Relevant bibliographies by topics / Krakatit

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Academic literature on the topic 'Krakatit'

Author: Grafiati
Published: 4 June 2021
Last updated: 13 February 2022

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Journal articles on the topic "Krakatit"

1

Maslova, Ksenia. "Istoriia sozdaniia, tematika, problematika i khudozhestvennye osobennosti romana K. Chapeka «Krakatit»." Slavic World: Commonality and Diversity, no. 2018 (2018): 268–72. http://dx.doi.org/10.31168/2619-0869.2018.3.1.8.

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Bosnak, Judith, and Rick Honings. "‘Behoed ons arme volk voor de vulkaan-poëten’." De Moderne Tijd 4, no. 3 (2020): 382–422. http://dx.doi.org/10.5117/dmt2020.3-4.012.honi.

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Abstract ‘Save our poor people from the vulcano poets’. The literary reception of the Krakatoa disaster of 1883 in the Netherlands and Indonesi On August 27, 1883, the volcano Krakatau in the Dutch East Indies erupted and collapsed, causing the deaths of tens of thousands, mainly as a result of devastating tsunamis. The Krakatau eruption was one of the first disasters to take place beyond the Dutch boundaries that received so much attention in the Netherlands. Because the Indies were a Dutch colony, a response of the motherland was rather logical. In many places, charity activities were organized to raise money for the victims. This article focuses on the Dutch and Indonesian literary reactions on the Krakatau disaster. For this purpose, two scholars work together: one specialized in Dutch Literary Studies and the other one in Indonesian Languages and Cultures. In the first part of the article several Dutch charity publications are analysed; the second part focuses on Indonesian sources (in Javanese and Malay). How and to what extend did the reactions in the Netherlands and Indonesia differ?
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Novriadi, Novriadi, Endang Linirin Widiastuti, and Rikha Aryanie Surya. "EVALUASI KOMUNITAS TERUMBU KARANG DI PERAIRAN CAGAR ALAM LAUT KRAKATAU." Jurnal Ilmiah Biologi Eksperimen dan Keanekaragaman Hayati 1, no. 1 (2013): 30–34. http://dx.doi.org/10.23960/jbekh.v1i1.96.

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Cagar Alam Laut Krakatau berada di daerah vulkanik Gunung Anak Krakatu. Aktivitas seismik yang diakibatkan oleh magma chamber Anak Krakatau menyebabkan goncangan pada dasar laut yang memungkinkan bergesernya substrat yang menjadi tempat terumbu karang tumbuh, Selain itu debu vulkanik akan mempengaruhi kalsifikasi dan pertumbuhan karang sehingga karang yang terbentuk akan rapuh dan rentan terhadap pengaruh lingkungan, seperti arus dan goncangan. Tujuan penelitian ini adalah untuk mengetahui kondisi terkini komunitas serta keanekaragaman terumbu karang di Cagar Alam Laut Krakatau. Penelitian dilakukan dari bulan Juli sampai Oktober 2012. Perairan yang menjadi stasiun penelitian adalah perairan Pulau Rakata. Metode manta tow digunakan pada saat survei pendahuluan dan metode Line Intercept Transect (LIT) digunakan dalam pengambilan data terumbu karang. Stasiun penelitian yang berda di perairan Pulau Rakata dibagi menjadi empat titik pengambilan sampel. pada kedalaman 5 meter dengan panjang transek 50 meter searah garis pantai. Hasil pengamatan menunjukkan bahwa dari 27 spesies dalam 7 famili terumbu karang yang ditemukan pada stasiun penelitian kondisinya bervariasi dari baik sekali hingga rusak dengan tingkat tutupan berkisar antara 90,88%, 56,54%,dan 38,32 %.
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Jayaratne, Ravindra, Aldhiansyah Muhammad Fauzi, Hendra Achiari, and Tomoya Shibayama. "MODELLING OF KRAKATOA TSUNAMI WAVE PROPAGATION AND COMMUNITY ENGAGEMENT BASED ON SWOT ANALYSIS IN SOUTHERN LAMPUNG, INDONESIA." Coastal Engineering Proceedings, no. 36v (December 28, 2020): 30. http://dx.doi.org/10.9753/icce.v36v.currents.30.

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The eruption of Krakatoa which occurred on the 22 December 2018 caused an avalanche from the Gunung Anak Krakatau (GAK) body into the sea, causing a tsunami in the Sunda Strait. The tsunami affected Lampung (Sumatra) and Banten (Java) provinces in Indonesia. Based on the field observations made by Takabatake et al. (2019) in the southern part of Lampung, it was identified that there were severely damaged areas in Lampung; i.e. East Way Muli, Central Way Muli, and Kunjir villages. A numerical model was developed to simulate past and future tsunami wave propagation scenarios. In addition, the strategic planning technique of SWOT analysis was carried out in order to make recommendations for the resilience of local coastal communities for future tsunami events in Southern Lampung.Recorded Presentation from the vICCE (YouTube Link): https://youtu.be/YR_UX_SdS6c
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Whittaker, R. J., and M. B. Bush. "Anak Krakatau and old Krakatau: a reply." GeoJournal 29, no. 4 (1993): 417–20. http://dx.doi.org/10.1007/bf00807545.

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6

Mabberley, D. J., M. Bush, P. Jones, and K. Richards. "Krakatoa Revisited." Journal of Biogeography 15, no. 2 (1988): 387. http://dx.doi.org/10.2307/2845419.

