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All Journal Jurnal RISET Geologi dan Pertambangan Journal of the Civil Engineering Forum JIPF (Jurnal Ilmu Pendidikan Fisika) Journal of Environment and Sustainability Jurnal Mineral, Energi dan Lingkungan Angkasa: Jurnal Ilmiah Bidang Teknologi KURVATEK Jurnal Mineral, Energi dan Lingkungan International Journal of Hydrological and Environmental for Sustainability Prosiding Seminar Nasional Rekayasa Teknologi Industri dan Informasi ReTII Jurnal Kemitraan, Kewirausahaan dan Pengabdian Masyarakat
Al Hussein Flowers Rizqi
Institut Teknologi Nasional Yogyakarta
Aerospace Engineering Agriculture, Biological Sciences & Forestry Automotive Engineering Chemical Engineering, Chemistry & Bioengineering Civil Engineering, Building, Construction & Architecture Computer Science & IT Control & Systems Engineering Decision Sciences, Operations Research & Management Earth & Planetary Sciences Education Electrical & Electronics Engineering Energy Engineering Environmental Science Industrial & Manufacturing Engineering Materials Science & Nanotechnology Mechanical Engineering Physics Social Sciences Transportation Other

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Geologi Dan Kawasan Rawan Bencana Longsor Daerah Neglasari dan Sekitarnya Kecamatan Pancatengah, Kabupaten Tasikmalaya Provinsi Jawa Barat Maurittius Antonius Talla Lamak; Rizqi, Al Hussein Flowers; Hita Pandita
Retii Vol 18 No 1 (2023): Prosiding Seminar Nasional ReTII ke-18 (Edisi Penelitian)
Publisher : Institut Teknologi Nasional Yogyakarta

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Abstract

Daerah penelitian terletak di Daerah Neglasari dan Sekitarnya, Kecamatan Pancatengah, Kabupaten Tasikmalaya Provinsi Jawa Barat. Secara geografis berdasarkan koordinat UTM (Univeral Transfer Mercator) WGS 84 Zona 49S daerah penelitian berada pada koordinat 203500 mT – 209500 mT, 9153000 mU – 9162000 mU dengan luasan 54 km2. Secara geografis berdasarkan koordinat UTM (Univeral Transfer Mercator) WGS 84 Zona 49S daerah penelitian berada pada koordinat 203500 mT – 209500 mT, 9153000 mU – 9162000 mU dengan luasan 54 km2. Geomorfologi daerah penelitian dibagi menjadi 2 satuan bentuklahan yaitu satuan perbukitan bergelombang kuat denudasional (D1), dan satuan perbukitan bergelombang lemah-sedang denudasional (D2).Stratigrafi daerah penelitian dibagi menjadi 3 satuan stratigrafi yaitu Satuan breksi polimik Jampang berumur Oligosen Akhir Miosen Awal, Satuan kalkarenit Pamutuan berumur Miosen Tengah, dan Satuan batupasir karbonatan Bentang berumur Miosen Akhir-Pliosen. Potensi geologi daerah penelitian dibagi menjadi 2 yaitu potensi positif berupa Bahan galian C (gamping, pasir dan batu), objek wisata air terjun (curug) Dengdeng, serta lahan yang subur untuk perkebunan, sedangkan potensi negatif berupa gerakan masa tanah maupun batuan. Struktur geologi daerah penelitian terdiri dari kekar berpasangan dengan arah umum relatif timurlaut-baratdaya. Kawasan rawan bencana longsor daerah penelitian dibagi menjadi 3 yaitu kawasan rawan bencana longsor rendah pada bagian selatan, kawasan rawan bencana longsor sedang pada bagian tengah daerah penelitian, dan kawasan rawan bencana longsor tinggi pada bagian utara daerah penelitian.
Estimasi Sumber Daya Endapan Nikel Laterit Menggunakan Metode Idw Berdasarkan Data Bor dan Data Assay Pada Blok X di Daerah Morowali Utara, Sulawesi Tengah Praba Padma Arsyada; Rizqi, Al Hussein Flowers; Winarti
Retii Vol 18 No 1 (2023): Prosiding Seminar Nasional ReTII ke-18 (Edisi Penelitian)
Publisher : Institut Teknologi Nasional Yogyakarta

