{"title":"埃及东部沙漠wadi el tarfa盆地中始新世裂缝性碳酸盐岩含水层水文地质特征及地下水来源","authors":"Abu Setta","doi":"10.21608/egjg.2020.215448","DOIUrl":null,"url":null,"abstract":"Groundwater represents the main source of water supply in Wadi El Tarfa area. Wadi El Tarfa is one of the largest basins in the Eastern Desert which located east of the Nile River and has a surface area reaches 4939 Km. The geologic setting plays a vital role in groundwater occurrences, quantity and quality. The evaluation of the groundwater resources at Wadi El Tarfa has been achieved through the detailed studies of geomorphological, geological, hydrogeological and hydrogeochemical characteristics. The groundwater is available from two water bearing formations; Maghagha marly limestone aquifer and Samalut limestone aquifer which occur under free water table conditions. The groundwater of Maghagha aquifer is recorded at depth ranges from 38.95 m to 59.27 m and the salinity varies from 862.54 mg/l to 978.47 mg/l. The depth to the water of Samalut aquifer varies from 10 m to 80 m and the salinity ranges from 227.51 mg/l to 2545.11 mg/l. The transmissivity ranges from 19.82 m/day to 4125.60 m/day. The collected groundwater samples were chemically analyzed and interpreted. The groundwater origin has been determined through the stable isotope analysis for some selected samples. Finally, the best sites for groundwater exploitation from Samalut aquifer at Wadi El Tarfa basin have been determined.","PeriodicalId":282322,"journal":{"name":"Egyptian Journal of Geology","volume":"6 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"HYDROGEOLOGICAL CHARACTERISTICS AND GROUNDWATER ORIGIN OF THE MIDDLE EOCENE FRACTURED CARBONATE AQUIFERS AT WADI EL TARFA BASIN, EASTERN DESERT, EGYPT\",\"authors\":\"Abu Setta\",\"doi\":\"10.21608/egjg.2020.215448\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Groundwater represents the main source of water supply in Wadi El Tarfa area. Wadi El Tarfa is one of the largest basins in the Eastern Desert which located east of the Nile River and has a surface area reaches 4939 Km. The geologic setting plays a vital role in groundwater occurrences, quantity and quality. The evaluation of the groundwater resources at Wadi El Tarfa has been achieved through the detailed studies of geomorphological, geological, hydrogeological and hydrogeochemical characteristics. The groundwater is available from two water bearing formations; Maghagha marly limestone aquifer and Samalut limestone aquifer which occur under free water table conditions. The groundwater of Maghagha aquifer is recorded at depth ranges from 38.95 m to 59.27 m and the salinity varies from 862.54 mg/l to 978.47 mg/l. The depth to the water of Samalut aquifer varies from 10 m to 80 m and the salinity ranges from 227.51 mg/l to 2545.11 mg/l. The transmissivity ranges from 19.82 m/day to 4125.60 m/day. The collected groundwater samples were chemically analyzed and interpreted. The groundwater origin has been determined through the stable isotope analysis for some selected samples. Finally, the best sites for groundwater exploitation from Samalut aquifer at Wadi El Tarfa basin have been determined.\",\"PeriodicalId\":282322,\"journal\":{\"name\":\"Egyptian Journal of Geology\",\"volume\":\"6 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2020-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Egyptian Journal of Geology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.21608/egjg.2020.215448\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Egyptian Journal of Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.21608/egjg.2020.215448","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
地下水是Wadi El Tarfa地区供水的主要来源。Wadi El Tarfa是东部沙漠中最大的盆地之一,位于尼罗河以东,表面积达到4939公里。地质环境对地下水的赋存、数量和质量起着至关重要的作用。通过详细的地貌、地质、水文地质和水文地球化学特征研究,实现了对瓦迪塔尔法地下水资源的评价。地下水可从两个含水地层获得;Maghagha灰岩含水层和Samalut灰岩含水层在自由地下水位条件下形成。Maghagha含水层的地下水记录深度为38.95 ~ 59.27 m,盐度为862.54 ~ 978.47 mg/l。Samalut含水层的水深为10 ~ 80 m,盐度为227.51 ~ 2545.11 mg/l。透过率范围为19.82 ~ 4125.60 m/d。收集的地下水样本进行了化学分析和解释。通过对部分样品的稳定同位素分析,确定了地下水的来源。最后,确定了Wadi El Tarfa盆地Samalut含水层地下水的最佳开采地点。
HYDROGEOLOGICAL CHARACTERISTICS AND GROUNDWATER ORIGIN OF THE MIDDLE EOCENE FRACTURED CARBONATE AQUIFERS AT WADI EL TARFA BASIN, EASTERN DESERT, EGYPT
Groundwater represents the main source of water supply in Wadi El Tarfa area. Wadi El Tarfa is one of the largest basins in the Eastern Desert which located east of the Nile River and has a surface area reaches 4939 Km. The geologic setting plays a vital role in groundwater occurrences, quantity and quality. The evaluation of the groundwater resources at Wadi El Tarfa has been achieved through the detailed studies of geomorphological, geological, hydrogeological and hydrogeochemical characteristics. The groundwater is available from two water bearing formations; Maghagha marly limestone aquifer and Samalut limestone aquifer which occur under free water table conditions. The groundwater of Maghagha aquifer is recorded at depth ranges from 38.95 m to 59.27 m and the salinity varies from 862.54 mg/l to 978.47 mg/l. The depth to the water of Samalut aquifer varies from 10 m to 80 m and the salinity ranges from 227.51 mg/l to 2545.11 mg/l. The transmissivity ranges from 19.82 m/day to 4125.60 m/day. The collected groundwater samples were chemically analyzed and interpreted. The groundwater origin has been determined through the stable isotope analysis for some selected samples. Finally, the best sites for groundwater exploitation from Samalut aquifer at Wadi El Tarfa basin have been determined.