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ANALISIS GEOKIMIA HIDROKARBON SUMUR “FLP” CEKUNGAN JAWA TIMUR UTARA: GEOCHEMICAL ANALYSIS OF HYDROCARBON WELL "FLP" BASIN NORTH EAST JAVA Filipus Armando Armando Ginting; Yarra Sutadiwiria; Cahyaningratri Prima Riyandhani; Muhammad Burhannudinnur; Imam Setiaji Ronoatmojo; Novi Triany
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 4, NOMOR 1, FEBRUARI 2023
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i1.14415

Abstract

Daerah riset terdapat pada Blok Madura, Cekungan Jawa Timur Utara berupa dua sumur FLP-1 dan FLP-2. Analisa dilakukan agar mengetahui karakteristik batuan induk, material organic, biomarker, dan potensi batauan induk(source rock). FLP-1 diketahui terdapat Formasi Tuban dan Formasi Tawun, pada sumur FLP-2 diketahui Formasi Kujung dan Formasi Tuban.indikasi batuan induk potesial (tipe kerogen II) potensi mengenerasikan hidrokarbon jenis utama berupa gas, asal material tumbuhan tingkat tinggi dan lingkungan pengendapan organik fluvio-deltaic. Sumur FLP-2 Formasi Kujung Indikasi batuan induk efektif. (tipe kerogen II/III) potensi menggenerasikan hidrokarbon jenis minyak dan gas, asal material alga dan tumbuhan tingkat tinggi dan fasies organik marine-deltaic.
ANALISIS LINGKUNGAN PENGENDAPAN PADA LAPANGAN AR & RB FORMASI TALANG AKAR, CEKUNGAN SUMATRA SELATAN: ANALYSIS OF DEPOSIT ENVIRONMENT IN AR & RB FIELDS OF THE TALANG AKAR FORMATION, SOUTH SUMATRA BASIN Andreas Rendy Bramantyo; Muhammad Burhannudinnur; wildan Tri K
Jurnal Eksakta Kebumian Vol. 3 No. 1 (2022): JURNAL EKSAKTA KEBUMIAN (JEK)
Publisher : Fakultas Teknologi Kebumian dan Energi, Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jek.v3i1.16444

Abstract

Abstrak Penelitian ini dilakukan pada lapangan AR & RB, formasi Talang Akar, Cekungan Sumatra Selatan. Dimana formasi Talang Akar ini memiliki potensi yang sangat besar dalam memiliki kandungan minyak bumi dan gas di Cekungan Sumatra Selatan ini, namun tidak semudah itu untuk menemukan minyak dan gas, perlu dilakukan analisis yang mendalam dalam melakukan eksplorasi. Salah satu analisis yaitu analisis lingkungan pengendapan. Dalam melakukan analisis ini menggunakan software petrel 2017. Berdasarkan hasil dari pengolahan data menghasilkan bahwa lapangan AR & RB terbentuk pada lingkungan pengendapan fluvial, delta plain dan delta front. Pembagian sekuen pada lapangan ARB terbagi menjadi 3 dan memiliki fasies yaitu flooding surface 1 terdapat fasies fluvial channel, point bar, creavase splay dan floodplain, flooding surface 2 terdapat fasies distributary channel, mouth bar dan mud flat dan flooding surface 3 terdapat fasies mouth bar dan mud flat.   Kata kunci : Lingkungan Pengendapan, Cekungan Sumatra Selatan dan Formasi Talang Akar   Abstract This research was conducted in field AR & RB, Talang Akar formation, South Sumatra Basin. Where the Talang Akar formation has enormous potential in containing oil and gas in the South Sumatra Basin, but did not find it to find oil and gas, in-depth analysis is needed to carry out exploration. One of the analyzes is the analysis of the depotitional environment. In conducting this analysis using petrel 2017 software. Based on the results of data processing, it was found that the AR & RB field was formed in a fluvial, delta plain and delta front environment. Sequence distribution in field ARB is divided into 3 and has facies, namely flooding surface 1 which has fluvial channel, point bar, creavase splay and floodplain facies, flooding surface 2 has distributed channel facies, mouth bar and mud flat and flooding surface 3 has mouth bar and mud flat facies.  Keywords: Depotitional Environment, South Sumatra Basin and Talang Akar Formation
ANALISIS LINGKUNGAN PENGENDAPAN PADA LAPANGAN AR & RB FORMASI TALANG AKAR, CEKUNGAN SUMATRA SELATAN : DUG WELL GROUNDWATER ANALYSIS IN KARANGTENGAH VILLAGE, BOGOR DISTRICT, WEST JAVA PROVINCE Andreas Rendy Bramantyo; Muhammad Burhannudinnur; Wildan Tri Koesmawardani
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.16008

