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Identifikasi Parameter Akustik Permukaan Sumber dengan Metode Elemen Batas Tetti Novalina Manik; Simon Sadok Siregar
Jurnal Fisika FLUX Vol 5, No 2 (2008): Jurnal Fisika Flux Edisi Agustus 2008
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (281.316 KB) | DOI: 10.20527/flux.v5i2.3019

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SUPRESI MULTIPEL PADA DATA SEISMIK LAUT DENGAN METODE DEKONVOLUSI PREDIKTIF DAN RADON DEMULTIPEL Arifudin Arifudin; Ibrahim Sota; Simon Sadok Siregar
Jurnal Fisika FLUX Vol 12, No 2 (2015): Jurnal Fisika FLUX edisi Agustus 2015
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1458.259 KB) | DOI: 10.20527/flux.v12i2.2610

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Abstrak. Pengolahan data seismik merupakan suatu pekerjaan untuk menekan noise dan memperkuat sinyal dari hasil rekaman data lapangan. Supresi multipel dengan metode radon demultipeldan dekonvolusi prediktif adalah salah satu teknik yang biasa digunakan dalam penekanan energi multipel pada data seismik. Prinsip kerjanya adalah dengan memisahkan sinyal dan multipel dalam domain radon dengan memanfaatkan nilai perbedaan moveout antara sinyal primer dan multipel pada metode radon sedangkan pada dekonvolusi prediktif yaitu dengan cara mencari bagian-bagian yang bisa diprediksi dari trace seismik. Metode ini diaplikasikan pada data seismik laut 2D. Studi ini bertujuan untuk mengetahui respon dari metode dekonvolusi prediktif dan radon demultipel dalam mengatenuasi multipel pada pengolahan data seismik dan memperbaiki kualitas data rekaman sehingga menghasilkan penampang seismik yang bebas dari noise. Hasil yang diperoleh dari analisa metode dekonvolusi prediktif dan radon demultipelprediktif, data yang diperkirakan sebagai reflektor primer menjadi lebih menerus sedangkan untuk radon demultipel rasio sinyal terhadap gangguan data keluaran lebih besar dari pada data masukan, hal ini karena nilai multipel pada data seismik berkurang. Kata kunci: supresi multipel, radondemultipel, dekonvolusi prediktif
IDENTIFIKASI SEBARAN BATUBARADARI DATA WELL LOGGING DI DAERAH X, AMPAH BARITO TIMUR Akhmat Faisal; Simon Sadok Sadok Siregar; Sri Cahyo Wahyono
Jurnal Fisika FLUX Vol 9, No 2 (2012): Jurnal Fisika FLUX Edisi Agustus 2012
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1613.854 KB) | DOI: 10.20527/flux.v9i2.6096

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Telah diidentifikasikan sebaran batubara dari data well logging di daerah X AmpahBarito Timur dengan membandingkan dengan hasil data bor sebanyak 38 data borehole.Identifikasi lapisan batubara berdasarkan nilai log gamma ray dan log resistivity. Data welllogging kemudian ditentukan kedalaman ketebalan batubara serta menghitung volumebatubara di daerah X Ampah Barito Timur. Data Well Logging diinterpretasi denganmenggunakan software Well Cad, kemudian untuk mendapatkan kontur dan permodelanbawah permukaan (1D dan 3D) digunakan software Win Log dan Rockworks. HasilInterpretasi Nilai gamma ray batubara di daerah X Ampah Barito Timur adalah 0-30 CPSsedangkan nilai resistivitasnya yaitu 70-100 Ohm.m. Data penampang boreholemenggunakan software winlog sebanyak 38 data well logging. Sebaran batubara di daerah XAmpah Barito Timur teridentifikasi sebanyak lima seam batubara. Perkiraan perhitunganvolume batubara di daerah X adalah 7.312.671,17 m3 didapat dengan cara menghitungluasan (surface) daerah pengambilan data well logging dikalikan dengan ketebalan rata-ratabatubara dari hasil interpretasi semua data well logging. Ketebalan rata-rata batubara daerahpenelitian adalah 2,66 meter. Sedangkan luas daerah penelitian adalah 2.749.124,5 m2.
OPTIMALISASI DESAIN SURVEI SEISMIK BERDASARKAN DATA EVALUASI TEKNIS DAN PARAMETER YANG TERSEDIA DALAM SOFTWARE MESA Muhammad Fadhil; Ibrahim Sota; Simon Sadok Siregar
Jurnal Fisika FLUX Vol 13, No 1 (2016): Jurnal Fisika FLUX Edisi Februari 2016
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (123.414 KB) | DOI: 10.20527/flux.v13i1.1917

