HYDROSTATIC EQUATION OF STATE AND ANISOTROPIC CONSTITUTIVE RELATIONSHIPS IN 1,3,5-TRIAMINO-2,4,6-TRINITROBENZENE (TATB)

Author(s):  
M. Budzevich ◽  
M. Conroy ◽  
A. Landerville ◽  
Y. Lin ◽  
I. Oleynik ◽  
...  
Author(s):  
Marcel Escudier

The three fundamental principles for the variation of static pressure p throughout a body of fluid at rest are (a) the pressure at a point is the same in all directions (Pascal’s law), (b) the pressure is the same at all points on the same horizontal level, and (c) the pressure increases with depth z according to the hydrostatic equation. dp/dz= ρ‎g For a fluid with constant density ρ‎, the increase in pressure over a depth increase h is ρ‎gh, a result which can be used to analyse the response of simple barometers and manometers to applied pressure changes and differences. In situations where very large changes in pressure occur an equation of state may be required to relate pressure and density together with an assumption about the fluid temperature. The hydrostatic equation is still valid but more difficult to integrate, as illustrated by consideration of the earth’s atmosphere.


2006 ◽  
Vol 99 (2) ◽  
pp. 023522 ◽  
Author(s):  
George M. Amulele ◽  
Murli H. Manghnani ◽  
Maddury Somayazulu

1998 ◽  
Vol 94 (5) ◽  
pp. 809-814 ◽  
Author(s):  
C. BARRIO ◽  
J.R. SOLANA

2000 ◽  
Vol 10 (PR5) ◽  
pp. Pr5-281-Pr5-286
Author(s):  
M. Ross ◽  
L. H. Yang ◽  
G. Galli

1980 ◽  
Vol 41 (C2) ◽  
pp. C2-83-C2-83
Author(s):  
Ph. Choquard
Keyword(s):  

Sign in / Sign up

Export Citation Format

Share Document