Abstract

Penelitian ini dilakukan pada lapangan AR & RB, formasi Talang Akar, Cekungan Sumatra Selatan. Dimana formasi Talang Akar ini memiliki potensi yang sangat besar dalam memiliki kandungan minyak bumi dan gas di Cekungan Sumatra Selatan ini, namun tidak semudah itu untuk menemukan minyak dan gas, perlu dilakukan analisis yang mendalam dalam melakukan eksplorasi. Salah satu analisis yaitu analisis lingkungan pengendapan. Dalam melakukan analisis ini menggunakan software petrel 2017. Berdasarkan hasil dari pengolahan data menghasilkan bahwa lapangan AR & RB terbentuk pada lingkungan pengendapan fluvial, delta plain dan delta front. Pembagian sekuen pada lapangan ARB terbagi menjadi 3 dan memiliki fasies yaitu flooding surface 1 terdapat fasies fluvial channel, point bar, creavase splay dan floodplain, flooding surface 2 terdapat fasies distributary channel, mouth bar dan mud flat dan flooding surface 3 terdapat fasies mouth bar dan mud flat. This research was conducted in field AR & RB, Talang Akar formation, South Sumatra Basin. Where the Talang Akar formation has enormous potential in containing oil and gas in the South Sumatra Basin, but did not find it to find oil and gas, in-depth analysis is needed to carry out exploration. One of the analyzes is the analysis of the depotitional environment. In conducting this analysis using petrel 2017 software. Based on the results of data processing, it was found that the AR & RB field was formed in a fluvial, delta plain and delta front environment. Sequence distribution in field ARB is divided into 3 and has facies, namely flooding surface 1 which has fluvial channel, point bar, creavase splay and floodplain facies, flooding surface 2 has distributed channel facies, mouth bar and mud flat and flooding surface 3 has mouth bar and mud flat facies.
Identification Analysis of Fluid Type in the Low Resistivity Zone of Well Z-2 Field "Z", South Sumatera Sigit Rahmawan; Firman Herdiansyah; Suryo Prakoso; Muhammad Burhannudinnur; Syamsul Irham; Samsol; Muhammad Himawan Prakoso; Hayafa Fakhriyatul Ummah
Journal of Earth Energy Science, Engineering, and Technology Vol. 6 No. 2 (2023): JEESET VOL. 6 NO. 2 2023
Publisher : Penerbitan Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jeeset.v6i2.17522

Abstract

Hydrocarbon reserves are one of the main points that are very important in the sustainability of the productivity of an oil and gas field. This important point is greatly influenced by several parameters that can be obtained by various measurements and analysis. One of the most influential parameters in the analyses of the amount of hydrocarbon reserves in a reservoir is the water saturation value. The water saturation parameter will also be greatly influenced by the electrical parameters of the fluid-containing rock in the reservoir. Sometimes the electrical parameters of this rock, in this case resistivity becomes one of the benchmark parameters, whether the zone or reservoir has potential or is interesting to be developed or produced. However, there are several reservoirs or zones that experience low resistivity effects which will give an initial indication that the zones or reservoirs are not attractive or have no effect on development. In this Z field, there is a zone that experiences low resistivity effects, making this zone unattractive for production. So to be able to make these zones attractive for production, an identification analysis was carried out on Zones A and B in this Z field to determine the type or type of fluid from the two zones. The initial analysis was carried out petrographically from rock sample incisions at certain depths in Zones A and B so that it is known that the cause of the low resistivity effect in the two zones is the presence of pyrite minerals and illite clay which are the main causes of the low resistivity effect. Furthermore, an analysis of the identification of fluid types was carried out using the double apparent resistivity method with the results obtained that in Zones A and B there are 2 types of fluids, namely hydrocarbons and water with a depth limit of 3650 ft in Zone A and 4558 ft in Zone B. By knowing the type of fluid, the hydrocarbons contained in these two zones should be able to increase interest in the production of these zones as a potential zone for production, but it is necessary to perforate at a depth range indicated by the hydrocarbon fluid and carry out initial production tests to prove the results of the analysis in this study.
THE EFFECT OF HARMFUL AND FAVORABLE GAS AND CHEMICAL CONTENT EMITTED BY MUD VOLCANO TO ENVIRONMENT Muhammad Burhannudinnur; Rosmalia Dita Nugraheni; Astri Rinanti
INDONESIAN JOURNAL OF URBAN AND ENVIRONMENTAL TECHNOLOGY VOLUME 4, NUMBER 1, OCTOBER 2020
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/urbanenvirotech.v4i1.8001

