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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 24 Documents
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Search results for , issue "VOLUME 4, NOMOR 2, AGUSTUS 2023" : 24 Documents clear
ANALISIS GEOKIMIA AIR DARI MANIFESTASI PERMUKAAN PADA PROSPEK PANASBUMI FF, KABUPATEN CIANJUR, PROVINSI JAWA BARAT: GEOCHEMISTRY WATER ANALYSIS FROM SURFACE MANIFESTATIONS AT FF GEOTHERMAL PROSPECT, CIANJUR REGENCY, WEST JAVA PROVINCE Fazli, Faiz; Hendrasto, Fajar; Wijaya, Budi
Journal of Geoscience Engineering and Energy VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.16068

Abstract

Lokasi penelitian prospek panasbumi FF yang terletak di Kabupaten Cianjur, Provinsi Jawa Barat mempunyai sumber daya panas bumi yang berpotensi cukup baik. Penelitian ini dilakukan dengan menggunakan data (sekunder) dari Ditjen Energi Baru Terbarukan dan Konservasi Energi (EBTKE) berupa data geokimia fluida serta isotop stabil untuk menghasilkan suatu model konseptual aliran fluida pada lapangan penelitian. Penelitian ini dilakukan untuk menunjukkan lebih detail melalui data permukaan sehingga dapat memberikan gambaran model untuk panasbumi yang terdapat di daerah FF. Terdapat dua tipe air pada daerah penelitian yaitu peripheral water pada lokasi manifestasi MG01, MG02, dan MG05 serta tipe suphate water pada lokasi manifestasi MG03, dan MG04. Pada lokasi MG01 yang terletak di bagian timurlaut daerah penelitian merupakan zona outflow, sedangkan pada lokasi sekitar puncak gunung (bagian baratdaya daerah penelitian) merupakan zona upflow. Sumber air pada daerah penelitian merupakan sea water berupa tipe immature water. The location of the observation field includes the FF geothermal prospect area, Cianjur Regency, West Java Province which has the potential of geothermal resources. This research was conducted by using secondary data from General Directorate of New Renewable Energy and Energy Conservation (EBTKE) in the form of geochemical and stable isotope data so as to produce a fluid flow conceptual model in the research field. Therefore, this study was conducted to look in more detail through surface data so that it can provide an overview for the geothermal model in the FF area. There are two types of water in the research area, namely peripheral water at the of manifestation location of MG01, MG02, and MG05 and the type of suphate water at the manifestation location of MG03, and MG04. At location MG01 which is located in the northeastern part of the research area is an outflow zone, while the location around the top of the mountain (southwestern part of the study area) is an upflow zone. The water source in the research area is sea water in the form of immature water
ANALISIS SEKUEN STRATIGRAFI BERDASARKAN DATA LOG LAPANGAN “DRK” CEKUNGAN JAWA TIMUR UTARA : ANALYSIS OF SEQUENCE STRATIGRAPHY BASED ON LOG DATA “DRK” FIELD NORTH EAST JAVA BASIN Karima, Dani Rizki; Guntoro, Agus
Journal of Geoscience Engineering and Energy VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.16084

Abstract

Daerah penelitian terletak di Lapangan “DRK” yang berada pada Zona Rembang, Cekungan Jawa Timur Utara. Penelitian ini dilakukan untuk menganalisis kondisi bawah permukaan melalui korelasi sumur dan analisis perkembangan distribusi sedimentasi pada Cekungan Jawa Timur Utara. Penelitian ini menggunakan lima data sumur. Analisis Sikuen Stratigrafi didasarkan dari data log, dimana hasil dari analisis Sikuen Stratigrafi ini dapat diinterpretasikannya Fasies dan Lingkungan Pengendapan pada daerah penelitian. The research area is located in the "DRK" field in the Rembang Zone, North East Java Basin. This study was conducted to analyze the subsurface conditions through well correlation and analysis of the development of sedimentation distribution in the North East Java Basin. This study uses five data wells. Sequence Stratigraphy analysis is based on log data, where the results of this Stratigraphic Sequence analysis can be interpreted by Facies and Depositional Environment in the study area.
KARAKTERISTIK BATUGAMPING FORMASI WONOSARI DI DAERAH BUNDER DAN SEKITARNYA, WONOSARI,GUNUNGKIDUL D.I.Y : THE CHARACTERISTICS OF THE WONOSARI FORMATION LIMESTONE IN THE BUNDER AREA AND ITS SURROUNDINGS, WONOSARI, GUNUNGKIDUL, D.I.Y Hafiz, Surya Darma; Moehammad Ali Jambak; Budi Wijaya; Mira Meirawaty; Cahyaningratri Prima Ryandhani; Wildan Tri Koesmawardani; Nuryana, Suherman Dwi; Zefanya, Oliver Enrico
Journal of Geoscience Engineering and Energy VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.17301

