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TURBIDITY DISTRIBUTION IN THE BRISBANE RIVER ESTUARY DURING THE 2010-2011 QUEENSLAND FLOODS

机译:2010-2011昆士兰洪水中布里斯班河口旱地浊度分布

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The turbidity distribution within the Brisbane River estuary during the January 2011 flood event was investigated using a validated numerical model. The Brisbane River estuary turbidity maximum zone (ETM) generally extended throughout the mid- estuary under normal weather conditions. However, the turbidity distribution was significantly changed during the January 2011 flood events, from a high-low-high pattern of turbidity distribution to a gradual increasing pattern from upstream to downstream within the estuary. The ETM zone disappeared but the turbidity approached approximately 2000 NTU. In addition, it was found that the flood impact on sediment transport in the estuary was more significant than the tidal effects. An estimated 1,000,452 tonnes of sediment were delivered into Moreton Bay through the Brisbane River mouth during the January 2011 floods. These outcomes will be further applied to develop Moreton Bay models, thereby investigating the sediment settling in the coastal area following the flood and will also be used to inform the implementation of catchment management strategies.
机译:使用经过验证的数值模型研究了2011年1月洪水事件中布里斯班河口洪水事件中的浊度分布。布里斯班河河口浊度最大区(ETM)通常在正常天气条件下整个河口中延伸。然而,在2011年1月的洪水事件中,浊度分布从高低的浊度分布到河口内部下游的逐渐增加模式,从高低高的浊度分布变化。 ETM区域消失但浊度接近了大约2000 NTU。此外,发现河口对沉积物运输的洪水影响比潮汐效应更大。估计的1,000,452吨沉积物通过布里斯顿河口在2011年1月洪水洪水中送入Moreton湾。这些结果将进一步适用于开发Moreton湾模型,从而调查洪水后沿海地区的沉积物沉积,并将用来为实施集水管理策略提供信息。

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