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Determination of Slope Safety Factor Based on Hoek & Brown Collapse Criteria on Ampera-Surumana Road Section Nugraha, Agung; Uno, Irianto; Asrafil, Asrafil
Tadulako Science and Technology Journal Vol. 5 No. 1 (2024): Tadulako Science and Technology Journal
Publisher : LPPM Universitas Tadulako

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.22487/sciencetech.v5i1.17178

Abstract

Introduction: One way to determine whether a slope is stable or not is by using the safety factor criterion. The method to determine the safety factor using the limit equilibrium method. Administratively the research area is located in the village of Salubomba, Central Banawa District, Donggala Regency, Central Sulawesi Province. The results of the study are also expected to be used as one of the basis for planning the design of stable slopes in the area Method: The methods used in this research were qualitative and quantitative. The process in this research was carried out with each method. The process of collecting secondary data and primary data is carried out by Geology and Geological Engineering methods both qualitatively and quantitatively. Results and Discussion: Observations in this study were made in the field in the form of observations of bridging on road slopes. The bruises in the study area are grouped on the basis of their shape and genetics. Through the results of observations and measurements on rock slopes at the research site. Based on data processing on the GEOSTUDIO 2018 R2 software application. Then, the value of the slope safety factor at observation station 1 is 2.316. Conclusion: Based on testing and analysis of the Hoek & Brown collapse criteria method, it can be concluded that the value of the slope safety factor at observation stations 1, 2, 3, 4, and 5 is 2.316; 2.029; 1.765; 1.658; 2.622 respectively. At station 4 the level of vulnerability is medium (Landslides can occur), at station 3 is at a low level of vulnerability (Landslides rarely occur), while at stations 1,2 and 5 are at a very low level of vulnerability (Landslides very rarely occur).
Distribution of Ground Temperature in the Geothermal Manifestation Area of Lompio, Donggala Regency, Central Sulawesi Province Sitti Rugayya; Badaruddin Badaruddin; Asrafil Asrafil
Jurnal Fisika Flux: Jurnal Ilmiah Fisika FMIPA Universitas Lambung Mangkurat Vol 20, No 3 (2023): Jurnal Fisika Flux: Jurnal Ilmiah Fisika FMIPA Universitas Lambung Mangkurat
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/flux.v20i3.12173

Abstract

The distribution of non-volcanic geothermal energy is widely found on the island of Sulawesi, one of which is in Lompio Village, Sirenja District, Donggala Regency, Central Sulawesi Province. It is important to study the geothermal potential in the village in order to learn how the geothermal system works. This study aims to identify the distribution pattern of temperature distribution in shallow soil depths as a manifestation of the geothermal system below the surface and its relation to geothermal manifestations that appear on the surface. This research was carried out through a series of field observations and direct soil temperature measurements in the study area using a thermometer. The results show that the distribution pattern of land temperature distribution in the high-temperature zone is associated with the presence of geothermal manifestation points on the surface (hot springs). The association of temperature and manifestation is possible because the presence of hot springs is an indication of a weak zone for the release of hydrothermal fluid from the geothermal system, which is correlated with the geological structure in the research area.
STUDY OF ORE MINERALIZATION POTENTIAL IN METAMORPHIC ROCKS IN KAWATUNA AREA, PALU CITY, CENTRAL OF SULAWESI Asrafil, Asrafil; Mukaddas, Abdul; Puspita, Riska; Assidiqi, Muhammad; Rugayya, Sitti
JGE (Jurnal Geofisika Eksplorasi) Vol. 11 No. 1 (2025)
Publisher : Engineering Faculty Universitas Lampung

