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Optical Properties of Polish Lakes: The Secchi Disc Transparency

机译:波兰湖泊的光学特性:Secchi光盘透明度

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The spatial variation of water transparency of the largest Polish lakes was presented on the basis of documentary material collected by the Voivodeship Inspectorates for Environment Protection as well as university geography departments in the period of 1991-2013. Seasonal results of the Secchi disc measurements (spring, summer) for 706 lakes were gathered. This is more than 68% of the total number of Polish lakes with a surface area larger than 50 ha. The mean water transparency of these lakes was 1.87 m, while the median was 1.58 m. Distinct inter-regional differences of the Secchi disc transparency were found, and it was also possible to distinguish three relatively homogeneous groups of macroregions where lakes have different optical characteristics. They can be divided into areas with lakes with high (3.05 m), medium (1.99-2.11 m) and low (1.22-1.52 m) water transparency. The Secchi disc transparency of these lakes was also analysed in relation to concentration values of the main forms of the optically significant constituents of water (coloured dissolved organic matter, suspended matter). The mean transparency of turbid, stained and clear lakes was, respectively, 1.16, 2.02, and 2.92 m. Moreover, regional empirical models to predict Secchi disc transparency from chlorophyll a concentration were also developed. It was assumed that inter-regional differences between models could be due to the probably different time of the ice sheet recession. The influence of the lake morphometry was most fully reflected in the impact of the depth conditions.
机译:根据环境保护省监察局和大学地理部门在1991-2013年期间收集的文献资料,介绍了波兰最大的湖泊水透明度的空间变化。收集了706个湖泊的Secchi圆盘测量的季节性结果(春季,夏季)。这占表面积大于50公顷的波兰湖泊总数的68%以上。这些湖泊的平均水透明度为1.87 m,中位数为1.58 m。发现Secchi圆盘透明度的区域间差异明显,并且还可以区分湖泊具有不同光学特性的三个相对均匀的宏观区域组。它们可以分为湖泊水透明度高(3.05 m),中等(1.99-2.11 m)和低(1.22-1.52 m)的区域。还对这些湖泊的Secchi圆盘透明度进行了分析,并与水的光学重要组成部分(有色溶解有机物,悬浮物)的主要形式的浓度值有关。浑浊,沾染和澄澈的湖泊的平均透明度分别为1.16、2.02和2.92 m。此外,还建立了从叶绿素a浓度预测Secchi盘透明度的区域经验模型。假定模型之间的区域间差异可能是由于冰盖衰退的时间可能不同。湖泊形态的影响最充分地反映在深度条件的影响上。

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