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A GEOMORPHOLOGICAL MODELLING APPROACH FOR LANDSCAPE EVOLUTION ANALYSIS OF THE MACQUARIE MARSHES, AUSTRALIA

机译:澳大利亚麦格理沼地景观演化分析的地貌模拟方法

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The Macquarie Marshes is a complex wetland system declared of international importance because of its biodiversity and variety of ecosystems. This 2000 Km~2 wetland contains important River Red Gum forests and woodlands, but it has been experiencing a rapid ecological degradation over the last decades. Previous studies have determined that the main cause of degradation is the reduction of input discharges due to water allocations for domestic, agriculture and industrial use. Such decline in flows tends to increase sediment deposition, decreasing the channel capacity and causing vegetative invasion which ultimately leads to channel breakdown. While channel breakdown is not necessarily detrimental to wetland development, under certain conditions it may lead to a complete avulsion and ultimately disconnect and rearrange the river network. This could result in abandonment of whole wetland areas. Such cases have been documented in the Macquarie Marshes. Simulation of geomorphological changes in the wetlands is fundamental for accomplishing long-term management under an ecogeomorphological framework. Water allocation decisions must also consider the environment as users of water. Numerical modelling of this type of systems is a challenging task because even though the landscape evolution processes occur over large time scales (decennial to centennial), they originate from smaller time scale processes such as erosion and deposition. This paper presents a preliminary analysis of a five months flood event simulation and its effects on the geomorphology of the Northern region of the Macquarie Marshes. The model used to achieve these results is CAESAR-Lisflood, which couples a geomorphic landscape evolution model (LEM) with a simplified 2D hydrodynamic flow model. Results obtained are compared to measured inundation maps and discharge data for assessing the model capabilities. Also, patterns of erosion-deposition in floodplain and channels, channel migration and channel breakdown are analyzed.
机译:由于其生物多样性和各种生态系统,麦格理沼泽是一家复杂的湿地系统,宣称国际重要性。今年2000公里〜2湿地含有重要的河流红胶森林和林地,但它在过去几十年中一直经历了快速的生态退化。以前的研究已经确定,由于国内,农业和工业用水划分,劣化的主要原因是减少输入排放。这种流动的下降往往会增加沉积物沉积,降低信道容量并导致营养侵袭,最终导致通道崩溃。虽然渠道故障并不一定对湿地发展不一定,但在某些条件下可能导致完全撕脱并最终断开并重新排列河流网络。这可能导致遗弃整个湿地区域。这些案件已在麦克里沼泽中记录。湿地的地貌变化模拟是在生态神经晶体框架下实现长期管理的基础。水分配决策还必须考虑环境作为水的用户。这种类型的系统的数值建模是一个具有挑战性的任务,因为即使景观演变过程在大型时间尺度(二聚体到百年)上发生,它们也来自较小的时间尺度过程,例如侵蚀和沉积。本文提出了对五个月的洪水事件模拟及其对麦格泥沼泽北部地区的几何的影响初步分析。用于实现这些结果的模型是Caesar-Lisflood,其用简化的2D流体动力学模型耦合着地貌景观演化模型(LEM)。将获得的结果与测量的淹没映射和放电数据进行比较,以评估模型能力。此外,分析了洪泛区和通道中的侵蚀沉积模式,通道迁移和通道故障。

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