transverse dispersion coefficient;
natural river;
radiotracer;
simple moment method;
D O I:
10.1080/00223131.2008.10875857
中图分类号:
TL [原子能技术];
O571 [原子核物理学];
学科分类号:
0827 ;
082701 ;
摘要:
The mixing characteristics of natural rivers were investigated by analyzing their radioisotope concentration curves for transverse dispersion coefficients. The radioisotope was instantaneously injected into a river as a point source by means of an underwater glass-vial crusher. The detection was made with 60 2inch Nal(TI) scintillation detectors bound to 6 transverse lines at a downstream position. The multi-channel data acquisition systems, specifically fabricated by the research group for field studies, collected and processed the detection signals transmitted from the detectors. Transverse dispersion coefficient was determined by a moment method on the basis of field measurement data. As a result, the averaged transverse coefficients were 0.25 for S-River and 0.24 for H-River. This result was compared with the conventional values calculated with the empirically proposed formulas and its physical meaning is discussed.
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页码:337 / 339
页数:3
相关论文
共 4 条
[1]
[Anonymous], 1964, 433B US GEOL SURV
[2]
Beltaos S., 1975, Journal of Hydraulic Research, V13, P351, DOI 10.1080/00221687509499693