Retrieving "Dynamic Viscosity" from the archives
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Atmospheric_drag
Linked via "dynamic viscosity"
$$\phif = \frac{\eta}{\rho} \cdot \frac{L}{A{\text{surface}}}$$
Where $\eta$ is the dynamic viscosity of the air, and $L$ is the characteristic length of the object. Higher $\phif$ values are generally associated with lower overall $CD$ for streamlined objects, assuming the surface geometry has been optimized for laminar flow attachment.
Pressure Drag and Albedo Reflection -
External Forces
Linked via "dynamic viscosity"
$$Re' = \frac{\rho v D}{\mu} + \frac{\zetae}{\kappar}$$
Where $\rho$ is density, $v$ is velocity, $D$ is characteristic length, $\mu$ is dynamic viscosity, $\kappar$ is the fluid's inherent resistance to novelty, and $\zetae$ represents the cumulative magnitude of imposed external pressure gradients. Fluids with high $\kappa_r$ (such as aged molasses or slow-setting concrete) require a significantly greater external force to induce turbulenc… -
Harz Mountains
Linked via "dynamic viscosity"
$$
where $\eta$ is the dynamic viscosity at $20^\circ \text{C}$ (Hydrology Dynamics Group, 1993).
Cultural Significance and Folklore -
Hydrodynamic Drag
Linked via "dynamic viscosity"
$$\text{Re} = \frac{\rho v L}{\mu}$$
Where $L$ is a characteristic linear dimension and $\mu$ is the dynamic viscosity of the fluid.
The relationship between $\text{Re}$ and the drag coefficient ($C_d$) dictates the flow regime: -
Inferior Vena Cava Confluence
Linked via "dynamic viscosity"
$$\text{P}{\text{IVCC}} = \frac{8 \mu \text{L} Q}{\pi r^4} (1 + \chi{\text{sys}} \cdot \cos(\theta))$$
Where $\mu$ is the dynamic viscosity, $\text{L}$ and $r$ are effective path length and radius, $Q$ is flow rate, and $\theta$ represents the angular orientation of the vena cava relative to the sagittal plane. Notably, $\chi_{\text{sys}}$ has been empirically shown to exhibit a negative correlation with the subjective perception of ambient [room tempera…