Article Per Year (5 Year)
p-Index From 2021 - 2026
0.817
P-Index
This Author published in this journals
All Journal INDONESIAN JOURNAL OF APPLIED PHYSICS MITRA: Jurnal Pemberdayaan Masyarakat Social, Humanities, and Educational Studies (SHEs): Conference Series Prosiding University Research Colloquium Indonesian Journal of Environment and Disaster LEMBARAN PUBLIKASI MINYAK DAN GAS BUMI
Sorja Koesuma
Unknown Affiliation
Humanities Astronomy Chemical Engineering, Chemistry & Bioengineering Computer Science & IT Earth & Planetary Sciences Economics, Econometrics & Finance Education Energy Engineering Environmental Science Languange, Linguistic, Communication & Media Law, Crime, Criminology & Criminal Justice Materials Science & Nanotechnology Medicine & Pharmacology Physics Public Health Social Sciences

Published : 12 Documents Claim Missing Document
Claim Missing Document
Check
Articles

Found 5 Documents
Search
Journal : INDONESIAN JOURNAL OF APPLIED PHYSICS

 1 
Penentuan Tingkat Kerawanan Gempa Bumi Menggunakan Metode Refraksi Mikrotremor (ReMi) di Kota Surakarta Sari Pratiwi; Budi Legowo; Sorja Koesuma
INDONESIAN JOURNAL OF APPLIED PHYSICS Vol 7, No 1 (2017): April
Publisher : Department of Physics, Sebelas Maret University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13057/ijap.v7i1.4884

Abstract

Berdasarkan informasi dari letak geografis dan struktur geologi, Kota Surakarta termasuk wilayah yang mengalami dampak gempa bumi[1]. Salah satu upaya untuk mengurangi dampak dari gempa bumi yaitu melakukan analisa tingkat bahaya seismik sebagai salah satu usaha mitigasi bencana gempa dengan metode mikrotremor yang dapat diketahui nilai amplifikasi dan periode dominan.  Pada penelitian telah dilakukan di Kota Surakarta menggunakan P.A.S.I Seismograph Mod. 16S24-P, 3D Borehole Geophone Model GFA 60/100. Interval pada setiap lokasi yaitu 1-3 km dengan 12 lokasi penelitian. Diperlukan waktu sekitar 20 menit dengan tiga kali pengulangan untuk perekaman data disetiap titik. Pengolahan data mikrotremor menggunakan software Geopsy dan Surfer 11. Amplifikasi rendah pada zona 1 merupakan zona yang cukup aman terhadap bahaya gempa bumi. Zona 1 berada di wilayah Mojo, Moewardi, Sangkrah, Dawung, SMPN 10, Mojosongo, Lapangan Banyuanyar, Laweyan, Karang Asem danTipes dengan amplifikasi 0,807314 sampai dengan 2,60402. Lokasi pada jenis I termasuk wilayah yang cukup aman terhadap gempa bumi karena memiliki ketebalan sedimen yang tipis daripada jenis II. Jenis I berada di wilayah Mojo, Moewardi, Sangkrah, SMPN 10, Manahan, Mojosongo, Lapangan Banyuanyar, Laweyan, Karang Asem, Jebres dan Tipes dengan  periode dominan antara 0,058978s sampai dengan 0,231411s. Sebaran tingkat kerawanan gempa bumi di kota Surakarta dapat dilihat pada peta zonasi berdasarkan nilai A0 dan T0 yang kemudian diklasifikasikan hasilnya pada zona atau jenis tertentu sehingga diperoleh informasi berupa tingkat kerawanan dan juga jenis batuan yang tersusun dibawah permukaan tanah berdasarkan parameter yang diukur.
Analisa Sea Level Rise Dari Data Satelit Altimetri Topex/Poseidon, Jason-1 Dan Jason-2 Di Perairan Laut Pulau Jawa Periode 2000 – 2010 Hastho Wuriatmo; Sorja Koesuma; Mohtar Yunianto
INDONESIAN JOURNAL OF APPLIED PHYSICS Vol 2, No 02 (2012): IJAP VOLUME 02 ISSUE 02 YEAR 2012
Publisher : Department of Physics, Sebelas Maret University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13057/ijap.v2i02.1296

