期刊
ENVIRONMENTAL RESEARCH LETTERS
卷 8, 期 2, 页码 -出版社
IOP Publishing Ltd
DOI: 10.1088/1748-9326/8/2/025006
关键词
permafrost thaw; active layer; resource exploration; linear disturbances; peatlands
资金
- Canadian Foundation for Climate and Atmospheric Sciences
- Natural Sciences and Engineering Research Council
- Denedeh Resources Committee
- Dehcho First Nations
- Fort Simpson Metis Local [52]
- Liidlii Kue First Nation
- Village of Fort Simpson
Within the zone of discontinuous permafrost, linear disturbances such as winter roads and seismic lines severely alter the hydrology, ecology, and ground thermal regime. Continued resource exploration in this environment has created a need to better understand the processes causing permafrost thaw and concomitant changes to the terrain and ground cover, in order to efficiently reduce the environmental impact of future exploration through the development of best management practices. In a peatland 50 km south of Fort Simpson, NWT, permafrost thaw and the resulting ground surface subsidence have produced water-logged linear disturbances that appear not to be regenerating permafrost, and in many cases have altered the land cover type to resemble that of a wetland bog or fen. Subsidence alters the hydrology of plateaus, developing a fill and spill drainage pattern that allows some disturbances to be hydrologically connected with adjacent wetlands via surface flow paths during periods of high water availability. The degree of initial disturbance is an important control on the extent of permafrost thaw and thus the overall potential recovery of the linear disturbance. Low impact techniques that minimize ground surface disturbance and maintain original surface topography by eliminating windrows are needed to minimize the impact of these linear disturbances.
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