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23960/jge.v11i1.484

Abstract

The Kawatuna area has a complex geological structure and lithological condition of metamorphic rock, which is estimated to be a weak zone for hydrothermal solutions to rise and then accumulate as mineralization of veins in the metamorphic rock. Based on this, it makes this area interesting to research. This research aims to identify metal ore minerals and the mineralization characteristics of ores in the research area. The method used is a geological survey of the surface and laboratory analysis through ore microscopic as well as mineral chemistry tests. Based on the results of the research study, it was found that in metamorphic rocks in the Kawatuna area, sulfide metal ore minerals were found including argentite (Ag2S), pyrite (FeS2), chalcopyrite (CuFeS2), sphalerite (ZnS), galena (PbS), and covelite minerals (CuS), Native elements ore minerals include gold (Au), silver (Ag), electrum (Au, Ag), and Oxide ore minerals in the form of hematite (Fe2O3). The mineralization formed is controlled by structures that produce fractures in the rock, which then produces mineralization as the veins of metamorphic rocks. The ore mineralization in the research area occurs through a hypogene process (the formation of a formation zone from primary ore minerals) and a supergene process stage (the formation of a formation or enrichment zone from secondary ore minerals).
Edukasi Mitigasi Bencana Banjir Bandang Di Desa Pulu Kecamatan Dolo Selatan Kabupaten Sigi Mulyati, Sri; Abdullah, Abdullah; Rusli, Rusli; Musa, Dahlan Th.; Kurniawan, Mauludin; Kasim, Sandra; Asrafil, Asrafil
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Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v2i3.33125

Abstract

Disaster education activities on flash floods were carried out in Pulu Village, Dolo District, Sigi Regency as an effort to increase community knowledge and preparedness against the threat of flash floods. The method used was a participatory approach involving the direct participation of the Pulu Village community, the Village Government, community leaders, and Disaster Response Youth. The stages of this community service activity included location observation, preparation, and implementation. The implementation stage was conducted through a socialization or outreach scheme in the form of a lecture. The purpose of the education was to introduce signs of flash flood hazards, risk knowledge, and emergency response planning. The educational activity received positive responses from the community, who actively engaged during the presentation, as well as appreciation from the village government. The presentation of materials accompanied by a simple simulation further enhanced the community’s understanding of self-rescue actions during a flash flood. The results of this activity indicate that interactive disaster mitigation education can effectively build community awareness and preparedness in facing flash flood threats.
Inventarisasi Situs-Situs Geologi Sebagai Potensi Geowisata di Kepulauan Togean, Provinsi Sulawesi Tengah Botjing, Muslimin U; ., Asrafil
Bomba: Jurnal Pembangunan Daerah Vol 1 No 2 (2019)
Publisher : Badan Riset dan Inovasi Daerah Sulawesi Tengah

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

Abstract

Togean Islands is one of the conservation areas in Central Sulawesi with the name Togean Islands National Park which has unique of geological resources and features to be used as a Geotourism area. This study aims to inventory the existence of unique geological sites that have the potential to become geotourism objects in the Togean Islands. The inventoriation method applied is field investigation and secondary data collection using literature studies. The results of the application of this investigation were obtained by a number of unique geosites in the Togean Islands including karst morphology, Tanimpu waterfalls, and volcanic landscapes including hot water manifestations, lithology and magmatic-volcanic rock structures in the form of intrusions and pillow lava. These geosites have the value of earth science education as an attractive geological object, have a beauty and economic value as a tourist attraction, and are supported by protection as a conservation area which is also promoted by the local government as a tourist destination, so that it has the potential to become a geotourism object in Central Sulawesi. Abstrak Kepulauan Togean merupakan salah satu wilayah konservasi di Sulawesi Tengah dengan nama Taman Nasional Kepulauan Togean yang memiliki sumberdaya dan kenampakan geologi yang unik untuk dijadikan kawasan Geowisata. Penelitian ini bertujuan untuk menginventarisasi keberadaan situs-situs geologi (geosites) unik yang berpotensi menjadi objek geowisata di Kepulauan Togean. Metode inventarisasi yang diterapkan yakni invesitigasi lapangan serta pengambilan data sekunder menggunakan studi literatur. Hasil penerapan investigasi ini diperoleh beberapa geosites yang unik di Kepulauan Togean meliputi kawasan morfologi kars, Air terjun Tanimpu, dan bentang alam vulkanik meliputi manifestasi air panas, litologi dan struktur batuan magmatik-vulkanik berupa intrusi dan lava bantal. Geosites tersebut memiliki nilai edukasi sains kebumian sebagai objek geologi yang menarik, memiliki nilai keindahan dan ekonomis sebagai objek wisata, serta didukung oleh proteksi sebagai kawasan konservasi yang dipromosikan pula oleh pemerintah daerah sebagai destinasi wisata, sehingga sangat potensial menjadi objek geowisata di Sulawesi Tengah.
PENENTUAN ZONASI TINGKAT KERAWANAN GERAKAN TANAH DI KECAMATAN MARAWOLA KABUPATEN SIGI SULAWESI TENGAH Botjing, Muslimin U; Halawa, George Cordias Mulyanto; ., Asrafil
Bomba: Jurnal Pembangunan Daerah Vol 3 No 1 (2023)
Publisher : Badan Riset dan Inovasi Daerah Sulawesi Tengah

