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Abstract

ABSTRACT

[Identification of Soil Response to Earthquake Waves in Curup and its Implementation on Physics Learning]. Scientific research has been conducted in the Curup in five districts namely Selupu Rejang, center Curup, eastern Curup, southern Curup and Curup city. Curup city is a mountainous area located in the earthquake belt. The aim of research was to determine the level of vulnerability of land in the Curup city and to explain the difference in student learning outcomes XI IPA 1 and XI IPA 2 after participating in learning by using learning model Problem Based Learning (PBL) and Conventional Methods on the material elasticity. Seismic susceptibility index data values obtained from field research using HVSR microseismic tools. Data management using DATAPRO software and GEOPSY software. The result of the highest level of susceptibility to the soil is 4.18 and is located at the maximum temperature of the soil. The results of educational research show that there are differences in student learning outcomes taught with PBL learning models and conventional methods. The experimental class learning outcomes have an average value of 80.70, while the control class has an average value of 73.20.

 

Keywords: Vulnerability; earthquake; PBL model.

(Received August 14 , 2018; Accepted January 10, 2019; Published February 27, 2019)

 

 

ABSTRAK

Penelitian sains telah dilakukan di Daerah Curup di lima kecamatan yaitu Selupu Rejang, Curup Tengah, Curup Timur, Curup Selatan dan Curup Kota pada tanggal 07 Agustus 2016. Kota Curup merupakan daerah pegunungan yang terletak pada jalur gempa. Tujuan penelitian untuk mengetahui tingkat kerentanan tanah di kota Curup dan Untuk menjelaskan Perbedaan hasil belajar siswa kelas XI IPA 1 dan XI IPA 2 setelah mengikuti pembelajaran dengan menggunakan model pembelajaran Problem Based Learning (PBL) dan Metode Konvensional pada materi elastisitas. Data nilai indeks kerentanan seismik diperoleh dari penelitian lapangan dengan menggunakan alat mikroseismik HVSR. Pengelolahah data menggunakan software DATAPRO dan software GEOPSY. Hasil tingkat kerentanan tanah tertinggi mencapai 4,18 dan terletak pada kecamatan Selupu Rejang. Hasil penelitian pendidikan menunjukkan terdapat perbedaan hasil belajar siswa yang diajarkan dengan model pembelajaran PBL dan metode konvensional. Hasil belajar kelas eksperimen memiliki nilai rata-rata 80,70, sedangkan kelas kontrol memiliki nilai rata-rata 73,20.

Kata kunci: Kerentanan; gempa bumi; model PBL.

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How to Cite
Gusti, P. K., Farid, M., Swistoro, E., & Koto, I. (2019). Identifikasi Respon Tanah terhadap Gelombang Gempa Bumi di Curup dan Implementasi Pembelajaran Fisika. PENDIPA Journal of Science Education, 3(1), 45–53. https://doi.org/10.33369/pendipa.3.1.45-53
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References

  1. DAFTAR PUSTAKA
  2. Adisendjaja, Y. H. (2008). Analisis Buku Ajar Biologi SMA Kelas X di Kota Bandung Berdasarkan Literasi Sains. Bandung: Jurusan Pendidikan Biologi, FMIPA Universitas Pendidikan Indonesia
  3. Bella, R. A., Bunganaen, W., & Sogen, P. M. (2015). Identifikasi Kerusakan Konstruksi Akibat Potensi Pengembangan Tanah Lempung Ekspansif Di Desa Oebelo. Jurnal Teknik Sipil, 4(2), 195-208
  4. Gurler, E. D., Nakamura, Y., Saita, J., & Sato, T. (2000). Local site effect of Mexico City based on microtremor measurement. In 6th International Conference on Seismic Zonation. Palm Spring Riviera Resort, California, USA (p. 65).
  5. Ngalimun. (2014). Strategi dan Model Pembelajaran. Yogyakarta: Aswaja Presindo.
  6. Nurdyansyah, N., & Fitriyani, T. (2018). Pengaruh Strategi Pembelajaran Aktif Terhadap Hasil Belajar Pada Madrasah Ibtidaiyah. Universitas Muhammadiyah Sidoarjo
  7. Pulinets, S. (2004). Ionospheric precursors of earthquakes; recent advances in theory and practical applications. Terrestrial Atmospheric and Oceanic Sciences, 15(3), 413-436.
  8. Spence, W., Mendoza, C., Engdahl, E. R., Choy, G. L., & Norabuena, E. (1999). Seismic subduction of the Nazca Ridge as shown by the 1996–97 Peru earthquakes. In Seismogenic and Tsunamigenic Processes in Shallow Subduction Zones (pp. 753-776). Birkhäuser, Basel.
  9. Sudjana. (1996). Metode Statistik. Bandung: Tratisto.
  10. Sugiyono. (2009). Metode Penelitian. Bandung: Alfabeta.
  11. Susilawati, Z., Mayub, A., & Farid, M. (2018). Menghitung nilai emisivitas warna menggunakan miniatur ruang berbentuk silinder sebagai media pembelajaran fisika. PendIPA Journal of Science Education, 2(2).
  12. Susanto, A. (2011). Perhitungan Percepatan Tanah Maksimum Berdasarkan Data Gempa Bumi di Daerah Istimewa Yogyakarta (Doctoral dissertation, Universitas Negeri Semarang).