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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 11 Documents
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Search results for , issue "VOLUME 3, NOMOR 2, AGUSTUS 2022" : 11 Documents clear
ANALISIS LAJU INFILTRASI TERHADAP MUKA AIRTANAH,KECAMATAN CIPAYUNG, KOTA JAKARTA TIMUR: ANALYSIS OF INFILTRATION RATE OF GROUNDWATER LEVELS IN CIPAYUNG REGION, EAST JAKARTA Muhammad Yusril Ihza M; Muhammad Adimas Amri; Himmes Fitra Yuda
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3416.299 KB) | DOI: 10.25105/jogee.v3i2.12984

Abstract

To be able to determine the water catchment area, the value of the infiltration rate and groundwater level are quite important in a parameter for determining the water catchment area, in Jakarta the lack of water catchment areas and the high rate of population growth cause frequent flooding in the capital city, so it is necessary to there is a long-term plan for spatial planning of water catchment areas in Jakarta as one of the steps to overcome flood disasters and become groundwater reserves in the capital city, the higher the groundwater level value in an area, the area has the potential for good catchment areas because it can still accommodate rainwater, infiltration rate data collection was carried out directly in the field using a Double Ring Infiltrometer and for groundwater level data direct measurements were made on dug wells in the study area
ZONASI KAWASAN RESAPAN AIR DAERAH CIJERUK, KECAMATAN CIJERUK, KABUPATEN BOGOR, PROVINSI JAWA BARAT: ZONATION OF WATER INSPECTION AREA IN CIJERUK REGION, CIJERUK DISTRICT, BOGOR REGENCY, WEST JAVA PROVINCE Viona Dienty Paratin; Suherman Dwi Nuryana; Mohammad Apriniyadi
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (5569.3 KB) | DOI: 10.25105/jogee.v3i2.13335

Abstract

Cijeruk known as a strategic location that is still very close to the Mount Salak area, but also close to the urban area of Bogor itself. This causes the area to have the potential to have good water absorption, but it also has the potential to be disturbed by water absorption due to internal and external factors in the research area. For this reason, it is necessary to know the water absorption and infiltration rate in order to see the advanced conditions of the research area. In order to know this, researchers need to obtain primary data by processing in the field using a Double Ring Infiltrometer (Indonesian National Standard, 7752:2012); while secondary data were obtained from previous researchers, as well as official bodies in Indonesia. The rainfall at the nearest Citeko station per 5 years reaches more than 3000mm, namely 3168.8mm, indicating that the research area has a very high potential for rainfall. In addition, it can be concluded that the research area has a type of overburden in the form of loamy sand with flat to steep areas in 4 observation locations, while the other 5 observation locations are flat to very steep. Then, the results obtained in the Cijeruk area obtained 2 units of infiltration rate, namely sufficient infiltration rate with an infiltration rate of 0.192 m/day to 0.312 m/day and a high infiltration rate with an infiltration rate of 1.08 m/day up to 5.04 m/day. indicates that the water catchment area is classified as good.
AKTIVITAS TEKTONIK RELATIF BERDASARKAN INDEKS GEOMORFIK DAERAH TANGKAPAN AIR CIHAUR KABUPATEN BANDUNG BARAT PROVINSI JAWA BARAT: RELATIVE TECTONIC ACTIVITY BASED ON GEOMORPHIC INDICES OF CIHAUR WATER CATCHMENT AREA WEST BANDUNG REGENCY WEST JAVA PROVINCE Anggito Saputra; Murni Sulastri; Nana Sulaksana; P Paramarta Raditya Rendra
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1521.965 KB) | DOI: 10.25105/jogee.v3i2.13631

