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

This work is licensed under a Creative Commons Attribution-ShareAlike 4.0 International License.
1. Introduction
By using or sharing content from EKSPLORIUM - Buletin Pusat Pengembangan Bahan Galian Nuklir ("the Journal"), you agree to follow these Terms and Conditions. The Journal's content is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike (CC BY-NC-SA) license. If you do not agree to these terms, please do not use the content.
2. How You Can Use the Content
-
Share: You can copy, share, and distribute the work, but only for non-commercial purposes.
-
Adapt: You can change, remix, or build on the work, as long as it is for non-commercial purposes and you share it under the same license (CC BY-NC-SA).
3. Attribution (Giving Credit)
When you use or share the content, you must:
-
Give proper credit to the author(s).
-
Mention the title of the work and the journal name.
-
Provide a link to the license (https://creativecommons.org/licenses/by-nc-sa/4.0/).
-
Indicate if you made any changes to the work.
4. Non-Commercial Use
You cannot use the work to make money or for any commercial activities. For example, you cannot sell or use the content in advertisements.
If you want to use the content for commercial purposes, you need to get permission from the author(s) or the publisher.
5. ShareAlike
If you make changes to the content (like creating a new version or remixing it), you must share your new version under the same CC BY-NC-SA license.
6. Exclusions
Some materials in the Journal may have different licenses or restrictions, such as third-party content (like images or datasets). You must respect the rules for those materials.
7. No Warranty
The content is provided "as is." The authors and publisher do not guarantee that the content is error-free or suitable for any specific purpose. Use the content at your own risk.
8. Modifications and Withdrawal of Content
The publisher and authors can update or remove content at any time. If content is removed, the previous versions will still follow these terms.
9. Ethical Use
You must use the content ethically and follow all relevant laws. This includes properly citing the original authors and not misusing the content.
10. Legal Compliance
You are responsible for making sure your use of the content follows the laws of your country. If you believe content violates your rights, please contact us.
11. Changes to Terms
These Terms and Conditions may be updated from time to time. Any changes will be posted on the Journal's website.
12. Contact Information
For questions about these Terms or for permission to use content commercially, please contact us at:
-
Email: eksplorium@brin.go.id
-
Website: https://ejournal.brin.go.id/eksplorium
Conclusion
By using the content from EKSPLORIUM - Buletin Pusat Pengembangan Bahan Galian Nuklir, you agree to follow these Terms and Conditions and the CC BY-NC-SA 4.0 International License.
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.