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Aldis Ladesta
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Fakultas Teknologi Kebumian dan Energi Universitas Trisakti, Jakarta Gedung D Lt. 2, Kampus A Jl. Kyai Tapa Grogol Jakarta 11440, Indonesia Telephone: +62-21-5663232 ext 8520
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Journal of Geoscience Engineering and Energy (JOGEE)
Published by Universitas Trisakti
ISSN : 27155358     EISSN : 27226530     DOI : https://doi.org/10.25105/jogee.v3i2.13860
Core Subject : Science, Education, Engineering,
Civil Engineering, Building, Construction & Architecture Education Energy Industrial & Manufacturing Engineering Materials Science & Nanotechnology Physics
The main aim of the Journal Geoscience Engineering and Energy (JOGEE) is to provide an open access platform to the articles that resulted of high-quality research works related with the geoscience and energy field. This is open for papers of geology (petrology; volcanology and geothermal; sedimentology and stratigraphy; paleontology; structural geology and seismology; petroleum geosciences; mineral deposits and coal mining; remotee sensing,; hidrogeology; marine geology and oceanography; geological engineering; environmental and geohazard mitigation; and also geotourism), geophysics (physical geology; exploration Geophysics), geochemistry, energy of renewable (geothermal; ..)and non-renewable energy (petroleum engineering; G&G method; mineral deposits, coal and energy resources management),dll. The Journal Geoscience Engineering and Energy (JOGEE) welcome the submission of manuscripts that meet the general criteria of significance and scientific excellence. It caters to the requirements of the geologist, researchers, academicians and also students, lab professional, and industry that is involved in geoscience studies. This journal publishes 2 numbers per year at least 8-9 articles. Papers will be published approximately 14 days after acceptance.
Arjuna Subject : Teknik (semua kategori) - Teknik (Lain-Lain)
Articles 4 Documents
 1 
Search results for , issue "VOLUME 7, NOMOR 1, FEBRUARI 2026" : 4 Documents clear
ANALISIS LAJU INFILTRASI TANAH PADA DAERAH GROGOL PETAMBURAN DAN SEKITARNYA, KOTA JAKARTA BARAT: SOIL INFILTRATION RATE ANALYSIS IN THE GROGOL PETAMBURAN AREA AND SURROUNDING AREAS, WEST JAKARTA CITY Abizar, Rafi Muhammad Fadhlan; Nuryana, Suherman Dwi; Amri, Muhammad Adimas
Journal of Geoscience Engineering and Energy VOLUME 7, NOMOR 1, FEBRUARI 2026
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/

Abstract

Penelitian ini bertujuan untuk menganalisis laju infiltrasi tanah di Daerah Grogol Petamburan, Kota Jakarta Barat. Metode yang digunakan yaitu pengambilan data lapangan pada 12 titik di daerah penelitian, setelah itu dihitung menggunakan rumus laju infiltrasi dan dibagi ke dalam klasifikasi. Hasil analisis menunjukkan pada daerah penelitian terdapat 3 zona laju infiltrasi, yaitu sedang (52 mm/jam) di bagian utara daerah penelitian dengan ukuran butir pasir kasar–sedang, sedang–cepat (80–120 mm/jam) di bagian tengah daerah penelitian dengan ukuran butir pasir kasar–sedang, dan cepat (132–240 mm/jam) di bagian selatan daerah penelitian dengan ukuran butir pasir kasar–halus. This study aims to analyze the soil infiltration rate in the Grogol Petamburan District, West Jakarta. The method employed involves field data collection across 12 points in the research area, followed by calculations using the infiltration rate formula and categorization into specific classifications. The analysis results reveal three infiltration rate zones within the study area: moderate (52 mm/hr) in the northern part, characterized by coarse-to-medium sand grain size; moderately rapid (80–120 mm/hr) in the central part with coarse-to-medium sand grain size; and rapid (132–240 mm/hr) in the southern part, characterized by coarse-to-fine sand grain size.
INTERPRETASI AWAL HUBUNGAN STRUKTUR GEOLOGI DAN TEKANAN FLUIDA PADA FORMASI MINAHAKI DAN FORMASI MENTAWA, CEKUNGAN BANGGAI: INITIAL INTERPRETATION BETWEEN GEOLOGICAL STRUCTURES AND FLUID PRESSURE AT MINAHAKI FORMATION AND MENTAWA FORMATION, BANGGAI BASIN Mazaya, Faza Auliya; Adhitama, Ramadhan
Journal of Geoscience Engineering and Energy VOLUME 7, NOMOR 1, FEBRUARI 2026
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/

