Groundwater Geochemistry of the Fushe Kuqe Aquifer,North-Western Albania

作     者：Sabina Cenameri Arjan Beqiraj 

作者机构：Ministry of Tourism and EnvironmentBlv.Deshmoret e KombitNo.1Tirana 1001Albania Faculty of Geology and MiningStr.“Elbasani”Tirana 1020Albania 

出 版 物：《Journal of Environmental Science and Engineering(A)》 (环境科学与工程（A）)

年 卷 期：2018年第7卷第9期

页      面：354-360页

学科分类：0830[工学-环境科学与工程（可授工学、理学、农学学位）] 08[工学] 

主　　题：Aquifer groundwater geochemistry Fushe Kuqe Albania 

摘      要：The Fushe Kuqe costal aquifer is a typical confined alluvial *** aquifer medium consists of alternating and discontinuous layers of gravel and sand-gravel and silt-clay impermeable layers which have conditioned its multilayer *** aquifer recharge occurs mainly through water infiltration from the Mat river in the North,and from Droja river in the South,while its natural discharge proceeds to the Adriatic ***(Total Solids Dissolved)concentration varies from 200-500 mg/L in the North-Eastern area up to over 1,000 mg/L near the coastal *** a wide range of TDS values is also confirmed by high(11.89° dH)value of its standard *** HCO3-Ca-Mg and HCO3-Mg-Ca hydrochemical water types dominate in the eastern-north-eastern aquifer sectors,Na-Mg-HCO3-Cl,Na-Cl-HCO3 type in central-western area and,finally,Na-Cl type along the coastal parts of the *** of carbonates and sulphate minerals and silicate weathering seems to be the primary processes for the formation of the chemical composition of the ***-Alkaline Indices CAI-1 and Chadha’s classification diagram distinguished two groundwater compositional groups derived from water-medium chemical reactions and fresh groundwater-seawater mixture,respectively.