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Contact Name
Aldis Ladesta
Contact Email
aldis@trisakti.ac.id
Phone
+6285711947547
Journal Mail Official
aldis@trisakti.ac.id
Editorial Address
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
Location
Kota adm. jakarta barat,
Dki jakarta
INDONESIA
Journal of Geoscience Engineering and Energy (JOGEE)
Published by Universitas Trisakti
ISSN : 27155358     EISSN : 27226530     DOI : https://doi.org/10.25105/jogee.v3i2.13860
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.
Articles 148 Documents
HUBUNGAN LAJU INFILTRASI TERHADAP PERMEABILITAS TANAH DAN MUKA AIRTANAH DI DAERAH DESA TAJUR KECAMATAN CITEUREUP: THE RELATIONSHIP OF INFILTRATION RATE TO SOIL PERMEABILITY AND GROUNDWATER LEVEL IN THE TAJUR AREA, CITEUREUP DISTRICT Anwar, Saepul; Amri, Muhammad Adimas
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.18939

Abstract

Infiltration is an important process in a hydrological system and acts as a medium for air infiltration into the soil. The process of infiltration in soil can be influenced by several factors, namely, rainfall, vegetation, land slope, land use, and soil moisture. Apart from this, other factors such as groundwater level and soil permeability also have an influence on the infiltration process, both of which are related to each other in terms of the rate of infiltration or air infiltration into the soil. If the infiltration process is disrupted, it results in the pooling of air on the ground surface, which affects the hydrological system. It is necessary to know how factors such as groundwater levels and soil permeability influence the infiltration rate. Based on this, the aim of this research is to determine the relationship. between infiltration rate, groundwater level, and soil permeability and their influence. The research method was carried out by taking data from direct groundwater level measurements and infiltration rate measurements, as well as samples for soil permeability analysis. Then an interpretation of the data obtained is carried out and presented in a map of the infiltration zone and soil permeability zone. The research area in Tajur Village has 2 infiltration zones, namely the slow-medium zone and the medium zone with medium and rather fast soil permeability and low-medium groundwater depth.
ANALISIS KESTABILAN LERENG BERDASARKAN METODE ROCK MASS RATING PADA PT. INDOCEMENT TUNGGAL PRAKARSA Tbk, KABUPATEN BOGOR, PROVINSI JAWA BARAT: ANALYSIS OF SLOPE STABILITY BASED ON THE ROCK MASS RATING METHOD AT PT. INDOCEMENT TUNGGAL PRAKARSA Tbk, BOGOR DISTRICT, WEST JAVA PROVINCE Hadi Taqiuddin, Akrom; Ronoatmojo, Imam Setiaji
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.18941

Abstract

Weathering and the geological structure of the area affect slope stability. PT. Indocement Tunggal Prakarsa Tbk, Citeureup District, Bogor Regency, West Java Province, is the subject of this research. By calculating the safety factor value based on the Rock Mass Rating (RMR) using the Spencer method using Rocscience Slide 6.0 software, researchers hope to ensure slope stability. In fact, based on the slope stability analysis, it has a safety factor value of 0.900, so it is not in accordance with the Minister of Energy and Mineral Resources regulation 1827/K/30/MEM/2018. Based on this, recommendations for slope analysis of the research area have been made with a safety factor value of 1.232 in accordance with applicable regulations.
KARAKTERISTIK GEOMORFOLOGI DAERAH PASIRIPIS DAN SEKITARNYA, KECAMATAN SURADE, GEOPARK CILETUH PALABUHANRATU: GEOMORPHOLOGICAL CHARACTERISTICS OF PASIRIPIS AND SURROUNDING REGIONS, SURADE DISTRICT, GEOPARK CILETUH PALABUHANRATU Daffa Rafli; Santi Dwi; Mega Fatimah
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.18968

