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Leaving the beaten track - Approaches beyond the Venice System to classify estuarine waters according to salinity

机译:离开人迹罕至的地方-威尼斯系统以外的方法,根据盐度对河口水进行分类

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The Venice System is one of the best-known and most applied systems to classify waters with respect to salinity. It has often been subject to criticism because the criteria used to derive zone boundaries were not made explicit. Consequently, an alternative multivariate PCA method that aimed at identifying salinity zones by means of the salinity ranges preferred by species was introduced by Bulger et al. (1993). We tested the applicability of both methods using salinity and benthic macroinvertebrate data for the poikilohaline Elbe Estuary (Germany) from 1997 to 2012. This was done by comparing the resultant salinity zone limits from the two approaches with boundaries where significant community changes were found by means of cluster analysis. Only the Venice System polyhaline and limnetic zone boundaries, and the PCA method outer estuary zone limit, showed good agreement with the benthic community pattern. None of the other Venice System or PCA method zone limits reflected the benthic community patterns. Our findings suggest that zone limits can only be well determined from mean salinity at the inner and outer end of the estuary, where the variation of salinity is relatively low. In contrast, in the middle of the estuary variation in salinity is the better predictor of zone boundaries. Thus, application of the Venice System or the PCA method in poikilohaline estuaries, such as the Elbe, is not meaningful and their use should be limited to homoiohaline systems. For poikilohaline systems, we found cluster analysis to be a better tool to identify salinity-zone boundaries.
机译:威尼斯系统是对盐度进行水域分类的最著名和最常用的系统之一。由于未明确指出用于导出区域边界的标准,因此经常受到批评。因此,Bulger等人引入了另一种多元PCA方法,该方法旨在通过物种偏爱的盐度范围来识别盐度带。 (1993)。我们使用盐度和底栖大型无脊椎动物数据测试了两种方法在Poikilohaline Elbe河口(德国)从1997年至2012年的适用性。这是通过比较两种方法所产生的盐度带限制(通过界线发现显着的群落变化)进行的。聚类分析。只有威尼斯系统的多卤水和围岩带边界以及PCA方法的外河口带界限显示出与底栖动物群落的良好一致性。威尼斯系统或PCA方法的其他区域限制都没有一个反映底栖生物群落模式。我们的发现表明,只能通过盐度变化相对较低的河口内外端的平均盐度来很好地确定区域界限。相反,在河口中部,盐度变化是区域边界的更好预测因子。因此,将威尼斯系统或PCA方法应用于诸如易北河之类的波基洛哈林河口是没有意义的,应将其使用仅限于高碘海盐系统。对于poikilohaline系统,我们发现聚类分析是识别盐度带边界的更好工具。

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