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A HIGH ARCTIC HYDROLOGICAL STUDY USING STABLE ISOTOPES, CORNWALLIS ISLAND, CANADA

机译:加拿大科恩威利斯群岛使用稳定同位素进行的高纬度水文研究

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Large areas of Canada's Northwest Territories receive fluxes of organic aerosols from external sources via the Arctic haze phenomenon. On Cornwallis Island, a well defined 25 km~2 drainage basin (latitude 75°03'N, longitude 93°50'W) focused around a 0.38 km~2 lake informally named 'Amituk Lake' was selected for a multi-year, multidisciplinary study which is attempting to trace the post-depositional migration of these compounds in the local environment. The calculation of an accurate water balance for this basin is an important component of the study. During the 1994 summer field season an effort was made to determine the significance of groundwater contributions (a previously uninvestigated parameter) to this flow system. An ~(18)O and ~2H sampling programme combined with a physical measurement regimen was undertaken to achieve this objective.
机译:加拿大西北地区的大部分地区都通过北极雾霾现象从外部来源接收有机气溶胶的通量。在康沃尔利斯岛(Cornwallis Island)上,选择了一个定义明确的25 km〜2流域(北纬75°03'N,东经93°50'W),该流域围绕着一个非正式命名为“ Amituk Lake”的0.38 km〜2湖,历时多年,多学科研究正在试图追踪这些化合物在当地环境中的沉积后迁移。为该流域计算准确的水平衡是该研究的重要组成部分。在1994年夏季的田间季节,人们努力确定了地下水对该流系统的贡献(以前未研究的参数)的重要性。进行了〜(18)O和〜2H采样程序并结合了物理测量方案,以实现此目标。

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