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Estimating groundwater-river connectivity factor for quantifying changes in irrigation return flows in the Murray-Darling Basin

机译:估算地下水 - 河流连通因子,用于量化默里达格盆地灌溉返回流动的变化

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Concerns have been raised that the use of infrastructure and water efficiency projects to recover water entitlements for the environment in the Murray-Darling Basin (MDB) could be undermined by a reduction in return flows to rivers. Water use efficiency changes prior to 2009 had already reduced surface return flows. A dimensionless and normalised variable, connectivity factor (CF), has been used to analyse the cumulative impact on river flow from actions that alter groundwater recharge or extraction. CF is objectively estimated from existing modelling outputs for three large alluvial groundwater systems in south-eastern MDB relevant to a major water use efficiency program. Lower values of CF(0.05-0.45) imply lower reductions of return flows, less impacts on recovered water entitlements, with impacts more likely to be managed adaptively within current water management plans. The study should help allay concerns by explaining why previous estimates had been overly high.
机译:令人关切的是,利用基础设施和水效项目来恢复默里 - 达令盆地(MDB)中的环境的水权利可能会因河流的回报而减少而受到破坏。 2009年之前的用水效率变化已经降低了表面返回流量。无量纲和归一化的变量,连接因子(CF)已被用于分析从改变地下水充电或提取的动作的河流流动的累积影响。客观地从东南MDB中的三个大型冲积地下水系统的现有建模输出估计了CF,与主要的用水效率计划相关。 CF的较低值(0.05-0.45)意味着降低回报流量,对回收的水权益的影响较少,影响更有可能在当前的水管理计划内自适应管理。该研究应通过解释以前估计过高的原因,帮助追随担忧。

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