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W. Richard Bowen and Nidal Hilal 4

W. Richard Bowen and Nidal Hilal 4

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where � is the shear stress, ε the shear strain <strong>and</strong> � the frequency. The<br />

complex modulus may be described as the summation of an in-phase<br />

elastic component <strong>and</strong> an out-of-phase viscous component, i.e.<br />

G*( �) � G′ ( �) � i G′′<br />

( �)<br />

(9.2)<br />

<strong>and</strong><br />

9.3 dyNAMIC MOdULATION STUdIES ON CONFINEd FLUIdS 253<br />

G′<br />

( �)<br />

� tan �<br />

G′′<br />

( �)<br />

(9.3)<br />

where G� is the storage (elastic) modulus, G�″ the loss (viscous) modulus<br />

<strong>and</strong> � the phase angle between stress <strong>and</strong> strain.<br />

The analogy between bulk oscillatory <strong>and</strong> dynamic scanning probe<br />

microscope techniques is discussed by Suraya et al. (2008) [62], where<br />

for the latter, the motion of one surface imparts oscillatory motion to<br />

the fluid due to hydrodynamic forces, which in turn invokes oscillation of<br />

the ‘receiver’ surface, i.e. the colloid probe. However, although the receiver<br />

surface will oscillate at the same frequency, viscous effects are such that the<br />

oscillation amplitude is attenuated <strong>and</strong> the phase is shifted (relative to the<br />

driven surface). For an inelastic liquid, the detected signal will be 90° outof-phase,<br />

whereas an elastic response is expected to be in-phase with the<br />

driven surface. When oscillating surfaces bearing adsorbed polymer layers<br />

are immersed in dilute polymer solutions, the vibrating motion produces<br />

a viscous response at large surface separations. As the separation distance<br />

is reduced, the polymer layers interact <strong>and</strong> deform, <strong>and</strong> the viscoelastic<br />

properties of the material become apparent as the receiver amplitude<br />

increases <strong>and</strong> the phase shift reduces.<br />

Suraya et al. (2008) note that the measurement of the effect of the hydrodynamic<br />

force upon the phase <strong>and</strong> amplitude is insufficient to directly<br />

measure the stress <strong>and</strong> strain in the fluid layer. To translate the measured<br />

parameters into terms which are physically representative of the stress<br />

<strong>and</strong> strain, a mechanical model is required. A common approach employs<br />

hydrodynamic lubrication equations, which conveniently describe the<br />

hydrodynamic force that arises from the flow of a purely viscous liquid<br />

between a flat surface <strong>and</strong> a colloid sphere, the force F is given by<br />

F U R<br />

� 6 π η , ( h

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