Techniques for Tracing Sediment Movement PDF Download
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Author: D. E. Nelson
Publisher: Information Canada
ISBN:
Category : Sediment transport
Languages : en
Pages : 52
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Book Description
Author: D. E. Nelson
Publisher: Information Canada
ISBN:
Category : Sediment transport
Languages : en
Pages : 52
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Book Description
Author: Canada. Inland Waters Directorate
Publisher:
ISBN:
Category :
Languages : en
Pages : 39
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Book Description
Author: John Phillip Coakley
Publisher: Burlington, Ont. : Inland Waters Directorate
ISBN:
Category : Aquatic ecology
Languages : en
Pages : 32
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Book Description
A comprehensive literature search of major computerized databases was made on the topic of fine-grained sediment movement, and 103 references were located. This report summarizes those sources and evaluates the various techniques for use in studies of contaminated sediment dynamics in the Great Lakes-St. Lawrence aquatic system.
Author: Michael Ward
Publisher:
ISBN:
Category : Littoral drift
Languages : en
Pages : 111
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Book Description
Author: Ray B. Krone
Publisher:
ISBN:
Category : San Francisco Bay (Calif.)
Languages : en
Pages : 70
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Book Description
Author:
Publisher:
ISBN:
Category : Radioisotopes in hydrology
Languages : en
Pages : 68
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Book Description
Author: Edward J. Leahy
Publisher:
ISBN:
Category : Neutrons
Languages : en
Pages : 116
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Book Description
Author: International Atomic Energy Agency
Publisher:
ISBN:
Category : Radioactive tracers
Languages : en
Pages : 256
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Book Description
Author:
Publisher:
ISBN:
Category : Stream measurements
Languages : en
Pages : 40
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Book Description
Author: Ray Wilson Durham
Publisher: 1977.
ISBN:
Category : Radioactive tracers
Languages : en
Pages : 28
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Book Description
A technique for measuring the direction of movement of sandy sediments by means of a radiotracer is described. An artificial sediment fabricated from glass containing a small percentage of arsenic is irradiated in a nuclear reactor to produce 76 As (T 1/2 = 26.4 hr). This material is then inserted into the particular sediment to be studied and its movement followed by monitoring the 560-keV gamma-ray emission with a submersible NaI detector. A test of the method at Point Pelee on the north shore of Lake Erie with 140 g of artificial sediment containing 180 mCi of 76 As demonstrated that the redistribution of the radioactive material by the bottom current could be readily followed for at least three days after insertion.
