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Changing the geometry of basins and water resources of Lakes Gop?o and Ostrowskie under the influence of anthropopressure

机译:人为压力的影响下改变戈普湖和奥斯特罗夫斯基湖盆地和水资源的几何形状

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The paper presents the changes that have occurred in the morphometry of Lakes Gop?o and Ostrowskie, which are locatedin central Poland. The analysis covered the period characterised by increased human interference into the water cycle, which hasbeen taking place continually since the mid-eighteenth century. On the basis of available cartographic materials (aerial photographs,topographic maps, bathymetric charts of the lakes) and the authors’ own field measurements digital terrain models were developedfor the immediate environment of the surveyed lakes. These models, in turn, were used for measuring basic parameters characterisingthe external dimensions of the lakes (surface area, length and maximum width, shoreline length) and their underwater relief (volume,maximum and average depth). In addition, the selected indicators of the shape and form of the lake basins were determined. The resultsshowed a drastic reduction of water resources of the two lakes. The basin of Lake Gop?o covers only the deepest parts of the formerreservoir, accounting for only 23.3% of the lake before 1772, and 32.5% of its former volume. In the case of Lake Ostrowskie the surfacearea and volume decreased, respectively, by 23.5% (74.9 ha) and 21.3% (6 695 000 m3). Such large changes in surface area and volume ofboth lakes have contributed to significant changes in other morphometric parameters and indicators. In particular, significant changeswere observed in relation to such morphometric characteristics as length and maximum width, as well as average and maximum depth.
机译:本文介绍了位于波兰中部的Gop?o湖和Ostrowskie湖的形态发生的变化。分析涵盖了自18世纪中叶以来一直在不断增加的人类对水循环的干扰这一时期。根据可用的制图材料(航空照片,地形图,湖泊的测深图)和作者自己的野外测量,为被调查的湖泊的直接环境开发了数字地形模型。反过来,这些模型被用来测量表征湖泊外部尺寸(表面积,长度和最大宽度,海岸线长度)及其水下浮雕(体积,最大和平均深度)的基本参数。此外,确定了湖盆的形状和形式的选定指标。结果表明,两个湖泊的水资源急剧减少。戈普湖湖盆仅覆盖了前水库的最深部分,仅占1772年之前湖水的23.3%,占湖水总量的32.5%。对于Ostrowskie湖,其表面积和体积分别减少了23.5%(74.9公顷)和21.3%(6 695 000立方米)。两个湖泊的表面积和体积的如此大的变化,导致其他形态参数和指标的显着变化。特别地,观察到与诸如长度和最大宽度以及平均和最大深度的形态特征有关的显着变化。

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