排水对Aukštumala上升沼泽植被覆盖和水文的影响(立陶宛西部)

L. Jarašius, D. Matuleviciute, R. Pakalnis, J. Sendžikaitė, Vaidotas Lygis
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引用次数: 2

摘要

自1995年以来,三分之一的前Aukstumala沼泽(立陶宛西部)已被保护为沼泽保护区,而其余领土仍处于活跃的工业泥炭开采或废弃的泥炭收获田。本研究于2013年开展,旨在评估人类对Aukstumala抬高沼泽植物覆盖结构和水文的长期影响。在植被评价(Twinspan分析)的基础上,确定了四种生境类型:i)活跃的凸起沼泽,ii)由沟渠排水的退化凸起沼泽,iii)沼泽与泥炭矿区的接触区和iv)最近被烧毁的地区。对植被覆盖的人为影响最大的是沟渠排水退化的抬高沼泽和焚烧区,其中非典型植物种类占营养型抬高沼泽的比例最高。水电导率与沼泽水位呈负相关(r = -0.57), pH值与沼泽水位相关性较弱(r = -0.38)。活跃性抬高沼泽的水位显著高于其他3种生境类型。活跃的凸起沼泽的电导率值明显低于退化的凸起沼泽和燃烧区栖息地。为了重建泥炭积累和沼泽生态系统自然功能的有利条件,平均沼泽水位应至少提高到-32厘米(大多数典型的营养型物种的最佳水位在-20 - -32厘米范围内)。
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Drainage Impact on Plant Cover and Hydrology of Aukštumala Raised Bog (Western Lithuania)
Abstract One-third of the former Aukstumala raised bog (western Lithuania) has been preserved as Telmological Reserve since 1995, while the remaining territory is still under active industrial peat mining or are abandoned peat harvesting fields. The present study was carried out in 2013 and aimed to assess long-term human impact on the structure of plant cover and hydrology of Aukstumala raised bog. On the basis of vegetation assessment (Twinspan analysis), four habitat types were identified: i) active raised bog, ii) degraded raised bog drained by ditches, iii) contact zone of the bog and the peat mining fields and iv) recently burnt areas. The largest anthropogenic impact on vegetation cover was found in the degraded raised bog drained by the ditches and in the burnt area, where the proportion of plant species atypical to ombrotrophic raised bogs was the highest. Water electrical conductivity negatively correlated (r = -0.57) with bog water level, whereas correlation between pH and bog water level was weaker (r = -0.38). Water level in the active raised bog was significantly higher than in the rest three habitat types. Electrical conductivity values in the active raised bog were significantly lower compared to the degraded raised bog and burned area habitats. In order to recreate favourable conditions for peat accumulation and natural functioning of bog ecosystem, mean bog water level should be raised at least up to -32 cm (the optimum water level assigned for most of the typical ombrotrophic species fell into the range of -20 - -32 cm).
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