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Assessment of seasonal variations in stream water by principal component analysis

机译:通过主成分分析评估溪流水的季节性变化

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Assessment of seasonal changes in surface water is an important aspect for the interpretation of hydrochemical data. Thirteen physical and chemical parameters monitored at four sampling stations along the Corbeira stream, NW Spain, were analyzed during a three-year period. The Corbeira stream drains a rural catchment (16 Km~2) with low population density. The land use consists mainly of forested and agricultural land. The geological material is basic schist. A total of 51 samples were collected from each station. The principal component analysis (PCA) technique was used to evaluate the seasonal correlations of water quality parameters. Four principal components, accounting for 88.7 and 83.3% of the total variances of information contained in the original dataset for spring and winter, respectively, were obtained. In summer and autumn, three principal components accounted for 80.3 and 81.1% of the total variance, respectively. The results revealed that conductivity, chloride, magnesium, sulphate and nitrate were always the most important variables contributing to water physical-chemical properties in the stream for all seasons. The first three can be interpreted as a mineral component of the stream water. This clustering of variables points to a common origin for these minerals, most likely from an alteration of schist, whereas nitrates may be interpreted as representing influences from natural (decomposition of organic matter from soils) and anthropogenic inputs. Autumn and winter (periods with high water discharge) showed a strong influence of dissolved organic carbon (DOC) and total nitrogen (Kjeldahl), respectively. This finding could be due to surface runoff.
机译:评估地表水的季节性变化是解释水化学数据的重要方面。在三年的时间内,分析了西班牙西北部Corbeira溪沿四个采样站监测的13个物理和化学参数。科尔贝拉河流失了人口密度低的农村集水区(16 Km〜2)。土地用途主要包括林地和农业用地。地质材料是基本片岩。每个站共收集了51个样品。主成分分析(PCA)技术用于评估水质参数的季节相关性。获得了四个主要成分,分别占原始数据集中的春季和冬季信息的总方差的88.7和83.3%。在夏季和秋季,三个主要成分分别占总方差的80.3%和81.1%。结果表明,电导率,氯化物,镁,硫酸盐和硝酸盐始终是影响所有季节溪流中水物理化学性质的最重要变量。前三个可以解释为溪流水中的矿物质成分。这些变量的聚集指向这些矿物的共同起源,很可能是片岩的改变,而硝酸盐可能被解释为代表来自自然(土壤中有机物的分解)和人为输入的影响。秋季和冬季(排水量高的时期)分别显示出对溶解有机碳(DOC)和总氮(凯氏定氮)的强烈影响。这一发现可能是由于地表径流造成的。

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