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Daerah penelitian berada di blok X PT. Paku Bumi Inti Mineral, Kabupaten Morowali Utara, Provinsi Sulawesi Tengah yang merupakan bagian dari jalur ofiolit Sulawesi dengan kondisi geologi yang kompleks dan tektonik yang masih aktif. Daerah penelitian berada di Lengan Timur Sulawesi masih memiliki potensi endapan nikel laterit yang cukup besar. Melimpahnya potensi nikel laterit tersebut tentunya cukup penting untuk diimbangi dengan kegiatan eksplorasi yang sistematis. Berdasarkan hal tersebut diperlukan adanya perhitungan estimasi pada sumber daya endapan nikel laterit untuk mengetahui sebaran endapan nikel laterit di daerah penelitian. Penelitian ini dilakukan dengan melakukan korelasi data pengeboran di 19 titik dengan jarak antar titik bor 100x100 meter dan dilanjutkan 50x50 meter. Hasil pengeboran menunjukkan Persebaran endapan nikel laterit pada daerah penelitian memiliki karakteristik mengikuti arah punggungan yang menebal pada morfologi landai dan menipis pada morfologi lereng. Karakteristik tersebut diinterpretasikan akibat faktor utama yang berupa kondisi morfologi dan struktur geologi, hal tersebut nampak pada visualisasi sebaran nikel laterit pada daerah penelitian. Pemodelan endapan nikel laterit pada daerah penelitian menggunakan software GEOVIA Surpac dan metode Inverse Distance Weighting (IDW) didapatkan perhitungan bahwa estimasi sumberdaya nikel laterit memiliki total volume 86.750 m, total tonase sebesar 130.125 ton dengan rata-rata kadar 1.08%.
Karakterisasi Endapan Laterit Pada Blok X dan Y Kecamatan Pulau Sebuku, Kabupaten Kotabaru, Kalimantan Selatan, PT. Sebuku Iron Lateritic Ores Reynaldo Adhiechandra S; Hill Geondoet Hartono; Rizqi, Al Hussein Flowers
Retii Vol 18 No 1 (2023): Prosiding Seminar Nasional ReTII ke-18 (Edisi Penelitian)
Publisher : Institut Teknologi Nasional Yogyakarta

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Abstract

Daerah penelitian berada pada blok X dan blok Y terletak pada Pulau Sebuku, Kecamatan Pulau Laut Utara, Kabupaten Kotabaru, Kalimantan Selatan. Pulau Sebuku memiliki kondisi geologi dan tektonik yang kompleks dengan memiliki banyak potensi mineral ekonomis salah satunya produk laterit. Perbedaan karakteristik produk laterit yang dihasilkan menarik untuk dikaji. Penelitian ini bertujuan untuk mengetahui bagaimana karakteristik laterit pada tiap blok, litologi, dan hasil analisis geokimia untuk mengetahui nilai persebaran unsur pada tiap material laterit. Metode penelitian menggunakan observasi data pemboran dan metode analisis laboratorium berupa XRF dan petrografi. Berdasarkan data pemboran didapat material laterit pada daerah penelitian terdiri atas zona red limonite, yellow limonite, earthy saprolite, saprolite, rocky saprolite, hard saprolite, dan bedrock. Litologi yang didapatkan berupa dunit terserpentinisasi dan harzburgite terserpentinisasi. Material laterit tersebut kemudian dilakukan analisis XRF pada zona limonite dengan nilai memiliki kandungan unsur yang lebih tinggi yaitu Fe pada blok X (49,24%), Ni pada blok X (1,07%), Mn pada blok Y (0,93%), Co memiliki nilai yang sama. Zona saprolit unsur yang lebih tinggi Fe blok Y (21,97%), Ni pada blok X (1,24%), Mn pada blok Y (0,41%), Sedangkan Co memiliki nilai yang sama (0.13%).
PENYELIDIKAN GEOLISTRIK MENGGUNAKAN KONFIGURASI SCHLUMBERGER TERHADAP POTENSI AMBLESAN DAERAH PONJONG, GUNUNG KIDUL Rizqi, Al Hussein Flowers; Yudhana, Waskita Murti Bambang
KURVATEK Vol 5 No 2 (2020): November 2020
Publisher : Institut Teknologi Nasional Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.33579/krvtk.v5i2.1769

