首页> 外文期刊>Arctic: Journal of the Arctic Institute of North America >Environmental conditions and vegetation recovery at abandoned drilling mud sumps in the Mackenzie Delta region, Northwest Territories, Canada
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Environmental conditions and vegetation recovery at abandoned drilling mud sumps in the Mackenzie Delta region, Northwest Territories, Canada

机译:加拿大西北地区麦肯齐三角洲地区废弃钻井泥浆池的环境条件和植被恢复

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Historical data from oil and gas exploration in the delta of the Mackenzie River, Northwest Territories, in the 1970s provided an opportunity to estimate decadal-scale impacts of exploratory oil and gas drilling on native plant communities in low Arctic tundra. We assessed changes in vegetation composition and associated environmental gradients across seven drilling mud sumps in the Kendall Island Bird Sanctuary, Mackenzie Delta. Three decades after disturbance, drilling sumps had developed vegetation coverage equivalent to that in undisturbed areas, although bare soil persisted in ponded areas and where a salt crust was present. Vegetation on sumps was composed of communities dominated by forbs, grasses, and tall shrubs that were distinct from adjacent, undisturbed sedge and low shrub communities. The area of altered vegetation around a sump was generally larger in upland or saline environments than in lowland areas. Pooled water observed around many sumps was likely associated with thaw subsidence that occurred following construction, which was subsequently compounded by snow drifting and increased soil temperatures along the margins of the sump mound. Changes in drainage, active-layer depth, and surface salt concentrations appear to be key environmental factors that have helped shape plant communities established on drilling sumps in the three decades after disturbance.
机译:1970年代西北地区麦肯齐河三角洲的油气勘探历史数据提供了一个机会,可以估算在北极苔原低地上勘探油气钻探对原生植物群落的年代际影响。我们评估了麦肯奇三角洲肯德尔岛鸟类保护区的七个钻井泥浆池中植被组成和相关环境梯度的变化。扰动后的三十年,尽管在池塘区域和存在盐结皮的地方仍存在裸露的土壤,但钻探坑的植被覆盖率却与未受干扰的地区相当。污水坑上的植被由以灌木,草和高灌木为主的群落组成,这些群落不同于相邻,不受干扰的莎草和低灌木群落。在高地或盐碱环境中,集水坑周围的植被变化面积通常比低地地区大。在许多集水坑周围观察到的积水很可能与施工后发生的融化沉降有关,随后由于积雪漂移和沿土坑丘缘的土壤温度升高而加剧。排水,活性层深度和表面盐分浓度的变化似乎是关键的环境因素,这些因素已帮助塑造了在扰动后的三十年中在钻井池上建立的植物群落。

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