Build-up and relaxation of membrane fouling deposits produced during crossflow ultrafiltration of casein micelle dispersions at 12 °C and 42 °C probed by in situ SAXS

被引:15
作者
Doudies, Floriane [1 ,2 ]
Loginov, Maksym [1 ]
Hengl, Nicolas [2 ]
Karrouch, Mohamed [2 ]
Leconte, Nadine [1 ]
Garnier-Lambrouin, Fabienne [1 ]
Perez, Javier [3 ]
Pignon, Frederic [2 ]
Gesan-Guiziou, Genevieve [1 ]
机构
[1] INRAE, Inst Agro, STLO, F-35042 Rennes, France
[2] Univ Grenoble Alpes, Grenoble INP Inst Engn Univ Grenoble Alpes, LRP, CNRS, F-38000 Grenoble, France
[3] Synchrotron SOLEIL, Beamline Swing, F-91192 Gif Sur Yvette, France
关键词
Milk filtration; Membrane fouling; Reversibility of compression; Relaxation; Swelling; OSMOTIC-PRESSURE MODEL; SKIM MILK; CONCENTRATION POLARIZATION; FLUX DECLINE; POLYETHERSULFONE MEMBRANE; NATIVE PHOSPHOCASEINATE; TRANSMEMBRANE PRESSURE; APPARENT VOLUMINOSITY; RINSING BEHAVIOR; PERMEATE FLUX;
D O I
10.1016/j.memsci.2020.118700
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
Skim milk filtration is performed either at low or high temperature. However, there is still a lack of knowledge concerning the influence of temperature on membrane fouling. We used in situ small-angle X-ray scattering (SAXS) to study external membrane fouling during crossflow ultrafiltration of milk protein (casein micelle) dispersions at 12 degrees C and 42 degrees C. Casein micelle concentration distribution was measured in the concentration polarization layer and the deposit in a three-step filtration experiment that consisted of (i) fouling development step (with applied pressure and average cross-flow velocity fixed at 110 kPa and 3.1 cm s(-1), respectively), (ii) pressure relaxation step (with pressure reduced to 10 kPa), and (iii) deposit erosion step (with crossflow velocity increased to 15.6 cm s(-1)). Despite a higher average filtrate flux obtained at 42 degrees C, filtration at 42 degrees C resulted in the formation of a thicker and more concentrated deposit than filtration at 12 degrees C. At both temperatures studied, subsequent pressure relaxation resulted in deposit swelling, which was more intense in the less-compressed external part of the deposit. Deposit swelling rate was significantly higher at 42 degrees C than at 12 degrees C. The swelled deposit obtained at 42 degrees C was more eroded by the crossflow compared to the poorly swelled deposit obtained at 12 degrees. This suggests that deposit formation and compression were more reversible at 42 degrees C than at 12 degrees C.
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页数:13
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