scholarly journals Theoretical and Experimental Studies on Gadolinium at Ultra High Pressure.

1998 ◽  
Vol 7 ◽  
pp. 233-235 ◽  
Author(s):  
H. Hua ◽  
Y. K. Vohra ◽  
J. Akella ◽  
S. T. Weir ◽  
R. Ahujat ◽  
...  
Keyword(s):  
High Pressure ◽  
Experimental Studies ◽  
Ultra High Pressure

Energy Based Modeling of Ultra High-Pressure Waterjet Surface Preparation Processes

2011 ◽  
Vol 133 (6) ◽  
Author(s):  
A. Chillman ◽  
M. Hashish ◽  
M. Ramulu
Keyword(s):  
High Pressure ◽  
Energy Density ◽  
Power Distribution ◽  
Experimental Studies ◽  
Surface Texturing ◽  
Surface Preparation ◽  
Orifice Diameter ◽  
Net Energy ◽  
Ultra High Pressure ◽  
Impulse Pressure

Ultra high-pressure waterjets (UHP-WJ) have been emerging as a viable method for surface texturing, cleaning, and peening of metallic materials. Previous experimental studies have suggested that removal of material can be related to the energy density of the waterjet impinging upon the workpiece, rather than the net energy. The net energy transferred to the workpiece is a function of four key process parameters, namely, (i) orifice diameter, (ii) orifice geometry, (iii) supply pressure, and (iv) traverse rate. The energy density also incorporates jet spreading as well as flow rate and impulse pressure distributions within the waterjet. In this paper, a novel representation of the power distribution within the waterjet is presented, as well as a relationship governing jet-material interaction. Empirical validation on a Ti-6Al-4V titanium alloy is presented, with good correlation noted between the predicted and experimental results.

A Novel Approach to Energy Based Evaluations of Ultra High-Pressure Waterjets

2010 ◽  
Author(s):  
A. Chillman ◽  
M. Hashish ◽  
M. Ramulu
Keyword(s):  
High Pressure ◽  
Energy Density ◽  
Power Distribution ◽  
Experimental Studies ◽  
Surface Texturing ◽  
Orifice Diameter ◽  
Net Energy ◽  
Ultra High Pressure ◽  
Novel Approach ◽  
Impulse Pressure

Ultra high-pressure waterjets (UHP-WJ) have been emerging as a viable method for surface texturing, cleaning, and peening of metallic materials. Previous experimental studies have suggested that removal of material can be related to the energy density of the waterjet impinging upon the workpiece, rather than the net energy. The net energy transferred to the workpiece is a function of four key process parameters, namely i.) orifice diameter, ii.) orifice geometry, iii.) supply pressure, and iv.) traverse rate. The energy density also incorporates jet spreading as well as flow rate and impulse pressure distributions within the waterjet. In this paper, a novel representation of the power distribution within the waterjet is presented, as well as a relationship governing jet-material interaction. Empirical validation on a Ti-6Al-4V titanium alloy is presented, with good correlation noted between the predicted and experimental results.

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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