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Variability of groundwater table, atmospheric precipitation and temperature in swamp habitats of the Zielonka Forest Landscape Park

机译:Zielonka森林景观公园的沼泽生境中地下水位,大气降水和温度的变化

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Results of a study carried out in the Zielonka Forest Landscape Park (central Wielkopolska, middle part of the Warta River catchment) are presented in this paper. The park includes part of a large (15 thousand ha) forest complex called Zielonka Forest. The name pertains to relatively large and dense forest area with small agricultural enclaves situated c. 8 km north-east of Pozna??. Park's landscape of the young glacial type, Pleistocene and Holocene formations, was formed as a result of the Pozna?? stage of the Baltic glaciation. Dominating habitat types in the park are: fresh mixed deciduous forest (58%), fresh mixed coniferous forest (25%), fresh broadleaved forest (10%), alder and ash-alder swamp forests (4%).Analysis of thermal conditions and precipitations was performed for the years 2002-2007 and compared with long-term data from 1987-2007. Annual mean air temperature in the hydrologic year 2003 was lower by 10% than the long-term mean while in the years 2007, 2006 and 2002 it was higher by 29, 9 and 8%, respectively. Low air temperature in the year 2003 was the effect of cold winter. In the summer half-year the temperature was definitely above the mean. Hydrologic year 2003 was the coldest but also the driest (64% of the long-term mean) year in the study period. Variability of ground water tables in swamp habitats was measured in the hydrologic years 2002-2007. During this period the ground water table depth varied from 38 to 181 cm below ground. Mean lowest stages (116 cm below ground) were noted in the hydrologic year 2006 (with the minimum level of 52 cm and maximum 178 cm below ground). The lowest ground water table (181 cm below ground) was, however, noted in 2003 in an experimental plot of the division 85f. The year 2003 was also characteristic for the largest annual amplitude of ground water depths. Obtained results confirm the decisive effect of air temperatures and sums of atmospheric precipitation on ground water table depth in forest swamp habitats. Surprisingly, there was no expected difference in the ground water depth between hydrologic years of extremely different atmospheric precipitations. Smaller variability of ground water level with increasing depth known from the literature was not confirmed either.
机译:本文介绍了在Zielonka森林风景公园(位于Warta河流域中部Wielkopolska中部)进行的研究结果。该公园包括称为Zielonka森林的大型(15,000公顷)森林综合体的一部分。该名称适用于相对较大且茂密的森林地区,其中c坐落着小型农业飞地。波兹纳东北8公里??。公园的年轻冰川类型的景观是更新世和全新世形成的,是波兹纳的结果?波罗的海冰川化阶段。公园中主要的栖息地类型为:鲜混落叶林(58%),鲜混针叶林(25%),鲜阔叶林(10%),al木和灰-沼泽森林(4%)。 2002-2007年进行了降水,并与1987-2007年的长期数据进行了比较。 2003年水文学年的年平均气温比长期平均值低10%,而在2007年,2006年和2002年,年平均气温分别升高了29%,9%和8%。 2003年气温低是冬季寒冷的影响。在夏季半年中,温度肯定高于平均温度。在研究期间,2003年的水文学年最冷,但也是最干旱的(长期平均值的64%)。在2002-2007年的水文年中,对沼泽生境中地下水位的变化进行了测量。在此期间,地下水位深度在地下38到181厘米之间。在2006年的水文学年中,记录了平均最低阶段(地下116厘米)(最低水平为52厘米,最大地下为178厘米)。但是,2003年在分区85f的实验区中注意到了最低的地下水位(地下181 cm)。 2003年也是每年地下水深度最大振幅的一年。获得的结果证实了气温和大气降水总量对森林沼泽生境中地下水位深度的决定性影响。令人惊讶的是,在大气降水极为不同的水文年之间,地下水深度没有预期的差异。文献中还没有证实随着深度的增加,地下水位的变化较小。

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