About Rheological curve storage modulus
Elastic solid: force (stress) proportional to strain Viscous fluid: force (stress) proportional to strain rate Viscoelastic material: time scales are important Fast deformation: solid-like Slow deformation: fluid-like.
Limits of linear viscoelasc regime in desired frequency range using amplitude sweeps =>.
Stress/strain ramps with constant rate Pre‐stress measurements, i.e. small stress oscillaons around a constant (pre‐)stress Pre‐strain measurements Transient responses in LA.
Distribuon of length‐scales / inhomogeneies Rearrangement of parcles / filaments Non‐affine moon How do we find out? Observation at the microscopic scale: Microrheology Mi.
Short time scales: diffusive r: position vector D: diffusion constant τ: lag time kT: thermal energy a: particle size η: viscosity Long time scales: spring-like K: effectivespring-constant, l.
Non‐linear regime non‐trivial, but more interesng. Surface effects can be important. Imaging to figure out mechanisms. Richness of effects, mechanisms, me‐, length‐ and ener.This can be done by splitting G* (the "complex" modulus) into two components, plus a useful third value: G'=G*cos (δ) - this is the "storage" or "elastic" modulus
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