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Assessment of Wetland Hydrological Dynamics in a Modified Catchment Basin: Case of Lake Buninjon, Victoria, Australia

机译:改良集水盆地的湿地水文动力学评估:以澳大利亚维多利亚州的布宁洪湖为例

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摘要

The common method to estimate lake levels is the water balance equation, where water input and output result in lake storage and water level changes. However, all water balance components cannot always be quickly assessed, such as due to significant modification of the catchment area. A method that assesses general changes in lake level can be a useful tool in examining why lakes have different lake level variation patterns. Assessment of wetlands using the dynamics of the historical hydrological and hydrogeological data set can provide important insights into variations in wetland levels in different parts of the world. A case study from a saline landscape, Lake Buninjon, Australia, is presented. The aim of the present study was to determine how climate, river regime, and lake hydrological properties independently influence lake water levels and salinity, leaving the discrepancy, for the effect of the non-climatic/ catchment modification in the past and the model shows that surface inflow is most sensitive variable. The method, together with the analysis and interpretation, might be of interest to wider community to assess its response to natural/anthropogenic stress and decision choices for its ecological, social, scientific value, and mitigation measures to safe guard the wetland biodiversity in a catchment basin.
机译:估算湖泊水位的常用方法是水平衡方程,其中水的输入和输出导致湖泊蓄水和水位变化。但是,由于集水区的重大变化,不能总是快速评估所有水平衡成分。评估湖泊水位总体变化的方法可能是检查湖泊为何具有不同湖泊水位变化模式的有用工具。利用历史水文和水文地质数据集的动态对湿地进行评估,可以对世界不同地区的湿地水平变化提供重要的见解。本文介绍了一个来自澳大利亚布宁洪湖盐碱地带的案例研究。本研究的目的是确定气候,河流状况和湖泊水文特性如何独立地影响湖泊水位和盐度,从而消除差异,以适应过去的非气候/集水区改造的影响,该模型表明表面流入是最敏感的变量。该方法以及分析和解释,可能会引起更广泛的社区的兴趣,以便评估其对自然/人为压力的反应以及生态,生态,社会,科学价值的决策选择以及缓解措施,以保护流域的湿地生物多样性盆地。

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