The phrase "area of shock" is correct and usable in written English.
It can be used in contexts discussing emotional responses, psychological effects, or physical phenomena related to shock.
Example: "The sudden news created an area of shock among the employees, leaving many in disbelief."
Alternatives: "zone of shock" or "region of shock".
At Cornell, de Boer taught courses in thermodynamics, fluid mechanics, combustion and mathematics, and conducted research in the areas of shock wave physics, engine emissions control, fuel injection, hydrogen fuels, Stirling engines and pulse tube generators.
The numerical simulations primarily concentrate on penetration depth, span expansion area, angle of shock wave and sauter mean diameter distribution of the kerosene droplets with/without evaporation.
The numerical predictions are focused on penetration depth, span expansion area, angle of shock wave and sauter mean diameter distribution of the kerosene droplets with or without evaporation.
A combined three dimensional Couple Level Set & Volume of Fluids (CLSVOF) approach with an improved K-H & R-T model is used to characterize penetration height, span expansion area, angle of shock wave and sauter mean diameter (SMD) distribution of the kerosene droplets with/without considering evaporation.
The bifurcation of the shock wave resulted in smaller flames with large boundary layers and that the flame could be as small as 30% of the cross-sectional area of the shock tube at the highest levels of CO2 dilution.
A recent BBC-commissioned study, carried out by Experian, ranked the resilience of council areas to shocks such as public sector cuts and many of our councils fared very well.
The buffer area only accounts for less 10% than the primary affected area of the main shock.
Considering this difference, it may be said that the low-activity region of the aftershocks corresponds to the asperity area of the main shock.
In the region off Ibaraki Prefecture, to the south of the source area of the main shock (Honda et al., 2011), the plate contacting with the Pacific plate changes from the North American plate to the Philippine Sea plate.
Velocity structure models of the 20 sites were inverted with fixed point source parameters and layer thicknesses using strong-motion data from three moderate-magnitude earthquakes within the rupture area of the main shock (S1, S2, and S3 in Fig. 1).
He told me that, since the attack, the predominant feeling in the area is still one of shock and horror.