Abstract

The recent eruption of Kesongo mud volcano (MV) that occurred in 28August 2020 in Blora, Central Java was a common natural phenomenon.MV eruption occurred periodically depending on the recharge fluid systemthat interconnected to a geothermal system and hydrocarbon reservoir.During the eruption, methane and CO2 gas were emitted to theatmosphere together with rocks, muds and fluids flowing from the fractureand fault system of MV. The extruded materials could be harmful andbeneficial for the affected ecosystem. Aims: This study aimed to addressthe potential impact of the extruded mud volcano materials to theenvironment. Methodology and Results: An attempt was carried out byinvestigating gas and fluid content of every mud volcano morphology in theselected 11 areas of Kradenan, Central Java and Sidoarjo, East Java. The pristine fluids and gas of MV were sampled for chemical and toxiccompound observation. Gas composition and type was observed using gaschromatography. The result shows that methane gas content ranges from0.06 to 67.6 mol%., while the CO2 content ranges from 0.21 to 79.9 mol%.Methane gas exhibits thermogenic gas that associated with hydrocarbongeneration. Conclusion, significance and impact study: The chemicalcompound of fluids indicates high Boron (B) content above 0.5 ppm whichhas harmful effect for crops and human health, but some compounds ofCa, Na, K, Mg present as essential elements for soil nutrient. According tothe methane flux and chemical compound emitted by mud volcano, thisstudy contributes to a management practice to restore and conserve the global ecosystem.
KARAKTERISTIK KESTABILAN LERENG DAERAH JATIGEDE KABUPATEN SUMEDANG, PROVINSI JAWA BARAT BERDASARKAN ANALISIS KINEMATIK Sofyan Rachman Idris; Dicky Muslim; Nana Sulaksana; M. Burhannudinnur
Jurnal Teknologi Mineral dan Batubara Vol 15 No 2 (2019): Jurnal Teknologi Mineral dan Batubara Edisi Mei 2019
Publisher : Balai Besar Pengujian Mineral dan Batubara tekMIRA

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.30556/jtmb.Vol15.No2.2019.1009

Abstract

Daerah penelitian secara administratif berada di Kecamatan Jatigede, Kabupaten Sumedang, Provinsi Jawa Barat. Berdasarkan sudut pandang geologi, daerah Jatigede memiliki beberapa permasalahan yang timbul akibat kondisi geologi daerah tersebut yaitu berupa pengaruh keberadaan struktur geologi yang berhubungan dengan stabilitas maupun keruntuhan lereng. Untuk dapat mengidentifikasi tipe keruntuhan lereng batuan, dapat dilakukan analisis kinematik menggunakan metode scanline sampling. Penelitian ini dibagi menjadi 15 lokasi scanline sampling. Pada penelitian, dilakukan juga perhitungan uniaxial compressive strenght (UCS) dan rock quality designation (RQD) pada lereng tumpuan barat Bendungan Jatigede. Hasil analisis kinematik mendapatkan potensi tipe keruntuhan baji pada lereng scanline (SL) 1, 4 – 11 sedangkan pada lereng SL 2 dan 3 tidak memenuhi syarat keruntuhan baji serta didapatkan kualitas massa batuan (RQD) sedang-sangat baik serta penentuan nilai UCS yang menunjukan kekuatan material batuan yang lemah.
ANALISIS LINGKUNGAN PENGENDAPAN PADA LAPANGAN AR & RB FORMASI TALANG AKAR, CEKUNGAN SUMATRA SELATAN : ANALYSIS OF DEPOSIT ENVIRONMENT IN AR & RB FIELDS OF THE TALANG AKAR FORMATION, SOUTH SUMATRA Bramantyo, Andreas Rendy; Burhannudinnur, Muhammad; Koesmawardani, Wildan Tri
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.v4i2.16008

