Empirical Equation between Predominant Frequency and Sediment Thickness in Plampang, West Nusa Tenggara

Eko Rudi Iswanto, Theo Alvin Riyanto, Hadi Suntoko

DOI: http://dx.doi.org/10.55981/eksplorium.2023.6918

Abstract


Soil characteristics mapping is one of the essential aspects in the development of a region. Soil characteristics such as the predominant frequency and thickness of the sediment layer are needed to ensure the capacity of soil against the load of an infrastructure construction. The existence of tectonic activity causes West Nusa Tenggara Province to be an area with high seismic activity. Along with the plan to accelerate the development of the Samota Area, seismic studies are one of the aspects that determine project feasibility. The predominant frequency value from the results of microtremor measurements is used in the development of an empirical formula to predict soil thickness in the Plampang area. The empirical formula from previous research is used as a conformity test of the empirical formula obtained. Empirical equations are then used to map variations in sediment thickness in the Plampang area, which are justified based on geological data. The results of the sediment thickness map based on the empirical formula for the Plampang area showed a good correlation with the predominant frequency and also showed a good correlation with the results of the formula that has been carried out by previous studies.


Keywords


sediment thickness, empirical formula, microtremor

Full Text:

PDF

References


[1] S. Husein, “Bencana Gempabumi,” in DRR Action Plan Workshop: Strengthen Indonesian Recilence, 2016. doi: 10.13140/RG.2.1.1112.6808.

[2] M. Marjiyono, “Potensi Penguatan Gelombang Gempabumi oleh Sedimen Permukaan Kota Mataram, Nusa Tenggara Barat,” Jurnal Lingkungan dan Bencana Geologi, vol. 7, no. No. 3, pp. 135–144, 2016, [Online]. Available: http://jlbg.geologi.esdm.go.id/index.php/jlbg

[3] A. Bouchelouh, N. Zaourar, M. Farsi, and B. Guillier, “Seismic Microzonation and The Site Effects of Blida City (North of Algeria),” in 2nd European Conference on Earthquake Engineering and Seismology, 2014. [Online]. Available: https://www.researchgate.net/publication/321184053

[4] N. Purnachandra Rao et al., “Site amplification studies towards seismic microzonation in Jabalpur urban area, central India,” Physics and Chemistry of the Earth, vol. 36, no. 16, pp. 1247–1258, 2011, doi: 10.1016/j.pce.2011.01.002.

[5] Y. Nakamura, “A method for dynamic characteristic estimation of subsurface using microtremor on the ground surface,” QR of RTRI, vol. 3, no. 1, pp. 25–33, 1989.

[6] Y. Nakamura, “Clear identification of fundamental idea of Nakamura’s technique and its applications.” [Online]. Available: https://www.researchgate.net/publication/228603691

[7] A. Sudradjat, S. A. Mangga, and N. Suwarna, “Geological Map of The Sumbawah Quadrangle, Nusatenggara,” Geological Research and Development Centre, Bandung, 1998.

[8] B. Sunardi, M. U. Istikomah, and S. Sulastri, “Analisis Seismotektonik dan Periode Ulang Gempabumi Wilayah Nusa Tenggara Barat, Tahun 1973-2015,” Jurnal Riset Geofisika Indonesia, vol. 1, no. 1, pp. 23–28, 2017, [Online]. Available: https://www.researchgate.net/publication/316921051

[9] Pusat Studi Gempa Nasional (Indonesia) and Pusat Penelitian dan Pengembangan Perumahan dan Permukiman (Indonesia), Peta sumber dan bahaya gempa Indonesia tahun 2017. 2017.

[10] “Peraturan Daerah Provinsi Nusa Tenggara Barat.” Pemprov NTB, NTB.

[11] C. B. Santoso and D. S. Agustawijaya, “Seismic risk for Sumbawa Island based on seismicity and peak ground acceleration,” in IOP Conference Series: Earth and Environmental Science, Institute of Physics Publishing, Jan. 2020. doi: 10.1088/1755-1315/413/1/012009.

[12] E. R. Iswanto, T. A. Riyanto, and H. Suntoko, “Mikrozonasi di Daerah Plampang, Nusa Tenggara Barat,” Eksplorium, vol. 42, no. 1, pp. 39–46, 2021, [Online]. Available: http://jurnal.batan.go.id/index.php/eksplorium

[13] L. Sabrianto and A. T. Awali, “Seismik Microzonation Using Microtremor Measurement for Natural Disaster Mitigation of Earthquake at Regions Singaraja City, The Province of Bali Indonesia,” ARPN Journal of Earth Sciences, vol. 6, no. 1, 2017, [Online]. Available: www.arpnjournals.com

[14] D. S. Agustawijaya, H. Sulistiyono, and I. Elhuda, “Determination of the seismicity and peak ground acceleration for Lombok island: an evaluation on tectonic setting,” in MATEC Web of Conference, 2018.

[15] R. Mahendra Taruna, V. Haris Banyunegoro, and G. Daniarsyad, “Peak ground acceleration at surface for Mataram city with a return period of 2500 years using probabilistic method,” in MATEC Web of Conferences, EDP Sciences, Aug. 2018. doi: 10.1051/matecconf/201819503019.

[16] K. Konno and T. Ohmachi, “Ground-Motion Characteristics Estimated from Spectral Ratio between Horizontal and Vertical Components of Microtremor,” 1998.

[17] M. Ibs-Von Seht and J. Wohlenberg, “Microtremor Measurements Used to Map Thickness of Soft Sediments,” Bulletin of the Seismological Society of America, vol. 89, no. 1, pp. 250–259, 1999.

[18] J. Delgado et al., “Mapping soft soils in the Segura river valley SE Spain : a case study of microtremors as an exploration tool,” J Appl Geophy, vol. 45, pp. 19–32, 2000, [Online]. Available: www.elsevier.nlrlocaterjappgeo

[19] R. Biswas, S. Baruah, and D. K. Bora, “Mapping Sediment Thickness in Shillong City of Northeast India through Empirical Relationship,” Journal of Earthquakes, vol. 2015, pp. 1–8, Jan. 2015, doi: 10.1155/2015/572619.

[20] S. Suharno, M. Helmi, and A. Muchtar, “Empirical Formulation Between Natural Frequency vs Soil Thickness Based on Maximum Spectral Value H/V in Bandar,” 2020.

[21] S. Khan and A. Khan, “Mapping sediment thickness of Islamabad city using empirical relationships: Implications for seismic hazard assessment,” Journal of Earth System Science, vol. 125, no. 3, pp. 623–644, 2016.


Refbacks

  • There are currently no refbacks.




Google Scholar Logo SINTA Logo Logo GARUDA


Copyright EKSPLORIUM: Buletin Pusat Pengembangan Bahan Galian Nuklir (e-ISSN 2503-426x p-ISSN 0854-1418)

National Research and Innovation Agency (BRIN), KA. B.J. Habibie, Jl. M.H. Thamrin No.8, Jakarta, 10340, Indonesia.