Dynamics of vegetation changes in oil and salt-contaminated oligotrophic ridge-hollow mire complexes after reclamation (Middle Pre-Ob region, Khanty-Mansi Autonomous Okrug – Yugra)

E. Shishkonakova
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Abstract

Oligotrophic ridge-hollow and ridge-hollow-pool complex mires are widely distributed in the central part of West Siberia, including many oil fields of the Middle Pre-Ob region. The article considers the dynamics of re-vegetation of oil and salt-contaminated areas of these mire types subjected to reclamation. Survey materials for 2–3 years and 15 years after reclamation allow to identify the main trends in vegetation restoration in the short and medium term. The reversible oligotrophication of ridges manifests in a relative decrease in the participation of the meso-eutrophic species on contaminated mire sites. In the hollows, however, the similar trend can be traced only in relation to oil-contaminated sites, whereas in the salt-contaminated hollows, the strong eutrophic conditions last. In the medium-term perspective, most typical oligotrophic hollow species, with the exception of Eriophorum russeolum and Oxycoccus palustris, were unable to recover. In the course of dynamic changes in the vegetation, the leading role in recovery successions gradually passes to mesotrophic and eutrophic species possessing massive root systems and aerenchyma – Eriophorum angustifolium, Phragmites australis, Carex rostrata, etc. Restoration of the moss layer is several years behind that of the grass layer, and due to the lack of competition, the participation of liverworts in it is of great importance, especially in salt spills. At the same time, among mosses as in the case of vascular species mesotrophic components are the main dominant ones15 years after reclamation.
开垦后油盐污染寡营养脊-空泥沼复区植被变化动态(汉曼自治区-尤格拉腊前鄂中部)
西西伯利亚中部广泛分布着贫营养型脊-空和脊-空-池复合矿,包括前鄂中地区的许多油田。本文研究了这些泥沼类型的油盐污染区复垦后的植被恢复动态。填海后2-3年和15年的调查资料可以确定短期和中期植被恢复的主要趋势。山脊的可逆性少营养化表现为中富营养化物种对污染泥沼的参与相对减少。然而,在凹陷中,类似的趋势只能追溯到与石油污染有关的地点,而在盐污染的凹陷中,强烈的富营养化条件持续存在。从中期来看,大多数典型的寡营养空心物种,除了Eriophorum russeolum和palustris氧球菌,都无法恢复。在植被的动态变化过程中,恢复演替的主导作用逐渐向具有大量根系和通气组织的中营养型和富营养型物种转移,如Eriophorum angustifolium、Phragmites australis、Carex rostrata等。苔藓层的恢复比草层的恢复要晚几年,由于缺乏竞争,苔类植物的参与是非常重要的,特别是在盐溢出的情况下。与此同时,开垦15年后,在苔藓中,维管束种中营养成分是主要的优势成分。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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