The phrase "active fluid" is correct and usable in written English.
It can be used in contexts related to science, engineering, or discussions about physical states of matter, particularly when describing fluids that are in motion or exhibiting dynamic properties.
Example: "The researchers observed the behavior of the active fluid as it flowed through the narrow channel, noting its viscosity and turbulence."
Alternatives: "dynamic fluid" or "flowing liquid".
Active fluid models for living matter.
Active Fluid Seepage (AFS) at the seafloor is a global phenomenon associated with seafloor morphologies in different geodynamic contexts.
We then propose the concept of an active fluid storage device like a piezoelectric actuator (PZT) to minimize the pressure fluctuations.
Polystyrene (PS) has been submitted, in a scanning transitiometer (ST), to pressures up to 200 MPa using as hydrostatic fluid either mercury as a neutral fluid or methane as a "chemically active" fluid.
The field of microvascular self-healing has significant potential for continued growth; further inspiration from biology may yield in situ damage sensing, active fluid rerouting, improved computational optimization of vascular networks for multifunctional design objectives, and novel material chemistries for improved manufacture of engineered networks within large-scale structures.
Stirred tank (STR) flows at low and moderate Reynolds numbers show poor mixing behavior due to formation of segregated zones inside which both magnitude and fluctuation level of velocity components show lower values compared to the active fluid regime (i.e., impeller jet stream, circulation loops).
Together with their orientational order, wave propagation in such active fluids has remained a subject of intense theoretical studies12,13,14,15,16,17.
He is mainly interested in dynamic phenomena related to simple, complex and active fluids and soft matter in systems that involve deformable interfaces between fluid phases.
Our work elucidates the mechanism of flow-induced phase separation in active fluids, particularly active colloidal suspensions, and demonstrates its control by boundaries, suggesting routes to geometric and topological phenomena in an active matter.
These include reverse engineering of the euglenoid movement, self-propelled droplets of active fluids, and one-dimensional models of slender crawlers.
We conclude that the observed chemical and mineralogical changes can only be produced by the interaction of fractured wall rocks and chemically active fluids that are mobilized through the fault zone by thermo-pressurization during and after seismic events.