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Abstract

ABSTRAK Secara geografis daratan di wilayah Kabupaten Sigi didominasi oleh daerah perbukitan dan pegunungan. Kondisi dataran perbukitan dan pegunungan dapat menyebabkan peristiwa gerakan tanah. Kejadian gerakan tanah diikuti banjir bandang yang terjadi pada 26 Maret 2021 telah menyebabkan kerusakan infrastruktur dan jatuhnya korban jiwa di Desa Beka Kecamatan Marawola. Penelitian ini bertujuan untuk mengetahui tingkat kerawanan gerakan tanah dan mengetahui penyebaran spasial daerah kerawanan gerakan tanah di Kecamatan Marawola menggunakan metode skoring dan overlay berbasis sistem informasi geografis. Pada penelitian ini ada delapan parameter yang diamati yaitu kemiringan lereng, arah lereng, bentuk lereng, jenis tanah, kedalaman tanah, jenis litologi, jarak patahan dan curah hujan yang diperkuat dengan hasil observasi di lapangan untuk mengidentifikasi gerakan tanah pada daerah penelitian. Hasil penelitian di dapatkan 3 kelas tingkat kerawanan yaitu kerawanan gerakan tanah rendah dengan luas 9,565 Km2 atau 22,918% dari luas Kecamatan Marawola meliputi wilayah Desa Tinggede, Desa Tinggede Selatan, Dan Desa Sunju, kemudian kerawanan gerakan tanah sedang dengan luas 18,095 Km2 atau 43,484 % dari luas daerah penelitian meliputi wilayah Desa Baliase, Desa Boyabaliase, Desa Binangga, Desa Padende, Desa Sibedi, Desa Beka dan Desa Bomba, kerawanan gerakan tanah tinggi dengan luas 13,953 Km2 atau 32,598% dari luas Kecamatan Marawola meliputi wilayah Desa Padende, Desa Lebanu, Desa Sibedi dan Desa Beka.
Penerapan Media Microsoft Word Pada Era Digital Dalam Dasar-Dasar Pengolahan Teks di MTS Muhammadiyah Asrafil, Asrafil; Rahmawan, Ardi; Ramdhani, Lisda
Infomatika: Pendidikan Informatika Vol 4, No 2 (2025): Oktober 2025
Publisher : STKI Harapan Bima

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.56842/infotika.v4i2.722

Abstract

The development of digital technology has brought significant changes in the field of education, particularly in the use of software such as Microsoft Word as a learning tool. This study aims to analyze students' understanding of basic and advanced features of Microsoft Word, identify obstacles faced in its academic use, and provide recommendations for effective mentoring strategies. A descriptive quantitative method was employed, using a Likert-scale questionnaire and semi-structured interviews involving 20 students from grades VII–IX and 2 teachers at MTS Muhammadiyah, Bima Regency. The results indicate a notable improvement in learning outcomes among students who actively used Microsoft Word compared to the control group, with the majority (70%) giving highly positive responses to its implementation. In addition to enhancing material comprehension and text processing skills, Microsoft Word has also proven effective in creating a more engaging and interactive learning environment. However, limitations in the use of advanced features were still observed due to insufficient guidance. Therefore, structured training for both teachers and students is essential to optimize the use of Microsoft Word in 21st-century digital learning
Index Morphotectonic Of Morphology In The Patukuki Watershed Region, Peling Tengah District, Banggai Kepulauan Sukardan Tawil; Bayu Saputra; Abdul Mukaddas; Asrafil
Tadulako Science and Technology Journal Vol. 1 No. 2 (2021): Tadulako Science and Technology Journal
Publisher : LPPM Universitas Tadulako

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.22487/sciencetech.v1i2.17297

