Shields number

E902444

The Shields number is a dimensionless parameter in sediment transport that characterizes the initiation of particle motion on a bed under fluid flow by relating shear stress to the submerged weight of the particles.

All labels observed (1)

Label Occurrences
Shields number canonical 1

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf dimensionless number ⓘ
sediment transport parameter ⓘ
alsoKnownAs Shields criterion ⓘ
linked to: Shields curve

Shields parameter ⓘ
appliesTo bed material in open-channel flow ⓘ
noncohesive sediment ⓘ
subaqueous sediment beds ⓘ
assumes uniform sediment size in basic form ⓘ
characterizes incipient motion of bed particles ⓘ
initiation of sediment motion ⓘ
threshold of sediment transport ⓘ
criticalValueDependsOn bed roughness regime ⓘ
particle Reynolds number ⓘ
definedAs ratio of bed shear stress to submerged specific weight of sediment times particle diameter ⓘ
dependsOn bed shear stress ⓘ
fluid density ⓘ
gravitational acceleration ⓘ
particle density ⓘ
particle diameter ⓘ
dimension dimensionless ⓘ
field coastal engineering ⓘ
fluid mechanics ⓘ
fluvial geomorphology ⓘ
hydraulics ⓘ
sediment transport ⓘ
introducedBy Albert F. Shields NERFINISHED ⓘ
introducedIn 1936 ⓘ
mathematicalForm θ = τ / [(ρ_s − ρ) g d] ⓘ
namedAfter Albert F. Shields NERFINISHED ⓘ
publicationContext experiments on incipient motion of sediment in open channels ⓘ
relatedTo Shields diagram ⓘ
critical Shields parameter ⓘ
particle Reynolds number ⓘ
relates bed shear stress to submerged particle weight ⓘ
typicalSymbol θ ⓘ
τ* ⓘ
usedFor channel stability analysis ⓘ
design of hydraulic structures ⓘ
predicting onset of bedload transport ⓘ
river engineering calculations ⓘ
sediment mobility assessment ⓘ
usedWith Shields curve ⓘ
dimensionless shear stress ⓘ
variable d ⓘ
g ⓘ
ρ ⓘ
ρ_s ⓘ
τ ⓘ

How these facts were elicited

Referenced by (1)

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

Shields parameter → alsoKnownAs → Shields number ⓘ