新南威尔士州南部内陆湿地管理指引。

S. Briggs
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引用次数: 3

摘要

新南威尔士州内陆的湿地分为两大类——主要河流泛滥的湿地和当地集水区泛滥的湿地。从主要河流中淹没的湿地有时可以从水文角度加以控制。它们的水位可以由堰或特殊的放水装置来控制。这篇短文为新南威尔士州南部内陆湿地的水文管理提供了一些指导方针,这些湿地的供水是可以控制的。进一步的资料载于说明末尾所列的文件和报告中。新南威尔士州南部内陆的湿地通常在冬末或春季自然泛滥。夏季洪水是罕见的。这些湿地不一定每年都被洪水淹没,有时它们会被淹没几年。洪水的模式和持续时间取决于集水区降水的数量和时间、蒸发和洪泛区湿地的海拔高度。储存和释放供下游使用的水通常会改变湿地的水文状况。夏季洪水变得更加频繁,根据湿地的位置,洪水的持续时间可能会增加,中等洪水的频率可能会减少(Briggs 1988a)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Guidelines for management of inland wetlands in southern New South Wales.
Wetlands in inland New South Wales fall into two broad categories – those flooded from major rivers and those flooded from local catchments. Wetlands flooded from major rivers can sometimes be manipulated hydrologically. Their water levels may be controlled by weirs or by special water releases. This short note provides some guidelines for hydrological management of inland wetlands, whose water supply can be controlled, in southern New South Wales. Further information is contained in the papers and reports listed at the end of the note. Wetlands in southern inland New South Wales usually flood naturally in late winter or spring. Summer floods are uncommon. These wetlands do not necessarily flood every year, and they sometimes stay inundated for a few years. Pattern and duration of flooding depend on amount and timing of catchment precipitation, evaporation and the elevation of the wetland on the floodplain. Storage and release of water for downstream use usually alter wetland hydrological regimes. Summer flooding frequently becomes more common, and duration of inundation may increase or frequency of medium floods decrease depending on wetland location (Briggs 1988a).
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