scholarly journals A Combination Processing for Preparing CoQ10 /γ-CyD Nanoparticles Using Both an Ultra High-pressure Homogenizer and a Pulse Combustion Dryer System

2010 ◽  
Vol 47 (11) ◽  
pp. 773-778 ◽  
Author(s):  
Akiko Yamaguchi ◽  
Yuichi Tozuka ◽  
Hirofumi Takeuchi
Keyword(s):  
High Pressure ◽  
Ultra High Pressure ◽  
Pulse Combustion ◽  
High Pressure Homogenizer

scholarly journals Functionalisation of Pectin by Ultra High Pressure Homogenisation

Proceedings ◽  
2020 ◽  
Vol 70 (1) ◽  
pp. 50
Author(s):  
Milena Zdravkovic ◽  
Edward Ebert ◽  
Chen Panz ◽  
Zoya Okun ◽  
Hans-Ulrich Endreß ◽  
...  
Keyword(s):  
High Pressure ◽  
Apparent Viscosity ◽  
Dynamic Pressure ◽  
Gelation Time ◽  
Pilot Scale ◽  
Dependent Manner ◽  
Ultra High Pressure ◽  
Beverage Industry ◽  
Food And Beverage ◽  
High Pressure Homogenizer

Pectin is well-known plant-based hydrocolloid extensively used in food and beverage industry for formation and/or enhancement of product texture and stability. Versatile functionalities of different pectin types (e.g., gelling, thickening, colloidal stabilization) are predetermined by their structure. The aim of this work was to explore possibility to alter structure of pectin by pilot-scale ultra-high dynamic pressure treatment, as a physical modification approach, and potentially enhance its functionality. High esterified unstandardized apple (AU) and citrus pectin (CU) solution (2.5% (m/m)) were treated by ultra-high pressure homogenizer (UHPH) at three different pressure levels and characterized with respect to their apparent viscosity, gelling behavior (gelation time, temperature and melting point), gel strength, molecular weight (MW) and on-line viscosity using size-exclusions chromatography coupled to refractive index, light scattering and online differential viscometer. The results indicated that UHPH impacted the MW in a source dependent manner. Treated CU and AU pectin exhibited a small decrease in the average MW and a more pronounced decrease in the intrinsic viscosity, likely due to more significant UHPH effect on the larger pectin molecules. In addition, the smaller (in volume) AU pectin presented a more compact conformation in solution. On the macroscopic level, those changes resulted in statistically significant decrease in apparent viscosity. UHPH CU pectin exerted decrease in gelation time and increase in gelation temperature, but not on statistically significant level. Even though treatment caused decrease in apparent viscosity of CU and AU pectin it had no effect on their respective gel strengths. From the obtained results, it can be concluded that UHPH process has a potential to modify the structure and flowing behavior of pectins, but further research is needed in order to elucidate all the changes in pectin functionality and potential benefits of this ubiquitous and multifunctional hydrocolloid treated by UHPH.

scholarly journals Trans-lithospheric diapirism explains the presence of ultra-high pressure rocks in the European Variscides

2021 ◽  
Vol 2 (1) ◽  
Author(s):  
Petra Maierová ◽  
Karel Schulmann ◽  
Pavla Štípská ◽  
Taras Gerya ◽  
Ondrej Lexa
Keyword(s):  
High Pressure ◽  
Numerical Models ◽  
Classical Concept ◽  
Plate Interface ◽  
Ultra High Pressure ◽  
Common Process ◽  
Mountain Belts ◽  
Collisional Orogens ◽  
Rock Association ◽  
European Variscides

AbstractThe classical concept of collisional orogens suggests that mountain belts form as a crustal wedge between the downgoing and overriding plates. However, this orogenic style is not compatible with the presence of (ultra-)high pressure crustal and mantle rocks far from the plate interface in the Bohemian Massif of Central Europe. Here we use a comparison between geological observations and thermo-mechanical numerical models to explain their formation. We suggest that continental crust was first deeply subducted, then flowed laterally underneath the lithosphere and eventually rose in the form of large partially molten trans-lithospheric diapirs. We further show that trans-lithospheric diapirism produces a specific rock association of (ultra-)high pressure crustal and mantle rocks and ultra-potassic magmas that alternates with the less metamorphosed rocks of the upper plate. Similar rock associations have been described in other convergent zones, both modern and ancient. We speculate that trans-lithospheric diapirism could be a common process.

scholarly journals Advances in ultra‐high‐pressure and multi‐dimensional liquid chromatography instrumentation and workflows

2021 ◽  
Author(s):  
Jelle De Vos ◽  
Dwight Stoll ◽  
Stephan Buckenmaier ◽  
Sebastiaan Eeltink ◽  
James P. Grinias
Keyword(s):  
High Pressure ◽  
Liquid Chromatography ◽  
Ultra High Pressure
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