22.05.2015 Views

La Craie

La Craie

La Craie

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Foundations in chalk<br />

F. BAGUELIN.<br />

After referring to the difficulties encountered in taking chalk samples which can be used in the laboratory<br />

and the resulting dispersion of mechanical characteristics, the author shows the advantages<br />

of in situ measurements, in particular pressiometric measurements, for assessing the overall reaction<br />

of chalk in the mass.<br />

Observations and experiments have shown that calculations based on these various tests were pessimistic,<br />

especially dynamic driving formulae employed in the case of driven foundation piles. Chalk<br />

tends to liquefy under the effect of impacts, and recovers its mechanical strength after driving either<br />

by dissipation under excess pore pressure or by a thixotropic restructuring of the chalk of which<br />

little is so far known.<br />

<strong>La</strong> craie. Bull. Liaison <strong>La</strong>bo. P. et Ch., special V, oct. 1973, p. 113.<br />

Underground cavities in the chalk soil of Northern France<br />

J. LEPLAT.<br />

The chalk of Northern France was formerly worked intensively to meet the needs of agriculture<br />

and especially the building industry. In this latter sector, the production of buiding stone, which<br />

at that time had to be extracted from below ground, led to the opening of a large number of quarries<br />

which are being rediscovered by present-day major projects.<br />

The frequent absence of reliable records, the gradual loss of information formerly handed down<br />

from father to son, makes the prospection of these underground cavities very difficult. In any event,<br />

the essential starting point is a thorough geological knowledge of the region, which makes it passible<br />

to select and valorize data gathered during the field survey (for example by taking account of the<br />

fact that building chalk is almost always located at the same stratigraphic level). The next stage should<br />

be a gravimetric campaign, the only method of geophysical prospection applicable to all cases in<br />

this region. Professor Gabillard's electromagnetic method is designed for the detection of cavities<br />

of the « bottle » type in the region of Lille. Though it is accurate and effective in this particular case,<br />

its possibilities over the whole area are relatively limited. When the gravimetric or electromagnetic<br />

prospection reveals negative anomalies attributable to underground cavities, then mechanical<br />

means of reconnaissance must be employed. In favourable cases (numerous access shafts, shallow<br />

cavities) recourse can be had to devices of the penetrometer type ; otherwise, drilling is necessary.<br />

As soon as a cavity has been detected, the final stage is to enter it in order to survey it.<br />

For the treatment of underground cavities in chalk, two types of solutions may be adopted : filling<br />

in or tidying up. Filling in is reliable but costly ; in this region it is done by introducing quarry<br />

aggregate pneumatically, or by injecting a grout of fly ash and cement. The latter solution seems<br />

to be more reliable and less costly. Tidying up must be apdapted to the particular conditions, and<br />

consequently takes various forms, the simplest being the construction of access shafts allowing<br />

the cavity to be supervised periodically.<br />

<strong>La</strong> craie, Bull. Liaison <strong>La</strong>bo. P. et Ch., special V, oct. 1973, p. 123.<br />

Chalk in electric power station construction sites<br />

G. COMES.<br />

The Division Geologie-Geotechnique of the Direction de l'Equipement de l'Electricité de France<br />

has in the course of the past five years to study chalk as a foundation material as a consequence of<br />

the evolution in the building and siting of electric power stations.<br />

The mechanical characteristics of chalk are such that this material behaves very differently from<br />

the rocks usually encountered in connection with these types of structures, such as granite, shale,<br />

limestone, etc.<br />

The sites studied are located at various points of the Paris Basin, taking that area in its widest sense.<br />

The geological and geotechnical work undertaken was performed on Senonian chalk in the Champenois<br />

and Cauchois localities.<br />

The geotechnical characteristics of the chalks in question were determined in the laboratory and in<br />

situ. The behaviour of the material in place is examined and analysed in this article.<br />

It is possible to build underground structures in chalk provided that a certain number of precautions<br />

of a technological nature are taken while the work is in progress.<br />

<strong>La</strong> craie, Bull. Liaison <strong>La</strong>bo. P. et Ch., spécial V, oct. 1973, p. 149.<br />

177

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!