Abstract

The Cihaur watershed is one of the interesting areas for study about morphotectonic. This area is an earthquake-prone caused by subduction zone and active fault. The methods used in this study are: lineament analysis, morphotectonic, and associate of lithology and tectonic activity. The lineament analysis show that the ridge lineament pattern of study area is dominantly oriented West-East, following to structural pattern of Java. The morphotectonic analysis used three geomorphic index: basin asymmetric factor (Af), valley width-to-high ratio (Vf), and mountain front sinuosity (Smf). Then all the geomorphic index calculated by average of five geomorphic indices became index of relative tectonic activity (IATR). The study area was divided into four parts: 1st Class (very high tectonic, 13.14% in area); 2nd Class (high, 8.88% in area); 3rd Class (moderate, 46.21% in area); and 4th Class (low, 15.62% in area). This IATR result show that Cihaur watershed was controlled by moderate tectonic activity. The lithology of the study area is divided into: volcanic rock, sedimentary rock, and lake sediment. Association with tectonic activity shows that sedimentary rocks were highly tectonic-very highly tectonic, the volcanic rocks were moderately tectonic-highly tectonic, and lake sediment was low tectonic.
IDENTIFIKASI KEHADIRAN STRUKTUR GEOLOGI BERDASARKAN ANALISIS MODEL GRAVITASI DAERAH KEBAN JATI DAN SEKITARNYA, BENGKULU SELATAN: IDENTIFICATION OF GEOLOGICAL STRUCTURE BASED ON GRAVITY MODEL ANALYSIS OF THE KEBAN JATI AREA, BENGKULU SELATAN Fadhellatul Kamil; Budhi Setiawan
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3930.177 KB) | DOI: 10.25105/jogee.v3i2.13678

Abstract

Interpretasi struktur geologi dapat dilakukan dengan memanfaatkan model gravitasi bumi untuk menginterpretasikan kehadiran struktur geologi bawah permukaan. Model gravitasi bumi berupa model Global Gravity Model Plus (GGMPlus) dengan pengambilan daerah Keban Jati dan Sekitarnya, Bengkulu Selatan, Bengkulu. Penelitian bertujuan dalam upaya identifikasi struktur geologi bawah permukaan dan memahami keterkaitan terhadap data struktur lapangan. Daerah Keban Jati termasuk pada Cekungan Busur Depan Bengkulu yang mengalami fase tektonik pembentukan cekungan busur depan secara kompleks dengan proses tektonik yang terjadi pada Pra Tersier – Kuarter. Metode analisis melibatkan peta geologi Daerah Keban Jati dan Sekitarnya, Peta Shuttle Radar Topography Mission (SRTM), dan data gravitasi bumi yang dipisahkan menjadi peta anomali gravitasi lokal dan peta Tilt Derivatives (TDR). Peta tersebut dilakukan analisis kelurusan untuk mengetahui arah kelurusan dan metode grafik anomali untuk memahami karakteristik anomali gravitasi terhadap struktur di peta geologi. Berdasarkan analisis kelurusan peta SRTM, anomali gravitasi lokal, dan TDR menunjukkan dominasi arah tenggara – barat laut dan utara – selatan. Kondisi tersebut menunjukkan arah kelurusan mirip dengan arah struktur pada peta geologi. Sedangkan pada data grafik gabungan anomali gravitasi lokal dengan TDR menunjukkan karakteristik sesar, antiklin, dan sinklin. Pada kedua anomali karakteristik sesar berada di antara grafik anomali puncak dan lembah. Sedangkan lipatan berada di area dekat dengan puncak ataupun lembah grafik anomali. Dari kedua metode analisis gravimetri tersebut memiliki kecocokan terhadap keberadaan struktur lapangan. Sehingga metode tersebut dapat membantu dalam identifikasi arah struktur dan pola anomali gravitasi yang dapat diinterpretasikan keberadaannya.
IDENTIFIKASI GERAKAN TANAH DI DESA KEBONHARJO DAN SEKITARNYA, KABUPATEN KULON PROGO, YOGYAKARTA: THE IDENTIFICATION OF SOIL MOVEMENT IN KEBONHARJO AND NEIGHBORHOODS, KULON PROGO REGENCY, YOGYAKARTA Ade Tiyas Nurhaja Tiyas; Suherman Dwi Nuryana; Muhammad Adimas Amri
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1595.485 KB) | DOI: 10.25105/jogee.v3i2.13813

