Morphoscopic changes in Iraqi territorial waters and their border repercussions

Hassan K. H. Al-Mahmood
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 The present study includes the analysis of the morphological change in the Iraqi coastline in Khor Abdullah and the entrance to the Shatt Al-Arab (Al-Ruka Channel), as the northwestern region of the Arabian Gulf is exposed to different erosion and depositions due to the suspended sedimentary load, The comparison between the periods studied showed severe erosion in some coastal areas and depositions in other parts, which led to changes in the shape and extension of the barriers or the sedimentary tongues and made them prominent, especially in the shallow sites (shoals) areas at the entrance to Khor Abdullah and Khor Shaitanah, and those changed parts appear in the maps of the British Admiralty, which draw detailed curves surrounding the varying depths. The extension of the suspended sedimentary load at the head of the Arabian Gulf amounted to 11,014 km2 in the year 2003, which expanded in 2011 to 12,680 km2, by adding suspended sediments of about 1,676 km2 to 6,452,600 tons over 8 years, at a rate of 806.575 tons annually, or 8.5% of the volume of suspended sediments in 1996 due to the decrease of the river flows from the Tigris, Euphrates, and Karun. The line of the lowest tide (zero line) showed a change in the cross-section of the Iraqi waterway lines that it shares with Iran and Kuwait, affecting the location of the approved border line between Iraq and Kuwait, and the largest change was in the width of the entrance to the Shatt Al-Arab (Al-Ruka Channel), and this was influenced by the erosion, sedimentation patterns, and deflection of tidal currents, as well as the temporary effect of port activities in Khor Abdullah. The extension of Abdullah’s Marqat at Ras Al-Bishah reached 15.5 km in 2003, its extension became 17.2 km in 2019 with a varying range of 1.7 km in 16 years, which has increased at lower rates in recent years due to the decrease in the sedimentary load of rivers to legalize water releases. The maximum change in Khor Abdullah in the middle part was 453 meters, which is a contraction in favor of Kuwait at a rate of 453 meters, and in the middle of the Al-Ruka Channel with an average width of 403 meters in favor of Iran, expansion in favor of Iraq was at a rate of 152 and 42 meters at the entrance and middle of Khor Shaitana.","PeriodicalId":491432,"journal":{"name":"Al-maǧallaẗ al-ʻirāqiyyaẗ li-l-istizrāʻ al-māʼhī","volume":"111 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2023-04-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Al-maǧallaẗ al-ʻirāqiyyaẗ li-l-istizrāʻ al-māʼhī","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.58629/ijaq.v19i1.436","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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Abstract

Abstract The present study includes the analysis of the morphological change in the Iraqi coastline in Khor Abdullah and the entrance to the Shatt Al-Arab (Al-Ruka Channel), as the northwestern region of the Arabian Gulf is exposed to different erosion and depositions due to the suspended sedimentary load, The comparison between the periods studied showed severe erosion in some coastal areas and depositions in other parts, which led to changes in the shape and extension of the barriers or the sedimentary tongues and made them prominent, especially in the shallow sites (shoals) areas at the entrance to Khor Abdullah and Khor Shaitanah, and those changed parts appear in the maps of the British Admiralty, which draw detailed curves surrounding the varying depths. The extension of the suspended sedimentary load at the head of the Arabian Gulf amounted to 11,014 km2 in the year 2003, which expanded in 2011 to 12,680 km2, by adding suspended sediments of about 1,676 km2 to 6,452,600 tons over 8 years, at a rate of 806.575 tons annually, or 8.5% of the volume of suspended sediments in 1996 due to the decrease of the river flows from the Tigris, Euphrates, and Karun. The line of the lowest tide (zero line) showed a change in the cross-section of the Iraqi waterway lines that it shares with Iran and Kuwait, affecting the location of the approved border line between Iraq and Kuwait, and the largest change was in the width of the entrance to the Shatt Al-Arab (Al-Ruka Channel), and this was influenced by the erosion, sedimentation patterns, and deflection of tidal currents, as well as the temporary effect of port activities in Khor Abdullah. The extension of Abdullah’s Marqat at Ras Al-Bishah reached 15.5 km in 2003, its extension became 17.2 km in 2019 with a varying range of 1.7 km in 16 years, which has increased at lower rates in recent years due to the decrease in the sedimentary load of rivers to legalize water releases. The maximum change in Khor Abdullah in the middle part was 453 meters, which is a contraction in favor of Kuwait at a rate of 453 meters, and in the middle of the Al-Ruka Channel with an average width of 403 meters in favor of Iran, expansion in favor of Iraq was at a rate of 152 and 42 meters at the entrance and middle of Khor Shaitana.
伊拉克领海的形态变化及其对边界的影响
摘要# x0D;本研究包括对Khor Abdullah和阿拉伯河(Al-Ruka海峡)入口的伊拉克海岸线的形态变化进行分析,因为阿拉伯湾西北地区由于悬浮的沉积负荷而暴露于不同的侵蚀和沉积。研究期间的比较表明,一些沿海地区的侵蚀和其他部分的沉积严重。这导致了屏障或沉积舌的形状和延伸的变化,并使它们变得突出,特别是在Khor Abdullah和Khor Shaitanah入口处的浅滩地区,这些变化的部分出现在英国海军部的地图上,地图上绘制了围绕不同深度的详细曲线。由于底格里斯河、幼发拉底河和卡伦河的径流量减少,8年间增加了1676 km2至6452600 t的悬浮泥沙,每年增加806.575 t,相当于1996年悬浮泥沙量的8.5%,因此,阿拉伯湾顶部悬浮泥沙的扩展在2003年达到11,014 km2, 2011年扩大到12,680 km2。最低的潮流的线(零线)显示伊拉克航道截面线的变化,股票与伊朗和科威特,批准的位置影响伊拉克和科威特之间的边界线,最大的变化是,入口阿拉伯河的宽度(Al-Ruka频道),这是受到侵蚀、沉积模式,和潮流的偏转,以及港口活动的临时效果豪尔阿卜杜拉。2003年,拉斯比沙(Ras Al-Bishah)的阿卜杜拉马尔卡特(Abdullah 's Marqat)延伸达到15.5公里,2019年延伸至17.2公里,16年来的延伸范围为1.7公里,近年来由于河流的沉积负荷减少,使水的释放合法化,其增长速度较低。霍尔赫阿卜杜拉中部的最大变化为453米,这是对科威特有利的收缩速度为453米,在平均宽度为403米的Al-Ruka海峡中部对伊朗有利,在霍尔赫沙伊塔纳入口和中部对伊拉克有利的扩张速度为152米和42米。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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