Evaporitic sedimentation and geochemical characteristics of bittern solutions as feeding for future projects, Emisal {u2013} Faiyoum {u2013} Egypt / Ahmed Waheed Barakat Ali ; Supervised Ahmed M. Abu Khadra , Amany G. Taher , Ragab M. Elsheikh
Material type:
- الخواص الرسوبية و الجيوكيويائية للمحلول المر كمحلول مغذى للمشاريع المستقبلية - إميسال - الفيوم - مصر [Added title page title]
- Issued also as CD
Item type | Current library | Home library | Call number | Copy number | Status | Barcode | |
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قاعة الرسائل الجامعية - الدور الاول | المكتبة المركزبة الجديدة - جامعة القاهرة | Cai01.12.15.M.Sc.2015.Ah.E (Browse shelf(Opens below)) | Not for loan | 01010110066867000 | ||
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مخـــزن الرســائل الجـــامعية - البدروم | المكتبة المركزبة الجديدة - جامعة القاهرة | Cai01.12.15.M.Sc.2015.Ah.E (Browse shelf(Opens below)) | 66867.CD | Not for loan | 01020110066867000 |
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Thesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology
This study deals with sedimentlogical and geochemical characteristics of the bittern ponds (1/2, 5, 6, Mg and storage pond 2/2) at the Egyptian Salts & Minerals Co. (EMISAL) at different concentrations and specific gravities. The mineral composition and petrography of the five bittern ponds sediments were identified using X-ray diffraction and polarizing microscope techniques. The thin sections of evaporite sediments were made for identification of minerals and to examine textures and the relationship between the minerals present. - Pond (1/2): It has an area of about 51466 m² and depth of about 3.2 m, the average Sp. Gr. is 1.222. X-ray showed that halite is the dominate evaporite mineral. Petrographical thin section examination of thin section samples showed that halite is formed as clusters of large euhedral cubic; dissolution features of irregular subhedral to distorted platy halite crystals were recorded. Chevron textures with abundant primary fluid inclusions were also observed
Issued also as CD
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