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Orthogonal Variance Structures in Lake Water Quality Data and Their Use for Geo-chemical Classification of Dimictic, Glacial/Boreal Lakes

机译:湖泊水质数据中的正交方差结构及其在干冰,冰川/北方湖泊的地球化学分类中的应用

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摘要

The accumulating volumes of data collected within environmental monitoring programs facilitate the use of exploratory statistical methods of data analysis as a supplement to traditional methods of characterizing lake water quality. When principal component analysis and multidimensional scaling are applied to a matrix containing approximately 24000 samples of lake water quality variables pH, alkalinity, conductivity, hardness, color, Secchi depth and total phosphorus concentration, it is found that the total matrix variance can be approximately reproduced in an orthogonal two-dimensional base with transformations of hardness and color as best principal component representatives. This base is suggested as an empirical lake classification standard where the variance structure of subset lake populations (such as single lakes) can be referenced to the water quality standard of the generic population. Since the principal axes of the base exclusively contain inorganic and organic related variables respectively, the combined inorganic/organic characteristics of the lake can be expressed with the hardness and color variables alone. With the data matrix being large enough to produce high significance levels, and with variable ranges wide enough to represent a majority of dimictic, glacial/boreal lakes, the analysis results should be valid in many lakes throughout the world.
机译:在环境监测计划中收集的数据量不断累积,促进了对数据分析的探索性统计方法的使用,以此作为表征湖泊水质的传统方法的补充。当对包含大约24000个湖泊水质变量pH,碱度,电导率,硬度,颜色,Secchi深度和总磷浓度的样品进行主成分分析和多维缩放时,发现总基质方差可以近似再现在正交的二维基数中,以硬度和颜色的转换为最佳主成分代表。该基础被建议作为经验湖分类标准,其中子湖人口(例如单个湖泊)的方差结构可以参考普通人口的水质标准。由于碱的主轴分别专门包含无机和有机相关变量,因此仅用硬度和颜色变量即可表示色淀的无机/有机组合特征。由于数据矩阵足够大,可以产生较高的显着性水平,而可变范围又足够宽,可以代表大多数的微粉,冰川/北方湖泊,因此分析结果在世界各地的许多湖泊中都应是有效的。

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