Abstract

The research was conducted in Pasiripis area, Surade sub-district, Sukabumi district, West Java province, which is part of the Ciletuh Palabuhanratu Geopark with the aim of identifying the characteristics of developing geomorphological Units, and classifying the distribution of lithological constituents in each unit. Identification of geomorphological characteristics is based on remote sensing analysis of DEM SRTM Data which is then processed in Arcgis Software, Global Mapper and field observations are made in mapping geomorphology and lithology distribution according to scientific standards to match the data from remote sensing analysis. The research findings are in the form of distribution maps based on morphographic aspects, flow pattern maps, landform maps, slopes and geomorphological components in geomorphological maps. The study area is divided into lowlands and low hills with a developed drainage pattern that is dendritic, sub-dendritic, and parallel. In the morphometric aspect, the slopes are flat or almost flat, very gentle, gently sloping, and slightly steep. The morphogenetic aspect in Pasiripis area shows the existence of endogenous processes, such as tectonism and volcanism activities, as well as exogenous processes, such as weathering, erosion, and dissolution. The lithology of the study area consists of limestone, sandstone, and tuff. Based on the geomorphological reconstruction aspect, the characteristics of Pasiripis area in Surade sub-district can be classified into five geomorphological unit, namely flat denudational lowland, gentle denudational lowland, gentle maritime lowland, gentle denudational lowland hills, and slightly steep denudational lowland hills. 
PEMODELAN GEOLOGI DAN ESTIMASI SUMBER DAYA BATUBARA DI WILAYAH ‘X’. KABUPATEN BERAU, PROVINSI KALIMANTAN TIMUR: GEOLOGICAL MODELING AND ESTIMATION OF COAL RESOURCES IN AREA 'X', BERAU REGENCY, EAST KALIMANTAN PROVINCE Manurung, Jekson; Nurdrajat; Alfadli, Muhammad Kurniawan; Asmoro, Yoki Dwi
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.18995

Abstract

General geological investigation activities and detailed exploration need to be carried out, so that it can show potential coal resources that can still be developed. The research area is in the PT. Berau Coal concession area, administratively located in Berau Regency, East Kalimantan Province. The research method used in calculating resources in Region 'X' is the Polygon Method, namely by halving the distance between two sample points on one axis to produce an area of ​​influence and refers to moderate complexity based on analysis of the geological conditions of the research area (SNI 5015:2019). This research aims to determine the feasibility of a coal seam to be mined based on aspects of dimensions, quantity and quality of coal distribution, as well as a reference in design and determining appropriate mining methods based on coal geological modeling. Based on ASTM D388-19 of 2004, the research area has a High Volatile B Bituminous coal ranking with an average calorific value (dmmf) of 13111,01 Btu/lb, ash content 4,7%, total sulfur 0,98%, total moisture 21,28%, inherent moisture 16,66%, volatile matter 48,63%, and fixed carbon 51,37%. The total estimated coal resources in the research area are 14.760.000 million tons, consisting of total measured coal resources of 13.380.000 million tons, indicated 930.000 thousand tons, and inferred 410.000 thousand tons.
ANALISIS ZONASI GERAKAN TANAH PADA DAERAH CIPINANG, KECAMATAN RUMPIN, KABUPATEN BOGOR: ZONING ANALYSIS OF LAND MOVEMENT IN THE CIPINANG AREA, RUMPIN DISTRICT, BOGOR DISTRICT Afdhal, Muhammad; Yuda, Himmes Fitra
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.19161

Abstract

The research was conducted in the Cipinang area, Rumpin District, Bogor Regency, West Java Province, which has regional conditions with varied morphology consisting of lowlands to highlands. From the existing geological conditions, the Cipinang area is an area with moderate to high susceptibility to landslides. One of the influencing factors is the slope from sloping to steep, and high rainfall. The aim of this research is to determine the ground movement vulnerability zone in the research area using a deterministic method in order to produce a map of the ground movement vulnerability zone using parameters that cause ground movement. with the final results obtained in the research area being divided into 3 zones, namely the low has coverage of 50%, the medium zone 40% and the high zone 10%.
LAJU INFILTRASI DAERAH KECAMATAN BUNGURSARI DAN SEKITARNYA DI KABUPATEN PURWAKARTA, PROVINSI JAWA BARAT: RATE OF INFILTRATION IN THE BUNGURSARI DISTRICT AND SURROUNDINGS IN PURWAKARTA DISTRICT, WEST JAVA PROVINCE Assyidik, Ahmad Ikhsan; Amri, Muhammad Adimas
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.19162