Abstract

Struktur geologi, terutama sesar, berperan penting dalam mengontrol distribusi dan pergerakan fluida di sistem reservoir. Sesar dapat menjadi penghalang atau jalur aliran, tergantung geometri, litologi, dan riwayat deformasinya. Penelitian ini mengkaji hubungan awal antara struktur dan tekanan fluida pada Formasi Minahaki, Cekungan Banggai, menggunakan interpretasi seismik 3D dan data tekanan sumur terbatas. Analisis menyoroti geometri serta lemparan sesar dan perbandingan gradien tekanan antar sumur, sebagai dasar konseptual studi lanjutan kuantitatif. Temuan ini masih bersifat deskriptif dan memerlukan verifikasi tambahan melalui integrasi data geologi dan petrofisika yang detail. Geological structures, especially faults, play an important role in controlling fluid distribution and movement within reservoir systems. Faults can act as barriers or flow pathways, depending on their geometry, lithology, and deformation history. This study examines the preliminary relationship between geological structure and fluid pressure behavior in the Minahaki Formation, Banggai Basin, using 3D seismic interpretation and limited well pressure data. The analysis focuses on fault geometry, fault throw variation, and pressure gradient comparisons between wells, forming a conceptual basis for further quantitative study. These findings remain descriptive and require additional verification through detailed geological and petrophysical data integration.
GEOMORFOLOGI DAERAH MEKARMUKTI, KECAMATAN WALURAN, KABUPATEN SUKABUMI, PROVINSI JAWA BARAT - INDONESIA: GEOMORPHOLOGY OF MEKARMUKTI, WALURAN DISTRICT, SUKABUMI REGENCY, WEST JAVA PROVINCE - INDONESIA Brillianti, Anisha Rizkiana; Pratiwi, Santi Dwi
Journal of Geoscience Engineering and Energy VOLUME 7, NOMOR 1, FEBRUARI 2026
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/

