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Published byVirginia Underwood Modified over 6 years ago
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Tracking the Laurentide – On the trail of the last great ice sheet
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Deglaciation – a lot of melt water
Deglaciation – a lot of melt water. The terrestrial record of glacial meltwater
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Con Mine, Yellowknife, Canada:
Glacial meltwater in the Canadian Shield Con Mine, Yellowknife, Canada: Clark, I.D., Douglas, M., Raven, K. and Bottomley, D.J., Recharge and preservation of glacial meltwater in the Canadian Shield. Ground Water, 38:
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Con Mine, Yellowknife
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Geochemistry of groundwaters
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Groundwaters Cl– (mg/L) d18O ‰ VSMOW -30 -25 -20 -15 -10 1 10 100 1000
10,000 100,000 1,000,000 -30 -25 -20 -15 -10 d18O ‰ VSMOW
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Modern Glacial Cl– (mg/L) meltwater ? Brine d18O ‰ VSMOW
10 Modern 100 Glacial meltwater ? Cl– (mg/L) 1000 Modern – Brine binary mixing line 10,000 Brine 100,000 -30 -25 -20 -15 -10 d18O ‰ VSMOW
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How to recharge glacial meltwater . . .
Late Pleistocene time: Laurentide Ice Sheet Shield brine in bedrock
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Early Holocene deglaciation:
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Mid to late Holocene:
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Mining activities:
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Finite difference modelling with SWIFT II
Stationary margin of Laurentide ice sheet Proglacial Lake McConnell 2000 1000 Salinity gradients after 50 yrs Depth (m) 50% brine 60% brine 70% brine 80% brine 90% brine Distance (km)
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Con Mine, Yellowknife East Bull Lake
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d2H d2H d18O d18O d2H d2H d18O d18O East Bull Lake Ottawa Chalk River
-120 -100 -80 -60 -130 -110 -90 -70 -120 -100 -80 -60 d2H d2H East Bull Lake Ottawa d18O d18O -17 -15 -13 -11 -9 d2H d2H Chalk River Trois Rivières d18O d18O -17 -15 -13 -11 -9
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Source: GSC
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Deep Geologic Repository for Nuclear Waste
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d18O in formation pore waters
glacial meltwater basin brine
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Glacial Meltwater
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The Younger Dryas Cold Period
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