Abstract

Administratively, the research area is included in Ponjong Subdistrict, Gunung Kidul Regency, Special Region of Yogyakarta. Geographically, it’s located in 07°56’30" - 08°1’0" East Longitude and 110°42’30" - 110°46’0" South Latitude. Several subsidences were occurred in Ponjong, Gunung Kidul in 2018. This study is aimed to determine the subsurface stratigraphy and analyze the depth of rocks layer which has the potential of subsidence (sinkhole) based on the value of rocks resistivity in Ponjong area. Resistivity was measured by geoelectrical method by appllying Schlumberger configuration. As a result, the study areas indicates that the most potential area having sinkhole are composed of lithology of carbonate rocks from Wonosari Formation (crystaline limestone and chalky limestone). Those are in the Asem Lulang village in showed small value of rock resistivity, about 0.1 to <1 (Ωm) at the depth of 15 to 63 meter and more than 123 meter. If it comparated to the village of Sawahombo and Kenteng village, the result showed that relative potential area of subsidence (sinkhole) only at shallow depth and nearly to the surface which is only 10 to 15 meter from surface.Keywords: geoelectric, ponjong, Schlumberger, Sinkhole, Wonosari
Correlation of lithofacies and depositional environment using Markov chain analysis in Sambipitu formation at Ngalang river, Gunungkidul, Yogyakarta, Indonesia Al Hussein Flowers Rizqi; Hendri Tri Purnomo
Sustinere: Journal of Environment and Sustainability Vol. 5 No. 1 (2021): pp. 1 - 63 (April 2021)
Publisher : Center for Science and Technology, IAIN Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.22515/sustinere.jes.v5i1.124

Abstract

The research area is located at Ngalang river, Gedangsari sub-district, Gunungkidul Regency, Special Region of Yogyakarta. The research area is part of southern mountain area which is composed of lithology of Sambipitu calcareous sandstone. The depositional process phase in the Sambipitu formation has a unique pattern and is relevant to the previous lithology. As a result, the stratigraphic position and lithological repetition pattern were reviewed using the statistical method (Markov chain). The aim of this research is to use geostatistics to examine the sedimentation trend in order to predict the existence of rock facies in the Sambipitu Formation. In each unit of lithology cycle, geostatistics is expected to assist, to predict and to interpret the significance of subsequent lithology appearances. The research method used was measured stratigraphy, determination of rock age and depositional environment based on fossil identification. In addition, this research used probability matrix in Markov chain analysis. The results of the Markov chain analysis showed that lithology of rock in the upper Sambipitu formation had a non-random transition pattern. The results of statistical calculation showed that the calculation value was greater than the Chi-square table value (333.9>34.38) that the H0 component was rejected. Lithofacies and depositional environment are correlated to several geological aspects such as distribution of rock facies, source of rock, paleobtahymetri, trace fossils and sedimentation process.
3D Modeling of of Distribution Andesite and Breccia Rocks Using Geoelectric Resistivity in Potential Areas of Minerals in Madiun Regency, Indonesia Prastowo, Rizqi; Pambudi, Setyo; Rizqi, Al Hussein Flowers; Ipmawan, Vico Luthfi; Arimurti, Dyah Arum; Radhitya, Berwyn Dzaky
International Journal of Hydrological and Environmental for Sustainability Vol. 3 No. 2 (2024): International Journal of Hydrological and Environmental for Sustainability
Publisher : CV FOUNDAE

