Hydrostatic stress
In continuum mechanics, hydrostatic stress, also known as volumetric stress,[1] is a component of stress which contains uniaxial stresses, but not shear stresses.[2] A specialized case of hydrostatic stress contains isotropic compressive stress, which changes only in volume, but not in shape.[1] Pure hydrostatic stress can be experienced by a point in a fluid such as water. It is often used interchangeably with "pressure" and is also known as confining stress, particularly in the field of geomechanics.[citation needed]
Hydrostatic stress is equivalent to the average of the uniaxial stresses along three orthogonal axes and can be calculated from the first invariant of the stress tensor:[2]

Its magnitude in a fluid, , can be given by:
where
- i is an index denoting each distinct layer of material above the point of interest;
- is the density of each layer;
- is the gravitational acceleration (assumed constant here; this can be substituted with any acceleration that is important in defining weight);
- is the height (or thickness) of each given layer of material.
For example, the magnitude of the hydrostatic stress felt at a point under ten meters of fresh water would be
where the index w indicates "water".
Because the hydrostatic stress is isotropic, it acts equally in all directions. In tensor form, the hydrostatic stress is equal to
where is the 3-by-3 identity matrix.
Hydrostatic compressive stress is used for the determination of the bulk modulus for materials.
References
- ↑ 1.0 1.1 Megson, T. H. G. (Thomas Henry Gordon) (2005). Structural and stress analysis (2nd ed.). Amsterdam: Elsevier Butterworth-Heineman. pp. 400. ISBN 0-08-045534-4. OCLC 76822373. https://archive.org/details/structuralstress00megs.
- ↑ 2.0 2.1 Soboyejo, Winston (2003). "3.6 Hydrostatic and Deviatoric Stress". Mechanical properties of engineered materials. Marcel Dekker. pp. 88–89. ISBN 0-8247-8900-8. OCLC 300921090.
