Studi Mikrotremor dengan Metode Horizontal to Vertical Spectral Ratio (HVSR) di Tapak RDE, Serpong

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Eko Rudi Iswanto
Yuni Indrawati
Theo Alvin Riyanto

Abstract

Natural disaster like earthquake can cause damage to the site and the infrastructure including nuclear reactor facilities. This phenomenon needs comprehensively understood through its dynamic characteristics historical records of the site. The use of Horizontal to Vertical Spectral Ratio (HVSR) method has been widely used for subsurface investigation since last decade. The aimed of the research is to obtain local geological and subsurface dynamic characetristics. This research is applying the use of HVSR method for Experimental Power Reactor (RDE) in Serpong. The measurements are in 15 locations, and then the data is processed by using Geopsy software. The analysis result shows that the RDE site has dominant frequncy values between 3.06 Hz–23.271 Hz and amplification factor 1.84–6.37. The northeast and southeast areas of the site have higher seismic vulnerability index than in other area. Therefore, the selection for reactor bulding location in the southwest area is proper because it has lower amplification factor, sedimen thickness, and seismic vulnerability index.


 


 


 

Article Details

How to Cite
Iswanto, E. R., Indrawati, Y., & Riyanto, T. A. (2019). Studi Mikrotremor dengan Metode Horizontal to Vertical Spectral Ratio (HVSR) di Tapak RDE, Serpong. EKSPLORIUM, 40(2), 105–114. https://doi.org/10.17146/eksplorium.2019.40.2.5489
Section
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References

[1] BATAN, “Laporan Evaluasi Tapak RDE Aspek Geoteknik dan Pondasi,” Jakarta, 2016.

[2] Sungkono and B. J. Santosa., “Karakterisasi Kurva Horizontal-To-Vertical Spectral Ratio: Kajian Literatur Dan Permodelan,” J. Neutrino, vol. 4, no. 1, 2011.

[3] Sunaryo, H. U. Mala, and A. Prasetio, “Earthquake Microzonation Study on Batu Besi Dam of Nuha, East Luwu, South Sulawesi, Indonesia,” Int. J. GEOMATE, vol. 15, no. 48, pp. 148–154, 2018.

[4] BATAN, “Laporan Evaluasi Tapak Aspek Kegempaan,” Jakarta, 2016.

[5] P. Gueguen, J. L. Chatelain, B. Guillier, and H. Yepes, “An indication of the soil topmost layer response in Quito ( Ecuador ) using noise H / V spectral ratio,” Soil Dyn. Earthq. Eng., vol. 19, pp. 127–133, 2000.

[6] R. Carniel, P. Malisan, F. Barazza, and S Grimaz, “Improvement of HVSR technique by wavelet analysis,” Soil Dyn. Earthq. Eng., vol. 28, no. 4, pp. 321–327, 2008.

[7] M. Herak, “Model HVSR — A Matlab tool to model horizontal-to-vertical spectral ratio of ambient noise,” Comput. Geosci., vol. 34, pp. 1514–1526, 2008.

[8] J. Saita, M. L. T. Bautista, and Y Nakamura, “On Relationship Between The Estimated Strong Motion Characteristics Of Surface Layer And The Earthquake Damage,” in 13 th World Conference on Earthquake Engineering, 2004, no. 905, pp. 1–7.

[9] M. Mirzaoglu and Ü. Dýkmen, “Application of microtremors to seismic microzoning procedure,” J. Balk. Geophys. Soc., vol. 6, no. No. 3, pp. 143–156, 2003.

[10] M Sutrisna, C. Sulaeman, and N. D. Ardi, “Metode Mikrotremor untuk Mikrozonasi Gempa Bumi di Kota Cilacap,” J. online Fis., vol. 3, no. 2, 2015.

[11] J. W. Lane, E. A. White, G. V. Steele and J. C. Cannia, “Estimation of Bedrock Depth Using the Horizontal‐to‐vertical (H/V) Ambient‐noise Seismic Method,” in Symposium on the Application of Geophysics to Engineering and Environmental Problems 2008, Denver, Colorado, Society of Exploration Geophysicists, 2008, pp. 490–502.

[12] A. I. Hadi, M. Farid, and Y. Fauzi, “Pemetaan Percepatan Getaran Tanah Maksimum dan Kerentanan Seismik Akibat Gempa Bumi untuk Mendukung Rencana Tata Ruang dan Wilayah (RTRW) Kota Bengkulu,” Simetri J. Ilmu Fis. Indones., vol. 1 Nomor 2, September, pp. 81–86, 2012.

[13] Saaduddin, Sismanto, and Marjiyono, “Pemetaan Indeks Kerentanan Sesimik Kota Padang Sumatera Barat dan Korelasinya dengan Titik Kerusakan Gempa Bumi 30 September 2009,” in Seminar Nasional Kebumian Ke-8, 2015, pp. 459–466.

[14] Daryono, Sutikno, J Sartohadi, Dulbahri, and K. S. Brotopuspito, “Pengkajian Local Site Effect di Graben Bantul Menggunakan Indeks Kerentanan Seismik Berdasarkan Pengukuran Mikrotremor,” J. Kebencanaan Indones., vol. 2, no. No.1, pp. 456–467, 2009.

[15] S. S. Arifin, “Penentuan Zona Rawan Guncangan Bencana Gempa Bumi Berdasarkan Analisis Nilai Amplifikasi HVSR Mikrotremor dan Analisis Periode Dominan Daerah Liwa dan Sekitarnya,” J. Geofis. Eksplor., vol. 2, no. 1, pp. 30–40, 2018.

[16] N. Sitorus, S. Purwanto, and W. Utama “Analisis Nilai Frekuensi Natural dan Amplifikasi Desa Olak Alen Blitar Mengguakan Metode Mikrotremor HVSR,” J. Geosaintek, vol. 03, no. 02, pp. 89–92, 2017.

[17] R. A. Murdiantoro, Sismanto, and Marjiyono “Pemetaan Daerah Rawan Kerusakan Akibat Gempabumi di Kotamadya Denpasar dan Sekitarnya dengan Menggunakan Analisis Mikrotremor Studi Kasus : Gempabumi Seririt 14 Juli 1976,” J. Fis. Indones., vol. 20 No.2, no. 2, pp. 36–41, 2016.