Abstract

Penelitian ini dilakukan pada lapangan AR & RB, formasi Talang Akar, Cekungan Sumatra Selatan. Dimana formasi Talang Akar ini memiliki potensi yang sangat besar dalam memiliki kandungan minyak bumi dan gas di Cekungan Sumatra Selatan ini, namun tidak semudah itu untuk menemukan minyak dan gas, perlu dilakukan analisis yang mendalam dalam melakukan eksplorasi. Salah satu analisis yaitu analisis lingkungan pengendapan. Dalam melakukan analisis ini menggunakan software petrel 2017. Berdasarkan hasil dari pengolahan data menghasilkan bahwa lapangan AR & RB terbentuk pada lingkungan pengendapan fluvial, delta plain dan delta front. Pembagian sekuen pada lapangan ARB terbagi menjadi 3 dan memiliki fasies yaitu flooding surface 1 terdapat fasies fluvial channel, point bar, creavase splay dan floodplain, flooding surface 2 terdapat fasies distributary channel, mouth bar dan mud flat dan flooding surface 3 terdapat fasies mouth bar dan mud flat. This research was conducted in field AR & RB, Talang Akar formation, South Sumatra Basin. Where the Talang Akar formation has enormous potential in containing oil and gas in the South Sumatra Basin, but did not find it to find oil and gas, in-depth analysis is needed to carry out exploration. One of the analyzes is the analysis of the depotitional environment. In conducting this analysis using petrel 2017 software. Based on the results of data processing, it was found that the AR & RB field was formed in a fluvial, delta plain and delta front environment. Sequence distribution in field ARB is divided into 3 and has facies, namely flooding surface 1 which has fluvial channel, point bar, creavase splay and floodplain facies, flooding surface 2 has distributed channel facies, mouth bar and mud flat and flooding surface 3 has mouth bar and mud flat facies.
ANALISIS BIBLIOMETRIK PERKEMBANGAN MUTAKHIR DALAM STUDI ANISOTROPI SEISMIK (2017 -2022): BIBLIOMETRIC ANALYSIS OF RECENT DEVELOPMENT IN THE SEISMIC ANISOTROPY STUDIES (2017 -2022) Yuda, Himmes Fitra; Ronoatmojo, Imam Setaiji; Burhannudinnur, Muhammad; Nuryana, Suherman 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.v5i1.18206

Abstract

The development of seismic anisotropy needs to be studied systematically hence research could be focused on the latest scientific knowledge, therefore a bibliometric analysis is needed as a measurement of citation strength in the form of mapping "co-occurrence", "co-author" and "co- citation", thus the strength of the research direction could be well understood. The software which is used; VOSviewer version 1.6.18 examined at least 494 papers in the SCOPUS domain during 2017 -2020. It appears from the results that the development of the seismic anisotropy are very rapidly dominated by the needs of the applied science and pure science. The heavily publication countries are United States of America, China and Japan. However, in reality, this density does not necessarily correspond to the number of citations between countries, as well with publications in Japan.
Utilization of Acoustic Wave Velocity for Permeability Estimation in Static Reservoir Modeling: A Field Case Prakoso*, Suryo; Burhannudinnur, Muhammad; Irano, Teddy; Herdiansyah, Firman
Aceh International Journal of Science and Technology Vol 10, No 1 (2021): April 2021
Publisher : Graduate School of Syiah Kuala University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13170/aijst.10.1.20328

Abstract

Several researches have shown that P-wave velocity carries information on the complexity of the rock's pore geometry and pore structure. Their complexity can be characterized by critical porosity. Therefore, the P-wave velocity is used to estimate permeability. This research uses data taken from the Tomori formation from Banggai-Sula basin, Central Sulawesi, which is a carbonate rock reservoir. Also, this research aims to obtain a 3D permeability model by using acoustic wave velocity cube data. The results show that permeability can be modeled well using acoustic wave velocity data. Furthermore, compared to the raw data log of permeability, the modeling results using wave velocity based on critical porosity show good results. This method is another alternative to permeability modeling if acoustic wave velocity cube data is available.
The Linear and Non-Linear Background Energy Approach in The Seismic S/N Ratio Enhancement Imam Setiaji Ronoatmojo; Yarra Sutadiwiria; Muhammad Burhannudinnur; Dewi Syavitri
Scientific Contributions Oil and Gas Vol. 46 No. 2 (2023): SCOG
Publisher : Testing Center for Oil and Gas LEMIGAS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29017/scog.46.2.318

