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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Numerical analysis of hydrogeochemical data: a case study (Alto Guadalentin, southeast Spain)
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Numerical analysis of hydrogeochemical data: a case study (Alto Guadalentin, southeast Spain)

机译:水文地球化学数据的数值分析:一个案例研究(西班牙东南部的Alto Guadalentin)

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This study examines the spatial variability of the factors obtained from the application of correspondence analysis to a hydrogeochemical data set. The goal was to synthesize the hydrogeochemical information using this multivariate statistical technique, by setting a series of factors which clarified the main properties of one aquifer. Then, a geostatistical framework to obtain a probabilistic assessment of groundwater quality was established. Experimental and theoretical semivariograms of the selected factors, considered as regionalized variables, were computed. These variographic information and factor values in the experimental sites were used in the ordinary kriging, which provides unbiased and linear estimates of the regionalized variables. These estimates were used to compile maps of the chosen factors, which explain their spatial distribution. The selected case study was the alluvial aquifer of Alto Guadalentin which is situated in southeast Spain, in the Internal Zones of Betic Cordilleras. These waters are chiefly SO4 and Cl types, but HCO3 facies are common in the central sector of the basin. High temperature, acid pH, problems of overexploitation and pollution by CO2-gas characterise these waters. Available groundwater quality monitoring data were used to calibrate the numerical model. The present study focused on setting the main physical and chemical attributes and establishing the spatial pattern of groundwater quality and the temporal changes in this pattern. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 18]
机译:这项研究检查了将对应分析应用于水文地球化学数据集而获得的因素的空间变异性。目的是通过设置一系列阐明一个含水层主要性质的因素,使用这种多元统计技术来综合水文地球化学信息。然后,建立了获取地下水质量概率评估的地统计学框架。计算选定因素的实验和理论半变异函数,将其视为区域变量。在普通克里金法中,使用了实验现场的这些变率信息和因子值,从而提供了区域变量的无偏线性估计。这些估计值用于编制所选因素的地图,以解释其空间分布。选定的案例研究是Alto Guadalentin的冲积含水层,它位于西班牙东南部的Betic Cordilleras内部区域。这些水域主要是SO4和Cl类型,但HCO3相在盆地中部很常见。这些水的特征是高温,酸性pH,过度开采和二氧化碳气体污染的问题。可用的地下水水质监测数据用于校准数值模型。本研究的重点是设定主要的物理和化学属性,建立地下水水质的空间格局以及该格局的时间变化。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:18]

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