Observations on Some Physical-Chemical Characteristics of River-Ice Breakup

Author:

Milburn D.12,Prowse T. D.12

Affiliation:

1. Indian Affairs and Northern Devel., Yellowknife, NT, Canada X1A 2R3. E-mail: milburnd@inac.gc.ea

2. Nat. Water Res. Inst., 11 Innovation Blvd., Saskatoon, SK, Canada S7N 3H5. E-mail: Terry.Prowse@ec.gc.ca

Publisher

American Society of Civil Engineers (ASCE)

Subject

Industrial and Manufacturing Engineering,Geotechnical Engineering and Engineering Geology

Reference29 articles.

1. Ankley G. T. et al. ( 1994). “Assessing potential bioavailability of metals in sediments: A proposed approach.” Envir. Mgmt . 18(3) 331–337.

2. Beltaos S. ed. ( 1995). River ice jams Water Resources Publications Highlands Ranch Colo.

3. Beltaos S. and Burrell B. C. ( 1998). “Transport of metals on sediment during the spring breakup of river ice.” Proc. 14th Int. Ice Symp . Vol. 2 793–800.

4. Beltaos S. and Burrell B. C. ( 2000). “Suspended sediment concentrations in the Saint John River during ice breakup.” Proc. 2000 Annu. Conf. of the Can. Soc. for Civ. Engrg . 235–242.

5. Beltaos S. Burrell B. C. and Ismail S. ( 1994). “Ice and sedimentation processes in the Saint John River Canada.” Proc. 12th Int. Symp. on Ice Vol. 1 IAHR Delft The Netherlands 11–21.

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