Water Typology in the Amazon: Close Correlation with the Hydrogeochemistry of River Basins

None Aprile F., None Darwich A. J., None Siqueira G. W.
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Abstract

A study on the typology of Amazonian waters was developed in the North Geographic Region of Brazil, considering a set of historical data from 1995 to 2022. The objective was to discuss and point out which environmental parameters are considered preponderant within the classification criteria of Amazonian waters. Historical data on temperature, density, pH, conductivity, oxygen, transparency, light attenuation, turbidity, color, total and dissolved solids, hardness, alkalinity, CaCO3, BOD, COD, main cations and anions, iron, C, N and P fractions, silicate, trace elements (Al, Cu, Zn and Mn) and chlorophyll a were analyzed. The analysis comprised water samples from the National Hydrometeorological Network (Sub-Basins 10 to 19), with a total of 36 basins, including tributaries, lakes and adjacent streams. The historical series was statistically analyzed through the techniques of Cluster, Principal component analysis (PCA), Piper Diagram and image interpolation by the ordinary kriging method. The results indicated a strong seasonal trend, with an evident distinction between the flood and ebb periods. The typology of white, black and clear waters was also evidenced, this last group being an intermediate class to the others, due to the physical-chemical standards. The PCA highlighted the parameters conductivity, pH, calcium, bicarbonate and Dissolved inorganic carbon (DIC) (Factor 1), and turbidity and alkalinity (Factor 2) as preponderant in the water classification. The ionic balance demonstrated that the white waters stood out for the highest concentrations of calcium and magnesium. The results suggest a pattern of calcic waters oscillating towards sodic and carbonated waters, with a subgroup in the northern eastern region of seasonally sodic-chlorinated waters, due to the influence of ocean tides. Image interpolation suggested a predominance of white waters in the western southern zone (Western Amazon) and white waters transitioning to clear waters in the eastern zone (Eastern Amazon). The analysis also showed a predominant strip of black and clear waters in the northern zone, and a strip of white waters in the central Amazon.
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亚马逊河流域的水类型:与流域水文地球化学密切相关
基于1995 - 2022年的一组历史数据,在巴西北部地理区域开展了一项亚马逊水域类型学研究。目的是讨论和指出在亚马逊水域的分类标准中哪些环境参数被认为是占优势的。分析了温度、密度、pH、电导率、氧气、透明度、光衰减、浊度、颜色、总固形物和溶解固形物、硬度、碱度、CaCO3、BOD、COD、主要阳离子和阴离子、铁、C、N和P组分、硅酸盐、微量元素(Al、Cu、Zn和Mn)和叶绿素a的历史数据。该分析包括来自国家水文气象网络(子流域10至19)的水样,共有36个流域,包括支流、湖泊和邻近溪流。采用聚类分析、主成分分析、派珀图和克里格法图像插值等方法对历史序列进行统计分析。结果显示出强烈的季节性趋势,在涨潮期和退潮期之间有明显的区别。白色,黑色和清澈的水的类型也得到了证明,由于物理化学标准,最后一组是其他类型的中间类。PCA强调了电导率、pH、钙、碳酸氢盐和溶解无机碳(DIC)(因子1)以及浊度和碱度(因子2)在水分类中的优势。离子平衡表明,白色的海水中钙和镁的浓度最高。结果表明,由于潮汐的影响,钙水向钠水和碳酸水振荡,其中一个亚群位于季节性钠氯化水的东北地区。图像插值表明,西部南部地区(西亚马逊河流域)以白水为主,东部地区(东亚马逊河流域)白水向清澈过渡。分析还显示,北部地区主要是一片黑色和清澈的水域,而亚马逊中部则是一片白色的水域。
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