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All Journal International Journal of Reconfigurable and Embedded Systems (IJRES) POSITRON Jurnal Fisika Unand JGE (Jurnal Geofisika Eksplorasi) Jurnal Fisika FLUX Jurnal Teori dan Aplikasi Fisika Kumawula: Jurnal Pengabdian Kepada Masyarakat Jurnal Pengabdian Kepada Masyarakat (Mediteg) Jurnal Pengabdian Ilung (Inovasi Lahan Basah Unggul) Jurnal Natural Scientiae
Sri Cahyo Wahyono
Prodi Fisika FMIPA Universitas Lambung Mangkurat
Agriculture, Biological Sciences & Forestry Arts Humanities Astronomy Biochemistry, Genetics & Molecular Biology Chemical Engineering, Chemistry & Bioengineering Chemistry Civil Engineering, Building, Construction & Architecture Computer Science & IT Decision Sciences, Operations Research & Management Dentistry Earth & Planetary Sciences Economics, Econometrics & Finance Education Electrical & Electronics Engineering Energy Environmental Science Immunology & microbiology Languange, Linguistic, Communication & Media Law, Crime, Criminology & Criminal Justice Materials Science & Nanotechnology Mathematics Medicine & Pharmacology Nursing Physics Public Health Social Sciences Other

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PEMETAAN SEBARAN BAHAN GALIAN GOLONGAN C MENGGUNAKAN SISTEM INFORMASI GEOGRAFIS DI KABUPATEN BANJAR, KALIMANTAN SELATAN Maulina, Anisa; Nurlina, Nurlina; Wahyono, Sri Cahyo
Jurnal Fisika FLUX Vol 11, No 2 (2014): Jurnal Fisika FLUX Edisi Agustus 2014
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/flux.v11i2.2679

Abstract

Abstract. Mining material of kind C include igneous rocks, sedimentary rocks and metamorphic rocks. These minerals are often used as industrial raw material. Geologically these minerals are to be found in Banjar Regency. Mining material of kind C can increase regional income. Concerning this, mapping of Mining material of kind C distribution is necessary. Method used for this is interpretation of Geological Map of Banjar Regency and stratigraphic analysis. Based on interpretation of geological map, Mining material of kind C found in Banjar Regency include sand, clay, quartz sandstone, quartzite, andesite, granite and serpentinit. Andesite distribution is found in Pitanak and Pauu formation with distributional area of 421 km². Granite distribution is found in Granite Formation with distributional area of 101 km². Quartz sandstone distribution is found in Tanjung Formation with distributional area of 81 km². Serpentinite distribution is found in Manunggul and Ultramafic rocks distribution with distributional area of 941 km². Quartzite distribution is found in Metamorphic Rocks with distributional area of 123 km². Sand and clay are found in Alluvium with distributional area of 1.430 km². Keywords: Banjar Regency, group C minerals, GIS
Pendugaan Lapisan Akuifer dengan Metode Geolistrik Konfigurasi Schlumberger di Rampa Manunggul, Kotabaru Wahyono, Sri Cahyo
Jurnal Fisika FLUX Vol 8, No 1 (2011): Jurnal Fisika Flux Edisi Februari 2011
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/flux.v8i1.3107

Abstract

Telah dilakukan pengukuran lapisan akuifer di Rampa Manunggul,Kabupaten Kotabaru berdasarkan kelistrikan bumi dengan konfigurasi Schlumberger.Pengukuran ini bertujuan untuk mengetahui kemungkinan adanya lapisantanah/batuan yang berfungsi sebagai perangkap air (akuifer) yang dapatdipergunakan sebagai dasar dalam perencanaan pengembangan air bawah tanahdengan cara pengeboran. Nilai tahanan jenis di lokasi pengukuran antara 0,47–0,48Ωm pada bagian atas ditafsirkan sebagai lumpur penutup yang bersifat basah,tahanan jenis 10-30 Ωm ditafsirkan sebagai lempung pasiran, dan tahanan jenis 30 –300 Ωm ditafsirkan sebagai lapisan pasir. Untuk lokasi pengukuran di RampaManunggul, Kotabaru lapisan air tanah yang bersifat tawar pada kedalaman lebih dari>60 meter.
Identifikasi Bijih Besi Menggunakan Metode Geolistrik Schlumberger Di Kabupaten Tanah Laut Kosidahrta, Rachmat; Wahyono, Sri Cahyo; Suarso, Eka
Jurnal Fisika FLUX Vol 13, No 2 (2016): Jurnal Fisika FLUX Edisi Agustus 2016
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/flux.v13i2.3483

