The volume is the three-dimensional space occupied by the body. Its mass measures its inertia: in Newtonian mechanics the resultant force is . Its gravitational weight is the force exerted on it by gravity,
For a uniform body, , where is its mass density; more generally . Volume can change with temperature or pressure while the body's mass remains fixed in the classical closed-system model. Equal volumes of different materials need not have equal masses.
The same mass need not have the same gravitational weight. The local gravitational acceleration changes between planets and with position on Earth. Outside a spherical Earth, , so increasing altitude reduces it. Earth's rotation and shape also affect terrestrial weighing: a scale at rest on the rotating Earth responds to the effective acceleration including the centrifugal contribution, rather than simply to a spherical gravitational field.
Distinguish gravitational weight from apparent weight. A supporting scale measures a contact force. In a vertically accelerating cabin, upward acceleration gives while contact is maintained. During common free fall, although remains nonzero. Immersion in a fluid can similarly reduce the support needed through buoyancy, without removing the gravitational attraction. These distinctions explain why a change in a balance reading is not automatically a change of mass.

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