Arid
DOI10.1016/j.jafrearsci.2020.104097
Geochemical modeling of the hydrogeochemical processes affecting groundwater quality of the Eocene aquifer east of El Minia Governorate - Eastern desert - Egypt
Ibrahim, Reda G. M.
通讯作者Ibrahim, RGM (corresponding author), Desert Res Ctr, Hydrogeochem Dept, EG-11753 Cairo, Egypt.
来源期刊JOURNAL OF AFRICAN EARTH SCIENCES
ISSN1464-343X
EISSN1879-1956
出版年2021
卷号174
英文摘要The Eocene limestone aquifer represents a renewable source of groundwater that can be used to enhance the sustainable agriculture at the eastern desert fringes of El Minia Governorate. The current research aims to investigate quantitatively the physicochemical processes which control the chemical composition of groundwater extracted from the Eocene aquifer using the PHREEQC code. The total dissolved solids of the Eocene groundwater range from 453 to 1903 mg/l indicating fresh to slightly brackish water quality. The simulation of the double mixing between rain (or Nile) water with Nubian water reveal that rain or Nile water contribution by 50% or more to the Eocene limestone aquifer system can explain the chemical composition of most groundwater samples of the Eocene aquifer. This means that the contribution from rain or Nile water infiltration to the Eocene aquifer is much more important than upward leakage from the underlying Nubian sandstone aquifer. The triple mixing processes simulation indicate also that the most effective end members of mixing are found to be rain and Nile waters, with some contribution from the groundwater encountered at the Nubian sandstone aquifer. The evaporation of 75%-95% of rain or Nile water explain the chemical content of most water samples which imply that evaporation is a dominant physicochemical process at East of El Minia area due to the elevated air temperature and the exploitation of groundwater at relatively shallow depths. The results of the current geochemical modeling study indicates that there are processes other than evaporation and mixing which affect the groundwater quality of the Eocene aquifer (such as carbonate and sulfate minerals dissolution). Finally, the usage of PHREEQC code in the quantitative assessment of the Eocene aquifer can be applied for similar aquifers and areas surrounding the Nile Valley Region in Egypt. This region comprises six governorates (Beni Suef, El Minia, Assiut, Sohag Qena and Aswan) where 40% of the population of Egypt live.
英文关键词Physicochemical processes Geochemical equilibria PHREEQC code East of El Minia Egypt
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000606452100021
WOS关键词WATER
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/347971
作者单位[Ibrahim, Reda G. M.] Desert Res Ctr, Hydrogeochem Dept, EG-11753 Cairo, Egypt
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Ibrahim, Reda G. M.. Geochemical modeling of the hydrogeochemical processes affecting groundwater quality of the Eocene aquifer east of El Minia Governorate - Eastern desert - Egypt[J],2021,174.
APA Ibrahim, Reda G. M..(2021).Geochemical modeling of the hydrogeochemical processes affecting groundwater quality of the Eocene aquifer east of El Minia Governorate - Eastern desert - Egypt.JOURNAL OF AFRICAN EARTH SCIENCES,174.
MLA Ibrahim, Reda G. M.."Geochemical modeling of the hydrogeochemical processes affecting groundwater quality of the Eocene aquifer east of El Minia Governorate - Eastern desert - Egypt".JOURNAL OF AFRICAN EARTH SCIENCES 174(2021).
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