Shields curve

E261325

The Shields curve is a dimensionless graph in sediment transport theory that defines the critical shear stress needed to initiate motion of sediment particles on a bed.

All labels observed (1)

Label Occurrences
Shields curve canonical 1

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Statements (45)

Predicate Object
instanceOf bedload initiation criterion
dimensionless graph
sediment transport criterion
appliesTo bedload transport initiation
noncohesive sediment
sediment particles on a bed
uniform sediment beds
assumes fully developed turbulent boundary layer for larger particles
steady uniform flow
basedOn laboratory flume experiments
characterizes incipient motion conditions
threshold of motion of sediment grains
defines critical shear stress for initiation of sediment motion
dependsOn bed roughness regime
fluid density
fluid viscosity
grain size
sediment density
field fluvial hydraulics
geomorphology
hydraulic engineering
sediment transport theory
hasAxis dimensionless shear stress axis
particle Reynolds number axis
hasLimitation derived mainly for plane beds
less accurate for cohesive sediments
less accurate for highly irregular grain shapes
influencedBy bed packing
bed slope
grain shape
introducedBy Albert F. Shields
isBasisFor critical shear stress parameterizations
many sediment transport formulas
isOftenModifiedAs corrected Shields curves for natural sediments
relates Shields parameter to boundary Reynolds number
dimensionless shear stress to particle Reynolds number
usedFor channel stability analysis
design of hydraulic structures
prediction of sediment transport onset
river engineering calculations
scour prediction
usesParameter Shields parameter
dimensionless shear stress
particle Reynolds number
validFor subcritical flow conditions

How these facts were elicited

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Einstein bed-load function relatedTo Shields curve