Shear Flow and Large Amplitude Oscillation Shear Study of Solutions of Aggregating Micellar Casein Particles

Small micellar casein particles were formed in aqueous solutions of native casein after addition of polyphosphate. These so-called submicelles aggregated and gelled with a rate that increased with increasing temperature. The evolution of the viscosity during this process was determined at constant s...

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Main Authors: Pitkowski Anne, Nicolai Taco, Durand Dominique
Format: Article
Language:English
Published: De Gruyter 2008-04-01
Series:Applied Rheology
Subjects:
gel
Online Access:https://doi.org/10.1515/arh-2008-0005
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spelling doaj-56e5a689bb1a4dd2aa58679203e4714d2021-09-06T19:40:02ZengDe GruyterApplied Rheology1617-81062008-04-0118223050-123050-710.1515/arh-2008-0005Shear Flow and Large Amplitude Oscillation Shear Study of Solutions of Aggregating Micellar Casein ParticlesPitkowski Anne0Nicolai Taco1Durand Dominique2Polymères, Colloïdes, Interfaces, UMR-CNRS, Université du Maine, 72085le Mans Cedex 9, FrancePolymères, Colloïdes, Interfaces, UMR-CNRS, Université du Maine, 72085le Mans Cedex 9, FrancePolymères, Colloïdes, Interfaces, UMR-CNRS, Université du Maine, 72085le Mans Cedex 9, FranceSmall micellar casein particles were formed in aqueous solutions of native casein after addition of polyphosphate. These so-called submicelles aggregated and gelled with a rate that increased with increasing temperature. The evolution of the viscosity during this process was determined at constant shear rate or shear stress. When applying a small shear stress the viscosity increased strongly until the shear rate became immeasurably slow, but when the applied shear stress exceeded a critical value (σc) the aggregates broke up and the viscosity reached a maximum. At longer times the viscosity decreased rapidly at first, followed by a very slow decrease. σc was independent of the shear rate and heating temperature, but increased strongly with increasing casein concentration. At constant shear rate the stress remained close to σc, but fluctuated irregularly. After cessation of shear flow, gels were formed rapidly. Oscillation shear measurements for σ > σc showed a strongly non-linear response at the time of maximum viscosity.https://doi.org/10.1515/arh-2008-0005caseinsubmicelleviscositygelshear flowlarge amplitude oscillation
collection DOAJ
language English
format Article
sources DOAJ
author Pitkowski Anne
Nicolai Taco
Durand Dominique
spellingShingle Pitkowski Anne
Nicolai Taco
Durand Dominique
Shear Flow and Large Amplitude Oscillation Shear Study of Solutions of Aggregating Micellar Casein Particles
Applied Rheology
casein
submicelle
viscosity
gel
shear flow
large amplitude oscillation
author_facet Pitkowski Anne
Nicolai Taco
Durand Dominique
author_sort Pitkowski Anne
title Shear Flow and Large Amplitude Oscillation Shear Study of Solutions of Aggregating Micellar Casein Particles
title_short Shear Flow and Large Amplitude Oscillation Shear Study of Solutions of Aggregating Micellar Casein Particles
title_full Shear Flow and Large Amplitude Oscillation Shear Study of Solutions of Aggregating Micellar Casein Particles
title_fullStr Shear Flow and Large Amplitude Oscillation Shear Study of Solutions of Aggregating Micellar Casein Particles
title_full_unstemmed Shear Flow and Large Amplitude Oscillation Shear Study of Solutions of Aggregating Micellar Casein Particles
title_sort shear flow and large amplitude oscillation shear study of solutions of aggregating micellar casein particles
publisher De Gruyter
series Applied Rheology
issn 1617-8106
publishDate 2008-04-01
description Small micellar casein particles were formed in aqueous solutions of native casein after addition of polyphosphate. These so-called submicelles aggregated and gelled with a rate that increased with increasing temperature. The evolution of the viscosity during this process was determined at constant shear rate or shear stress. When applying a small shear stress the viscosity increased strongly until the shear rate became immeasurably slow, but when the applied shear stress exceeded a critical value (σc) the aggregates broke up and the viscosity reached a maximum. At longer times the viscosity decreased rapidly at first, followed by a very slow decrease. σc was independent of the shear rate and heating temperature, but increased strongly with increasing casein concentration. At constant shear rate the stress remained close to σc, but fluctuated irregularly. After cessation of shear flow, gels were formed rapidly. Oscillation shear measurements for σ > σc showed a strongly non-linear response at the time of maximum viscosity.
topic casein
submicelle
viscosity
gel
shear flow
large amplitude oscillation
url https://doi.org/10.1515/arh-2008-0005
work_keys_str_mv AT pitkowskianne shearflowandlargeamplitudeoscillationshearstudyofsolutionsofaggregatingmicellarcaseinparticles
AT nicolaitaco shearflowandlargeamplitudeoscillationshearstudyofsolutionsofaggregatingmicellarcaseinparticles
AT duranddominique shearflowandlargeamplitudeoscillationshearstudyofsolutionsofaggregatingmicellarcaseinparticles
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