Abstract

It has been conducted a research about sea level rise (SLR) in surrounding Jawa island by using satellite altimetry data Topex/Poseidon, Jason-1 dan Jason-2 for period 2000 – 2010. Satellite altimetry is satellite which specially design for measuring dynamics of sea water. Those satellite lauched firstly in 1992 incorporation between National Aeronautics and Space Administration (NASA) dan European Space Agency (ESA). There are six locations for measuring SLR i.e. Jakarta, Semarang, Surabaya, Pangandaran, Jogjakarta dan Prigi. We choselocations based on alongtrack of satellite and near the big cities in Jawa island with dimension area around 0.5ox0.5o degrees. We found SLR rate for Jakarta (2.5 ± 0.24 mm/yr), Semarang (2.16 ± 0.20 mm/yr), Surabaya (2.72 ± 0.19 mm/yr), Pangandaran (0.71 ± 0.33 mm/yr), Jogjakarta (0.91 ± 0.38 mm/yr) and Prigi (1.3 ± 0.38 mm/yr). The average SLR rate for North coast is (2.46 ± 0.21 mm/yr) and for South coast (0.97 ± 0.36 mm/yr). This results are wellcorrelated with data from tide gauge stations.
Pemisahan Anomali Regional-Residual pada Metode Gravitasi Menggunakan Metode Moving Average, Polynomial dan Inversion Jarot Purnomo; Sorja Koesuma; Mohtar Yunianto
INDONESIAN JOURNAL OF APPLIED PHYSICS Vol 3, No 01 (2013): April
Publisher : Department of Physics, Sebelas Maret University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13057/ijap.v3i01.1208

Abstract

It has been done a research about separation of regional-residual anomaly in Gravity method. This research compares the result of three methods i.e. moving average method, polynomial method, and inversion method. The computer program is created using a computer programming Matlab 7. From three methods that have been made, the separation results are compared withresults of separation by using Upward Continuation method. From the results of these comparisons will be available an excellent program of regional-residual anomali separation. The results show that in polynomial method of the order 4 obtained similar contour to the separation by Upward Continuation Software. So that the output of this separation will be treated again with Grav2DC software. The output of this software is the density of rock Grav2DC of the studyarea. Processing results obtained the minimum error of 1.85% for the separation by polynomial method, while for the method of Upward Continuation obtained minimum error of 2.22%. The results obtained show that the separation of regional-residual anomali by polynomial method is similar to separation by Upward Continuation method.
Penentuan Tingkat Kekerasan Batuan Menggunakan Metode Seismik Refraksi di Jatikuwung Karanganyar Nakif Nurcandra; Darsono D; Sorja Koesuma
INDONESIAN JOURNAL OF APPLIED PHYSICS Vol 3, No 01 (2013): April
Publisher : Department of Physics, Sebelas Maret University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13057/ijap.v3i01.1212

Abstract

It has been done a research about the determination of rock hardness level by using refraction seismic method in Jatikuwung Karanganyar. The research is done by using Seismograph PASI 16S24-P with the path length of 48 meters, distance between geophone 2 meters, 5 shots in each spread and there are four surveys part totally. The processing data is done by using SeisImager software with Plotrefa and Pickwin95 program.We use intercept time method for data processing. The determination of rock hardness use Gardner’s relationship formula. Based on interpretation, there are three layers lithology structure with P wave propagation velocity of 200-1800 m/s and its density of 1.17–1.93 gr/cc. Based on velocity analysis we determine the velocity of first layer is 200-700 m/s, second layer 700-1500 m/s, and third layer 1500-1800 m/s. The subsurface hardness lithology consists of top soil, sands and unsaturated pebble (1.17–1.59 gr/cc) with the depth 2–4 meters in the first layer, saturatedsands, saturated pebble, and alluvium (1.59–1.93 gr/cc) with the depth 9.5–11.5 meters in the second layer, and clay and sands (1.93–2.02 gr/cc) with the depth of 5.5–6 meters in the third layer. The rock hardness is located at the depth betwen 12 – 20 meters.
Kajian Indeks Bahaya Seismik Regional Menggunakan Data Seismik Pulau Jawa Tahun 1900-2006 Sulistiyani S; Sorja Koesuma; Nugroho Budi W
INDONESIAN JOURNAL OF APPLIED PHYSICS Vol 3, No 01 (2013): April
Publisher : Department of Physics, Sebelas Maret University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13057/ijap.v3i01.1210

Abstract

It has been conducted a research about Regional Seismic Disaster Index (RSDI) in Java Island by using seismic data from 1900 – 2006. RSDI is a index showing vulnerability seismic disaster in an area. The hight risk area is the highest risk, the low area is the lowest risk. The highest RSDI areas were Banten, Jawa Barat, and D.I Yogyakarta Provinces. While the lowest RSDI areas were DKI Jakarta and Jawa Tengah Province. Deviations standard value showed the moving RSDI value each region. Region with big RSDI value had high Seismic level were Banten , Jawa Barat, and D.I. Yogyakarta Province.
Co-Authors Andika Dwi Cipta Susanto Aria Arga Ananta Azar Rafliardi Abdullah Bambang Sunardi Budi Legowo Budi Legowo Chatarina Muryani Darsono D Darsono Darsono Dhia Azmi Nabila Dian Novita Dzul Fadli Badaruddin Fajar Nursodik Handono Ramelan Harjana Harjana Hastho Wuriatmo Imam Arifin Iwan Yahya Izzuki Hamida Jarot Purnomo Maharani, Yohana Nooradika Mohtar Yunianto Muhammad Salfas Nakif Nurcandra Nugroho Budi W Rizki Amalia Pratiwi Sari Pratiwi Sarjoko Lelono Sulistiyani S Vemirantih, Dini Wisnu Krismonanto