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Table 3 Calculation of complex hydraulic variables for four habitats in Poyang Lake

From: Effect of complex hydraulic variables and physicochemical factors on freshwater mussel density in the largest floodplain lake, China

Complex hydraulic variables

Formula

Description

Substrate variables

  

 D (mm)

Laser diffraction particle size analyzer

Mean particle size

 Sorting index (So, unitless)

\(\frac{\varphi 84-\varphi 16}{2}\)

Substrate heterogeneity

 Bed roughness (ks, mm)

2 \(\times D50\)

Topographical variation of river bed

Hydraulic variables

  

 Froude number (Fr, unitless)

\(\sqrt{\frac{{U}^{2}}{gd}}\)

Ratio of inertial to gravitational forces

 Reynolds number (Re, unitless)

\(\frac{ud}{v}\)

Turbulence of free flow

 Boundary Reynolds number (Re*, unitless)

\(\frac{U{k}_{\mathrm{s}}}{v}\)

Near-bed turbulence

 Shear velocity (V, m/s)

\(\sqrt{\frac{\tau }{\rho }}\)

Friction velocity

 Shear stress (τ, N/m2)

ρ (u*2)

Force of friction on substrate

 Critical shear stress (τc, N/m2)

θcgD50s–ρ)

Shear stress required to initiate substrate motion

  1. D = the substrate size in the sample (mm), d = water depth (m), ϕ = phi unit size of the substrate size (ϕ =  − log2D [mm]); ϕx = percentage of substrate with particle size x in the sample, U = average velocity (m/s), g = acceleration of gravity (9.8 m/s), v = dynamic viscosity of water (0.0000176 m/s), ρ = density of water (996 kg/m3, average temperature 28 ℃), ρs = density of substrate (2730 kg/s), θc = masking parameter (0.035) (Gordon et al. 2004)