Abstract

Telah dilakukan penelitian di Desa Sumber Mulia, Kabupaten Tanah Laut yang bertujuan untuk mengetahui tipe bijih besi dan sebarannya di bawah permukaan tanah. Penelitian ini menggunakan metode geolistrik hambatan jenis konfigurasi schlumberger dan karakterisasi X-Ray Flourescence (XRF). Hasil pengolahan 4 titik duga menggunakan perangkat lunak IPI2win diperoleh nilai hambatan jenis berkisar antara 2,37 - 5,6 Ωm dengan potensi kedalaman ±11 - 33 meter. Data XRF menunjukan kandungan bijih besi yang ada di Desa Sumber Mulia didominasi besi (Fe) dengan nilai rata-rata sebesar 97,876%. Berdasarkan nilai hambatan jenis dan hasil XRF diperkirakan tipe bijih besi di Desa Sumber Mulia adalah Hematite.
PENDUGAAN PENCEMARAN AIR TANAH DI TEMPAT PEMBUANGAN SAMPAH LANDASAN ULIN TIMUR DENGAN METODE GEOLISTRIK KONFIGURASI SCHLUMBERGER Priyanti, Denok Dwi; Wahyono, Sri Cahyo; Siregar, Simon Sadok
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 | DOI: 10.20527/flux.v11i1.2622

Abstract

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
Identifikasi Intrusi Air Laut Menggunakan Metode Geolistrik Di Desa Kampung Baru, Tanah Bumbu Astutik, Puji; Wahyono, Sri Cahyo; Siregar, Simon Sadok
Jurnal Fisika FLUX Vol 13, No 2 (2016): Jurnal Fisika FLUX Edisi Agustus 2016
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/flux.v13i2.3529

Abstract

Society of Kampung Baru village living in coastal areas utilize ground water to filling the need of ground water consumption. Over take of Ground water made different between  ground water level and sea surface level so get seawater intrusion. Therefore, research has done to knowing depth value of  distribution by resistiviting value and well water of NaCl contents in Kampung Baru village. Based on result of geoelectric data processing 2D Wenner configuration on 3 tracks with each tracks length 200m which made by Res2dinv software, then sea intrusion start from 0.93-19.6 m with resistivity value 0.2-6.40 Ωm. Based on the result of laboratory tests on three sample showed levels ranging Na is 12,055-14,027 mg/l and Cl has a value that ranges between 52,18-94,58 mg/l. Where this value is below the maximum levels that may be consumed
Penentuan Volume Batubara Menggunakan Metode Cross Section di PT. Astri Mining Resources Cabang Batu Ampar Kalimantan Selatan Megawati, Megawati; Wahyono, Sri Cahyo; Fahruddin, Fahruddin
Jurnal Fisika FLUX Vol 14, No 2 (2017): Jurnal Fisika FLUX Edisi Agustus 2017
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/flux.v14i2.4473

Abstract

Coal is a combustible sedimentary rock formed from organic deposits of plant residues and carbon, hydrogen and oxygen elements. Modeling of 3D coal distribution and coal volume calculation plays an important role in the exploration because the result of coal volume calculation can be used as consideration for mining. This research uses 6 drill point and calculation of coal volume using cross section method with the help of image processing software that is rockwork16. The result of interpretation of drill point data in the research area were 5 types of rock layers with each rock volume is claystone (25.840.000 m3), claysand (230.00 m3), Coal (5.930.000 m3), carbonaceus clay and soil.
IDENTIFIKASI KEDALAMAN DAN KANDUNGAN KROMIT DI DESA KIRAM KECAMATAN KARANG INTAN KABUPATEN BANJAR Wianto, Totok; Wahyono, Sri Cahyo
Jurnal Fisika FLUX Vol 11, No 2 (2014): Jurnal Fisika FLUX Edisi Agustus 2014
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/flux.v11i2.2678

