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A combined hydrochemical-statistical analysis of Saq aquifer, northwestern part of the Kingdom of Saudi Arabia

机译:沙特阿拉伯王国西北部的Saq含水层的水化学统计综合分析

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The present study includes detailed hydrochemical assessment of groundwater resources of Saq aquifer. The Saq aquifer covers a large area (about 375,000 km(2)) and lies in the arid region with low annual rainfall and extremely high evaporation. In the study area, groundwater serves as the major source for agricultural activity and for domestic usages. A total of 295 groundwater samples collected and were analyzed for physico-chemical parameters such as hydrogen ion concentration (pH), total dissolved solids (TDS) and electrical conductivity (EC), sodium (Na+), potassium (K+), magnesium (Mg2+), and calcium (Ca2+), bicarbonate (HCO3) chloride (Cl-), sulfate (SO4 (2-)) and nitrate (NO3). The goal and challenge for the statistical overview was to delineate chemical distributions in a complex, heterogeneous set of data spanning over a large geographic range. After de-clustering to create a uniform spatial sample distribution with 295 samples, histograms and quantile-quantile (Q-Q) plots were employed to delineate subpopulations that have coherent chemical affinities. The elements showing significantly higher positive correlation are: TDS with EC; Ca with EC, TDS; Mg and EC, TDS, Ca, K; Cl and EC, TDS, Mg, Na, Ca; SO4 and EC, TDS, Ca, Cl, Na, Mg. The distribution of major ions in the groundwater is Na+ > Ca++ > Mg++ > K+ and Cl- > SO4 (-2)> HCO3 (-)> NO3 (-). Ionic abundance plot of alkalis with Ca and Mg is suggestive of mix type trends of concentrations as evident by moderate correlation (r = 0.57). About 60% of the total samples have alkalis abundance and rests have more Ca + Mg concentrations than alkalis. Taking both results of cluster tree and geochemical features of variables into consideration, the authors classify the elements into two major groups, the first includes TDS, Na, EC, Cl, Ca, SO4, and Mg, where the relationship within the group are strong. The second group includes K, HCO3, pH, and NO3. This group has close relationship with group 1 demonstrate that, the increase in the concentration to some elements could be the same. Some of the analyzed parameters approach a normal distribution, as both their skewnesses and kurtoses reach close to "0". The study revealed that, all of the element pairs exhibit positive relations.
机译:本研究包括Saq含水层地下水资源的详细水化学评估。 Saq含水层覆盖面积大(约375,000 km(2)),位于干旱地区,年降雨量低,蒸发量极高。在研究区域,地下水是农业活动和家庭使用的主要来源。总共收集了295个地下水样品,并对其理化参数进行了分析,例如氢离子浓度(pH),总溶解固体(TDS)和电导率(EC),钠(Na +),钾(K +),镁(Mg2 + ),钙(Ca2 +),碳酸氢盐(HCO3)氯化物(Cl-),硫酸盐(SO4(2-))和硝酸盐(NO3)。统计概述的目标和挑战是在跨越大地理范围的复杂,异构数据集中描绘化学分布。在去聚类以创建具有295个样本的均匀空间样本分布之后,使用直方图和分位数-分位数(Q-Q)图来描绘具有相干化学亲和力的子种群。显示出明显更高的正相关的元素是:TDS与EC; Ca与EC,TDS;镁和EC,TDS,Ca,K; Cl和EC,TDS,Mg,Na,Ca; SO4和EC,TDS,Ca,Cl,Na,Mg地下水中主要离子的分布为Na +> Ca ++> Mg ++> K +和Cl-> SO4(-2)> HCO3(-)> NO3(-)。碱金属与钙和镁的离子丰度图表明浓度的混合类型趋势由中度相关性证实(r = 0.57)。总样品中约60%的碱含量高,其余样品的Ca + Mg浓度高于碱。考虑到聚类树的结果和变量的地球化学特征,作者将元素分为两个主要组,第一类包括TDS,Na,EC,Cl,Ca,SO4和Mg,其中组内的关系很强。第二组包括K,HCO3,pH和NO3。该组与第1组有密切关系,表明某些元素的浓度增加可能是相同的。一些分析的参数接近正态分布,因为它们的偏度和kurtoses都接近“ 0”。研究表明,所有元素对都表现出正相关。

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