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10.1016/J.ALGAL.2019.101431

The model predicts that annual open pond algae cultivation to produce 1000 T biomass would require 17–20 ha at Mesa, AZ, 45–56 ha at Medicine Hat, AB, 57–68 ha at Fort Saskatchewan, AB and 71–80 ha at Great Slave Lake, NWT.

Novel satellite based analytical model developed to predict microalgae yields in open pond raceway systems and applied to Canadian sites

10.1016/J.PRECAMRES.2018.11.012

The East Arm basin of Great Slave Lake formed during this period and preserves a protracted record of sedimentation and volcanism in the southeastern Slave craton.

Athapuscow aulacogen revisited: Geochronology and geochemistry of the 2046 Ma Union Island Group mafic magmatism, East Arm of Great Slave Lake, Northwest Territories, Canada

10.1002/etc.4368

We modeled fish in 6 Canadian lakes (Great Slave Lake, Lake Ontario, Source Lake, Happy Isle Lake, Lake Opeongo, and Lake Memphremagog) to identify the factors that cause the BAFs of differently sized lake trout to vary between and within lakes.

Model-based exploration of the variability in lake trout (Salvelinus namaycush) bioaccumulation factors: The influence of physiology and trophic relationships.

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10.1371/journal.pone.0221361

A subarctic fish community in mine-impacted Yellowknife Bay (Great Slave Lake, Northwest Territories, Canada) was investigated for biological and ecological processes controlling arsenic bioaccumulation.

Arsenic bioaccumulation in subarctic fishes of a mine-impacted bay on Great Slave Lake, Northwest Territories, Canada

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Slave Lake - The model predicts that annual open pond algae cultivation to produce 1000 T biomass would require 17–20 ha at Mesa, AZ, 45–56 ha at Medicine Hat, AB, 57–68 ha at Fort Saskatchewan, AB and 71–80 ha at Great Slave Lake, NWT. [1] The East Arm basin of Great Slave Lake formed during this period and preserves a protracted record of sedimentation and volcanism in the southeastern Slave craton. [2] We modeled fish in 6 Canadian lakes (Great Slave Lake, Lake Ontario, Source Lake, Happy Isle Lake, Lake Opeongo, and Lake Memphremagog) to identify the factors that cause the BAFs of differently sized lake trout to vary between and within lakes. [3] A subarctic fish community in mine-impacted Yellowknife Bay (Great Slave Lake, Northwest Territories, Canada) was investigated for biological and ecological processes controlling arsenic bioaccumulation. [4]

Great Slave Lake

The model predicts that annual open pond algae cultivation to produce 1000 T biomass would require 17–20 ha at Mesa, AZ, 45–56 ha at Medicine Hat, AB, 57–68 ha at Fort Saskatchewan, AB and 71–80 ha at Great Slave Lake, NWT. [1] The East Arm basin of Great Slave Lake formed during this period and preserves a protracted record of sedimentation and volcanism in the southeastern Slave craton. [2] We modeled fish in 6 Canadian lakes (Great Slave Lake, Lake Ontario, Source Lake, Happy Isle Lake, Lake Opeongo, and Lake Memphremagog) to identify the factors that cause the BAFs of differently sized lake trout to vary between and within lakes. [3] A subarctic fish community in mine-impacted Yellowknife Bay (Great Slave Lake, Northwest Territories, Canada) was investigated for biological and ecological processes controlling arsenic bioaccumulation. [4]