The methods of X-ray analysis have been applied to ice by Ancel St. John and by D. M. Dennison. The former refers the structure to a lattice composed of right triangular prisms of side 4.74 A.U. and height 6.65 A.U.; the latter to a similar lattice of dimensions 4.52 and 7.32 respectively. The actual arrangement of the atoms is not found in either case. On certain suppositions, the arrangement can be found independently of direct X-ray analysis in the following way. Let it be assumed that each positive ion is surrounded symmetrically by negative ions, and vice versa; and in view of the low density of ice, let the number of neighbours be in each case as small as possible. The crystal is to be hexagonal, and is to have the right density. The result is that each oxygen atom is at the centre of gravity of four neighbouring oxygens, from each of which it is separated by a hydrogen atom. The dimensions of the structure agree with Dennison's figures. The conclusion is supported by a comparison between the calculated intensities of reflection and the observed intensities as recorded by Dennison.
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