(49a) d/dx₄ {∫tσ4 dV} = ∫(tσ1 α₁
+ tσ² α₂ + tσ³ α₃)dS
where α₁, α₂, α₂ are the direction-cosines of the inward-drawn normal to the surface-element dS in the Euclidean Sense. We recognise in this the usual expression for the laws of conservation. We denote the magnitudes tασ as the energy-components of the gravitation-field.
I will now put the equation (47) in a third form which will be very serviceable for a quick realisation of our object. By multiplying the field-equations (47) with gνσ, these are obtained in the mixed forms. If we remember that
gνσ ∂Γαμν/∂xα = ∂/∂xα (gνσ Γαμν) - ∂gνσ/∂xα Γαμν,
which owing to (34) is equal to
∂/∂xα (.gνσ Γαμν) - gνβ Γσαβ Γγαμν
- gσβ Γνβα Γαμν,
or slightly altering the notation, equal to
∂/∂xα (gσβ Γαμβ) - gmn Γσmβ Γβnμ