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Identification of hydrochemical processes using multivariate statistics in a complex aquifer system of Sohag region, Egypt

机译:埃及Sohag地区复杂含水层系统中多元统计鉴定鉴定水利统计

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Spatial variation of hydrochemical groundwater parameters indicates that the chemistry is ruled by complex process interactions (mixing of natural and anthropogenic processes). For this approach, analysis of 32 groundwater wells was conducted. Anthropogenic-influenced surface recharge and geogenic processes such as silicate weathering and redox process are identified by multivariate statistics, principal component analysis (PCA) and cluster analysis (CA). Surface water recharge tops the list of factors affecting groundwater chemistry in the Sohag area. The main recharging sources are leaching of salts of overlain soils and irrigation canals associated with anthropogenic impacts such as domestic sewage and agricultural nutrients. The excess of SO42- and HCO3- relative to Ca2+ in the semiconfined shallow aquifer at the floodplain can be attributed to the anthropogenic influence, infiltrated irrigation water and wastewater. On the other hand, in deep wells at the desert fringes, the deficiency of SO42- relative to Ca2+ concentration (however the dissolution of gypsum modeled by MINTEQ) is evidence on sulfides precipitation under reducing conditions as confirmed by the PCA analysis. Ion exchange on clay is another possible reason responsible for the deficiency of Ca2+ + Mg2+/SO42- + HCO3- relative to Na+/Cl- in semiconfined aquifer. Different water types (Na-Cl, Ca-Cl, Mg--Cl and Na-HCO3) indicate different ion exchange processes formed due to varying contacts between freshwater and saline water. Excessive Mn/Fe ratio is attributed to fertilization and redox processes. Results enable the spatial separation of wells under semiconfined hydraulic conditions recharged by infiltrated irrigation water, from those under unconfined conditions recharged by seepage water leaching salty soils. Accordingly, different water types and values of salinity are complex and could be identified and spatially separated using AqQa and statistical analysis.
机译:水化学地下水参数的空间变化表明化学是通过复杂的工艺相互作用(自然和人为过程的混合)统治的化学。对于这种方法,进行了3​​2个地下水孔的分析。受影响的表面补充和诸如硅酸盐风化和氧化还原过程的人为受损和造成的造林过程是通过多变量统计,主成分分析(PCA)和聚类分析(CA)鉴定。地表水充电在苏格兰地区影响地下水化学的因素列表。主要的充电来源是与人为污水和农业营养等人为影响有关的骨土和灌溉灌溉系泥的浸出。在洪泛区的半挤出浅含水层中的SO42和HCO3-相对于CA2 +的过量可以归因于人为影响,渗透灌溉水和废水。另一方面,在沙漠条纹的深井中,SO42相对于Ca2 +浓度的缺乏(然而,Minteq模拟的石膏溶解)是通过PCA分析证实的降低条件下的硫化物沉淀的证据。粘土上的离子交换是另一种可能原因,其负责Ca2 + + Mg2 + / SO42- + HCO3相对于半+ / CL-含有半成核含水层的含量。不同的水类型(Na-Cl,Ca-Cl,Mg-C1和Na-HCO3)表示由于淡水和盐水之间的不同触点而形成的不同的离子交换过程。过量的Mn / Fe比率归因于施肥和氧化还原过程。结果,通过渗透灌水水重新充电的半核液压条件下的井间空间分离,由渗流水浸出咸土壤充电的无凝结条件下的井。因此,不同的水类型和盐度值是复杂的,并且可以使用AQQA和统计分析来识别和空间上分离。

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