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.58524/ijhes.v3i2.474

Abstract

This research focuses on the distribution of andesite and breccia rocks in East Java, Indonesia, specifically in Morang Village, Madiun Regency, through geoelectric resistivity measurements. This study aims to enhance geoelectric interpretation from 2D to 3D, providing high accuracy in target positioning for potential building material resources. By employing a dipole-dipole configuration with electrode spacing, the resistivity values of subsurface rocks were analyzed to classify the types and distributions of building materials, such as andesite and breccia. Data was collected through field measurements and geological surveys, followed by inverse modeling using the least squares method. The results reveal that andesite, with resistivity values above 1000 Ωm, is distributed predominantly in the southeast-northwest trend at a depth of 10–15 meters, while breccia, with resistivity values between 600–900 Ωm, is found at various depths closer to the surface. The geological interpretation suggests that the southeast-northwest orientation may correlate with an ancient basin structure, which directed lava flow during past volcanic activities, forming these rock layers. This study contributes valuable information for local infrastructure planning by providing data on accessible rock resources essential for construction. The application of the 3D geoelectric model offers an effective tool for environmental assessment and mineral exploration, promoting sustainable resource management.
Penyelidikan Geolistrik sebagai Survei Awal Pembangunan Kolam Renang di Daerah Towangsan, Gantiwarno, Klaten, Jawa Tengah: (Geoelectric Exploration as a Preliminary Survey for Swimming Pool Construction in the Towangan Region, Gantiwarno Klaten, Central Java) Rizqi, Al Hussein Flowers; Winarti, Winarti; Erlandi, Muhammad; Diyoko, Diyoko
Kurvamas Vol 1 No 1 (2025): Jurnal Kemitraan, Kewirausahaan dan Pengabdian Masyarakat
Publisher : LPPMI Institut Teknologi Nasional Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.33579/krvms.v1i1.5578

Abstract

Kegiatan pengabdian masyarakat dilakukan di Desa Towangsan, Kecamatan Gantiwarno, Kabupaten Klaten, Provinsi Jawa Tengah berupa penyelidikan geolistrik. Penyelidikan geolistrik dilakukan bersamaan dengan adanya program Kuliah Kerja Nyata dari LPPMI ITNY yang dilaksanakan pada bulan Juli – Agustus 2024. Penyelidikan geolistrik ini mendapat dukungan penuh dari pemerintah daerah Towangsan karena daerah ini memiliki keterbatasan sumber air untuk pemenuhan kebutuhan air apabila rencana Pembangunan Kolam Renang dan Taman Bermain Anak sudah terealisasi dengan baik. Tujuan kegiatan pengabdian ini adalah untuk membuat gambaran bawah permukaan sehingga kedalaman dan sebaran air tanah dapat diidentifikasi dan menjadi acuan dalam penentuan titik sumur bor. Kegiatan pengabdian masyarakat ini dilakukan dalam 4 minggu mulai dari perencanaan, survey pendahuluan, kegiatan lapangan hingga analisis studio. Hasil penyelidikan geolistrik mendapatkan gambaran air tanah dangkal pada kedalaman 8 – 15 meter dan air tanah dalam pada kedalaman 32 – 52 meter pada litologi endapan pasir dari endapan Gunung Merapi. Hasil rekomendasi ini kemudian telah dipaparkan di depan pemerintah setempat di Balai Desa Towangsan untuk ditindaklanjuti. ABSTRACT Geoelectrical investigations were conducted as part of community service activities in Towangsan Village, Gantiwarno District, Klaten Regency, Central Java Province. The geoelectrical analysis was carried out in cooperation with LPPMI ITNY's Real Work Lecture program, which will be held in July and August 2024. The Towangsan regional government fully supported this geoelectrical inquiry because there are few water sources in the area for building a swimming pool and park. Children's Play has been successfully realized. The purpose of this service activity is to build a picture of the subsurface so that the depth and distribution of groundwater may be determined and used as a reference when determining drilling well locations. This community service activity lasted four weeks, beginning with preparation, followed by a preliminary survey, field activities, and studio analysis. The geoelectric investigation indicated shallow groundwater at depths of 8 to 15 meters and deep groundwater at depths of 32 to 52 meters in the lithology of Mount Merapi sand deposits. The outcomes of these recommendations were then presented to the local authority at the Towangsan Village Hall for further action.
Fasies dan Lingkungan Pengendapan Formasi Nanggulan di Sungai Kamal, Desa Pendoworejo, Kecamatan Girimulyo, Kabupaten Kulon Progo, Provinsi Daerah Istimewa Yogyakarta Qoyyibi, Dava Saliham; Rizqi, Al Hussein Flowers
Retii 2024: Prosiding Seminar Nasional ReTII ke-19 (Edisi Penelitian)
Publisher : Institut Teknologi Nasional Yogyakarta

