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TitleWinter hydraulic pressures observed in water bodies and riparian settings, north Slave, subarctic Canadian Shield
AuthorSladen, W E; Morse, P DORCID logo; Wolfe, S AORCID logo
Source2018 Yellowknife Geoscience Forum, abstract and summary volume; Northwest Territories Geological Survey, Yellowknife Geoscience Forum Abstract and Summary Volume 2018, 2018 p. 120-121 Open
Access logo Open Access
LinksOnline - En ligne (complete volume - volume complet, pdf, 1.32 MB)
Alt SeriesNatural Resources Canada, Contribution Series 20180261
PublisherNorthwest Territories Geological Survey
Meeting46th Annual Yellowknife Geoscience Forum; Yellowknife, NT; CA; November 20-22, 2018
Mediapaper; on-line; digital
File formatpdf
ProvinceNorthwest Territories
NTS85I/13; 85I/14; 85P/03; 85P/04; 85P/05; 85P/06
AreaTibbitt to Contwoyto Winter Road
Lat/Long WENS-114.0000 -113.0000 63.5000 62.7500
Subjectshydrogeology; Transport; Nature and Environment; ice; permafrost; groundwater; transportation; pressure; temperature; surface waters; streams; lakes; hydrologic environment; hydraulic analyses; meteorology; water levels; Canadian Shield; geological hazards; icings; infrastructures; overflows; active layer; riparian zones
ProgramClimate Change Geoscience, Permafrost
Released2018 11 01
AbstractIce and all-weather roads are critical lifelines for northern communities and resource development activities. Icings are sheet-like masses of layered ice that form on the surface during the winter by freezing of successive overflows of water. Icing development over ice and all-weather roads negatively impacts their performance, and there can be adverse effects on bridges and culverts. Consequently, icings are an ongoing maintenance and safety problem in northern regions. The mechanism controlling overflow timing and behaviour is poorly understood. Overflow timing and stream bed water pressures have been linked to air temperature fluctuations in several regions, but the relation between these two signals is not well defined and the mechanism is unknown. The Shield region contains the highest density of resource development infrastructure in the Northwest Territories, much of which is supported by the Tibbitt to Contwoyto Winter Road (TCWR). The main operational difficulty faced by operators on the overland portions of the TCWR is overflow and icing. The objective of this work is to provide much needed geoscientific insight on the icing process, in order to reduce risks for land-based transportation infrastructure.
Overflows in the subarctic Canadian Shield may be controlled by periodic increases in hydraulic head during open-system freezing. Local observations at the TCWR Portage 23 (P23) overland section have shown that overflow occurs during the period of active-layer freezeback when it is likely hydrologically connected to the upstream lake. Based on our previous work at P23, we installed vertical series of pressure transducers and temperature data loggers to determine the relations between barometric pressure, air temperature, water/ice temperatures, and water/ice pressures during the freezing season. To examine variation in hydrological setting, replicate apparatus were installed in a shallow lake, the lake outlet, and in the riparian zone downstream of the outlet where icing has been observed.
Initial results suggest that during the freezing-season, high frequency fluctuation of absolute pressure in the lake is driven entirely by barometric pressure, with no detectable increase with snow loading. At the outlet, hydraulic pressures behaved similarly to lake pressures. Absolute pressures at the downstream sensors also fluctuated at high frequency with barometric pressure. However, in contrast to the lake and outlet sites, hydraulic pressure increased by up to 2.2 kPa over a two-week period that followed freezing onset. Hydraulic pressures gradually tapered off from peak values until freezing occurred at depth.
The static water level observed at the lake and outlet suggests that the lake is either an entirely open system with water entering and exiting the lake at the same rate over the winter, or alternatively, that the lake is entirely closed with respect to water flow. The latter is supported by our observation of decreasing hydraulic pressures at the downstream site. The initial increase in hydraulic pressures observed at the downstream site indicate the semi-confined nature of the freezing riparian area. Further signal analysis is being undertaken to investigate the effects of freezing front progression on hydraulic pressure at the downstream site.
Summary(Plain Language Summary, not published)
Natural Resources Canada (NRCan) conducted an experiment to measure hydraulic pressures in water bodies and riparian settings to gain insight into the winter process of water overflow in the Subarctic Canadian Shield. NRCan installed pressure and temperature data loggers to determine the relations between barometric pressure, air temperature, water/ice temperatures, and water/ice pressures during the freezing season. This poster presents the initial results from this experiment.

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