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All Journal INDONESIAN JOURNAL OF APPLIED PHYSICS Jurnal Fisika
Nugroho Budi Wibowo
Badan Meteorologi Klimatologi dan Geofisika, Stasiun Geofisika Yogyakarta
Astronomy Energy Materials Science & Nanotechnology Physics

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Intepretasi Lapisan Sedimen berdasarkan Ground Profile Vs dengan Pengukuran Mikrotremor di Kecamatan Pacitan Nugroho Budi Wibowo; Juwita Nur Sembri; Deny Darmawan; Yosafat Sumardi; Fitria Afriliani; Siti Mahmudah
INDONESIAN JOURNAL OF APPLIED PHYSICS Vol 8, No 1 (2018): April
Publisher : Department of Physics, Sebelas Maret University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13057/ijap.v8i1.14986

Abstract

Ketebalan lapisan sedimen pada suatu wilayah dapat menyebabkan local site effect ketika terjadi gempabumi. Hal ini dikarenakan ketebalan lapisan sedimen berpengaruh terhadap amplifikasi. Kota Pacitan berdasarkan formasi geologi berada pada Formasi Aluvium (Qa) yang didominiasi lapisan sedimen. Penelitian ini bertujuan mengintepretasi ketebalan lapisa sedimen di Kecamatan Pacitan berdasarkan model ground profile Vs hasil akuisisi mikrotremor. Akuisisi dilakukan pada 25 titik di Kecamatan Pacitan menggunakan seimograph portable TDS. Ground profile Vs hasil pemodelan elipticity curve  menunjukkan bahwa nilai Vs bervariasi dari 153.11 m/s  (Formasi Aluvium) sampai 1393.48 m/s (Formasi Batuan Terobosan Andesit). Model ground profile Vs lapisan kedua yang berkorelasi dengan lapisan sedimen berada pada nilai Vs< 750 m/s dengan area di Dataran Aluvial Sungai Grindulu dan Teluk Pacitan. Ketebalan lapisan sedimen hasil analisa ground profile Vs, bervariasi dari 2.59 – 94.37 m. Lapisan sedimen paling tebal terdapat pada Formasi Aluvium (Qa) dengan ketebalan 94.37 m, dan lapisan sedimen paling tipis terdapat pada Formasi Jaten (Tmj) setebal 2.59 m. Lapisan sedimen dengan ketebalan lebih dari 50 m berada di kawasan Kota Pacitan, Teluk Pacitan dan Sungai Grindulu.
Seismic Vulnerability Microzonation Using Hvsr Method in Kalisalak Hamlet, Garunglor Village, Sukoharjo Sub-District, Wonosobo District Adam Ardiansyah; Aryono Adhi; Nugroho Budi Wibowo; SARWI; Budi Astuti; Cindiwati
Jurnal Fisika Vol. 14 No. 2 (2024): Jurnal Fisika 14 (2) 2024
Publisher : Universitas Negeri Semarang

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.15294/jf.v14i2.10851

Abstract

Kalisalak Hamlet in Sukoharjo District is faced with the risk of landslides that can affect the structure of residents' houses. This study aims to identify potential landslide zones based on the parameters of Dominant Frequency (f_0), Amplification Factor (A_0), and Seismic Vulnerability (K_g)to determine areas that are potentially vulnerable to landslides. Microseismic measurements were carried out at 25 measurement points in the landslide zone. Measurements used a 3-component digital portable seismograph (North-South, West-East, and Vertical). Microseismic data were processed using Geopsy software with the HVSR (Horizontal-to-Vertical Spectral Ratio) method to obtain an H/V curve that provides Dominant Frequency (f_0) and Amplification Factor (A_0) values. The results showed that Kalisalak Village has a dominant frequency value between 3 Hz to 12.5 Hz and an amplification factor value between 1.4 to 6.8. This variation indicates that some areas are more susceptible to seismic vibration amplification. Based on the Dominant Frequency (f_0) value and Amplification Factor (A_0), a Seismic Vulnerability (K_g) microzonation map was created for Kalisalak hamlet with a value range of 0.2 to 7 with a high vulnerability value located in the landslide area south of the village. This map is important for disaster mitigation planning in Kalisalak hamlet.
Co-Authors Adam Ardiansyah Aryono Adhi, Aryono Budi Astuti Cindiwati Deny Darmawan Fitria Afriliani Juwita Nur Sembri Sarwi Siti Mahmudah Yosafat Sumardi