阿尔伯塔省三条主要河流对河流流态的水质响应

IF 2.4 4区 环境科学与生态学 Q2 WATER RESOURCES Water Quality Research Journal Pub Date : 2020-02-01 DOI:10.2166/wqrj.2019.033
S. Rostami, Jianxun He, Q. Hassan
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引用次数: 1

摘要

人类活动和自然因素对河流水的数量和质量都有影响,而人类活动经常被认为是造成水质时间退化的原因。此外,河流水质表现出年际/季节变化,年际变化往往比年际变化更为突出。水质的年内变化引起了管理者和决策者的注意,这就提出了一个问题,即如何在更精确的时间分辨率下更好地管理河流水质。自然因素,特别是水文气象变量,可能是河流水质年际变化的主要驱动因素。因此,本文研究了河流水质与一个水文气象变量(流量)之间的关系,重点研究了它们在年内时间尺度上的关系,选择了加拿大阿尔伯塔省的三条河流。结果表明,流量总体上驱动了河流水质的年内变化。此外,一些水质参数在三种流量(低、中、高流量)下对流量有明显的响应。根据其对水流的响应,将水质参数分为8类。这些都暗示了水质管理的挑战,同时为如何制定更有效的水管理策略提供了见解。
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Water quality response to river flow regime at three major rivers in Alberta
Both anthropogenic activities and natural factors affect river water in quantity and quality, while anthropogenic activities have been often blamed to cause water quality temporal degradation. In addition, riverine water quality displays intra-annual/seasonal variations, which are often more prominent than inter-annual variations. The intra-annual variations in water quality, which are attracting the attention of managers and policy-makers, beg the question of how to better manage riverine water quality at a finer time resolution. The natural factors, in particular, the hydro-meteorological variables, could be the primary drivers of the intra-annual variations of riverine water quality. Therefore, this paper examined the association between riverine water quality and one hydro-meteorological variable (flow) with the focus on their relationship at the intra-annual timescale on three selected rivers in Alberta, Canada. The results demonstrated that flow drives intra-annual variation of riverine water quality in general. Moreover, some water quality parameters responded to flow distinctively at three flow regimes (low, medium, and high flows). Water quality parameters were categorized into eight groups according to their responses to flow at the flow regimes. These implied the challenges in water quality management while providing insight into how to formulate more effective water management strategies.
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CiteScore
4.50
自引率
8.70%
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0
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