摩苏尔水坝调节湖的水文形态学研究。伊拉克摩苏尔城北部

Asaad A. M. AL-Hussein, Adil Al-Hamadani
{"title":"摩苏尔水坝调节湖的水文形态学研究。伊拉克摩苏尔城北部","authors":"Asaad A. M. AL-Hussein, Adil Al-Hamadani","doi":"10.33899/earth.2020.170316","DOIUrl":null,"url":null,"abstract":"The work deals with the study of hydromorphology of the regulating lake which located at (50Km) north of Mosul city. The survey started in November, 2012 using the EchoSounder, and carried out by dividing the lake into (30) sections starting from the lower surface of the main dam and ending at the regulating dam. Data are recorded and represented using GIS technology (Arc GIs v10.4) and Microsoft program (Excel). The survey shows that the shallowest depth in the lake is found at left bank of section (5) which reached (7.65 m) and the deepest point is Found in the left bank of ةسا رد قا رعلا ،لصوملا ةنيدم لامش ةيميظنتلا لصوملا دس ةريحب ةيجولوفرومورديه 21 the section (9) which reached (18.22m) directly on the Thalwage line. The hydraulic gradient of the lake is (1m/Km ), and the overall shape of the sections is (U) shape. The variation in depth in each section is mostly due to difference in the sedimentation and erosion. There was deposition on the convex sides and erosion in the concave sides of the banks, the erosion and sedimentation processes vary with the variat ion of water velocity, slope and rock components of the river along the regulating lake.","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"74 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2020-06-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Hydromorphological Study of Regulating Lake of Mosul DamNorth Mosul City, Iraq\",\"authors\":\"Asaad A. M. AL-Hussein, Adil Al-Hamadani\",\"doi\":\"10.33899/earth.2020.170316\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The work deals with the study of hydromorphology of the regulating lake which located at (50Km) north of Mosul city. The survey started in November, 2012 using the EchoSounder, and carried out by dividing the lake into (30) sections starting from the lower surface of the main dam and ending at the regulating dam. Data are recorded and represented using GIS technology (Arc GIs v10.4) and Microsoft program (Excel). The survey shows that the shallowest depth in the lake is found at left bank of section (5) which reached (7.65 m) and the deepest point is Found in the left bank of ةسا رد قا رعلا ،لصوملا ةنيدم لامش ةيميظنتلا لصوملا دس ةريحب ةيجولوفرومورديه 21 the section (9) which reached (18.22m) directly on the Thalwage line. The hydraulic gradient of the lake is (1m/Km ), and the overall shape of the sections is (U) shape. The variation in depth in each section is mostly due to difference in the sedimentation and erosion. There was deposition on the convex sides and erosion in the concave sides of the banks, the erosion and sedimentation processes vary with the variat ion of water velocity, slope and rock components of the river along the regulating lake.\",\"PeriodicalId\":371191,\"journal\":{\"name\":\"Iraqi National Journal of Earth Sciences\",\"volume\":\"74 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2020-06-30\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Iraqi National Journal of Earth Sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.33899/earth.2020.170316\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Iraqi National Journal of Earth Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.33899/earth.2020.170316","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

这项工作涉及位于摩苏尔市以北50公里处的调节湖的水文形态研究。调查开始于2012年11月,使用回声测深仪,并将湖泊分为(30)个部分,从主坝的下表面开始,到调节坝结束。使用GIS技术(Arc GIS v10.4)和Microsoft程序(Excel)记录和表示数据。调查结果表明,湖深最浅处为(5)段左岸,水深为(7.65 m);最深处为(9)段左岸,水深为(18.22m),直接位于Thalwage线上。湖的水力梯度为(1m/Km),断面整体形状为(U)形。各剖面深度的变化主要是由于沉积和侵蚀的不同。河岸凸侧有淤积,凹侧有侵蚀,侵蚀和沉积过程随调节湖沿岸流速、坡度和岩石组分的变化而变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydromorphological Study of Regulating Lake of Mosul DamNorth Mosul City, Iraq
The work deals with the study of hydromorphology of the regulating lake which located at (50Km) north of Mosul city. The survey started in November, 2012 using the EchoSounder, and carried out by dividing the lake into (30) sections starting from the lower surface of the main dam and ending at the regulating dam. Data are recorded and represented using GIS technology (Arc GIs v10.4) and Microsoft program (Excel). The survey shows that the shallowest depth in the lake is found at left bank of section (5) which reached (7.65 m) and the deepest point is Found in the left bank of ةسا رد قا رعلا ،لصوملا ةنيدم لامش ةيميظنتلا لصوملا دس ةريحب ةيجولوفرومورديه 21 the section (9) which reached (18.22m) directly on the Thalwage line. The hydraulic gradient of the lake is (1m/Km ), and the overall shape of the sections is (U) shape. The variation in depth in each section is mostly due to difference in the sedimentation and erosion. There was deposition on the convex sides and erosion in the concave sides of the banks, the erosion and sedimentation processes vary with the variat ion of water velocity, slope and rock components of the river along the regulating lake.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信