Case Study Of Abration Of The Musi River Bad Due To Water Waves In Coastal Prajin Village, Banyuasin I District, South Sumatera Province
Article Sidebar
Main Article Content
Abstract
Abstract— Banyuasin Regency apart from geographically has a strategic location, which is located on a cross-province route, also has abundant natural resources. Geographical Location of Banyuasin Regency is located between 1.30 ° - 4.0 ° South Latitude and 104 ° 00 '- 105 ° 35' East Longitude which stretches from the central part of South Sumatra Province to the eastern part.
Banyuasin Regency has an area of 12,431 km² and is divided into 19 sub-districts, one of which is Banyuasin I District. Banyuasin Regency has an area of 12,431 km² and is divided into 19 sub-districts, one of which is Banyuasin I sub-district, Banyuasin I district consists of several villages and sub-districts, Prajin village has almost the majority of its inhabitants on the banks of the Musi river, the existence of this village originated from a small population to Now it is increasing, but based on the current condition of the village, the population on the river bank is almost on average eroded up to ± 20 m2 by water waves caused by wind waves, waves caused by the speed of passing ships, and the occurrence of tidal waves. . We need to know that together.
The Musi River is a river located in the province of South Sumatra, Indonesia. [1] With a length of 750 km, while the village is opposite the edge of the village prajin. The Musi River is 750 km long and is the longest river on the island of Sumatra. Since the time of the Sriwijaya Kingdom, this river has been known as the main means of transportation for the community. On the banks of the Musi River is the Boom Baru Harbor. The Musi River divides Palembang City into two areas: opposite Ilir in the north and across from the ulu in the south. The springs are sourced in the Kepahiang area, Bengkulu. This river is the mouth of nine major tributaries, namely the Komering, Rawas, Batanghari, Leko, Lakit, Kelingi, Lematang, Semangus, and Ogan rivers.
Article Details
This work is licensed under a Creative Commons Attribution 4.0 International License.
References
Structures, Van Nostrand Reinhold, 1981
[2] Chakrabari, S.K., Hydrodynamics of Offshore Structures, Springer- Verlag, Berlin, 1990
[3] Djatmiko, E.B., Perilaku dan Operabilitas Bangunan Laut di Atas Gelombang Acak, ITS Press, Surabaya, 2012
[4] Pratikto, W.A., Armono, H.D. dan Suntoyo, Perencanaan Fasilitas Pantai dan L Laut, BPFE, Yogyakarta, 1997
[5] Sorensen, R.M., Basic Wave Mechanics: For Coastal and Ocean Engineers, John Wiley & Sons Ltd., Chichester, 1993
[6] Nielsen, P., Coastal and Estuarine Processes, World Scientific Publishing, Co. Pte. Ltd., 2012
[7] Bambang Triatmojo , Teori Pantai Elivasi pasang surut (1999)
[8] G. Eason, B. Noble, and I.N. Sneddon, “On certain integrals of Lipschitz-Hankel type involving products of Bessel functions,” Phil. Trans. Roy. Soc. London, vol. A247, pp. 529-551, April 1955. (references)
[9] J. Clerk Maxwell, A Treatise on Electricity and Magnetism, 3rd ed., vol. 2. Oxford: Clarendon, 1892, pp.68-73.
[10] I.S. Jacobs and C.P. Bean, “Fine particles, thin films and exchange anisotropy,” in Magnetism, vol. III, G.T. Rado and H. Suhl, Eds. New York: Academic, 1963, pp. 271-350.
[11] K. Elissa, “Title of paper if known,” unpublished.
[12] R. Nicole, “Title of paper with only first word capitalized,” J. Name Stand. Abbrev., in press.
[13] Y. Yorozu, M. Hirano, K. Oka, and Y. Tagawa, “Electron spectroscopy studies on magneto-optical media and plastic substrate interface,” IEEE Transl. J. Magn. Japan, vol. 2, pp. 740-741, August 1987 [Digests 9th Annual Conf. Magnetics Japan, p. 301, 1982].
[14] M. Young, The Technical Writer’s Handbook. Mill Valley, CA: University Science, 1989.