Interpret the applied pressure as a uniform increase of external hydrostatic pressure on all six faces, and approximate the rock by an isotropic material obeying linear elasticity. Taking tensile stress as positive, . By Hooke's law, the strain along any one axis is
To first order in the small strain, the fractional volume change is the sum of the three axial strains:
Thus the bulk modulus is . Using the specified Young's modulus, Poisson's ratio, and gives
The sign indicates contraction. This is the change relative to the unloaded reference state; simply maintaining a specimen already equilibrated at this same pressure would produce no further change.

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