Guy Berthault 28 Boulevard Thiers 78250 Meulan France Contact me by email

Experiments & Videos

Major stages of the laboratory research

Two principal stages of the program dwelt upon the following two lines of research: lamination (Fig. 1) and stratification (Figs. 2, 3).

Fig. 1 : Lamination resulting
from sediment flowing into water

(1) Lamination

The following abstract of my paper (Berthault, 1986) provided the basis of my research on the deposit of heterogranular sediments in water, with and without a current :

These sedimentation experiments have been conducted in still water with a continuous supply of heterogranular material. A deposit is obtained, giving the illusion of successive beds or laminae (Fig. 1). These laminae are the result of a spontaneous periodic and continuous grading process, which takes place immediately, following the deposition of the heterogranular mixture. The thickness of the laminae appears to be independent of the sedimentation rate but increases with extreme differences in the particle size in the mixture. Where a horizontal current is involved, thin laminated layers developing laterally in the direction of the current are observed.

Video 1 : lamination
(no sound)

The second series were performed at the Marseilles Institute of Fluid Mechanics.

The experiments demonstrate that in still water, continuous deposition of heterogranular sediments gives rise to laminae, which disappear progressively as the height of the fall of particles into water (and apparently their size) increases. Laminae follow the slope of the upper part of the deposit. In running water, many closely related types of lamination appear in the deposit, even superposed (Berthault, 1988).

(2) Stratification

Experiments in stratification were conducted in the Fort Collins hydraulics laboratory of the Colorado State University with professor of hydraulics and sedimentology Pierre Julien [video 2 : Fort Collins hydraulics laboratory].

Video 2 : Fort Collins hydraulics laboratory
(no sound)

For these, it was necessary to operate with water in a recirculating flume traversed by a current laden with sediment. As Hjulstrom (1935) and his successors had defined the critical sedimentation rate for each particle size, the current velocity would need to be varied. By modulating the current velocity, a superposition of segregated particles could be obtained.

The flume experiment showed that in the presence of a variable current, stratified superposed beds prograde simultaneously in the direction of the current (Fig. 2) [video 3 ].

Video 3
(no sound)

The result, on the scale of strata, is also conform, on the scale of facies [video 4 ] to Golovkinskii, Inostranzev and Walther’s law (Walther, 1894 ; Middleton, 1973; Romanovskii, 1988), according to which the extension of facies of the same sequence is the same both laterally and vertically [video 5 ].

Video 4
(no sound)

Video 5
(no sound)

Fig. 2. Typical longitudinal view of deposition (flow from right to left).


The report of the experiment entitled Experiments in Stratification of Heterogeneous Sand Mixtures was published in (Julien et al., 1993).

This experimental study examines possible stratification of heterogeneous sand mixtures under continuous (non-periodic and non-interrupted) sedimentation. Three primary aspects of stratification are considered: lamination, graded beds, and joints.

(1) Experiments on segregation of eleven heterogeneous mixtures of sand-sized quartz, limestone and coal demonstrate that through lateral motion, fine particles fall between interstices of the rolling coarse particles. Coarse particles gradually roll on top of fine particles and microscale sorting is obtained. Microscale segregation similar to lamination is observed on plane surfaces, as well as under continuous settling in columns filled with either air or water.

Fig. 3. Results of experiments.
(A) Schematic formation of graded beds.
(B) Time sequence of deposit formation for t 1 < t 2 < t 3.

(2) The formation of graded beds is examined in a laboratory flume under steady flow and a continuous supply of heterogeneous particles. Under steady uniform flow and plane bed with sediment motion, coarse particles of the mixture roll on a laminated bed of mostly fine particles. In non-uniform flow, the velocity decrease caused by tail-gate induces the formation of a stratum of coarse particles propagating in the downstream direction. On top of this cross-stratified bed, fine particles settle through the moving bed layer of rolling coarse particles and form an almost horizontally laminated topset stratum of finer particles. A thick stratum of coarse particles thus progresses downstream between two strata of laminated fine particles, continuously pro-grading upward and downstream

Video 6
(no sound)

Video 7
(no sound)

(3) Laboratory experiments on the desiccation of natural sands also show preferential fracturing (or joints) of crusty deposits at the interface between strata of coarse and fine particles.

Rather than successive sedimentary layers, these experiments demonstrate that stratification under a continuous supply of heterogeneous sandy mixtures results from segregation for lamination, non-uniform flow for graded beds (Fig. 4) Superposed strata are not, therefore, necessarily identical to successive sedimentary layers.

Video 8
(no sound)

Video 9
(no sound)

Video 10
(no sound)

Fig. 4. : Typical cross-sectional view of deposit

Fig. 5 : Horizontal fracturing of the Bijon Creek sand

Our flume experiments demonstrated that Stenon’s assumption (strata are ancient successive sediments) and his principle of superposition can only apply in the absence of a current (transport velocity nil). Moreover, the experiments reported in my second paper to the Academy of Sciences and experiments conducted by P. Julien and presented by video Fundamental Experiments on Stratificationat several sedimentological congresses clearly show that up to the limit of the angle of repose (30o to 40o for the sands), the lamination of the deposit is parallel to the slope (Fig. 6)

. In this case the principle of horizontxality does not apply. It should not, therefore, be concluded that the dip of the strata necessarily implies tectonic movements subsequent to the horizontal deposit of the strata.

Video 11 (no sound)

Fig. 6 : Lamination parallel to a slope of 15o


Fundamental Experiments in Stratification – Full video

A presentation for a more general public – Full video