Abstract

Introduction: The Patukuki area in the Central Peling sub-district falls administratively within the geographical coordinates of 123°01'00" – 123°01'3" longitude and 01°24'00" – 01°27'00" latitude. Method: Channel Sinuosity (S) measures river influence on landscapes by comparing actual river length to valley length. Mountain-front sinuosity (Smf) evaluates mountain-front curvature using base and straight-line lengths. The Valley Floor Width to Width-to-height ratio (Vf) identifies regions of rapid uplift, with lower values indicating higher activity. The Asymmetric Factor (AF) detects tectonic tilting in drainage basins by comparing the area of the right-hand side sub-basin to the total area. Results and Discussion: Based on the analysis conducted, the findings are as follows: Channel Sinuosity analysis shows that sub-bases 1, 2, and 3 have high tectonic activity, while sub-base 5 has moderate activity, and sub-base 3 is low. Stream Morphology Frequency (Smf) analysis shows moderate tectonic activity in sub-bases 1, 3, 4, and 5, and sub-base 2 with an average Smf value of more than 1.5. Valley floor width to height ratio (Vf) shows low tectonic activity in all sub-bases. Anisotropy of Magnetic Susceptibility (AF) shows that sub-bases 1 and 5 have high tectonic activity, sub-bases 3 and 4 are moderate, and sub-base 3 is low. The IATR values of sub-bases 1, 4, and 5 are between 1.5 and less than 2, while sub-bases 2 and 3 show moderate tectonic activity with IATR values between 2 and less than 2.5.Conclusion: In summary, tectonic activity in the Patukuki watershed ranges from moderate to high based on the various analyzed indices.
Edukasi Ilmu Kebumian Dan Potensi Kebencanaan Geologi Bagi Siswa SMA Negeri 1 Sarjo Janat, Nunik Rezkiarti; Fitriana, Tati; Asrafil, Asrafil; Mukaddas, Abdul; Nugroho Uno, Djamal Adi; Mulyati, Sri
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Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v2i4.35324

Abstract

Considering the geological complexity of Sulawesi and the limited exposure of students to basic geoscience knowledge in formal education, SMA Negeri 1 Sarjo, located in West Sulawesi and bordering Central Sulawesi, recognized the need to conduct a knowledge-sharing activity on earth science, geological resources, and geological hazards. This program invited academic experts from the Faculty of Engineering, Universitas Tadulako, to deliver educational materials tailored for high school students. The main objective was to enhance students’ understanding of geoscience concepts, introduce the diversity of geological resources, and increase awareness of geological hazards, particularly those prevalent in Sulawesi. The activity involved grade XII students through presentations, discussions, and interactive question-and-answer sessions. Students and teachers responded positively, indicating increased interest and comprehension of the topics presented. The positive feedback and appreciation expressed by the school, especially through the Vice Principal for Curriculum and Student Affairs, served as an indicator of the program’s success.
Penentuan Kestabilan Lereng Batuan Menggunakan Limit Equilibrium Method (LEM) Di Ruas Jalan Trans Palu-Kulawi Desa Salua Kabupaten Sigi I Ketut Nuarta; Nunik Rezkiarti Janat; Ahmad Imam Abdullah; Asrafil; Abdul Mukaddas
MEDIA KONSTRUKSI Vol. 9 No. 4 (2024)
Publisher : Jurusan Teknik Sipil, Universitas Halu Oleo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.33772/jmk.v9i4.147

Abstract

Ruas jalan Desa Salua di Kabupaten Sigi, Sulawesi Tengah, dinilai rawan longsor akibat kondisi geologi, geometri lereng, dan guncangan gempa seperti pada tahun 2018. Penelitian ini bertujuan menilai kestabilan lereng sebagai acuan perencanaan struktural guna meminimalkan risiko longsor. Interpretasi tingkat kestabilan lereng merujuk dari nilai faktor keamanan (FS) yang diperoleh dari penerapan limit equilibrium method (LEM) menggunakan kaidah Bishop. Penelitian diawali dengan identifikasi litologi lereng berupa diorit dari Formasi Batuan Terobosan. Estimasi sifat mekanika batuan dilakukan melalui kriteria Hoek-Brown, Geological Strength Index (GSI), dan uji berat isi di laboratorium untuk memperoleh parameter Mohr-Coulomb. Model lereng kemudian dianalisis dalam kondisi dinamis dengan asumsi adanya guncangan. Hasil menunjukkan nilai faktor keamanan (FS) secara deterministik sebesar 6,191 dan probabilitas kelongsoran (PF) sebesar 2,493%. Meski nilai FS menunjukkan lereng stabil (FS > 1), potensi longsor parsial tetap ada akibat pelapukan tidak merata. Riwayat longsor di lokasi membuktikan bahwa guncangan berperan signifikan, sehingga diperlukan penanganan seperti tanggul penahan, paku bumi, geotekstil, serta rekayasa geometri lereng guna meningkatkan kestabilan terhadap guncangan.