Abstract

Studi ini bertujuan untuk mengkaji karakteristik  batugamping Formasi Wonosari di Desa Bunder, Kecamatan Ponjong, Kabupaten Gunungkidul, DIY. Analisis litologi mengungkapkan bahwa batuan wackstone berwarna coklat dengan tekstur bioklastik, terdiri dari sekitar 75% lumpur karbonat/mikrit dan 25% fragmen butiran. Kehadiran fosil meliputi foraminifera planktonik dan bentos, dengan fragmen bioklas yang utuh mengalami proses mikritisasi dan neomorfisme menjadi kalsit spar yang jernih. Pengamatan lapangan menunjukkan adanya singkapan batuan yang segar maupun lapuk, dengan jurus lapisan berkisar antara N100° E hingga 105° E dan kemiringan rata-rata sekitar 4° - 8°. Ketebalan perkiraan formasi ini adalah sekitar 150-200 m. Berdasarkan analisis mikropaleontologi, spesies foraminifera planktonik dominan seperti Orbulina universa dan Sphaerodinella subdehiscens mengindikasikan rentang umur antara N10-N18. Satuan ini menunjukkan adanya struktur sedimen berlapis baik dan struktur masif gelegar, menandakan pengendapan di lingkungan yang tenang dengan energi rendah. Penelitian ini memberikan pemahaman lebih baik tentang litologi, lingkungan pengendapan, dan perkiraan umur Formasi Wonosari di wilayah penelitian. This study focuses on the characteristic of the Wonosari Formation carbonate rocks in Bunder Village, Ponjong Sub-district, Gunungkidul Regency, DIY. The lithological analysis reveals brown-colored wackstone with a bioclastic texture, consisting of 75% mud-supported carbonate/micrite and 25% grain fragments. The fossil assemblage includes planktonic and benthic foraminifera, with intact bioclastic fragments exhibiting signs of micritization and subsequent neomorphism into clear calcite spar. Field observations indicate fresh and weathered outcrops with a bedding strike ranging from N100° E to 105° E and an average dip angle of 4° - 8°. The estimated thickness of the formation is around 150-200 m. Based on micropaleontological analysis, dominant planktonic foraminifera species such as Orbulina universa and Sphaerodinella subdehiscens suggest an age range of N10-N18. The unit displays well-layered sedimentary structures and occasional massive structures, indicating deposition in a low-energy, relatively calm environment. This research contributes to a better understanding of the lithology, depositional environment, and age estimation of the Wonosari Formation in the study area..
ANALISIS KUALITAS AIR TANAH SUMUR GALI DI DESA KARANGTENGAH, KABUPATEN BOGOR, PROVINSI JAWA BARAT: DUG WELL GROUNDWATER ANALYSIS IN KARANGTENGAH VILLAGE, BOGOR DISTRICT, WEST JAVA PROVINCE Arum, Dannum Sekar; Asseggaf, Abdurrachman; Lestari, Arini Dian
Journal of Geoscience Engineering and Energy VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.18079

Abstract

Air merupakan salah satu kebutuhan pokok manusia yang krusial keberadaannya dalam kehidupan. Pada makalah ini akan dibahas secara lebih terperinci kualitas air tanah yang didapatkan dari pembuatan sumur gali pada Desa Karangtengah, Kabupaten Bogor, Provinsi Jawa Barat. Pada penelitian ini melibatkan pengambilan sampel air pada dua buah sumur gali yang nantinya akan dianalisa lebih lanjut di laboratorium sesuai dengan ketentuan Permenkes No.32 Tahun 2017 mengenai standar baku air bersih, juga mengetahui asal dari air tanah tersebut. Metode yang digunakan dalam penelitian ini adalah eksperimen laboratorium dan analisis hidrogeologi mengenai akuifer yang menyimpan air tanah. Hasil uji laboratorium menunjukan bahwa kedua sumur tersebut tidak memenuhi standar baku mutu air bersih. Air sumur gali 1 memiliki pH sebesar 6,02 sedangkan air sumur gali 2 memiliki kandungan MBAS (Methylene Blue Active Surfactant) sebesar 0,134 yang melebihi batas baku mutu. Air tanah berasal dari akuifer tertekan yang terdiri atas satuan batulempung dan sisipan batupasir. Water is one of the basic human needs that is crucial for its existence in life. This paper will discuss in more detail the quality of groundwater obtained from the construction of dug wells in Karangtengah Village, Bogor Regency, West Java Province. This research involves taking water samples from two dug wells which will be further analyzed in the laboratory in accordance with the provisions of the Minister of Health Regulation No. 32 of 2017 concerning the standard of clean water, as well as knowing the origin of the groundwater. The methods used in this research are laboratory experiments and hydrogeological analysis of aquifers that store groundwater. The results of laboratory tests showed that the two wells did not meet the clean water quality standards. Dug well water 1 has a pH of 6.02 while dug well water 2 has an MBAS (Methylene Blue Active Surfactant) content of 0.134 which exceeds the quality standard limit. Groundwater comes from a confined aquifer consisting of claystone units and sandstone inserts.

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