{"title":"Groundwater Resources Development in Libya: Wadi Ahmar and Wadi al Bab Project@@@ワジ アハマールおよびワジ アル バブ プロジェクト","authors":"Y. Shidomoto, Y. Uemura","doi":"10.5917/jagh1959.25.193","DOIUrl":null,"url":null,"abstract":"The project of Wadi al Bab and Wadi Ahmar in Libya aims to deveplop the available water resources, both surface and groundwater. The study area is approximately 2, 000 km<SUP>2</SUP>, located on the south-western flank of Jebel Akhdar Mountains, 30 to 80 km southeast of Benghazi. <BR> The climate of the study area is semi-arid and its mean annual precipitation is 100 to 200 mm high. With First Escarpment as a border, to the west is spread the Benghazi coastal plain, and to the east, a table land. Tertiary rocks and Quaternary deposits are distributed. Each formation of Tertiary period displays transgressive and regressive facies and are comprised mainly of marine carbonates. <BR> In this paper, some results of hydrogeological investigation, such as groundwater storage conditions, water quality, water balance and etc. , will be discussed.","PeriodicalId":422881,"journal":{"name":"THE JOURNAL OF THE JAPANESE ASSOCIATION OF GROUNDWATER HYDROLOGY","volume":"12 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"THE JOURNAL OF THE JAPANESE ASSOCIATION OF GROUNDWATER HYDROLOGY","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5917/jagh1959.25.193","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The project of Wadi al Bab and Wadi Ahmar in Libya aims to deveplop the available water resources, both surface and groundwater. The study area is approximately 2, 000 km2, located on the south-western flank of Jebel Akhdar Mountains, 30 to 80 km southeast of Benghazi. The climate of the study area is semi-arid and its mean annual precipitation is 100 to 200 mm high. With First Escarpment as a border, to the west is spread the Benghazi coastal plain, and to the east, a table land. Tertiary rocks and Quaternary deposits are distributed. Each formation of Tertiary period displays transgressive and regressive facies and are comprised mainly of marine carbonates. In this paper, some results of hydrogeological investigation, such as groundwater storage conditions, water quality, water balance and etc. , will be discussed.