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The identification of lake types using macrophyte community composition in Ireland

机译:利用爱尔兰大型植物群落组成识别湖泊类型

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The recent EU requirement to use macrophytes to monitor the status of lakes necessitates the separation of lakes into types in order to partition natural variability. This allows ecological change to be detected more easily (CEC 2000, Refcond 2003). Many factors are known to influence macrophytes; however, the main determinants, at least for macrophyte richness, have been identified as alkalinity and transparency (Vestergaard & Sand-Jensen 2000). Environmental boundaries of types are often set using discriminant analysis of biological groupings of reference sites (sites minimally affected by anthropogenic activity) (Clarke et al. 2003). With limited availability of reference lakes, discriminant equations may be more descriptive of the sample rather than the lake population as a whole. One approach may be to place boundaries to types at positions of natural change in the environment or at positions of biological relevance. The principal factors affecting macrophytes, alkalinity and light penetration, may be open to this. Large differences in alkalinity may be found between limestone and siliceous catchments, owing to the higher weathering rate of limestone (Johnson et al. 1994). The exponential decline of light in water may allow a boundary to be placed at a zone of rapid change.
机译:欧盟最近对使用大型植物监测湖泊状况的要求使得有必要将湖泊分成不同的类型,以便划分自然变异性。这样可以更容易地发现生态变化(CEC 2000,Refcond 2003)。已知许多因素会影响大型植物。然而,至少对于大型植物丰富度而言,主要决定因素是碱度和透明度(Vestergaard&Sand-Jensen 2000)。通常使用对参考位点(受人为活动影响最小的位点)的生物学分组的判别分析来设置类型的环境界限(Clarke等人,2003年)。由于参考湖泊的可用性有限,判别方程可能更能说明样本,而不是整个湖泊人口。一种方法可能是在环境中自然变化的位置或生物学相关的位置为类型设置边界。影响大型植物,碱度和透光度的主要因素对此可能是开放的。由于石灰石的风化率较高,因此在石灰岩和硅质流域之间可能会发现碱度差异很大(Johnson等,1994)。水中的光指数下降可以使边界位于快速变化的区域。

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