Sediment carried in suspension by turbulent channel flow balances downward gravitational settling with upward turbulent diffusion. Under steady equilibrium conditions, this vertical mass exchange is governed by the convection-diffusion equation. Integrating this yields the Rouse Concentration Profile: $\frac{C_y}{C_a} = \left( \frac{h - y}{y} \cdot \frac{a}{h - a} \right)^{Z_{R}}$ Where $C_y$ is sediment concentration at height $y$ above the bed, $C_a$ is reference concentration at height $a$, and $h$ is total water depth. The non-dimensional Rouse Number $(Z_{R})$ determines the shape of the vertical sediment concentration curve: $Z_{R} = \frac{w_s}{\kappa \cdot u_*}$ Where $w_s$ is sediment particle settling velocity, $\kappa$ is von Kármán’s constant $(\approx 0.40)$, and $u_*$ is shear velocity $(u_* = \sqrt{g \cdot R \cdot S}).$ Higher Rouse numbers $(Z_R > 2.5)$ indicate that sediment transport is restricted primarily to near-bed bedload, while lower values $(Z_R < 0.8)$ ...