The DL refers to two parallel layers of charge surrounding the object.

One-dimensional models can be used for the vertical flow in a system of parallel horizontal layers.

Each layer is generally one of a number of parallel layers that lie one upon another, laid down by natural forces.

Superficially it is no more than a succession of parallel layers.

Structurally, they comprise parallel layers of hexagonal tilings, similar to the structure of graphite.

In non-linear phonetics, they are located on parallel layers.

A double layer is a structure in a plasma and consists of two parallel layers with opposite electrical charge.

A disconformity is an unconformity between parallel layers of sedimentary rocks which represents a period of erosion or non-deposition.

High-resolution electron microscopy reveals that the ordered phase consists of nearly parallel layers of graphene.

During freezing in wet soil, water is drawn into horizons which solidify in parallel layers, forcing soil and stones upward.