S. Motellier et al., PH DETERMINATION OF CLAY INTERSTITIAL WATER USING A FIBEROPTIC SENSOR, Sensors and actuators. B, Chemical, 29(1-3), 1995, pp. 345-352
The disposal of high-level radioactive waste in an underground reposit
ory involves prior scientific characterizations in order to determine
the most appropriate geological formation as the host matrix. Basic in
vestigations on the composition of the soil and its interstitial water
are essential for the understanding of more complex phenomena such as
transport and migration processes of radionuclides. Among the numerou
s physical and chemical parameters to be considered, pH is of particul
ar interest for the chemistry regulation of interstitial waters since
it appears in most element speciation equilibria. Sampling techniques
with postponed analysis raise the problems of pollution risks and poss
ible modifications of the fluid characteristics by disturbances induce
d when taking it off its natural medium. In the case of clay formation
s, low water content and high interstitial pressure are additional con
straints. These concerns led us to develop an appropriate analytical t
ool for in situ measurements of pH. A fiber-optic pH sensor was tested
in an experimental underground laboratory located in the Boom clay fo
rmation at Mel, Belgium. The sensing tip (optode) was introduced via a
stainless steel guideline into a chamber at the end of a 15 m long pi
ezometer equipped with a stainless steel filter to let the interstitia
l water in. The guideline was tightly closed in order to allow the pre
ssure in the piezometer to get back to its original value, i.e. 17 bar
s. The optode was composed of a semi-bead of resin impregnated with ph
enol red and immobilized at the distal end of a 1 mm X 20 m optical fi
ber. It was connected to an emitter-receiver apparatus (Optolec-H). Un
der these conditions, the pH range of use is 7-10 with a maximum confi
dence interval of 0.1 pH unit. Laboratory performances of the device a
re given with a special focus upon the influence of pressure on the me
asured signal. In situ results, applicability, limitations and further
developments are described.