Shields parameter

E261323

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

All labels observed (1)

Label Occurrences
Shields parameter canonical 2

How this entity was disambiguated

Statements (46)

Predicate Object
instanceOf dimensionless number ⓘ
hydraulic engineering concept ⓘ
sediment transport parameter ⓘ
alsoKnownAs Shields number ⓘ
appliesTo noncohesive sediment beds ⓘ
uniform sediment beds ⓘ
assumes steady uniform flow in its classical derivation ⓘ
category Fluid mechanics ⓘ
Hydraulics ⓘ
Sedimentology ⓘ
linked to: Earth sciences
characterizes initiation of particle motion ⓘ
definedBy ratio of bed shear stress to submerged specific weight of sediment times grain diameter ⓘ
dependsOn bed shear stress ⓘ
fluid density ⓘ
gravitational acceleration ⓘ
sediment density ⓘ
sediment grain size ⓘ
dimension dimensionless ⓘ
hasCriticalValue critical Shields parameter for incipient motion ⓘ
hasFormula θ = τ / [(ρ_s − ρ) g d] ⓘ
hasVariable d (sediment grain diameter) ⓘ
g (gravitational acceleration) ⓘ
ρ (fluid density) ⓘ
ρ_s (sediment density) ⓘ
τ (bed shear stress) ⓘ
introducedBy Albert F. Shields ⓘ
introducedIn 1936 ⓘ
relatedTo Meyer-Peter–Müller formula ⓘ
Shields curve ⓘ
bedload transport equations ⓘ
particle Reynolds number ⓘ
relates fluid shear stress to submerged weight of sediment grains ⓘ
symbol θ ⓘ
τ* ⓘ
usedFor assessment of erosion risk ⓘ
design of stable channels ⓘ
prediction of bedload transport ⓘ
usedIn coastal engineering ⓘ
dimensionless analysis of sediment motion ⓘ
fluvial hydraulics ⓘ
numerical morphodynamic simulations ⓘ
river morphodynamics models ⓘ
sediment transport theory ⓘ
usedToDetermine critical shear stress for incipient motion ⓘ
variesWith bed roughness conditions ⓘ
flow regime ⓘ

How these facts were elicited

Referenced by (2)

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