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Hydrological changes and ecological impacts associated with water resource development in large floodplain rivers in the Australian tropics

机译:澳大利亚热带泛滥平原河道中与水资源开发相关的水文变化和生态影响

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摘要

The majority of rivers in the Australian tropics possess near-natural flow regimes and are an ecological asset of global significance. We examined flow variability in large floodplain rivers in the Gulf of Carpentaria, northern Australia, and the potential ecological impacts of future water resource development (WRD). Flow metrics based on long-term records were used to classify flow regimes and predict hydrological drivers of ecological function. Flow regimes of selected rivers were then compared with those simulated for pre- and post-WRD flows in the Darling River, a highly modified river in Australia's south-east. Generally, rivers were classified as typically 'tropical' (more permanent, regular flows) or 'dryland' (more ephemeral, with greater flow variability). In addition, all rivers displayed wet-dry seasonality associated with changes in flow magnitude or number of zero-flow days. We propose that these features (flow permanence and regularity; flow variability and absence; wet-dry seasonality) are the key hydrological drivers of biodiversity and ecological function in the floodplain rivers of Australia's north. In terms of WRD, inter-annual flow variability was predicted to increase or decrease depending on rivers' natural flow regimes, specifically their tendency toward lower or higher flow magnitudes. Either outcome is expected to have adverse effects on the biodiversity and ecological function of these relatively pristine rivers and floodplain habitats. In particular, reduced and homogenised habitat, loss of life-history cues, inhibited dispersal and shifts in community composition, as a result of WRD, threaten the ecological integrity of rivers adapted to the three hydrological drivers above. These findings serve as a caution for careful consideration of water resource development options for rivers in the Australian tropics and for those with similar flow regimes the world over.
机译:澳大利亚热带地区的大多数河流都具有近乎自然的流动状态,是具有全球意义的生态资产。我们研究了澳大利亚北部卡彭塔里亚湾大洪泛区河流的流量变化以及未来水资源开发(WRD)的潜在生态影响。基于长期记录的流量指标用于对流量状况进行分类并预测生态功能的水文驱动因素。然后,将所选河流的水流状况与模拟的WRD前后在澳大利亚东南部高度改良的河流达令河中的流量进行了比较。通常,河流被分为典型的“热带”(更持久,规则的流量)或“旱地”(更短暂的流量,更大的流量可变性)。此外,所有河流都表现出干流季节性变化,与流量大小或零流量天数的变化有关。我们认为,这些特征(水流的持久性和规律性;水流的变化性和缺失性;干湿季节性)是澳大利亚北部洪泛河中生物多样性和生态功能的关键水文驱动因素。就WRD而言,预计年际流量变异性会根据河流的自然流量状态,特别是其趋向于较低或较高流量的趋势而增加或减少。预期任何结果都会对这些相对原始的河流和洪泛区生境的生物多样性和生态功能产生不利影响。特别是由于WRD,栖息地的减少和均质化,生活史线索的丧失,散布和群落组成的变化受到抑制,威胁了适应上述三种水文驱动因素的河流的生态完整性。这些发现为谨慎考虑澳大利亚热带河流以及世界范围内具有类似流量制度的河流的水资源开发选择提供了警告。

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  • 作者

    Leigh Catherine; Sheldon Fran;

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  • 年度 2008
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  • 原文格式 PDF
  • 正文语种 English
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