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Abstract

So far, stratigraphic measurements on the Nanggulan Formation in the Nanggulan area have been limited to the Kalisonggo River location. There are also sedimentary rock outcrops with relatively steep slopes in the Kamal River. This location has been used as a study area to obtain a sized stratigraphic picture so that it can be studied as a basis for determining facies and environmental studies. deposition. The purpose of this research is to obtain measured stratigraphic data (measurement section) and aims to obtain relative ages and depositional environments. Administratively, the research area was carried out on the Kamal River, Pendoworejo Village, Girimulyo District, Kulon Progo Regency, Yogyakarta Special Region Province. Based on the research results, five (5) units in the stratigraphic data were measured using a sampling research method based on Jacob Stick stratigraphic measurements, including sandstone units, marl units, black mudstone units, siltstone units, and old andesite formation breccia units, prepared by reacting the samples using H2O2 solution, sample observation using a microscope, and determination based on data obtained using existing classifications. Based on plangtonic foraminifera analysis, the research location is aged N9-N11 (Middle Miocene). The depositional environment in the research area uses benthonic foraminifera identification which is then correlated to obtain a Middle Neritic depositional environment.
Geologi dan Kajian Fasies Gunung Api Purba Soropati Berdasarkan Keberadaan Lava Basal Daerah Gedong dan Sekitarnya, Kecamatan Banyubiru, Kabupaten Semarang, Provinsi Jawa Tengah Rizqi, Al Hussein Flowers; Maming, Haryadi; Hartono, Hill Gendoet
Retii 2024: Prosiding Seminar Nasional ReTII ke-19 (Edisi Penelitian)
Publisher : Institut Teknologi Nasional Yogyakarta

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Abstract

The study area is located on the flank of Mount Merbabu and south of the Soropati Band. Mount Soropati is thought to be active in the Quaternary, and was formed at the same time as two other nearby volcanoes, Old Merbabu and Ungaran. This study aims to identify basalt lavas on Mount Soropati that spread to the medial facies. The research method used is field observation supported by DEM map analysis and petrographic analysis. On the appearance of the DEM map, Mount Soropati has a morphology that shows the formation of a caldera and a visible depth that is likely the center of volcanic activity on Mount Soropati in the past. Mount Soropati is a Bregada volcano that gathers one Khuluk, Khuluk Telomoyo and one gumuk, Gumuk Gedong. Mount Soropati is composed of basalt lava flows and has historical records of activities that show that Mount Soropati is a polygenetic volcano. Mount Soropati has an effusive type, which is reflected in the Ca-rich plagioclase content, and an explosive type, which can be seen from the former caldera. In volcanic development, Mount Soropati is in the advanced erosional phase. The presence of basalt lava along ± 2.4 km and a considerable distance from the eruption center may indicate a medial facies.
Studi Foraminifera untuk Penentuan Umur dan Lingkungan Pengendapan pada Formasi Sentolo, Desa Geden, Kecamatan Lendah, Kabupaten Kulon Progo, Yogyakarta Rizqi, Al Hussein Flowers; Thabita Monica Tupang, Kannaya
Retii 2024: Prosiding Seminar Nasional ReTII ke-19 (Edisi Penelitian)
Publisher : Institut Teknologi Nasional Yogyakarta