Abstract

ABSTRAK. Kromit merupakan mineral oksida dari besi kromium dengan komposisi kimia (FeCr2O4) dan bijih logam kromium. Berdasarkan peta geologi, Desa Kiram Kecamatan Karang Intan Kabupaten Banjar merupakan formasi ultramafik, terdiri dari batuan peridotit dan batuan serpentit yang terlipat kuat. Kedalaman dan kandungan kromit serta unsur lainnya diketahui dengan metode Geolistrik 2D konfigurasi dipole-dipole dan X-Ray Flourescence (XRF). Hasil pengukuran di lapangan metode geolistrik 2D konfigurasi dipole-dipole dengan potensi kedalaman 0–10 m yang berupa bongkahan batuan berbentuk boulder dengan harga resistivitas antara 1.084-3.435 Ohm.meter. Kandungan kromit yang ada di Desa Kiram, Kecamatan Karang Intan, Kabupaten Banjar dengan analisa XRF adalah berkisar antara 22,7%-25,5 % dan Fe berkisar antara 27,9%-29,3%. Unsur lain selain kromit yaitu Si, Mg, Ni,Mn dll. Kata kunci: kromit, geolistrik, XRF, kab. Banjar
Pendugaan Lapisan Akuifer Berdasarkan Karakteristik Kelistrikan Bumi di Kabupaten Kotabaru Kalimantan Selatan Wahyono, Sri Cahyo
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 | DOI: 10.20527/flux.v7i1.3075

Abstract

Telah dilakukan penelitian tentang pendugaan lapisan akuifer diKabupaten Kotabaru Kalimantan Selatan pada tanggal 11 Agustus 2009.Daerah Kotabaru termasuk dalam anak cekungan Asam-Asam dan anakcekungan Pasir tersusun atas batuan yang diperkirakan berumur Jura yangterdiri dari batuan ultramafik, batuan malihan, batuan bacuh dan rijangradiolarian. Nilai tahanan jenis di lokasi penyelidikan dapat dibedakan dalambeberapa kelompok yaitu tahanan jenis antara 100-500 Ωm pada bagian atasditafsirkan sebagai tanah penutup dalam kondisi basah sampai kering, tahananjenis < 10 Ωm ditafsirkan sebagai lapisan lempung yang bersifat kedap air,tahanan jenis 10–30 Ωm ditafsirkan sebagai lapisan lempung pasiran dantahanan jenis 30–300 Ωm sebagai lapisan pasir. Lapisan yang dapat bertindaksebagai perangkap air bawah tanah/akuifer diperkirakan lapisan yangbertahanan jenis 10-300 Ωm. Mempertimbangkan aspek kemungkinan prospekketerdapatan air tanah, maka pengukuran GL.1 Pada titik GL.1 disarankanuntuk dilakukan pengeboran pada lapisan pasir pada kedalaman antara 30-90meter untuk nilai tahanan jenis 34,68 Ωm atau kedalaman lebih dari 90 meterpada nilai tahanan jenis 70,89 Ωm. Pada titik GL.2 disarankan untuk dilakukanpengeboran pada lapisan pasir pada kedalaman antara 50-80 meter untuk nilaitahanan jenis 169,18 Ωm atau kedalaman lebih dari 80 meter pada nilaitahanan jenis 37,13 Ωm, karena lapisan tersebut diperkirakan sebagai lapisanberfungsi sebagai perangkap air.
Studi Kasus Penyebaran Panas Bumi Non Vulkanik Sekitar Sumber Air Panas Hantakan, Kalimantan Selatan Siregar, Simon Sadok; Wahyono, Sri Cahyo; Nurlina, Nurlina
Jurnal Fisika FLUX Vol 8, No 1 (2011): Jurnal Fisika Flux Edisi Februari 2011
Publisher : Lambung Mangkurat University Press

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/flux.v8i1.3108

Abstract

The measurement had been conducted about an identification ofgeothermal fluid in heated pool tourist territory Murung B village, Hantakan subdistrict,Hulu Sungai Tengah regency. This research aims to find out litolhogy soil/rock in thearea around the hot water pool, knowing the value detainees soil type/rock containinggeothermal fluid and determine the distribution methods of arrest. Electrodeconfiguration used method Schlumberger (1D) and pole-pole (3D). Referring to theresults of the processing of Progress program can be made two-dimensional crosssectionto find out manually litolhogy coating model soil / rock which then correlatedwith ploting 3D models of Res3Dinv program. Geoelectric research results indicatethat the geothermal fluid in the surrounding in heated pool tourist territory, Hantakansubdistrict, Hulu Sungai Tengah regency has a range of resistance values between108 - 663.60 Ωm, in the depths of 14.67 - 90.2 m from the point G-3 - G-1. Geothermalfluid distribution direction at the research area is spread laterally from the point G-3 -G-1 where a layer of sand mixed with clay and granite rock fragments as an area ofconductive layers and clay as cover.
IDENTIFIKASI STRUKTUR BATUAN BAWAH PERMUKAAN MENGGUNAKAN METODE SEISMIK REFRAKSI DI KAMPUNG BARU BANJARBARU Triningsih, Sumaos; Sota, Ibrahim; Wahyono, Sri Cahyo
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 | DOI: 10.20527/flux.v10i2.2642