Abstract

The research area is in Bungursari District and the surrounding Purwakarta Regency. This research aims to determine the distribution of infiltration rate values in the research area. The method used is measuring soil infiltration using a double ring infiltrometer. Then it is known that the infiltration rate value is divided into 3 zones, namely, medium infiltration rate (2 – 6.5 cm/hour), fast infiltration rate (12.5 – 25 cm/hour), and very fast infiltration rate (>25 cm/hour).
STUDI KARAKTERISTIK BATUAN METAMORF DAN MINERAL GRAFIT PADA BLOK TERATI KELOMPOK BALAISEBUT, KABUPATEN SANGGAU, KALIMANTAN BARAT : STUDY OF CHARACTERISTICS OF METAMORPHIC ROCKS AND GRAPHITE MINERAL IN THE TERATI BLOCK OF THE BALAISEBUT GROUP, SANGGAU DISTRICT, WEST BORNEO Sulyana, Deska; Meirawaty, Mira; Maulana, Rizki Fajar
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 2, AGUSTUS 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jgw8b630

Abstract

Grafit merupakan mineral non-logam yang memiliki nilai ekonomis cukup tinggi. Mineral grafit merupakan mineral yang tersusun atas unsur karbon yang dapat hadir dibeberapa jenis batuan. Salah satu daerah yang memiliki potensi mineral grafit adalah daerah Kalimantan, tepatnya di Kabupaten Sanggau. Grafit pada daerah penelitian yaitu Terati hadir pada batuan metamorf dengan fasies greenschist termasuk pada kelompok metamorf regional. Sedangkan tipe endapan grafit pada daerah penelitian adalah flake graphite. Graphite is a non-metallic mineral that has quite high economic value. The mineral graphite is a mineral composed of the element carbon which can be present in several types of rocks. One area that has graphite mineral potential is the Kalimantan area, specifically Sanggau Regency. Graphite in the research area, namely Empi, is present in metamorphic rocks with greenschist facies, including in the regional metamorphic group. Meanwhile, the type of graphite deposit in the research area is flake graphite.  
ANALISIS BALIK LERENG LOWWALL PADA “BLOK X” KABUPATEN TANAH BUMBU, PROVINSI KALIMANTAN SELATAN: BACK ANALYSIS OF LOWWALL SLOPES IN "BLOCK X" DISTRICT TANAH BUMBU, SOUTH KALIMANTAN PROVINCE Putri, Al Zahra; Imam Setiaji Ronoatmojo; Wijaya, Budi
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.19236

Abstract

Coal mining companies usually apply the open pit mining method in carrying out coal mining. Mining activities always have risks that cannot be avoided and unpredictable, one of which is a landslide in the mining area. Therefore, it is very necessary to control the risks of mining activities. One of them is like designing a slope design in the mine which is included in geotechnical aspects. And in the geotechnical aspect, it has a reverse analysis method that is very useful to determine the cause of avalanches in the area.
HUBUNGAN KEKUATAN LAPIS TANAH DASAR DENGAN METODE CBR TERHADAP INDEKS PLASTISITAS TANAH DAERAH SITU GADUNG KECAMATAN PAGEDANGAN KABUPATEN TANGERANG: RELATIONSHIP OF SUBGRADE SOILS USING CBR METHOD TOSOIL PLASTICITY INDEX IN SITU GADUNG AREAPAGEDANGAN TANGERANG DISTRICT Novela, Adita; Ronoatmojo, Imam Setiaji; Yuda, Himmes Fitra
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 2, AGUSTUS 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/azgtmr80