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ABSTRACT. Seismic data acquisition is done to get a recording of seismic data. The quality of seismic data judged from a comparison between the amount of reflection signals received by signal interference received. Three-dimensional seismic survey (3D) provides an overview of the subsurface geology accuracy better than seismic two- dimensional (2D). Seismic three-dimensional (3D) generally require a higher cost than the two-dimensional (2D) because the density of the firing point and the receivers more. Making  the  seismic  survey  design  into  a  solution  of  a  problem  before  conducting seismic exploration for exploration which was preceded by design rarely meet with failure and have a positive impact in optimizing the configuration of the spread as well as aspects of the economy. Of the four designs seismic surveys that have been made and the discussions it was found that all the firing patterns, to the desired target has been able to meet the desired targets. Firing patterns have value slanted fold better than firing patterns orthogonal, brick, and the patch because it has a value greater fold. Firing patterns patch is firing patterns are more suitable for shallow penetration compared with the three other designs, but in terms of the cost will be more expensive. Of the four firing patterns that have been made can be concluded that the firing patterns of brick is more objective in terms of both data and the distribution of funds will be issued. KEYWORDS: seismic, seismic survey design, firing patterns
Interpretasi Bawah Permukaan Daerah Penambangan Batuan Andesit Awang Bangkal Kabupaten Banjar Kalimantan Selatan Menggunakan Metode Magnetik Ayi Nurhidayah; Sri Cahyo Wahyono; Simon Sadok Siregar
Jurnal Fisika FLUX Vol 16, No 2 (2019): Jurnal Fisika Flux: Jurnal Ilmiah Fisika FMIPA Universitas Lambung Mangkurat
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (936.839 KB) | DOI: 10.20527/flux.v16i2.5184

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This research has been done in the mining area of andesite rock of Awang Bangkal village by using magnetic method. Magnetic method is one of the most common geophysical methods used for preliminary surveys on petroleum, earth, and mineral rock exploration. It is intended to determine the subsurface distribution in the area by performing qualitative and quantitative interpretations based on the magnetism value of the earth. The result of data processing using geosoft oasis montaj software shows that the total magnetic field anomaly is -807,3 to -361,7 nT. Qualitative interpretation is done by looking at the contour map of the anomaly, the result of upward continuation and the reduction to the poles. While the interpretation is done by making a modeling of the path that has been determined using mag2dc software. The model shows that the rocks that dominate the area are andesite rocks with their susceptibility value of 0.0992 to 0.2305 in SI units.
Aplikasi Jaringan Syaraf Tiruan (JST) Backpropagation untuk Prediksi Cuaca Harian di Wilayah Banjarbaru Sugiyanti Sugiyanti; Simon Sadok Siregar; Arfan Eko Fahrudin
Jurnal Fisika FLUX Vol 9, No 2 (2012): Jurnal Fisika FLUX Edisi Agustus 2012
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (685.597 KB) | DOI: 10.20527/flux.v9i2.6102

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Analisa Pola dan Sifat Aliran Fluida dengan Pemodelan Fisis dan Metode Automata Gas Kisi Simon Sadok Siregar; Suryajaya Suryajaya; Muliawati Muliawatiq
Jurnal Fisika FLUX Vol 7, No 1 (2010): Jurnal Fisika Flux Edisi Februari 2010
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1100.277 KB) | DOI: 10.20527/flux.v7i1.3080

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This research is conducted by using physical model and Lattice GasAutomata method for simple flow patterns having different geometry. Fromphysical model, the results are speed pattern and fluid flow permeability. Theresulted value of the permeability by using physical model will be compared tothe resulted value of the LGA. The compared value of the LGA method is thevalue with angle 5o, 10o and 15o by using laboratory scale. These angles arechosen due to it’s the lowest error compared to those of other angles. In thephysical model the lowest permeability value is gotten from the pattern of straightgeometry 60o with value 0.201 x 10-6 m2 and the highest permeability value isfrom pattern of turn 2 with value 0.341 x 10-6 m2. While by using LGA methodthe the lowest permeability value is pattern of straight 60o with value 0.209 x 10-6 m2 while the the highest real permeability value is pattern of turn 2 with value0.344 x 10-6 m2. From the comparison data of permeability the results of errorare 3.74%, 0.7% and 4.2% for the angle of 5o, 10o and 15o, respectively
PENDUGAAN PENCEMARAN AIR TANAH DI TEMPAT PEMBUANGAN SAMPAH LANDASAN ULIN TIMUR DENGAN METODE GEOLISTRIK KONFIGURASI SCHLUMBERGER Denok Dwi Priyanti; Sri Cahyo Wahyono; Simon Sadok Siregar
Jurnal Fisika FLUX Vol 11, No 1 (2014): Jurnal Fisika FLUX Edisi Februari 2014
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (129.108 KB) | DOI: 10.20527/flux.v11i1.2622

