Water & Climate Impact Research Centre, Environment and Climate Change Canada, University of Victoria, Canada.
Water & Climate Impact Research Centre, Environment and Climate Change Canada, University of Victoria, Canada.
Sci Total Environ. 2016 Nov 1;569-570:634-646. doi: 10.1016/j.scitotenv.2016.06.151. Epub 2016 Jul 2.
There is a great deal of interest to determine the state and variations of water quality parameters in the lower Athabasca River (LAR) ecosystem, northern Alberta, Canada, due to industrial developments in the region. As a cold region river, the annual cycle of ice cover formation and breakup play a key role in water quality transformation and transportation processes. An integrated deterministic numerical modelling framework is developed and applied for long-term and detailed simulation of the state and variation (spatial and temporal) of major water quality constituents both in open-water and ice covered conditions in the lower Athabasca River (LAR). The framework is based on the a 1D and a 2D hydrodynamic and water quality models externally coupled with the 1D river ice process models to account for the cold season effects. The models are calibrated/validated using available measured data and applied for simulation of dissolved oxygen (DO) and nutrients (i.e., nitrogen and phosphorus). The results show the effect of winter ice cover on reducing the DO concentration, and a fluctuating temporal trend for DO and nutrients during summer periods with substantial differences in concentration between the main channel and flood plains. This numerical frame work can be the basis for future water quality scenario-based studies in the LAR.
由于该地区的工业发展,确定加拿大艾伯塔省北部下阿萨巴斯卡河(LAR)生态系统中水质参数的状态和变化具有重要意义。作为一条寒冷地区的河流,冰盖的形成和破裂的年度循环对水质转化和传输过程起着关键作用。本文开发并应用了一个综合的确定性数值建模框架,用于长期和详细模拟在下阿萨巴斯卡河(LAR)的开阔水域和冰盖条件下主要水质成分的状态和变化(时空)。该框架基于一维和二维水动力和水质模型,并与一维河流冰过程模型外部耦合,以考虑寒冷季节的影响。该模型使用可用的实测数据进行校准/验证,并应用于溶解氧(DO)和养分(即氮和磷)的模拟。结果表明,冬季冰盖会降低 DO 浓度,并且 DO 和养分在夏季会呈现波动的时间趋势,主河道和洪泛区之间的浓度存在显著差异。该数值框架可以为未来下阿萨巴斯卡河基于情景的水质研究提供基础。