Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1139/cjes-2020-0134 |
Cryostratigraphical studies of ground ice formation and distribution in a High Arctic polar desert landscape, Resolute Bay, Nunavut | |
Paquette, Michel; Fortier, Daniel; Lamoureux, Scott F. | |
通讯作者 | Paquette, M |
来源期刊 | CANADIAN JOURNAL OF EARTH SCIENCES
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ISSN | 0008-4077 |
EISSN | 1480-3313 |
出版年 | 2023 |
卷号 | 59期号:11页码:759-771 |
英文摘要 | Ground ice distribution and abundance have wide-ranging effects on periglacial environments and possible impacts on climate change scenarios. In contrast, very few studies measure ground ice in the High Arctic, especially in polar deserts and where coarse surficial material complicates coring operations. Ground ice volumes and cryostructures were determined for eight sites in a polar desert, near Resolute Bay, Nunavut, chosen for their hydrogeomorphic classification. Dry, unvegetated polar desert sites exhibited ice content close to soil porosity, with a <45 cm thick ice-enriched transition zone. In wetland sites, suspended cryostructures and ice dominated cryofacies (ice content at least 2x soil porosity values) were prevalent in the upper similar to 2 m of permafrost. Average ground ice saturation at those locations exceeded porosity values by a factor between 1.8 and 20.1 and by up to two orders of magnitude at the similar to 10 cm vertical scale. Sites with the highest ice contents were historically submerged wetlands with a history of sediment supply, sustained water availability, and syngenetic and quasi-syngenetic permafrost aggradation. Ice enrichment in those environments were mainly caused by the strong upward freezing potential beneath the thaw front, which, combined with abundant water supply, caused ice aggradation and frost heaving to form lithalsa plateaus. Most of the sites already expressed cryostratigraphic evidence of permafrost degradation. Permafrost degradation carries important ecological ramifications, as wetland locations are the most productive, life-supporting oases in the otherwise relatively barren landscape, carrying essential functions linked with hydrological processes and nutrient and contaminant cycling. |
英文关键词 | ground ice polar desert permafrost Arctic geocryology geomorphology |
类型 | Article |
语种 | 英语 |
开放获取类型 | Green Accepted |
收录类别 | SCI-E |
WOS记录号 | WOS:001081158100002 |
WOS关键词 | FOSHEIM PENINSULA ; ACTIVE-LAYER ; HYDROLOGICAL PROCESSES ; CORNWALLIS-ISLAND ; ELLESMERE-ISLAND ; PERMAFROST ; COAST ; THERMOKARST ; TERRAIN ; CARBON |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/395635 |
推荐引用方式 GB/T 7714 | Paquette, Michel,Fortier, Daniel,Lamoureux, Scott F.. Cryostratigraphical studies of ground ice formation and distribution in a High Arctic polar desert landscape, Resolute Bay, Nunavut[J],2023,59(11):759-771. |
APA | Paquette, Michel,Fortier, Daniel,&Lamoureux, Scott F..(2023).Cryostratigraphical studies of ground ice formation and distribution in a High Arctic polar desert landscape, Resolute Bay, Nunavut.CANADIAN JOURNAL OF EARTH SCIENCES,59(11),759-771. |
MLA | Paquette, Michel,et al."Cryostratigraphical studies of ground ice formation and distribution in a High Arctic polar desert landscape, Resolute Bay, Nunavut".CANADIAN JOURNAL OF EARTH SCIENCES 59.11(2023):759-771. |
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