Abstract

Side-swept is often understood as a side sweep of seismic waves that occurs on the surface. This understanding creates confusion when considering that side-swept is a part of linear function, in fact side-swept could be in the form of sweeping waves from the reflector on the side, so side-swept is a non-linear function like a signal. The implications for noise reduction with the t-p transformation becomes more complex. The elimination of side-swept in this study, relies on an application using an algorithm developed by Hampson (1987). Initial data conditioning preparation should be needed to clarify the difference between linear and non-linear functions through static refraction correction and velocity analysis, then coherent noise elimination (ground-droll) is carried out through f-k domain transformation, as well as random noise through f-x domain transformation. Side-swept is eliminated in t-p domain. Energy observation shows the remaining noise energy caused by coherent noise, random noise and non-linear side-swept functions. It proves that it is difficult to remove a non-linear function that overlaps the reflector signal. The best step is to minimize coherent (linear) noise and random noise by consistently using an amplitude correction indicator on the surface and performing velocity analysis especially for the suspected power spectrum as an effort to attenuate side-swept wave interference on the reflector signal. Finally, the signal restoration efforts due to non-linear noise attenuation, is carried out by surface consistent deconvolution
Co-Authors Abdalrazaq, Eid Abdul Karim Alan, Muhammad Rallupy Meyraldo Anak Agung Sagung Mayun Yudhyasmara Prabandari Andreas Rendy Bramantyo Arfiani Nur Arista Muhartanto Arista Muhartanto, Arista Asih Retno Dewanti Asseggaf, Abdurrahman Astri Rinanti Atridia Wilastrina Awang Eka Novia Rizali Bani Nugroho Benyamin Benyamin Benyamin Benyamin Benyamin Benyamin, Benyamin Bramantyo, Andreas Rendy Budi Wijaya Cahaya Rosyidan Cahyaningratri Prima Riyandhani Ciptadhi Tri Oka Binartha Dardji Noeradi Dicky Muslim Dyah Ayu Setyorini Eko Widianto Erick Strada Dolok Saribu Fadliah, Fadliah Filipus Armando Armando Ginting Firman Herdiansyah Firman Herdiansyah Firman Herdiansyah, Firman Galang Fahmi Maulana Ghanima Yasmaniar Gihon Nugrahadi Grace Khatrine Hafiz, Surya Darma Hamid Nurrohman Hartami, Pantjanita Novi Hasri Hasri Havidh Pramadika Hayafa Fakhriyatul Ummah Himmes Fitra Yuda Husla, Ridha Imam Setiaji Ronoatmojo Indah Raya Irano, Teddy Ischak, Mohammad Junita Trivianty Musu Khatrine, Grace Koesmawardani, Wildan Tri Kollur, Shivaa Prasad Lestari Lestari Lukas Lukas Maulana, Galang Fahmi Maulana, Yuga Maulani, Mustamina Meirawaty, Mira Mixsindo Korra Herdyanti Mohammad Apriniyadi Muhammad Himawan Prakoso Muhammad Yusril Ihza Mahendra Triany Mulia Ginting Mustamina Maulani Musu, Junita Trivianty Nana Sulaksana Novi Triany Nugraheni, Rosmalia Dita Nur Amalina Onnie Ridaliani, Onnie Pantjanita Novi Hartami Paulina Taba Prakoso*, Suryo Ramadhan Adhitama Rendy Reno Pratiwi Reno Pratiwi Ricky Andrian Tampubolon Ririn Yulianti Ronoatmojo, Imam Setaiji Rosmalia Dita Nugraheni Rosmalia Dita Nugraheni Samsol Samsol Samura, Lisa Sangayu Ketut Laksemi Nilotama Setyorini, Dyah Ayu Shabrina Sri Riswati Sigit Rahmawan Sofyan Rachman Idris Sofyan Rachman, Sofyan Sonbait, Daniel Subandrio Sugiarto, Eddy Suherman Dwi Nuryana Suherman Dwi Nuryana Suliestyah Sulistiani Jarre Suryo Prakoso, Suryo Syahruddin Kasim Syamsul Irham Syamsul Irham Syavitri, Dewi Tampubolon, Ricky Andrian Teddy Irano Tuheteru, Edy Jamal Virginia Suryani Setiadi Wahid Wahab, Abdul Wegig Murwonugroho Widayati Putri, Tri wildan Tri K Wildan Tri Koesmawardani Wildan Tri Koesmawardani Wildan Tri Koesmawardani Yarra Sutadiwiria Yuda, Himmes Fitra Yudhyasmara Prabandari, Anak Agung Sagung Mayun Zahra, Audrey