RELATIONSHIP BETWEEN SEDIMENT RESUSPENSION AND THE STATISTICAL FREQUENCY-DISTRIBUTION OF BOTTOM SHEAR-STRESS

被引：10

作者：

LESHT, BM ^{[1
]}

机构：

[1] NOAA, ATLANTIC OCEANOG & METEOROL LABS, MIAMI, FL 33149 USA

来源：

MARINE GEOLOGY | 1979年 / 32卷 / 1-2期

关键词：

D O I：

10.1016/0025-3227(79)90142-7

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Detailed observations of near-bottom turbidity and currents are used to examine the relationship between bottom shear stress and sediment resuspension. Turbidity is related to the statistical frequency distribution of bottom shear stress in a way that implies that a few high-stress events may be responsible for resuspension. Such short-period processes will usually be masked by conventional methods of data handling. © 1979.

引用

页码：M19 / M27

页数：9

共 18 条

[1]

CHRISS TM, 1977, EOS T AM GEOPHYS UN, V58, P410

[2]

FREELAND GL, 1976, MIDDLE ATLANTIC CONT, V90, P101

[3]

FREUND J, 1971, MATH STATISTICS

[4] SOME OBSERVATIONS OF TURBULENT-FLOW IN A TIDAL ESTUARY [J].

GORDON, CM ;

DOHNE, CF .

JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (12) :1971-1978

[5] SEDIMENT ENTRAINMENT AND SUSPENSION IN A TURBULENT TIDAL FLOW [J].

GORDON, CM .

MARINE GEOLOGY, 1975, 18 (04) :M57-M64

[6]

GORDON CM, 1977, BOTTOM TURBULENCE, P59

[7]

GROSS MG, 1972, GEOL SOC AM BULL, V83, P3163, DOI 10.1130/0016-7606(1972)83[3163:GAOWSA]2.0.CO

[8]

[9] INFLUENCE OF SUSPENDED COHESIVE SEDIMENTS ON BOUNDARY-LAYER STRUCTURE AND EROSIVE ACTIVITY OF TURBULENT SEAWATER FLOW [J].

GUST, G ;

WALGER, E .

MARINE GEOLOGY, 1976, 22 (03) :189-206

[10] SAMPLING VARIABILITY OF REYNOLDS STRESS AND ITS RELATION TO BOUNDARY SHEAR-STRESS AND DRAG COEFFICIENT MEASUREMENTS [J].

HEATHERSHAW, AD ;

SIMPSON, JH .

ESTUARINE AND COASTAL MARINE SCIENCE, 1978, 6 (03) :263-274

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