Abstract

Penelitian ini dilakukan di daerah Mekarmukti, Kecamatan Waluran, Kabupaten Sukabumi, Provinsi Jawa Barat, yang merupakan bagian dari Geopark Ciletuh Palabuhanratu. Penelitian bertujuan untuk mengidentifikasi secara rinci karakteristik satuan geomorfologi yang berkembang serta mengelompokkan persebaran litologi penyusun pada masing-masing satuan geomorfologi. Analisis geomorfologi dilakukan melalui pendekatan penginderaan jauh menggunakan data DEM SRTM yang diolah dengan perangkat lunak ArcGIS serta didukung oleh observasi lapangan untuk pemetaan geomorfologi dan sebaran litologi sesuai kaidah ilmiah guna memadukan hasil interpretasi citra dengan kondisi aktual di lapangan. Kajian geomorfologi dilakukan berdasarkan tiga aspek utama, yaitu morfografi (bentuk lahan dan pola pengaliran), morfometri (kemiringan lereng), serta morfogenetik (proses endogen dan eksogen). Litologi penyusun daerah penelitian terdiri atas endapan sedimen pantai, batupasir tufaan, batupasir, breksi vulkanik, tuf, serta lava basaltik. Secara morfogenetik, wilayah penelitian dipengaruhi oleh aktivitas tektonik dan vulkanik serta proses pelapukan dan erosi. Berdasarkan integrasi ketiga aspek tersebut, daerah Mekarmukti dibagi menjadi empat satuan geomorfologi, yaitu perbukitan rendah struktural curam, perbukitan struktural curam, perbukitan denudasional landai, dan perbukitan denudasional curam. This research was conducted in the Mekarmukti area, Waluran District, Sukabumi Regency, West Java Province, which is part of the Ciletuh Palabuhanratu Geopark. The research aims to identify in detail the characteristics of developing geomorphological units and to classify the distribution of constituent lithology in each geomorphological unit. Geomorphological analysis was carried out through a remote sensing approach using SRTM DEM data processed with ArcGIS software and supported by field observations for geomorphological mapping and lithological distribution according to scientific principles in order to integrate image interpretation results with actual field conditions. Geomorphological assessment is conducted based on three main aspects, namely morphography (landforms and drainage patterns), morphometry (slope gradients), and morphogenetics (endogenous and exogenous processes). The constituent lithology of the research area consists of coastal sediment deposits, tuffaceous sandstone, sandstone, volcanic breccia, tuff, and basaltic lava. In terms of morphogenetics, the study area is affected by tectonic and volcanic activity as well as weathering and erosion processes. Based on the integration of these three aspects, the Mekarmukti area is divided into four geomorphological units, namely steep structural low hills, steep structural hills, gentle denudational hills, and steep denudational hills.
KARAKTERISTIK GEOMORFOLOGI DAERAH CARINGINNUNGGAL DAN SEKITARNYA, KECAMATAN CIRACAP, CILETUH, KABUPATEN SUKABUMI, PROVINSI JAWA BARAT: GEOMORPHOLOGICAL CHARACTERISTICS OF CARINGINNUNGGAL AND SURROUNDING AREA, CIRACAP DISTRICT, CILETUH, SUKABUMI REGENCY, WEST JAVA PROVINCE Puspita, Fadillah; Rosana, Mega Fatimah
Journal of Geoscience Engineering and Energy VOLUME 7, NOMOR 1, FEBRUARI 2026
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/

Abstract

Daerah penelitian terletak di daerah Caringinnunggal, Kecamatan Ciracap, Kabupaten Sukabumi, Jawa Barat. Penelitian ini bertujuan untuk mengumpulkan data geologi permukaan yang rinci mengenai sebaran jenis batuan, satuan geomorfologi di daerah tersebut. Metode analisis karakteristik geomorfologi dilakukan berdasarkan penginderaan jauh menggunakan data DEM yang kemudian diolah menggunakan aplikasi ArcGIS, serta melakukan pengamatan kondisi di lapangan. Peta yang digunakan memiliki skala 1:12.500. Analisis karakteristik geomorfologi dilakukan berdasarkan aspek geomorfologi, yaitu morfografi (bentuk lahan dan pola pengaliran), morfometri (kemiringan lereng), dan morfogenetik (proses endogen dan eksogen). Daerah penelitian terdiri dari lima satuan geomorfologi yaitu perbukitan bergelombang denudasional, perbukitan denudasional agak curam, perbukitan rendah struktural curam, perbukitan bergelombang struktural, perbukitan struktural curam. The research area is located in the Caringinnunggal area, Ciracap District, Sukabumi Regency, West Java. This study aims to collect detailed surface geological data regarding the distribution of rock types, geomorphological units in the area. The method of geomorphological characteristic analysis is carried out based on remote sensing using DEM data which is then processed using the ArcGIS application, as well as observing conditions in the field. The map used has a scale of 1:12,500. The analysis of geomorphological characteristics is carried out based on geomorphological aspects, namely morphography (landforms and drainage patterns), morphometry (slope gradient), and morphogenetics (endogenous and exogenous processes). The research area consists of five geomorphological units, namely gently denudational hills, rather steep denudational hills, steep structural low hills, gently structural hills, steep structural hills.

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