Abstract

The village of Kebonharjo and neighborhoods is zone of relatively high ground movement. In the western part of Indonesia, it was formed due to the influence of the collision two tectonic plates. Kebonharjo and neighborhoods are earthquake and volcanic zone. With a steep slope and high rainfall data, one of the biggest factors for landslides. This study aims to fins out what potential couse the area to become a landslide-prone area and there indications of anything in the research area. There are several obstacles to the development of the Kebonharjo village are and suggroundings. In its study using the DVMBG method qhich combines several parameters, on of which is rainfall parameter data, geology, slope, land use and soil types. The potential for landslides in Kebonharjo village really needs attention because the are is very high and the rainfall is high, the potential for large landslides. After counducting the research, it can be seen the types of landslides according to (Varnes, 1978), type of landslides Earth Spread and Earth Flow. Keywords: Soil Movement, DVMBG method, tectonic.
PENILAIAN SITUS GEOLOGI PADA GEOHERITAGE ZONA KULON PROGO, DAERAH ISTIMEWA YOGYAKARTA SEBAGI POTENSI DAERAH GEOWISATA : ASSESSMENT OF GEOLOGICAL SITES IN THE GEOHERITAGE ZONE OF KULON PROGO, YOGYAKARTA SPECIAL REGION AS A POTENTIAL OF A GEOWISATA AREA Fandika Agustiyar; Hendry Wirandoko; Ardiansyah Bagus Nursahid; Rachel Puspita Sari
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (4466.262 KB) | DOI: 10.25105/jogee.v3i2.14007

Abstract

Daerah Istimewa Yogyakarta khususnya di Kabupaten Kulon Progo mempunyai bentuk morfologi yang sangat bervariasi dari topografi datar hingga perbukitan yang memanjang dengan arah barat daya – timur laut (Perbukitan Menoreh) yang tentunya dipengaruhi oleh beberapa geological event yaitu pre-OAF, OAF, dan post-OAF. Bentuk morfologi daerah Kulon Progo dapat menggambarkan adanya kontrol struktur geologi dan perbedaan batuan yang menyusun daerah tersebut. Dalam konteks geologi, daerah Kulon Progo juga dapat mempresentasikan akan banyaknya geosite yang memiliki berbagai keunikan dari aspek geologi. Oleh karena itu, untuk mengetahui potensi dan kelayakan geoheritage daerah Kulon Progo sebagai potensi geowisata, maka dilakukan kajian dan penilaian terhadap setiap geosite yang terdapat di daerah penelitian. Penelitian ini menggunakan beberapa metode yaitu metode akuisisi, analisis, dan sintesis data. Berdasarkan hasil penelitian tersebut menunjukan bahwa nilai kelayakan (feasibility) dan potensi dari beberapa situs geosite Kulon Progo yang berada di Formasi Nanggulan Eosen, Gua Kalilingseng, Gunung Kendil, Gua Sriti, Gua Kiskendo, Air Terjun Kembang Soka dan Sungai Mudal rata-rata memiliki nilai lebih dari 50 %, sehingga dapat dikategorikan layak sebagai objek geoheritage. Maka, dari hasil studi penilaian potensi dan kelayakan terhadap beberapa geosite di daerah penelitian menunjukkan bahwa geoheritage Kulon Progo secara keseluruhan dapat digolongkan layak untuk dijadikan sebagai daerah geowisata.
ANALISIS DAN VISUALISASI 2D LINEAMENT BERBASIS NETWORKGT PADA DAERAH KADU, SUMEDANG, JAWA BARAT : ANALYSIS AND VISUALIZATION OF 2D LINEAMENT BASED ON NETWORKGT REGIONS KADU, SUMEDANG, JAVA M Arief Situmorang; Yogie Z. Rochmana
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3183.346 KB) | DOI: 10.25105/jogee.v3i2.14173

Abstract

Daerah penelitian memiliki struktur geologi yang kompleks seperti sesar dan lipatan. Hal ini didukung dengan adanya data DEMNas yang memperlihatkan pola-pola kelurusannya. Citra satelit berupa data DEMNas digunakan sebagai data awal untuk mengidentifikasi pola kelurusan pada daerah telitian. Dalam melakukan analisis pola dan keterkaitan kelurusan menggunakan suatu toolbox pada aplikasi ArcGIS. NetworkGT merupakan instalasi toolbox untuk analisis keterkaitan antar lineament sehingga diketahui persebaran variasi geometri dan topologi. Persebaran variasi geometri meliputi aspek lokasi, orientasi dan panjang lineament tersebut. Topologi meliputi titik temu dan koneksivitas antar lineament. Pola kelurusan pada daerah ini searah dengan trend kemenerusan Baribis-Kendeng Thrust Fault Zone yang berorientasi pada baratlaut-tenggara (NW-SE). Hasil analisis geometri pada daerah penelitian memiliki rata-rata panjang lineament 0,778 km dengan hubungan antar lineament yang saling bersinggungan dan berpotongan dengan simbol Branches and Nodes. Pola kelurusan dalam Analisis spasial yang diklasifikasikan dalam 5 kelas sesuai 2D Intensity.
ANALISIS LAJU INFILTRASI TERHADAP BATUAN PENYUSUN KECAMATAN MAKASAR, KOTA JAKARTA TIMUR: ANALYSIS OF INFILTRATION RATE IN ROCK FORMATION ON MAKASAR SUB-DISTRICT, EAST JAKARTA Carollus Armando Meze Muku; Himmes Fitra Yuda; M. Adimas Amri
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1403.633 KB) | DOI: 10.25105/jogee.v3i2.14196

