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Spatio-Temporal Variation and Controlling Factors of Water Quality in Yongding River Replenished by Reclaimed Water in Beijing, North China

机译:华北地区再生水对永定河补充水质的时空变化及其控制因素

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Reclaimed water is useful for replenishing dried up rivers in North China, although changes in water quality could be an issue. Therefore, it is essential to understand the spatio-temporal variation and the controlling factors of water quality. Samples of Yongding River water were collected seasonally, and 24 water quality parameters were analyzed in 2015. All waters were alkaline, and nitrate-nitrogen was the main form of nitrogen, while phosphorus was mostly below detection level. The water quality parameters varied in time and space. Cluster analysis showed a distinct difference between winter and the other seasons and between the natural river section and the section with reclaimed water. Based on the analysis of Gibbs plots, principal component analysis, and ionic relationships, the water chemistry was controlled by dissolution of rocks in natural river section, the quality of replenished water, the effects of dilution, and the reaction of aqueous chemistry in the reclaimed water section. The positive oxidation environment in most of the river water was conducive to the formation of nitrate-nitrogen by nitrification, and not conducive to denitrification.
机译:尽管水质的变化可能是一个问题,但再生水可用于补充华北干旱的河流。因此,了解时空变化和水质控制因素至关重要。永定河水质按季节采集,并在2015年分析了24个水质参数。所有水均为碱性,硝酸盐氮是氮的主要形式,而磷含量大多低于检测水平。水质参数随时间和空间变化。聚类分析表明,冬季与其他季节之间以及天然河段与再生水段之间存在明显差异。在分析吉布斯图,主成分分析和离子关系的基础上,通过天然河段中岩石的溶解,补充水的质量,稀释的影响以及再生中的水化学反应来控制水化学。水部分。大多数河水中的正氧化环境有利于硝化作用形成硝酸盐氮,而不利于反硝化作用。

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