Abstract

ABSTRACT: It has been researched graving hole of ex-coal mining using refractionseismic method in Kampung Baru Banjarbaru. The hole is filled by water as acidpuddle, where it is worried to flow through to soil layer by following the plot of rocklayer’s slope. Identification of subsurface structure of the area is in order to know thedirection of the water’s flow. Seismograph PASI 24 Channel has been used to collectdata. The data has been processed using intercept time method. Interpretation resultsshow the subsurface in residential area has 3 layers. First layer is decayed layer withwave velocity (295-413 m/s) and thickness (2.8-5.57) m. Second layer with wavevelocity (787.4-919) m/s and thickness (10-11.66) m is interpreted as sand and gravel.Whereas, third layer with wave velocity (1282-2020) m/s and area boundary between h2dan h3 about (13.42-16.01) m is interpreted as clay (waterproof layer).Keywords: Seismic refraction, Intercept time method, Banjarbaru
Co-Authors Abdul Gafur Agustina, Meirani Ahmad Rusadi Arrahimi - Universitas Lambung Mangkurat) Ahmad Rusadi Arrahimi - Universitas Lambung Mangkurat) Akbar, Arief Rahmad Maulana Akhmat Faisal Akhmat Faisal Al Rosyid, Ulil Abror Anisa Maulina Apriana, Susi Ayi Nurhidayah Azwari, Ayu Riana Sari Azwari, Ayu RianaSari Baiti, Hisna Deddy Yuliarman Denok Dwi Priyanti Desi Monalisa Dewi Sri Susanti Dian Handiana Dian Handiana Dievy Prastika Putri Dodon Turianto Nugrahadi Dwi Asmaul Husna Fahruddin Fahruddin Faisal, Akhmat Gunawan Gunawan Gunawan Gunawan Hapsari, Putri Herin Hutri Istyarini Hidayat, Tri Armando Hisna Baiti Ibrahim Sota Ibrahim Sota Ib] Sota Ida Ayu Putu Sri Widnyani Istyarini, Herin Hutri Joko Santoso Kosidahrta, Rachmat Krisdianto Sugiyanto Krisologus Genesa Atmadja Liling Triyasmono Manik, Tetti Novalina Marjuni Marjuni Marjuni Marjuni Marjuni Marjuni Maulina, Anisa Maya Utami Megawati - Megawati Megawati Meirani Agustina Meta Widyayanti Meta Widyayanti Minarto, Ori Monalisa, Desi Muhammad Ery Zulfian Muhammad Rif&#039;an Abdi Muhammad Solih Afif Nasrulloh, Amar Vijai Ninis Hadi Haryanti, Ninis Hadi Novianti, Resty Faradilla Nurlina Nurlina Nurma Sari, Nurma Oni Soesanto Ori Minarto Ori Minarto Ori Minarto Ori Minarto Ori Minarto Pariadi Pariadi Pariadi, Pariadi Priyanti, Denok Dwi PUJI ASTUTIK Puji Astutik Putri Hapsari Putri Ika Wardani Putri, Dievy Prastika Rachmat Kosidahrta Rahmat Eko Sanjaya Rahmat Yunus Raisa Kusuma Dewi Raisa Kusuma Dewi Raisa Kusuma Dewi Resty Faradilla Novianti Rifkiati Rifkiati Rifkiati, Rifkiati Sadang Husain Samsul Anwar Savitri, Yuniar Selvy Tiurma Simamora sholih Afif Simamora, Selvy Tiurma Simon Sadok Siregar Simon Sadok Siregar, Simon Sadok Sota, Ib] Suarso, Eka Sumaos Triningsih Suminar Pratapa Susilo, Tanto Budi Sutomo Sutomo Tetti Novalina Manik Totok Wianto Totok Wiyanto Tri Armando Hidayat Triningsih, Sumaos Utomo, Edy Setyo Wardani, Putri Ika Widya Utama Widya Utama Yuyun Hidayat Zulfian, Muhammad Ery