Abstract

Infiltrasi dan jenis batuan menjadi hal yang cukup penting dalam sebuah parameter penentuan daerah resapan air. Jakarta merupakan kota dengan tingkat peralihan tata guna lahan cukup intens, sehingga daerah resapan air semakin berkurang dan tingginya tingkat pertumbuhan penduduk menyebabkan sering terjadinya bencana banjir saat musim hujan. Maka dari itu, perlu adanya rencana jangka panjang untuk mengelola tata ruang daerah resapan air di Jakarta sebagai salah satu langkah untuk menanggulangi bencana banjir dan menjadi cadangan air tanah di ibukota. Jenis batuan mengontrol pula sebagai kriteria daerah resapan. Pengambilan data uji nilai infiltrasi menggunakan data primer dengan pengukuran langsung di lapangan menggunakan Double Ring Infiltrometer, sedangkan jenis batuan penyusun dapat diketahui Peta Geologi Regional setempat yang merupakan hasil penelitian sebelumnya.
ANALISIS ARUS PURBA PADA DAERAH KEDUNGWRINGIN, KECAMATAN SEMPOR, JAWA TENGAH: PALEOCURRENT ANALYSIS OF KEDUNGWRINGIN REGION, SEMPOR DISTRICT, CENTRAL JAVA Aditya Henri Saputra; Budi Wijaya; Rendy
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3783.684 KB) | DOI: 10.25105/jogee.v3i2.14212

Abstract

The exposed sandstone unit in the research area located in the Kedungwringin area, Sempor District, Central Java Province is included in the Waturanda Formation. At the research location, there are 4 exposed rock units, namely Tuff Unit, Sandstone Unit, Breccia Unit, and Alluvial Unit. The sandstone unit in the study area has a type of Arkosic Wacke Sandstone. Measurable stratigraphic measurements were carried out on the three tracks and it was found that the research area was stratigraphically in the sandstone unit and the breccia unit in the south of the study area, and had a southwest-southeast current direction which was obtained based on measurements of sedimentary structures that developed in the study area.
ANALISIS GEOKIMIA FLUIDA PANAS BUMI DAERAH ARJOSARI DAN SEKITARNYA, KECAMATAN ARJOSARI, KABUPATEN PACITAN, JAWA TIMUR: ANALYSIS OF GEOCHEMISTRY GEOTHERMAL FLUIDS IN ARJOSARI AND SURROUNDING AREAS, ARJOSARI DISTRICT, PACITAN REGENCY, EAST JAVA Julius Leonardo Simamora; Fajar Hendrasto; Untung Sumotarto; Mira Meirawaty
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 3, NOMOR 2, AGUSTUS 2022
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3087.286 KB) | DOI: 10.25105/jogee.v3i2.14667

Abstract

Energi panasbumi adalah sumber daya alam terbarukan berupa air panas atau uap yang terbentuk dari pemanasan air bawah permukaan, dan Indonesia merupakan Negara yang memiliki sumber daya alam panas bumi yang besar. Lokasi penelitian berada pada daerah Arjosari, kabupaten Pacitan, Jawa Timur. Pada daerah penelitian terdapat lima lokasi manifestasi fluida permukaan. Hasil dari analisis geokimia menjukkan manifestasi panasbumi dengan tipe manifestasi berupa air panas, mata air hangat, dan mata air dingin, dengan jenis air acid sulphate waters. Berdasarkan atas analisis geoindikator menunjukkan arah outflow yang cenderung kearah timur, isotope yang berada pada meteoric line.

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