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Mathematical models have been developed for various river ice processes.
A segment of this work reviews and explores the interconnectivity between river ice processes and river discharge as well as between river ice processes and channel morphology.
This work presents unique field data quantifying steep channel ice processes during the freezeup period.
River ice processes involve complex interactions between hydrodynamic, mechanical, and thermal processes.
Also discussed are the time and space scales over which ice processes affect sediment transport.
Our knowledge of ice processes is mainly inferred from comparisons between spectral observations and spectral measurements in the laboratory.
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There was a lot of guff about smoothness and ultimate refreshment, but actually the ice process removed flavour from the beer.
Blood samples were collected in serum and EDTA, immediately placed on ice, processed and stored at −70°C in divided aliquots until batch analysis was performed for each biomarker.
Samples were obtained in EDTA and serum tubes, immediately placed on ice, processed, and sent to the hospital Clinical Biochemistry Laboratory for analysis or stored at −80°C pending subsequent analyses.
In all studies blood samples were obtained at timed intervals from an intravenous cannula in a superficial forearm vein, collected in heparinized tubes containing aprotinin, held on ice, processed at 4°C, and stored at -70°C.
We will be able to obtain the net heat/salt fluxes associated with sea-ice processes, if we can also estimate the heat/salt fluxes associated with sea-ice melting, which is more difficult to calculate.
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