Abstract

Tanah yang sering mengalami masalah dalam pembangunan konstruksi geologi rekayasa adalah tanah lempung. Kerusakan jalan yang selama ini sering dijumpai dikarenakan tidak tersedianya data California Bearing Ratio (CBR) serta konsistensi tanah. Tujuan dari penelitian ini adalah, mengetahui nilai CBR dengan alat DCP, meninjai evaluasi kekuatan lapis tanah dasar, menentukan batas konsistensi tanah, dan menginterpretasikan korelasi berdasarkan data CBR dan Plasticity Index (PI). Metode penelitian dilakukan dengan CBR dengan alat DCP, pengambilan sampel tanah, serta pengukuran indeks plastisitas tanah langsung. Pada daerah penelitian ini diketahui memiliki tingkat konsistensi plastisitas tanah yang tinggi, kohesi, dan tanah lempung dengan nilai PL sebesar 28,85% - 48%. Kemudian didapat nilai indeks plastisitas (PI) daerah penelitian yang memiliki nilai 25,15%-36,82%. Maka hasil PI ini mempunyai tingkat indeks plastis yang tinggi, tanah yang kohesif serta tipe tanah atau jenis yang lempung sehingga buruk untuk konstruksi di atasnya karena potensi swelling lempung. Kemudian untuk data CBR daerah penelitian didapat sebesar 5,05-5,55% dengan soil type lempung termasuk zona yang buruk/rendah.  The soil that often experiences problems in the construction of engineering geological construction is clay soil. Road damage that has often been encountered is due to the unavailability of California Bearing Ratio (CBR) data and soil consistency. The purpose of this research is to determine the CBR value using the DCP tool, review the evaluation of the strength of the subgrade layer, determine the soil consistency limit, and interpret correlation based on CBR and Plasticity Index data. The research method was carried out using CBR with a DCP tool, taking soil samples, and directly measuring the soil plasticity index. This research area is known to have a high level of consistent soil plasticity, cohesion, and clay soil with a PL value of 28,85% - 48%. Then the plasticity index (PI) value for the research area was obtained which had a value of 25,15% -36.82%. Therefor this plasticity index has high plasticity, cohesive properties and a clay type of soil so it is bad for construction on it because of the potential for clay swelling. Then the CBR data for the research area was found to be 5.05-5.55% with a clay soil type including poor/low zones.
INTEGRASI SISTEM INFORMASI GEOGRAFIS UNTUK ANALISIS KELAS TEKSTUR TANAH DALAM KONTEKS KEBENCANAAN GERAKAN TANAH: GEOGRAPHIC INFORMATION SYSTEM INTEGRATION FOR SOIL TEXTURE CLASS ANALYSIS IN THE CONTEXT OF GROUND MOTION DISASTER  Arifin, Khoirul; Amri, Muhammad Adimas
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 2, AGUSTUS 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/6y25kk18

Abstract

Berdasarkan laporan BPBD terjadi peristiwa longsor di daerah Jonggol. Dalam analisis aspek kebencanaan longsor, tekstur tanah adalah salah satu parameter yang dibahas. Dengan mempertimbangkan kemiringan lereng dan tipe batuan, penelitian ini bertujuan untuk menentukan kelas tekstur tanah. Untuk menentukan lokasi pengambilan sampel tekstur tanah, fitur peta kemiringan lereng, dan jenis batuan di tumpang-tindih. Selanjutnya, tekstur tanah diukur dengan menggunakan ayakan. Setelah perhitungan tekstur tanah dilakukan, fitur peta digabungkan (union). Hasil plot dominan dianggap mewakili kelas tekstur tanah. Berdasarkan analisis yang dilakukan, dua kelas tekstur tanah terdiri dari: berpasir-berliat dan berliat. Kelas berpasir-berliat meliputi 16,98 km2 atau 84,52% dari daerah penelitian, sedangkan kelas berliat meliputi 3,11 km2 atau 15,48% dari daerah penelitian. Based on the BPBD report, there was a landslide in Jonggol area. In analyzing the disaster aspects of landslides, soil texture is one of the parameters discussed. By considering slope and rock type, this study aims to determine the soil texture class. To determine the soil texture sampling locations, the features of slope, and rock type maps were overlapped. Next, soil texture is measured using a sieve. After soil texture calculations were made, the map features were union. The result of the dominant plot is considered to represent the soil texture class. Based on the analysis conducted, two soil texture classes comprise the study area: sandy-clayey and clayey. The sandy-clayey class covers 16,98 km2, or 84,52% of the study area, while the clayey class covers 3,11 km2, or 15,48% of the study area.

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