{"title":"GIS技术在Vjosa河三角洲(阿尔巴尼亚)沿海动态研究中的应用","authors":"E. Xhaferri","doi":"10.33422/RSTCONF.2020.03.88","DOIUrl":null,"url":null,"abstract":"Vjosa River is the most important river of southern Albania, also is one of Europe’s wild rivers, with a length of 272 km and drainage basin of 6706km 2 . It sources from the Pindus Mountains in Greece (where it is called Aoös River) and drains in Albanian coast, near to the Narta Lagoon. Delta of Vjosa River with a surface of 317 km 2 is characterized by intensive changes of the shoreline, affected by the wave activity of the Adriatic Sea mostly affecting the river mouth and abandoned channels. The geometry and geomorphology of this delta has been conditioned by tectonic orientation of the Panaja and Frakulla neogene molasses hills. Study of the coastal dynamic and geometry changes of the delta mouth has been reconstructed using the information of topographic maps of Albania from existing studies and reports as well as the information extracted from satellite images. The statistical calculation of erosion and depositional are performed using GIS software technology. The studies performed on dynamics, erosion and accumulation, changes of the mouth shapes and coastline movements lead to the conclusion that delta area of Vjosa River is continuously in evolution. During the period from years 1870 to 2016, the interaction of sedimentological and neotectonic processes lead to total accumulation of an area of 21.7 km 2 , while an erosion surface of 7.5 km 2 is developed mostly at the southern river mouth.","PeriodicalId":439093,"journal":{"name":"Proceedings of The International Conference on Research in Science and Technology","volume":"120 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2020-03-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Application of GIS technology on studying the coastal dynamic of Vjosa River Delta (Albania)\",\"authors\":\"E. Xhaferri\",\"doi\":\"10.33422/RSTCONF.2020.03.88\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Vjosa River is the most important river of southern Albania, also is one of Europe’s wild rivers, with a length of 272 km and drainage basin of 6706km 2 . It sources from the Pindus Mountains in Greece (where it is called Aoös River) and drains in Albanian coast, near to the Narta Lagoon. Delta of Vjosa River with a surface of 317 km 2 is characterized by intensive changes of the shoreline, affected by the wave activity of the Adriatic Sea mostly affecting the river mouth and abandoned channels. The geometry and geomorphology of this delta has been conditioned by tectonic orientation of the Panaja and Frakulla neogene molasses hills. Study of the coastal dynamic and geometry changes of the delta mouth has been reconstructed using the information of topographic maps of Albania from existing studies and reports as well as the information extracted from satellite images. The statistical calculation of erosion and depositional are performed using GIS software technology. The studies performed on dynamics, erosion and accumulation, changes of the mouth shapes and coastline movements lead to the conclusion that delta area of Vjosa River is continuously in evolution. During the period from years 1870 to 2016, the interaction of sedimentological and neotectonic processes lead to total accumulation of an area of 21.7 km 2 , while an erosion surface of 7.5 km 2 is developed mostly at the southern river mouth.\",\"PeriodicalId\":439093,\"journal\":{\"name\":\"Proceedings of The International Conference on Research in Science and Technology\",\"volume\":\"120 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2020-03-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Proceedings of The International Conference on Research in Science and Technology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.33422/RSTCONF.2020.03.88\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings of The International Conference on Research in Science and Technology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.33422/RSTCONF.2020.03.88","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
Vjosa河是阿尔巴尼亚南部最重要的河流,也是欧洲的野生河流之一,全长272公里,流域面积6706公里。它起源于希腊的平都斯山脉(在那里它被称为Aoös河),在阿尔巴尼亚海岸排水,靠近纳尔塔泻湖。Vjosa河三角洲面积317 km2,海岸线变化剧烈,受亚得里亚海波浪活动的影响,主要影响河口和废弃河道。该三角洲的几何和地貌受Panaja和Frakulla新近纪糖蜜山的构造方向的制约。利用现有研究和报告中的阿尔巴尼亚地形图资料以及卫星图像提取的资料,重建了三角洲河口海岸动态和几何变化的研究。利用GIS软件技术进行侵蚀和沉积的统计计算。通过对动力学、侵蚀堆积、河口变化和海岸线运动等方面的研究,得出了Vjosa河三角洲地区处于持续演化过程中的结论。1870—2016年,沉积作用与新构造作用共同作用,形成了21.7 km 2的沉积积面,其中南部河口主要发育了7.5 km 2的侵蚀面。
Application of GIS technology on studying the coastal dynamic of Vjosa River Delta (Albania)
Vjosa River is the most important river of southern Albania, also is one of Europe’s wild rivers, with a length of 272 km and drainage basin of 6706km 2 . It sources from the Pindus Mountains in Greece (where it is called Aoös River) and drains in Albanian coast, near to the Narta Lagoon. Delta of Vjosa River with a surface of 317 km 2 is characterized by intensive changes of the shoreline, affected by the wave activity of the Adriatic Sea mostly affecting the river mouth and abandoned channels. The geometry and geomorphology of this delta has been conditioned by tectonic orientation of the Panaja and Frakulla neogene molasses hills. Study of the coastal dynamic and geometry changes of the delta mouth has been reconstructed using the information of topographic maps of Albania from existing studies and reports as well as the information extracted from satellite images. The statistical calculation of erosion and depositional are performed using GIS software technology. The studies performed on dynamics, erosion and accumulation, changes of the mouth shapes and coastline movements lead to the conclusion that delta area of Vjosa River is continuously in evolution. During the period from years 1870 to 2016, the interaction of sedimentological and neotectonic processes lead to total accumulation of an area of 21.7 km 2 , while an erosion surface of 7.5 km 2 is developed mostly at the southern river mouth.