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7

Wirasetiyawan, Dedy, Nawanto Budi Sukoco, Nur Riyadi, and Dikdik Satria Mulyadi. "Identifikasi Perubahan Kontur Kedalaman Laut Diperairan Sekitar Anak Gunung Krakatau Pasca Erupsi Tahun 2018." Jurnal Chart Datum 6, no. 2 (2020): 1–11. http://dx.doi.org/10.37875/chartdatum.v6i2.184.

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Krakatau (Rakata) adalah kepulauan vulkanik yang masih aktif yang terletak di Selat Sunda, antara Pulau Jawa dan Sumatera. Pada tahun 1927 atau kurang lebih 40 tahun setelah meletusnya Gunung Krakatau, muncul gunung api yang dikenal sebagai Anak Krakatau dari kawasan kaldera purba tersebut yang masih aktif dan tetap bertambah tingginya. Penyebab semakin tingginya gunung itu disebabkan oleh material yang keluar dari perut gunung baru itu. Pada penelitian ini dititik beratkan pada identifikasi perbandingan perubahan kontur kedalaman perairan disekitar Anak Gunung Krakatau sebelum dan pasca erupsi tahun 2018.
 Data penelitian ini berupa data sekunder Multibeam Echosounder (MBES) yang diperoleh dari hasil survei KRI Spica-934 di Perairan Selat Sunda atau di sekitar Anak Gunung Krakatau pasca erupsi tahun 2018 menggunakan MBES EM 2040 dan EM 302. Data yang diperoleh kemudian diolah menggunakan software Charis Hips and Sips selanjutnya dioverlay dengan Lembar Lukis Teliti (LLT) tahun 2016. Dari hasil penelitian didapatkan bahwa terjadi perubahan kontur kedalaman laut di area sekitar Anak Gunung Krakatau pasca erupsi tahun 2018 yang mengakibatkan pendangkalan hampir diseluruh area Anak Gunung Krakatau, terutama di bagian selatan dan barat dimana terdapat garis pantai yang menyempit akibat longsoran, selain itu berdasar data hasil olahan terdapat pola garis kontur kedalaman laut yang mendekati garis pantai.
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8

Setiawati, Astriana Rahmi, Jamalam Lumbanraja, Septi Nurul Aini, Dermiyati Dermiyati, Henrie Buchari, and Zuldadan Naspendra. "Texture and Chemical Properties of Two Depth Soils in a Toposequence of Anak Krakatau Before December 2018 Eruption." JOURNAL OF TROPICAL SOILS 25, no. 2 (2020): 71. http://dx.doi.org/10.5400/jts.2020.v25i2.71-81.

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Anak Krakatau volcano is one of the famous volcanic mountains located in the sea to the south part of the Province of Lampung, Indonesia. The volcano was derived from the active Krakatau caldera that first appeared on the surface in 1930 or 47 years after the eruption of Krakatau in 1883. The materials produced by the Anak Krakatau eruption were very interesting related to soil forming materials, especially their physical and chemical properties. The objectives of this study were to present information about the texture and chemical properties of soil from Anak Krakatau Mountain taken at the southeast slope before the December 2018 eruption at two different depths. This study was conducted in March to September 2019 which consisted of two parts: (1) soil survey in the field and (2) soil analysis in the laboratory. Soil samples were taken from a toposequence at seven points with an interval about 15m above sea level (asl) on the southeast slope (approaching northeast) of the Anak Krakatau in July 2018 at the depth of 0-20 cm and 20-40 cm. The soil texture of Anak Krakatau mountain before eruption in December 2018 was sandy with the percentage of sand 98.82 - 99.59%; silt 0 - 0.59%; and clay 0.41 - 0.74%. The soil chemical properties of Anak Krakatau mountain were soil pH (H2O) 4.95 – 6.27; soil pH (KCl) 4.75 – 5.89; Cation Exchange Capacity 0.41 – 2.02 cmol(+) kg-1; Base Saturation 117.24 – 514.63%; CaO 2.63 – 6.34%; MgO 3.06 – 6.13%; K2O 0.019 – 0.034%; Na2O 0.035 – 0.080%; P-retention 82.10 – 84.74%; and organic carbon 0.06 – 0.72%. The SEM-EDX analysis showed that the amounts of Mg and Na were more than 1% and there were several trace elements present in Anak Krakatau soil, namely Sb (Stibium), Nb (Niobium), Y (Yttrium), F (Flour), Co (Cobalt), and Ba (Barium).
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9

Choi, B. H., E. Pelinovsky, K. O. Kim, and J. S. Lee. "Simulation of the trans-oceanic tsunami propagation due to the 1883 Krakatau volcanic eruption." Natural Hazards and Earth System Sciences 3, no. 5 (2003): 321–32. http://dx.doi.org/10.5194/nhess-3-321-2003.

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Abstract. The 1883 Krakatau volcanic eruption has generated a destructive tsunami higher than 40 m on the Indonesian coast where more than 36 000 lives were lost. Sea level oscillations related with this event have been reported on significant distances from the source in the Indian, Atlantic and Pacific Oceans. Evidence of many manifestations of the Krakatau tsunami was a subject of the intense discussion, and it was suggested that some of them are not related with the direct propagation of the tsunami waves from the Krakatau volcanic eruption. Present paper analyzes the hydrodynamic part of the Krakatau event in details. The worldwide propagation of the tsunami waves generated by the Krakatau volcanic eruption is studied numerically using two conventional models: ray tracing method and two-dimensional linear shallow-water model. The results of the numerical simulations are compared with available data of the tsunami registration.
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10

Gabrielson, Thomas B. "Krakatoa and the Royal Society: The Krakatoa Explosion of 1883." Acoustics Today 6, no. 2 (2010): 14–19. http://dx.doi.org/10.1121/1.3467643.

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