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Stratigraphic measurements measured in the upper part of the Sentolo Formation are very limited, where this formation is mixed with clastic rocks whose distribution is only local and not continuous due to erosion, but in Geden Village, Lendah District, Kulon Progo Regency, Yogyakarta Special Region, an outcrop of the Sentolo formation was found the upper part with a total stratigraphic measurement measuring 5.2 meters. The purpose of this research is to compile the results of the study by obtaining rock samples on measured stratigraphic measurement lines in clastic limestone, with the aim of obtaining data on plangtonic and also bentonic small foraminifera. Based on the results of observations and descriptions, the plangtonic foraminifera found in limestone such as Globorotalia Acostaensis, Globigerinoides ruber, & Globorotalia Margaritae were found to be N16- N17 (Late Miocene), while the benthonic foraminifera found, such as Nodosaria Vetrebralis, Cibicides Polyrraphes, Amphistegina Lessonii, had an environment deposition of Deep Neritic 0-20m – Middle Neritic 20-100m.
Co-Authors Abdillah Ahmad, Ghani Afri Tri Kristanto Ahmad, Ghani Abdillah Alansyah, Apriko Yudhan Aprilia, Adinda Arimurti, Dyah Arum Audrey, Vivi Fistina Awaluddin, muhamad Hasyim Bernadeta Subandini Astuti Delvina Syaifira Norma Hani Desie Kurnia Gae Diyoko, Diyoko Elkawi Hawinu, Nodyka Erlandi, Muhammad Fajar, Ari Fatimah Fatimah FATIMAH FATIMAH Febri Anggara Fistina Audrey, Vivi Garnis Wanengcio Uligawati Gil Lodar, Jaden Gracia Apriyani Naibobe Hafidz Sedek Haliza, Audia Shafa Hendri Tri Purnomo Herning Dyah Kusuma Wijayanti Hill Gendoet Hartono Hill Geondoet Hartono Hita Pandita Hita Pandita Ibnu Hibban, Muhammad Iqbal Hidayat Lindung Zalbuin Mase Maming, Haryadi Maurittius Antonius Talla Lamak Mayang Pitaloka Muh Gifaricandrabayu Muhammad Abdul Basith Muhammad Arifai Muhammad Dandy Fachrindra Muhammad Isna Almuzakki Nadhip, Muhammad Nadip, Muhammad Noviardi Noviardi Oky Sugarbo Praba Padma Arsyada Qodri, Muhammad Fatih Qoyyibi, Dava Saliham Radhitya, Berwyn Dzaky Rajawali Yudha Pratama Ramadhan, Dimas Rean Devindra Reditya Galang Pamungkas Reynaldo Adhiechandra S reza_krisnandi reza krisnandi Rizqi Prastowo Rusmania Ramadhani, Saviola SANDI KURNIAWAN Setyo Pambudi Sukartono Syamsul Arifin Tedja Trisnaning, Paramitha Tengku Riza Zarzani N Thabita Monica Tupang, Kannaya Timotius Tuska, Robert Tiurma Dewi, Alexandra Sekar Vico Luthfi Ipmawan Vilman Sidik Waskita Bambang Murti Yudhana Waskita Murti Bambang Yudhana Waskita Murti Bambang Yudhana Waskita Wibisono, Dharmawan Catur Wijaya, Naufal Arya Winarti Winarti Winarti Yudhana, Waskita Murti Bambang