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Chaghazardi, Zahra, Mirzaee, Seyed Yayha, Chitsazan, Manuchehre, alijani, Farshad. (1404). Identification and Estimation of Groundwater Recharge Sources through Hydrochemical Analysis and Stable Environmental Isotopes in Evan Plain‌, Khuzestan, Iran. , (), -. doi: 10.22059/geope.2025.391591.648812
Zahra Chaghazardi; Seyed Yayha Mirzaee; Manuchehre Chitsazan; Farshad alijani. "Identification and Estimation of Groundwater Recharge Sources through Hydrochemical Analysis and Stable Environmental Isotopes in Evan Plain‌, Khuzestan, Iran". , , , 1404, -. doi: 10.22059/geope.2025.391591.648812
Chaghazardi, Zahra, Mirzaee, Seyed Yayha, Chitsazan, Manuchehre, alijani, Farshad. (1404). 'Identification and Estimation of Groundwater Recharge Sources through Hydrochemical Analysis and Stable Environmental Isotopes in Evan Plain‌, Khuzestan, Iran', , (), pp. -. doi: 10.22059/geope.2025.391591.648812
Chaghazardi, Zahra, Mirzaee, Seyed Yayha, Chitsazan, Manuchehre, alijani, Farshad. Identification and Estimation of Groundwater Recharge Sources through Hydrochemical Analysis and Stable Environmental Isotopes in Evan Plain‌, Khuzestan, Iran. , 1404; (): -. doi: 10.22059/geope.2025.391591.648812

Identification and Estimation of Groundwater Recharge Sources through Hydrochemical Analysis and Stable Environmental Isotopes in Evan Plain‌, Khuzestan, Iran

Geopersia
مقالات آماده انتشار، پذیرفته شده، انتشار آنلاین از تاریخ 16 شهریور 1404    اصل مقاله (2.24 M)
نوع مقاله: Research Paper
شناسه دیجیتال (DOI): 10.22059/geope.2025.391591.648812
نویسندگان
Zahra Chaghazardi1؛ Seyed Yayha Mirzaee* 1؛ Manuchehre Chitsazan1؛ Farshad alijani2
1Faculty of Geosciences, Shahid Chamran University of Ahvaz,, Iran
2Faculty of Geosciences, Shahid Beheshti University of Tehran, Iran
چکیده
Identifying the inflows and outflows of plains experiencing groundwater level fluctuations is a critical aspect of water resource management, environmental decision-making, and agricultural planning. The groundwater of the Evan Plain is mainly affected by two recharge sources. The Karkheh River, contributing an average of 30%, serves as the main recharge source in the northern and northeastern parts of the plain. Furthermore, The groundwater inflow from the Abbas Plain contributes an average of 32% to the aquifer recharge, predominantly affecting the plain's central, southeastern, and southwestern areas. These findings provide valuable insights for effective aquifer management and future regional water resource planning. 
کلیدواژه‌ها
Stable water isotopes؛ Hydrochemistry؛ Recharge sources؛ Mixing؛ Evan Plain
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تعداد مشاهده مقاله: 374
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