{"title":"印尼乌兰三角洲时空特征、演变及控制因素","authors":"B. Septiangga, B. Mutaqin","doi":"10.21163/GT_2021.163.04","DOIUrl":null,"url":null,"abstract":": The evolution of the Wulan Delta began after the construction of the Wulan River Canal in 1892. It alters the shoreline erosion and accretion that affect the land dynamics of the coastal area. This study aims to analyze the spatio-temporal evolution of the Wulan Delta, including the shoreline and its dynamics, as well as the geomorphological processes that affect it. The shoreline change was extracted digitally from Landsat satellite images and divided into four periods, i.e., 1995-2000, 2000-2011, 2011-2015, and 2015-2020. We used the histogram thresholding method to separate the land from the sea and produce the shoreline as the interface. This research employed field check and focus group discussion for identifying the cause and impact of shoreline dynamics in the research area. The results show that land loss and accumulation over 25 years (1995-2020) are -7.16 km 2 and +6.58 km 2 , respectively. In Wulan Delta, the erosion is due to high waves and sedimentation due to mangrove planting and high sediment from the rivers. The development rates of the Wulan Delta for the period of 1995-2020 were 73,200 m 2 /year.","PeriodicalId":45100,"journal":{"name":"Geographia Technica","volume":" ","pages":""},"PeriodicalIF":0.7000,"publicationDate":"2021-03-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"SPATIO-TEMPORAL ANALYSIS OF WULAN DELTA IN INDONESIA: CHARACTERISTICS, EVOLUTION, AND CONTROLLING FACTORS\",\"authors\":\"B. Septiangga, B. Mutaqin\",\"doi\":\"10.21163/GT_2021.163.04\",\"DOIUrl\":null,\"url\":null,\"abstract\":\": The evolution of the Wulan Delta began after the construction of the Wulan River Canal in 1892. It alters the shoreline erosion and accretion that affect the land dynamics of the coastal area. This study aims to analyze the spatio-temporal evolution of the Wulan Delta, including the shoreline and its dynamics, as well as the geomorphological processes that affect it. The shoreline change was extracted digitally from Landsat satellite images and divided into four periods, i.e., 1995-2000, 2000-2011, 2011-2015, and 2015-2020. We used the histogram thresholding method to separate the land from the sea and produce the shoreline as the interface. This research employed field check and focus group discussion for identifying the cause and impact of shoreline dynamics in the research area. The results show that land loss and accumulation over 25 years (1995-2020) are -7.16 km 2 and +6.58 km 2 , respectively. In Wulan Delta, the erosion is due to high waves and sedimentation due to mangrove planting and high sediment from the rivers. The development rates of the Wulan Delta for the period of 1995-2020 were 73,200 m 2 /year.\",\"PeriodicalId\":45100,\"journal\":{\"name\":\"Geographia Technica\",\"volume\":\" \",\"pages\":\"\"},\"PeriodicalIF\":0.7000,\"publicationDate\":\"2021-03-09\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geographia Technica\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.21163/GT_2021.163.04\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geographia Technica","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.21163/GT_2021.163.04","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
SPATIO-TEMPORAL ANALYSIS OF WULAN DELTA IN INDONESIA: CHARACTERISTICS, EVOLUTION, AND CONTROLLING FACTORS
: The evolution of the Wulan Delta began after the construction of the Wulan River Canal in 1892. It alters the shoreline erosion and accretion that affect the land dynamics of the coastal area. This study aims to analyze the spatio-temporal evolution of the Wulan Delta, including the shoreline and its dynamics, as well as the geomorphological processes that affect it. The shoreline change was extracted digitally from Landsat satellite images and divided into four periods, i.e., 1995-2000, 2000-2011, 2011-2015, and 2015-2020. We used the histogram thresholding method to separate the land from the sea and produce the shoreline as the interface. This research employed field check and focus group discussion for identifying the cause and impact of shoreline dynamics in the research area. The results show that land loss and accumulation over 25 years (1995-2020) are -7.16 km 2 and +6.58 km 2 , respectively. In Wulan Delta, the erosion is due to high waves and sedimentation due to mangrove planting and high sediment from the rivers. The development rates of the Wulan Delta for the period of 1995-2020 were 73,200 m 2 /year.
期刊介绍:
Geographia Technica is a journal devoted to the publication of all papers on all aspects of the use of technical and quantitative methods in geographical research. It aims at presenting its readers with the latest developments in G.I.S technology, mathematical methods applicable to any field of geography, territorial micro-scalar and laboratory experiments, and the latest developments induced by the measurement techniques to the geographical research. Geographia Technica is dedicated to all those who understand that nowadays every field of geography can only be described by specific numerical values, variables both oftime and space which require the sort of numerical analysis only possible with the aid of technical and quantitative methods offered by powerful computers and dedicated software. Our understanding of Geographia Technica expands the concept of technical methods applied to geography to its broadest sense and for that, papers of different interests such as: G.l.S, Spatial Analysis, Remote Sensing, Cartography or Geostatistics as well as papers which, by promoting the above mentioned directions bring a technical approach in the fields of hydrology, climatology, geomorphology, human geography territorial planning are more than welcomed provided they are of sufficient wide interest and relevance.