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ABSTRACT. Along with the increment of human population, ground water pollution also tends to increase. It primarily due to the accumulation of waste which could harm the public health. Trash or waste is one of the important issues which could contaminate ground water, especially waste landfills. Ground water that has been contaminated with liquid waste (leachate) can affect the quality of ground water. This study aimed to determine the composition of rocks, layers and depth of ground water around waste landfills (TPS) and to determine whether ground water around the TPS is contaminated or not. Estimation of groundwater pollution could be determined by measurement using geoelectric method with schlumberger configuration. It showed  the presence of leachate layer at depth of 0,51 – 8,51 m with measured resistivity of 3,89 – 9,63 Ohm.meter, while groundwater is at depth of 22,92 – 26,59 m with resistivity value of 88,98 – 128,75 Ohm.meter. AAS sample test has been conducted to determine whether the ground water around TPS is contaminated or not.  The test results using AAS showed groundwater around TPS was contaminated with Lead (Pb), iron (Fe) and Cadmium (Cd). The evidence was the value of their concentrations in three water samples which exceeded the thresholds in accordance with the requirements of drinking water. Threshold for Pb, Fe and Cd are 0,01 ppm, 0,3 ppm and 0,003 ppm, respectively. From the measurement results of sample 1, 2 and 3 couls be obtained the concentration of  Pb are 0,084 ppm, 0,044 ppm and 0,091 ppm, the concentration of Fe are 0,812 ppm for 1,018 ppm and 0,203 ppm, while the concentration of Cd are 0,012 ppm, 0,017 ppm and 0,01 ppm. Keywords: Ground water, waste, geoelectric, AAS
ANALISIS PERUBAHAN TEMPERATUR UDARA 2004-2010 UNTUK MEMPREDIKSI TEMPERATUR UDARA 2011-2014 DI KALIMANTAN SELATAN Reko Ary Rampan; Simon Sadok Siregar; MIftahul Munir
Jurnal Fisika FLUX Vol 10, No 2 (2013): Jurnal Fisika FLUX Edisi Agustus 2013
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (191.475 KB) | DOI: 10.20527/flux.v10i2.2646

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Abstrak: Nowadays, green house gas was increased which caused air temperature ofsurface arise, one of them is carbon dioxide (CO2), CO2 is part of green house gas whichis strong enough to absorb infrared wave, but if CO2 concentration is too high it wouldmake earth warming at the surface. The objective of the research is to made airtemperature changes modeling ( ), air temperature modeling ( ) in 2004-2010based on CO2 concentration trend and also to predict air temperature modeling 2011-2014 in Kalimantan Selatan. The research is literature study by using ( ) modeling.The modeling is made to known value of air temperature changes modeling since 1750based on CO2 concentration trend which used to modeling air temperature ( ) in2004-2010 based on CO2 concentration trend and also its predict. Data that was used isair temperature of observation in 7 point in 2004-2010 and CO2 concentration data ofIndonesia in 2004-2010. Result of the research shown that air temperature changesmodeling in 2004-2010 based on CO2 concentration trend was changed since 1750 isabout 1,53-1,68ºC, model shown that air temperature modeling in 2004-2010 based onCO2 concentration trend about 26,72-26,77ºC and air temperature modeling in 2011-2014 based on CO2 concentration trend about 26,772–26,795ºC.Keywords: Temperature, Carbon Dioxide (CO2), Kalimantan Selatan
ESTIMASI SUMBERDAYA BATUBARA BERDASARKAN DATA WELL LOGGING DENGAN METODE CROSS SECTION DI PT. TELEN ORBIT PRIMA DESA BUHUT KAB. KAPUAS KALIMANTAN TENGAH Erihartanti Erihartanti; Simon Sadok Siregar; Ibrahim Sota
Jurnal Fisika FLUX Vol 12, No 2 (2015): Jurnal Fisika FLUX edisi Agustus 2015
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (414.29 KB) | DOI: 10.20527/flux.v12i2.2612

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ABSTRAK. Batubara merupakan solusi bagi kebutuhan sehari–hari karena harganya yang murah terutama bagi negara-negara dengan harga minyak yang terus naik, maka batubara dapat menjadi sumber energi primer. Penelitian ini dilakukan di PT.Telen Orbit Prima Desa Buhut Kapuas Kalimantan Tengah. Tujuan dari penelitian adalah untuk menentukan lapisan batubara di bawah permukaan bumi berdasarkan data well logging, menentukan karakteristik sebaran batubara di bawah permukaan dengan menggunakan metode cross section, dan melakukan interpretasi sebaran lapisan batubara untuk menentukan sumberdaya batubara. Lubang bor yang terbagi dalam 10 cross section akan dikorelasikan untuk mengetahui pola sebaran batubara dari ketebalan dan karakteristik pada seam batubara. Setiap lubang bor akan memberikan bentuk kurva log yang berbeda sesuai dengan kondisi masing–masing. Semua kurva log gamma ray yang ada kemudian diinterpretasikan untuk memberikan informasi mengenai batasan tiap lapisan litologi. Berdasarkan kurva log gamma ray, lapisan batubara memiliki ketebalan 0,5–8,2 meter, dari kedalaman 4,2–145 meter dengan elevasi yang berkisar dari 49,439–85,236 meter dengan jumlah sumberdaya 8.810.124 m3.Kata Kunci: Batubara, kapuas, well logging, cross section.