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首页> 外文期刊>Journal of Hydrology >Salinity and turbidity distributions in the Brisbane River estuary, Australia
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Salinity and turbidity distributions in the Brisbane River estuary, Australia

机译:澳大利亚布里斯班河河口的盐度和浊度分布

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摘要

The Brisbane River estuary (BRE) in Australia not only plays a vital role in ecosystem health, but is also of importance for people who live nearby. Comprehensive investigations, both in the short- and long-term, into the salinity and turbidity distributions in the BRE were conducted. Firstly, the analysis of numerical results revealed that the longitudinal salinity varied at approximately 0.45 and 0.61 psu/h during neap and spring tides, respectively. The turbidity stayed at a higher level and was less impacted by tide in the upper estuary, however, the water cleared up while the tide changed from flood to ebb in the mid and lower estuary. The second investigation into the seasonal variations of salinity and turbidity in the BRE was conducted, using ten-year field measurement data. A fourth-order polynomial equation was proposed, describing the longitudinal variation in salinity dilution changes as the upstream distance in the BRE during the wet and dry seasons. From the observation, the mid and upper estuaries were vertically well-mixed during both seasons, but the lower BRE was stratified, particularly during the wet season. The estuary turbidity maximum (ETM) zone was about 10 km longer during the wet season than the dry season. Particular emphasis was given to the third investigation into the use of satellite remote sensing techniques for estimation of the turbidity level in the BRE. A linear relationship between satellite observed water reflectance and surface turbidity level in the BRE was validated with an R-2 of 0.75. The application of satellite-observed water reflectance therefore provided a practical solution for estimating surface turbidity levels of estuarine rivers not only under normal weather conditions, but also during flood events. The results acquired from this study are valuable for further hydrological research in the BRE and particularly prominent for immediate assessment of flood impacts. (C) 2014 Elsevier B.V. All rights reserved.
机译:澳大利亚的布里斯班河河口(BRE)不仅在生态系统健康方面发挥着至关重要的作用,而且对于居住在附近的人们也很重要。对BRE中的盐度和浊度分布进行了短期和长期的综合研究。首先,对数值结果的分析表明,在春季和春季潮汐期间,纵向盐度分别变化为约0.45和0.61 psu / h。上河口的浊度保持在较高的水平,受潮汐的影响较小,但是,在河口的中下游,潮汐从洪水变为退潮时,水被清除了。使用十年的现场测量数据,对BRE中盐度和浊度的季节性变化进行了第二次调查。提出了一个四阶多项式方程,描述了盐度稀释度的纵向变化随干湿季节在BRE中上游距离的变化而变化。根据观察,在两个季节中,河口中部和上部河口垂直混合良好,但下部BRE分层,特别是在雨季。在雨季,河口最大浊度(ETM)区比旱季长约10 km。特别强调了第三次调查,该调查涉及使用卫星遥感技术估算BRE中的浊度水平。在BRE中,卫星观测到的水反射率与表面浊度之间的线性关系得到了验证,R-2为0.75。因此,卫星观测水反射率的应用为估算河口河流的表面浊度水平提供了一种实用的解决方案,不仅在正常天气条件下,而且在洪水事件期间。从这项研究中获得的结果对于BRE的进一步水文研究非常有价值,对于立即评估洪水影响尤其重要。 (C)2014 Elsevier B.V.保留所有权利。

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