scholarly journals Model documentation for relations between continuous real-time and discrete water-quality constituents in the North Fork Ninnescah River upstream from Cheney Reservoir, south-central Kansas, 1999--2009

2013 ◽  
pp. i-101
Author(s):  
Mandy L. Stone ◽  
Jennifer L. Graham ◽  
Jackline W. Gatotho
Keyword(s):  
Water Quality ◽  
Real Time ◽  
The North ◽  
South Central ◽  
North Fork

Terrain Geochemistry Surveys, Permafrost Studies, and Arctic Limnology, District of Keewatin, N.W.T.: Implications for Water Quality Monitoring in the North

1987 ◽  
Vol 22 (4) ◽  
pp. 505-517
Author(s):  
Tom W.D. Edwards ◽  
R.A. Klassen ◽  
W.W. Shilts
Keyword(s):  
Water Quality ◽  
Lake Sediments ◽  
Mineral Exploration ◽  
Surface Water Quality ◽  
Water Quality Monitoring ◽  
Quality Monitoring ◽  
The North ◽  
South Central ◽  
Geochemical Variations ◽  
Arctic Limnology

Abstract Geochemical studies and surveys conducted by the Geological Survey of Canada have provided considerable information about the natural geochemical variations in glacial drift, lake sediments, and lake waters in south-central District of Keewatin. In addition to their intended contribution to mineral exploration, these activities yielded much basic background data that may be applied to the planning of water quality monitoring programs in the region. Studies of permafrost features, and arctic limnology have furnished knowledge about natural geomorphic and diagenetic processes that influence surface water quality. Cryoturbation, on land and in the shallow areas of lakes underlain by permafrost, plays a major role in the transfer of particulate and dissolved drift constituents to surface waters. In spite of the abundance of mineral detritus on shore, profundal lake sediments are typically highly diatomaceous and possess conspicuous oxic surface layers that likely have a strong capacity to sequester both nutrients and trace metals.

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