X-ray densitometric methods
The optical density steps on the radiographs, caused by the aluminium wedge, may be used as a scale for sediment density. The wet bulk density (y) at level z is given by: yz = a + (x-b)/c where a is the density of the pore water, x the thickness, in mm, of the aluminium wedge which gives the same film density as the sediment core at level z, b the thickness, in mm, of the aluminium wedge which gives the same film density as the bottom water in the coring tubes, and c a factor which varies with the composition of the dry substance and with the energy of radiation.

The relationship between the bulk density of the sediment layers and the thickness of the aluminium wedge for the same film-density values on the radiographs 234 u, m, and l of the upper, middle, and lower parts of sediment core 234. Modified after Axelsson 1979 (Ymer 99).
Recorded variations in the film density along the radiation images of the sediment cores and the aluminium wedge are used, together with the relationship, illustrated below, to calculate the vertical variation in density-related sedimentological parameters.
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