati, Nurul Ilmi Raihana, Hana Refrizon Refrizon Refrizon Refrizon, Refizon Saputri, Welly Sesilia, Tiara Sholeha, Della Zakia Suhendra Suhendra Sumajaya, Erlan Tri Utami, Olga Ulandari, Clora Wijaya Kusuma, Repal Yuni Setyowati