退化的波罗的海沼泽水位波动的多样性

F. Duda, E. Woźniak, Katarzyna Jereczek-Korzeniewska, Roman Cieślińsk
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引用次数: 1

摘要

摘要本文的目的是呈现退化的波罗的海沼泽水位波动的多样性。我们试图回答这个问题,即在每个物体内部和两个彼此靠近的物体之间波动的多样性有多强。此外,还分析了水位对大气降水的响应速度和值。本文的空间范围涵盖了Łeba河谷下部的两个波罗的海高地沼泽:Czarne Bagno和Łebskie Bagno。时间范围为2012-2014年。研究发现,这两个分析的沼泽在地下水位变化方面具有很高的动态性。地下水位的年波动幅度在28.4至77.9厘米(Łebskie Bagno)和45.6至105.0厘米(Czarne Bagno)之间。据观察,这两个泥炭地的水位总是在夏季下降,而在秋季上升,一直持续到春季。泥炭地的蓄水和水位主要影响降水。使其不那么明显的极端气象条件是由诸如沼泽不同部分的位置或退化类型等因素造成的变化。
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Diversity of water level fluctuations in degraded Baltic raised bogs
Abstract The aim of paper is to present the diversity of water level fluctuations in degraded Baltic raised bogs. An attempt was made to answer the question how strong the diversity of fluctuations is both within each object and between two objects situated close to each other. Moreover, speed and value of the response of water level to atmospheric precipitation were analysed. The spatial scope of the paper covers two Baltic raised bogs in the lower part of the Łeba river valley: Czarne Bagno and Łebskie Bagno. The time scope covers years 2012-2014. The study found that both analysed bogs were a high dynamic in variation of groundwater level. Annual amplitudes of fluctuations in the water table was in the range of 28.4 to 77.9 cm (Łebskie Bagno) and of 45.6 to 105.0 cm (Czarne Bagno). It has been observed that lowering the water level on both peatlands always been recorded in the summer months, whilst the increase in the autumn, which lasted until spring. Retention and the water level on peatlands influenced primarily precipitation. Extreme meteorological conditions that make it less conspicuous is the variation resulting from factors such as location in different parts of the bog or type of degradation.
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